Nil
| Nil | |
|---|---|
|
| |
| General information | |
| Height above mean sea level (en) | 2,700 m |
| Tsawo |
6,650 km 6,650 km 2,850 km |
| Labarin ƙasa | |
|
| |
| Tsarin Daidaiton Labarin Kasa | 15°38′25″N 32°30′20″E / 15.64014°N 32.5055°E |
| Kasa | Sudan, Misra, Uganda, Sudan ta Kudu, Burundi, Ruwanda da Habasha |
| Hydrography (en) | |
| Tributary (en) |
duba
|
| Watershed area (en) | 3,400,000 km² |
| Ruwan ruwa | Nile Basin |
| River source (en) | Tafkin Victoria, White Nile da Blue Nile |
| River mouth (en) | Bahar Rum |
Nilu babban kogi ne da ke arewa maso gabashin Afirka, yana gudana zuwa Bahar Rum. Tsawonsa ya kai 7,088 kilometers (4,404 mi), kuma shi ne mafi tsawo a duniya, duk da cewa ba ya ɗaukar ruwa da yawa kamar Amazon ko Congo. Nilu ya taka muhimmiyar rawa a tarihin muhalli, tattalin arziki, da al’adu na Afirka tsawon dubban shekaru.
Nilu yana da manyan rassan ruwa guda biyu: Farin Nilu da Bakin Nilu. Farin Nilu ya fi tsawo kuma ana ɗaukar shi a matsayin asalin kogin, amma Bakin Nilu yana kawo ruwa fiye da sau biyu na Farin Nilu. Farin Nilu yana farawa kusa da Lake Victoria, yana gudana ta Uganda da Sudan ta Kudu; Bakin Nilu kuma yana farawa kusa da Lake Tana a Habasha, yana shiga Sudan daga kudu maso gabas. Sannan sukan haɗu a Khartoum, babban birnin Sudan. Daga nan Nilu yana gudana ta hamadar Nubia zuwa Cairo, sannan ya zube cikin Bahar Rum kusa da Alexandria, inda ya kafa babban kwarin Nilu Delta.
Kwarin Nilu yana ratsa ƙasashe 11. Yawancin ruwan Nilu yana fitowa daga ruwan sama a ƙasashen da ke sama kamar Habasha, Kenya, Tanzaniya da Uganda. Ƙasashen da ke ƙasa kamar Masar da Sudan suna dogara da ruwan Nilu don ban ruwa. Sauran ƙasashen da ke cikin kwarin sun haɗa da Burundi, DR Congo, Eritrea da Rwanda.
Nilu ya kasance ginshiƙin ƙasar Masar ta dā, inda ambaliyar shekara-shekara ta kawo ƙasa mai gina amfanin gona. Wannan ƙasa ta tallafa wa noma da rayuwa a cikin hamada. Nilu ya sauƙaƙa kasuwanci, sadarwa, sufuri, da mulki. A kudu da cataract na biyu akwai Nubia, inda tsoffin al’ummomi irin su Kerma da Daular Kush suka zauna. A ƙarni na 19, Turawa sun yi bincike a kusa da Lake Victoria don gano asalin kogin. A yau, al’ummomin Nilotic suna rayuwa a gefen Nilu, suna kiwon shanu ta hanyar yin hijira bisa yanayin ambaliyar Nilu.
A zamanin yau, Nilu yana da muhimmanci ga tattalin arzikin Masar da Sudan, inda ake amfani da shi wajen ban ruwa da samar da wutar lantarki. Tun daga ƙarshen ƙarni na 20, an gina dam fiye da goma sha biyu a kwarin Nilu. Wadannan dam sun canza tsarin ambaliyar shekara-shekara, sun rage yawan laka da ke zuwa ƙasa, wanda ya sa Nilu Delta ke raguwa. Wasu dam kamar Aswan High Dam da Grand Ethiopian Renaissance Dam sun haifar da rikice-rikicen siyasa kan ƙarancin ruwa, tsaro, abinci, da tilasta ƙaura.
Sunaye da Asalin Suna
[gyara sashe | gyara masomin]Kalmar Turanci "Nile" ta samo asali daga Latin Nilus da Greek Neilos, wanda wataƙila ya samo asali daga kalmar Semitic naḥal ma’ana 'kogi'.[1]
A cikin tsohuwar harshen Masar, kalma ɗaya ake amfani da ita don 'Nilu' da 'kogi': jtrw.[2] Masarawa sun kira ƙasarsu kmt ma’ana 'baƙi', don nuni da launin ruwan ambaliyar Nilu mai ɗauke da laka daga sama.[3] Sunan Turanci "Blue Nile" fassarar sunan Larabci ne Al-Baḥr Al-Azraq.[1]
A zamanin yau, kogin yana da sunaye daban-daban a cikin kwarin Nilu. A Masar ana kiransa Al-Nīl, Baḥr Al-Nīl ko Nahr Al-Nīl.[4] A Sudan ta Kudu ana kiransa Baḥr el-Jebel ma’ana 'Kogin Dutsen'.[5] A Uganda, masu magana da Luganda suna kiransa Kiyira.[6] Wasu mutanen Nubia na Masar da Sudan suna amfani da sunan Nobiin Áman Dawū ('Babban Ruwa').[7]
Wasu rassan ruwa da sassan kogin suna ɗauke da sunan "Nile", ciki har da:
- Albert Nile — ɓangaren Farin Nilu daga Lake Albert zuwa Nimule[8]
- Black Nile — wani suna na Atbarah River[9]
- Blue Nile — ɗaya daga cikin manyan rassan Nilu
- Kyoga Nile — ɓangaren Farin Nilu daga Lake Kyoga zuwa Lake Albert[10]
- Main Nile — ɓangaren Nilu bayan haɗuwar Bakin Nilu da Farin Nilu[11]
- Mountain Nile — ɓangaren Farin Nilu daga duwatsun Uganda zuwa filayen Sudan ta Kudu[12]
- Victoria Nile — ɓangaren Farin Nilu daga Lake Victoria zuwa Lake Kyoga[13]
- White Nile — ɗaya daga cikin manyan rassan Nilu
- Yellow Nile — Wadi Howar, tsohon rassa da ya bushe shekaru dubban da suka wuce[11]
Asali
[gyara sashe | gyara masomin]
Asalin Nilu yana daga wani rassa na Rukarara River, a cikin Nyungwe National Park, Rwanda, a 2°19′35″S 29°21′30″E / 2.32639°S 29.35833°E, a tsayin 2,539 meters (8,330 ft).[14][lower-alpha 2] Asalin yana nufin farkon ruwan da ke gudana duk shekara a cikin kwarin Nilu.[14] Daga wannan asali, kogin yana gudana 7,088 kilometers (4,404 mi) zuwa bakin Bahar Rum.[14][lower-alpha 3] Tsawon an auna shi a 2009 ta hanyar hotunan tauraron dan adam.[14]
Mafi tsayin asalin Nilu yana kan duwatsun Rwenzori a Uganda.[15] Duwatsun da ake kira “Mountains of the Moon” da Ptolemy ya bayyana sun danganta da Rwenzori.[15]
Asalin da ya fi kudu yana Burundi a Ruvyironza River, wanda ke shiga Kagera River.[16] An gina wani abin tunawa a kusa da Rutovu a 1937 ta Burkhart Waldecker.[16][lower-alpha 4]
Lake Victoria — wanda Tanzaniya, Uganda da Kenya ke rabawa — wani lokaci ana ɗaukar shi a matsayin asalin Nilu, saboda yana ciyar da Farin Nilu daga Jinja, Uganda.[18][lower-alpha 5] Wasu kuma suna ganin asalin gaskiya shi ne gajimare na ruwan sama da ke sama da Lake Victoria, saboda su ne ke kawo mafi yawan ruwan tafkin.[20]
Asalin Bakin Nilu yana kusa da Gish Abay, kudu da Lake Tana.[21][lower-alpha 6]
Yanayin ƙasa
[gyara sashe | gyara masomin]
Kogin Nilu babban kogi ne a arewa maso gabashin Afirka wanda ke kwarara zuwa Tekun Bahar Rum. Kwarin Nilu shi ne dukkan yankin ƙasa da ruwansa ke gangarowa zuwa Kogin Nilu, kuma yana da faɗin kilomita murabba'i 2,927,843 – kimanin kashi 10% na nahiyar Afirka (duba taswirar da ke kusa).[22] Kasashe goma sha ɗaya ne gaba ɗaya ko wani ɓangarensu ke cikin wannan kwari: Burundi, Jamhuriyar Dimokuraɗiyyar Kongo, Masar, Eritrea, Habasha, Kenya, Rwanda, Sudan ta Kudu, Sudan, Tanzaniya da Uganda.[23][lower-alpha 7]
Wannan kwari ya ƙunshi nau'o'in yanayi, tsarin muhalli da siffofin ƙasa iri-iri – daga hamada masu yashi da fari a arewa, zuwa filayen fadama masu laushi a tsakiyar yankin, zuwa tsaunuka masu dazuzzuka da yawan ruwan sama a kudu.[25]
Ana iya raba Kwarin Nilu zuwa yankuna bakwai; biyar daga cikinsu suna ɗauke da mafi tsawon hanyar da Kogin Nilu yake bi. Idan aka bi daga sama zuwa ƙasa, waɗannan yankuna biyar su ne: Tafkunan Manyan Afirka, Nilu na Tsaunuka, Farin Nilu, Babban Nilu, da Delta ta Nilu. Yankuna biyu na ƙari suna ɗauke da manyan rafukan da ke shiga Nilu: Shuɗin Nilu da Kogin Atbarah.[1]
Tafkunan Manyan Afirka
[gyara sashe | gyara masomin]Yankin Tafkunan Manyan Afirka yana ɗauke da asalin Kogin Nilu tare da wasu manyan tafkuna da suke cikin tsarin Kogin Nilu: Tafkin Victoria, Tafkin Albert, Tafkin George da Tafkin Edward.[26]
Asalin Kogin Nilu shi ne Kogin Rukarara da ke cikin Gandun Dajin Ƙasa na Nyungwe a Rwanda,[14] kuma yana kaiwa zuwa Kogin Kagera wanda ke zubowa cikin Tafkin Victoria.[1][lower-alpha 8]
Ko da yake babban tafki ne – na biyu mafi girman tafkin ruwa mai ɗanɗano a duniya idan aka auna faɗi[lower-alpha 9] – Tafkin Victoria ba shi da zurfi sosai, domin matsakaicin zurfinsa kusan mita 40 ne.[28]
Kogin yana fara ɗaukar sunan “Nilu” ne a inda Tafkin Victoria ke zubar da ruwa daga arewacinsa: sashen daga nan zuwa Tafkin Albert ana kiransa Victoria Nile.[1]
Ruwan faɗuwa guda biyu – Ripon Falls da Owen Falls – sun kasance a wurin da Nilu ke fita daga Tafkin Victoria, amma an nutsar da su bayan gina Dam ɗin Nalubaale. Bayan Bujagali Falls da Tashar Wutar Lantarki ta Bujagali, Victoria Nile yana zubowa cikin Tafkin Kyoga. Bayan ya fita daga Tafkin Kyoga, Kogin Kafu yana shiga cikinsa, sannan ya ratsa Murchison Falls ya shiga Tafkin Albert.
Ba kamar Tafkin Victoria ba, Tafkin Albert tafki ne mai zurfi wanda tsaunuka suka kewaye shi. Kogin yana fita daga tafkin a gefen arewarsa, inda ake kiransa Albert Nile; wannan sashe na kogin yana da shimfiɗa kuma faffaɗa, kuma ya dace da zirga-zirgar jiragen ruwa masu tururi.[29]
Nilu na Tsaunuka
[gyara sashe | gyara masomin]Yanki na biyu na Kwarin Nilu idan aka bi daga sama zuwa ƙasa shi ne Nilu na Tsaunuka (Script error: The function "langx" does not exist.).[30]
Wannan yanki yana farawa kusa da garin Nimule, yana kaiwa zuwa Tafkin No, kuma gaba ɗayansa yana cikin Sudan ta Kudu. Bayan ya ratsa Nimule, kogin yana wucewa ta Fula Rapids sannan ya isa Juba – babban birnin Sudan ta Kudu. Bayan Juba, Nilu yana ratsa garin Bor sannan ya shiga Sudd, wata babbar fadama da ke kan shimfiɗaɗɗen fili.[31]
Gangarar ƙasar a yankin Sudd kusan 1:13,000 ce kawai, saboda haka kogin yana tafiya a hankali kuma yana faɗaɗa. Tsire-tsire masu yalwa ciki har da sedges, papyrus da water hyacinth na gama gari (wani nau'in tsiro mai mamaye muhalli) suna toshe hanyoyin ruwa kuma suna wahalar da zirga-zirga. A gefen arewa na fadamar Sudd, Nilu yana wucewa ta Tafkin No, ƙaramin tafki inda Kogin Bahr el Ghazal (wato “kogin barewa” a Larabci) ke shiga cikinsa daga yamma.[29]
Yankin Farar Nilu
[gyara sashe | gyara masomin]
Yayin da ake ci gaba da tafiya ƙasa, yankin na uku na kwarin Nilu shi ne yankin Farar Nilu[lower-alpha 10] wanda ya hada da tsawon 800 kilometers (500 mi) daga kusa da Malakal zuwa Khartoum, babban birnin Sudan. A nan ne Bakar Nilu ya hade da shi. Wannan bangaren kogin yana da faɗi, kwanciyar hankali, tare da ciyayi da fadamomi a bakin koguna. Kogin nan ba shi da zurfi kuma yana rasa ruwa sosai ta hanyar ƙura.[1]
Inda Farar Nilu ya hade da Bakar Nilu, launukansu suna bambanta sosai. Farar Nilu ya fi haske saboda yashi da yake dauke da quartz da feldspar. Wannan ya bambanta da Bakar Nilu wanda ke dauke da laka mai duhu daga duwatsun basaltic rock na Habasha.[32]
Kogin Sobat shi ne rafi wanda ke hade da Farar Nilu kusa da garin Malakal (bayan haduwar Bahr el Ghazal, kafin Bakar Nilu). Yankinsa – wanda ya hada da Machar Marshes[5] – yana dauke da kusan kilomita murabba’i 225,000.[33] Sobat yana ambaliya tsakanin Yuli da Disamba.[1]
Babban Nilu
[gyara sashe | gyara masomin]Yankin na hudu na kwarin Nilu – babban Nilu[lower-alpha 11] – yana daga Khartoum zuwa Cairo, babban birnin Misira.[29] Wannan bangaren yana da faɗi da zurfi mai daidaito: kusan 500 meters (1,600 ft) faɗi da 10 meters (33 ft) zurfi a wurin da ya fi zurfi (idan ba ambaliya ba).[36] Da zarar ya bar Khartoum, kogin ya shiga Sabaloka Game Reserve kuma ya ratsa manyan rafuka masu ƙarfi da ba a iya ketarewa da jirgin ruwa. Wannan shi ne na shida (kuma mafi kusa da sama) daga cikin rafuka shida na Nilu. Kogin Atbarah – babban rafi – yana hade da Nilu, wanda daga nan ya bi babban lankwasawa S zuwa yamma. Ana samun sauran rafuka hudu (lamba 5, 4, 3, da 2) a cikin wannan lankwasawa S, wanda ya sa kogin ba ya iya ketarewa; duk da haka jiragen ruwa na iya tafiya a wasu wuraren da ba su da rafuka. Kogin daga nan ya shiga tafkin Nasser. Wannan tafki – tafki na biyu mafi girma da mutum ya yi a duniya – an kafa shi ne lokacin da aka gina Babban Dam na Aswan a Misira, kuma ya mamaye fiye da 480 kilometers (300 mi) na Nilu. Dam na Aswan Low – wanda ya fi tsoho kuma ya fi ƙanƙanta – yana ƙasa da Babban Dam na Aswan, kusa da wurin rafin farko na Nilu (wanda yanzu ya nutse). Daga wadannan dam-dam, Nilu yana gudana kusan 800 kilometers (500 mi) ta cikin dutsen limestone, tare da gonaki masu ban ruwa, har sai ya isa Cairo.[29]
Delta na Nilu
[gyara sashe | gyara masomin]
Yankin na biyar, kuma na ƙarshe, wanda ya kunshi Kogin Nilu shi ne Delta na Nilu, babban delta mai siffar alwatika (kimanin 22,000 kmSamfuri:Super)[37] wanda ya fara daga Cairo zuwa Bahar Rum.[1] Kogin ya rabu zuwa manyan hanyoyi biyu a cikin delta: reshen Rosetta da reshen Damietta. Jimillar girman delta (ciki har da bangaren da ya nutse) kusan 150,000 kmSamfuri:Super. Delta an gina shi tsawon miliyoyin shekaru, daga yashi da kogin ya kawo daga sama.[38] Tun bayan kammala Babban Dam na Aswan a 1970, delta ya fara raguwa saboda lalacewar ruwan Bahar Rum. A da, lalacewar tana daidaita da sabbin ƙasa daga yashi da kogin ya kawo; amma dam yana rike yashi a tafkin sa, yana hana sabuwar ƙasa isa delta.[39]
Rafin Bakar Nilu
[gyara sashe | gyara masomin]
Tsawon hanyar Nilu – wanda ya hada da rafi Farar Nilu – yana da wasu rafuka. Yankunan kwaruruwan Bakar Nilu da Atbarah su ne yankuna na ƙarshe na kwarin Nilu.[1]
Bakar Nilu yana fitowa daga tsaunuka a Habasha inda yake farawa a matsayin rafin da ake kira Abay kusa da garin Gish Abay: Gish kalma ce ta Amharic wadda ke nufin 'tushen', kuma Abay shi ne sunan rafin.[40] Gish Abay yana shiga Tafkin Tana, tafki mai faɗi kuma ba shi da zurfi, wanda ke da hanya guda ta fita inda ya karɓi sunan "Bakar Nilu". Kogin daga nan yana yin babban lankwasawa: da farko zuwa kudu, sannan yamma ta cikin kwarin mai ban mamaki mai zurfin 2 kilometers (6,600 ft), sannan arewa yana shiga Kudancin Sudan zuwa Sudan, inda ya hade da Farar Nilu a Khartoum ya zama Babban Nilu.[41] A hanyarsa, Bakar Nilu yana samar da wutar lantarki a wurare da dama, ciki har da Tis Abay hydropower project a Bakar Nilu Falls, Grand Ethiopian Renaissance Dam kusa da iyakar Habasha da Kudancin Sudan, Roseires Dam kusa da garin Ad Damazin, da Sennar Dam.[42] Girman kwaruruwan Bakar Nilu ya fi kilomita murabba’i 306,000.[43]
Rafin Atbarah
[gyara sashe | gyara masomin]Kogin Atbarah rafi ne na Nilu wanda yake fitowa daga arewacin Habasha, kuma yana hade da Nilu kusan 320 kilometers (200 mi) arewa da Khartoum.[44] Yankin kwaruruwansa ya fi kilomita murabba’i 204,000.[43] Atbarah yana da gudu mai yawa a lokacin da bayan damina a Habasha (lokacin bazara da kaka), amma yana iya bushewa a lokacin hunturu da bazara. Duk da kasancewar rafin yana yawan yankewa, yana bayar da fiye da kashi 10% na jimillar ruwan shekara na Nilu.[44] Dam-dam da ke kan Atbarah sun hada da Khashm el-Girba Dam, Upper Atbara and Setit Dam Complex, da Tekezé Dam (a kan rafin Tekezé).[45]
Ruwan Kogin
[gyara sashe | gyara masomin]
Gudun ruwa da ambaliya
[gyara sashe | gyara masomin]Samfuri:Further Ko da yake Nilu shi ne mafi tsawo a duniya, ba shi da mafi girman gudun ruwa. Gudunsa – kimanin 87 km³ a shekara[lower-alpha 13] – ya yi ƙanƙanta idan aka kwatanta da manyan koguna. Gudun Nilu kusan kashi 1% ne na Amazon, 6% na Congo, da 12% na Yangtze.[47][lower-alpha 14]
Gudun shekara-shekara daga manyan rassan uku na Nilu: 54% daga Blue Nile, 32% daga White Nile (ciki har da gudun Bahr el Ghazal da Sobat), da 14% daga Atbarah.[48]
Dutsen White Nile da Blue Nile suna samun ruwan sama na yanayi, amma gudun White Nile ya fi daidaito fiye da Blue Nile.[1] Wannan saboda tafkuna da fadamomi da yawa a White Nile suna rage tasirin yanayin ruwan sama.[49] Yayin da White Nile ke wucewa ta cikin fadamar Sudd, kusan rabin ruwan yana ɓacewa ta hanyar ƙura.[50]
A gefe guda, gudun Blue Nile yana bambanta sosai: yana ambaliya daga Yuli zuwa Oktoba saboda ruwan sama na damina.[1] Ruwan Blue Nile ya yi yawa a lokacin damina har White Nile ke ja baya a wurin haɗuwar koguna.[51] A lokacin ambaliya, gudun ruwa zuwa babban Nilu kusan 70% daga Blue Nile, 20% daga Atbarah, da 10% daga White Nile.[1] A kololuwar ambaliya, gudun yau da kullum zuwa Lake Nasser kusan 0.71 km³, sau uku fiye da matsakaicin gudun yau da kullum na shekara 0.23 km³.[52][lower-alpha 12][lower-alpha 15]
Kafin a gina madatsun ruwa a Nilu, gudun ruwan Nilu a Masar yana bambanta da yanayi: ya fi yawa a lokacin bazara/damina; ya fi ƙanƙanta a lokacin sanyi/bazara.[lower-alpha 16] Amma bayan gina Aswan High Dam – wanda ya ƙirƙiri tafkin da zai iya riƙe kusan shekaru biyu na gudun ruwa – gudun ruwan da ke ƙasa ya fi daidaito a duk shekara.[55][lower-alpha 17]
Jigilar laka
[gyara sashe | gyara masomin]Nilu yana ɗaukar laka zuwa ƙasa. Motsin laka ana rarrabe shi zuwa laka mai shawagi (wanda ke shawagi a cikin ruwa) ko laka mai nauyi (wanda ke kan ƙasan kogi).[57] Kashi 97% na laka da Nilu ke ɗauka daga Atbarah da Blue Nile ne, dukkansu daga Habasha.[58] Ƙasa a Delta ta Nilu ta samo asali daga duwatsu a Habasha. Jimillar duwatsun da aka nika cikin shekaru miliyan 30 daga asalin Nilu a Habasha kusan 102,000 km³, wanda ya yi daidai da ƙasar Delta ta Nilu kusan 150,000 km³.[59]
Muhalli
[gyara sashe | gyara masomin]Dabbobi
[gyara sashe | gyara masomin]Jimillar nau’in kifaye da aka samu a kwarin Nilu an kiyasta fiye da 800. A cikin kogin kaɗai, nau’in kifaye 128 ne aka samu, daga iyalai 27.[60] Yawancin nau’in kifaye suna cikin iyalai huɗu: Cichlidae (cichlids), Cyprinidae (carp), Mormyridae (elephantfish), da Mochokidae (catfish).[61] Wasu nau’in Cichlid suna cikin Tafkunan Manyan Afirka.[60]
Baya ga kifaye, dabbobin da ke rayuwa a cikin ruwan Nilu a wasu lokuta sun haɗa da hipopotamus, kada na Nilu, da buffalo na Afirka. Wasu halittun ruwa sun haɗa da molluscs, crab, da shrimp. [62] Dabbobi da yawa suna rayuwa a cikin muhallin bakin kogi, ciki har da giwaye, antelope, da giraffe.[62] Ƙwaryar da aka samu a tafkunan Nilu suna ɗauke da ƙwari masu cutarwa (blood flukes) waɗanda ke haifar da schistosomiasis ga dabbobi da mutane.[63]
Tsuntsaye da ke rayuwa a bakin Nilu sun haɗa da herons, kingfishers, ospreys, da nau’o’in storks ciki har da shoebills.[62] Wasu nau’in tsuntsaye suna da alaƙa da kwarin Nilu kaɗai (misali blue-winged goose), yayin da wasu suna da yaduwar duniya (misali moorhen da osprey).[64] Wasu nau’in heron, ducks, geese, da egrets suna rayuwa a kwarin duk shekara, kuma nau’in ducks da geese 14 suna zuwa ne kawai a lokacin sanyi.[64] Yawancin gulls da terns a kwarin suna yin hijira. A cikin shekaru dubu da suka gabata, wasu nau’in tsuntsaye sun ragu saboda mamayar ɗan adam a muhallinsu.[65]
Tsirrai
[gyara sashe | gyara masomin]
Yankin Tafkunan Manyan Afirka na kwarin Nilu ya ƙunshi tsirrai kamar water lily, papyrus, da water hyacinth. Water hyacinth tsiro ne mai mamaya, kuma ya shafi tsirrai na asali a Lake Kyoga.[67] Tsirrai da aka saba a fadamar Sudd sun haɗa da Vossia, hippo grass, reed mace, ambatch, da papyrus. Sudd kuma tana ɗauke da tsirrai da ke rayuwa a cikin ƙaramin ambaliya, misali Oryza, antelope grass, da Phragmites.[68]
Gurbatar muhalli
[gyara sashe | gyara masomin]A tarihi, ruwan Nilu ya kasance mai kyau don sha, amma a ƙarshen ƙarni na 20, ya zama ba shi da lafiya a wasu wurare.[69][lower-alpha 18] Gurɓatawa ya fi yawa a Lake Tana, kusa da manyan birane, da Delta ta Nilu.[71]
Asalin gurɓatawa a Nilu sun haɗa da aikin gona, masana’antu, da shara na gida. Akwai masana’antu 36 da ke zubar da gurɓataccen ruwa kai tsaye cikin Nilu, da 41 cikin tashoshin ban ruwa. Waɗannan masana’antu sun haɗa da: sinadarai, lantarki, injiniya, takin zamani, abinci, ƙarfe, hakar ma’adinai, mai da sabulu, takarda, masana’antar zane da itace. Akwai fiye da magudanan aikin gona 90 da ke zubar da gurɓataccen ruwa cikin Nilu.[72]
Gurbatar kogi ya fi yawa tsakanin Aswan da Tekun Bahar Rum. Gurɓatar nan ya fito daga ayyukan ɗan adam, zubar aikin gona, da shara na masana’antu. Gurɓataccen abu yana ƙaruwa yayin da kogi ke tafiya ƙasa saboda taruwar gurɓatawa.[73] Delta tana da sauƙin taruwar gurɓatawa saboda rashin motsin ruwa mai kyau, ƙasa mai laushi, da yawan laka a ƙasan kogi.[74]
Kariya da tasirin ɗan adam
[gyara sashe | gyara masomin]
Kwarin Nilu ya kasance mai ɗanɗano da danshi daga shekaru 15,000 da suka gabata zuwa 5,000, wanda ya ba da damar fara aikin gona mai girma a kusan shekaru 5,000 da suka gabata.[75] Ci gaban aikin gona ya ƙara tasiri ga muhalli tun daga lokacin, yana haifar da sare dazuzzuka da lalacewar ƙasa.[76] Tasirin ya ƙara muni saboda yanayin ƙanƙara da ya fara kusan shekaru 4,000 da suka gabata. Wannan ya haifar da yunwa, rikice-rikicen zamantakewa, da lalacewar muhalli.[76]
Wasu nau’in dabbobi sun bace a kwarin Nilu saboda ayyukan ɗan adam. Sacred ibis ya kasance mai muh
Tarihin ɗan Adam
[gyara sashe | gyara masomin]Kafin Tarihi
[gyara sashe | gyara masomin]
Tsofaffin kakanni na jinsin ɗan Adam sun zauna kusa da kwarin Nilu. An gano ƙashin Australopithecus afarensis da aka fi sani da Lucy a gabashin iyakar kwarin. Olduvai Gorge – inda aka fara gano ƙashin Homo habilis – yana kudu da kwarin.[77] A cikin kwarin Nilu, wurin binciken Nyayanga a gabashin gabar Tafkin Victoria yana da kayan aikin Oldowan tun shekaru miliyan 2.6 da suka wuce.[78][lower-alpha 19] An gano zaman ɗan Adam a bakin Nilu tsakanin shekaru 12,000 zuwa 20,000 da suka wuce a wurin kusa da garin Qurta (Masar). Waɗannan mutane sun sassaka petroglyphs a cikin duwatsu, suna nuna aurochs, tsuntsaye, hippopotamids, barewa, hartebeest, da kifi. Wasu masana sun yi hasashen cewa waɗannan mutane, ko wasu da ke kusa, sun iya fara kiwon tumaki, awaki, ko shanu.[80] Saharar gabas – ciki har da Masar da Sudan – ta kasance mai ɗan danshi a lokacin African humid period wanda ya ɗauki daga kusan shekaru 10,000 zuwa 5,000 da suka wuce. Al’ummomin makiyaya sun bunƙasa a lokacin, amma lokacin da yanayi ya bushe kusan 3,900 K.Z., mutane sun tilasta yin hijira zuwa kwarin Nilu don tsira. Wannan ne asalin al’ummomin Nubiya a Sudan da kuma wayewar Masar ta dā.[75]
Wayewar Masar ta dā
[gyara sashe | gyara masomin]
Kogin Nilu ya kasance cibiyar rayuwar Masar: yana ba da abinci ta hanyar amfanin gona da ya shayar, kuma yana jawo mutuwa lokacin da fari ya jawo gazawar amfanin gona da yunwa. Nilu ya ƙarfafa ci gaban kimiyya da gwamnati: ban ruwa, hasashen ambaliya da haraji duk sun buƙaci sabbin ƙwarewar lissafi da gudanarwa. Hasashen yanayi da taurari ma sun bunƙasa saboda buƙatar Masarawa su fahimci kogin da ambaliyarsa.[82]
Kalanda ta Masar ta dā ta dogara da zagayen ambaliyar Nilu. Shekara ta kasu kashi uku, kowanne yana da watanni huɗu na kwanaki talatin. Lokutan su ne Akhet ('ambaliya'), Peret ('girbi'), da Shemu ('amfani'). Akhet shi ne lokacin da Nilu ya yi ambaliya, yana barin sabuwar ƙasa mai albarka; Peret shi ne lokacin girma; Shemu kuma lokacin girbi ba tare da ruwan sama ba.[83] Nilu ya shafi harshensu: kalmomin kwatance sun dogara da mutum da yake fuskantar sama da kogin: kalma ɗaya na iya nufin sama da kudu; wata kalma na hagu da gabashi; da wata kalma na dama da yamma.[84] Wani lokaci suna kiran ruwan sama da "Nilu a sama".[85]
Al’ummomin Nubiya, Habasha, da Nilotic
[gyara sashe | gyara masomin]
Kudu da ambaliyar Nilu ta biyu akwai Nubia, inda al’ummomi suka zauna a bakin Nilu (yanzu Sudan) tun ƙarshen lokacin danshi na Afirka.[87][lower-alpha 20] Waɗannan al’ummomin Nubiya sun bunƙasa tare da wayewar Masar a arewa, amma ba su yi hulɗa sosai ba har sai lokacin Old Kingdom of Egypt kusan 3,000 K.Z.[88] Wayewar farko ta Nubia ita ce Kerma culture, daga kusan 2600 K.Z. zuwa 1500 K.Z. Kerma ta fara da kiwon shanu, amma daga baya ta koma noma yayin da Saharar ta bushe.[87] Kusan 780 K.Z., Kushite Empire ta taso a bakin Nilu, ta mamaye yawancin Masar ƙarƙashin Black Pharaohs.[86] Bayan zuwan Kiristanci, masarautun Kirista a Nubia (ciki har da Nobatia, Makuria, da Alodia) sun bunƙasa a bakin Nilu.[89]
A yankin Eritrea da arewacin Ethiopia, Kingdom of Aksum ta bunƙasa daga ƙarni na 1 zuwa 960 Z.Z. Aksum ta fi amfani da Tekun Ja wajen sufuri, amma kogunan Atbarah da Blue Nile suna cikin mulkinsa.[90] Funj Sultanate (1504–1821) ta yi mulki a yankin Sudan na zamani.[91] Ethiopian Empire (1270–1974) ta mamaye yankin Habasha da Eritrea.[92]
Kogin Nilu ya kasance gida ga Nilotic peoples, manyan al’ummomi da suka samo asali a Sudan ta Kudu, suka yi hijira zuwa Uganda da Kenya.[93] Nilotic sun haɗa da Dinka da Nuer, manyan kabilu a Sudan ta Kudu; dukkansu makiyaya ne masu yin hijira bisa yanayin ambaliyar Nilu.[94]
Masar daga zamanin Roma zuwa mulkin mallaka
[gyara sashe | gyara masomin]
Kogin Nilu ya taka muhimmiyar rawa wajen bunƙasar Daular Roma, wadda ta yi mulkin Masar tsawon ƙarni da dama. Romawa sun shigo da hatsi mai yawa daga Masar, wanda aka noma da ruwan ambaliyar Nilu.[96] A ƙarni na farko, sarkin Trajan ya gina wani canal da ya haɗa Nilu da Tekun Ja.[97] Tsakanin 945 da 977 Z.Z., ambaliyar Nilu ta yi ƙasa sosai; hakan ya jawo gazawar amfanin gona da rikice-rikicen siyasa wanda ya haifar da Fatimid Caliphate.[98][lower-alpha 21] Canals a Masar sun ci gaba da gina su da gyara su ta hannun Fatimiyawa (ƙarni na 10–11), Mamluk Sultanate (ƙarni na 13–16), da Ottoman Egypt (ƙarni na 16–19).[100] Duk da ƙwarewar Masarawa wajen gina canals, ba su yi nasarar gina manyan dam ba sai ƙarni na 19, lokacin da auduga — da aka shayar da ruwan Nilu — ta zama muhimmin amfanin kasuwanci.[95] Waɗannan dam ɗin farko an gina su a lokacin mulkin Muhammad Ali na Masar. An fara gina ƙananan dam a Delta da kusa da Cairo, domin tsawaita lokacin girma. Ali ya kuma gina canals ciki har da Mahmoudiyah Canal, wanda aka fara a 1818.[95] Ismail Pasha (Viceroy na Masar, 1863–1879) ya gina Ibrahimiya Canal — an kammala a 1873 — wanda yake tafiya a layi da Nilu kuma ana amfani da shi wajen ban ruwa.[101]
Binciken asalin Nilu
[gyara sashe | gyara masomin]
Tun daga zamanin Helenawa, Turawa sun yi sha’awar gano asalin Nilu da ambaliyarsa.[103] Herodotus ya ziyarci Masar a 457 K.Z. ya yi tafiya har zuwa Aswan; ya yi mamakin ambaliyar Nilu da ke farawa a lokacin bazara — lokacin da ba a samun ruwan sama a Masar.[104] Masana ilimin ƙasa daga Turai, Afirka, da Larabawa tun daga Eratosthenes ƙarni na 2 K.Z. sun yi hasashen cewa asalin Nilu daga manyan tafkuna a Afirka ta tsakiya.[105] Duk da haka, har zuwa ƙarni na 17, taswirar da aka yi ba ta da tushe na kimiyya.
Asalin Blue Nile an gano shi ta hannun mishan Pedro Páez wanda ya ziyarci Gish Abay a farkon ƙarni na 17, ya rubuta littafin História da Ethiópia. Daga baya Jerónimo Lobo da James Bruce sun yada labarinsa, suna hasashen ya ziyarci wurin tsakanin 1613–1618.[106]
Asalin White Nile ya fi wahala a gano. Tafkin Victoria ba a tabbatar da shi a matsayin babban asalin White Nile ba sai bayan shekaru 260 da aka gano Blue Nile.[107] A 1858, John Hanning Speke ya fara ganin Tafkin Victoria, daga baya ya gano wani kogi da ke fita daga arewacin tafkin, ya ce shi ne Nilu.[108] Amma bai bi kogin har zuwa Sudan ba, hakan ya sa wasu suka yi shakku.
A farkon ƙarni na 20, Richard Kandt ya ce asalin White Nile daga wani reshen Kagera River a Nyungwe Forest.[14] A 1969, masu bincike daga Waseda University sun gano wani reshe na Kagera. A 2006, masu yawon buɗe ido sun sake gano wurin, suka sanya alama a jikin itace. A 2009, masana sun yi amfani da hoton tauraron dan adam don ƙara tabbatar da wurin, suka gano tushen a wani rijiya kusa da wurin da aka gano a baya.[14]
Siyasar ruwa a zamanin zamani
[gyara sashe | gyara masomin]Kogin Nilu yana ketare iyakokin ƙasashe da dama, yana mai da shi kogi na ƙasashe da dama kuma ya zama abin rikici na siyasa.[109]
Zamanin mulkin mallaka
[gyara sashe | gyara masomin]Bayan mulkin mallaka na Birtaniya a Masar ya fara a 1882,[lower-alpha 22] suka fara ƙarin ayyukan ruwa don ƙarfafa samar da auduga da tallafawa yawan jama’ar Masar da ke ƙaruwa da sauri.[111][lower-alpha 23] Babban dam na farko da aka gina a kan Nilu shi ne Aswan Low Dam, an kammala shi a 1902. An ƙara tsayinsa sau biyu: a 1912 da 1933.[112] Wasu dam da aka gina a lokacin mulkin mallaka sun haɗa da Sennar Dam (1914–1925) a kan Blue Nile a Sudan, da Jebel Aulia Dam, wanda aka kammala a 1937 kusa da Khartoum.[113] Babban manufar dam ɗin da aka gina a ƙarni na 20 ita ce tallafawa ban ruwa; samar da wutar lantarki ta hydropower ba ta da muhimmanci sosai.[114]
A 1929, an cimma yarjejeniya tsakanin Masar da Anglo-Egyptian Sudan.[115] Yarjejeniyar ta tanadi cewa Masar da Sudan za su yi amfani da biliyan 48 da biliyan 4 na ruwan Nilu a kowace shekara, bi da bi. Masar ta tanadi ikon sa ido kan ruwan Nilu a ƙasashen sama, ta gudanar da ayyukan da suka shafi kogi ba tare da amincewar ƙasashen sama ba, kuma ta yi veto kan duk wani gini da zai iya cutar da Masar.[116]
Bayan mulkin mallaka
[gyara sashe | gyara masomin]File:Großer Tempel (Abu Simbel) 31.jpg|thumb|An ɗaga haikalin Abu Simbel zuwa sama lokacin da aka gina Aswan High Dam wanda ya nutse wurin da suka kasance a dā.[117] |alt=Babban sassaka na dutse na sarakuna huɗu suna zaune a kujeru.]
Masar da Sudan sun samu ‘yancin kai daga Birtaniya a tsakiyar shekarun 1950s.[118][lower-alpha 23] A 1959 Masar da Sudan suka sabunta yarjejeniyar raba ruwa ta 1929. Sabuwar yarjejeniyar ta raba ruwa tsakanin Masar da Sudan da biliyan 55.5 da biliyan 18.5, bi da bi.[120] Ƙasashen sama a cikin kwarin Nilu ba su shiga yarjejeniyar ta 1959 ba — ciki har da Habasha, wadda ke samar da fiye da rabin ruwan Nilu.[121]
Yarjejeniyar ta 1959 ta ba da damar gina dam, wanda aka yi: Masar ta gina Aswan High Dam (an kammala 1970); Sudan ta gina Khashm el-Girba Dam (1964), Roseires Dam (1966), Merowe Dam (2009), da Upper Atbara and Setit Dam Complex (2017).[121][lower-alpha 24]
A 1960, Masar ta fara gina Aswan High Dam wanda ke adana kusan ruwan Nilu na shekaru biyu.[123] Dam ɗin ya mai da sashen Nilu daga dam zuwa teku a matsayin babban canal na ban ruwa.[124] Dam ɗin ya kawo fa’ida: ƙarin ruwa don ban ruwa, da wutar lantarki don masana’antu. Amma ya kawo illa: ingancin ruwa ya ragu, ƙasar ta rasa albarkar laka, ƙasar ta ƙara gishiri, cutar schistosomiasis, asarar muhalli, da korar Nubians.[125]
Rikice-rikice da tattaunawa na ƙarshen ƙarni na 20
[gyara sashe | gyara masomin]A duk ƙarni na 20, akwai babban bambanci a ƙarfin siyasa a cikin kwarin Nilu: Masar da Sudan a arewa sun fi ƙarfi fiye da sauran ƙasashe goma a kudu.[126] Bayan Masar da Sudan suka ƙirƙiri yarjejeniyar 1959, wasu daga cikin ƙasashen sama (ciki har da Kenya, Tanzania, Uganda, da Habasha) suka fara bayyana adawa da sharuɗɗan yarjejeniyar, suna cewa ba su da alhakin bin ta saboda ba su shiga ba.[127] Ƙasashen sama sun yi hujja cewa dam ɗin da Masar da Sudan suka gina sun kare waɗannan ƙasashe daga fari, yunwa, da ambaliya, amma ƙasashen sama kamar Habasha har yanzu suna fuskantar fari da yunwa.[128] Misali, Aswan High Dam ya samar da kusan biliyan 10 na kilowatt-hours a kowace shekara; kuma ya ba manoma na Masar damar yin girbi sau uku a shekara, maimakon sau ɗaya kafin dam.[129] Shugabannin Masar sau da yawa sun bayyana cewa za su iya amfani da ƙarfin soja don kare haƙƙoƙinsu bisa yarjejeniyar 1959.[130]
A ƙarshen ƙarni na 20, ƙasashen Afirka sun shiga ƙoƙari da dama don kafa manufofin rabon ruwa — ciki har da Undugu Commission (1983–1993) da TECCONILE (1993–1998) — amma ba su yi nasara wajen ƙirƙirar yarjejeniyoyi na dogon lokaci ba.[131] A 1999, ƙasashe tara daga cikin goma na kwarin Nilu — Burundi, Jamhuriyar Dimokuradiyyar Kongo, Masar, Habasha, Kenya, Rwanda, Sudan, Tanzania da Uganda — suka kafa Nile Basin Initiative don inganta tattaunawa cikin lumana kan batutuwan da suka shafi kwarin Nilu.[132]
Sauyin ƙarfi zuwa ƙasashen sama
[gyara sashe | gyara masomin]File:GERD 3.jpg|thumb|upright=1.3|Grand Ethiopian Renaissance Dam, an kammala a 2025, yana samar da fiye da gigawatts 5.[133]|alt=Hoton babban dam na kankare da tafkin da ya haifar, daga sama.]
A farkon ƙarni na 21, ƙarfi ya koma ga ƙasashen sama yayin da suka fara gina dam ba tare da amincewar Masar ko Sudan ba.[126] A 2008, Habasha ta gina Tekezé Dam ba tare da neman izini daga Masar ko Sudan ba.[134] A 2010, ƙasashe biyar na sama — Uganda, Habasha, Rwanda, Tanzania, da Kenya — suka rattaba hannu kan sabuwar yarjejeniya, Cooperative Framework Agreement, wadda ta nufi raba ruwan cikin adalci ga ƙasashen sama. Kenya ta rattaba hannu saboda tana da shirin fitar da ruwa daga Tafkin Victoria don ban ruwa. Masar da Sudan sun yi adawa da yarjejeniyar.[135][136][137][138] A 2011, Sudan ta Kudu ta samu ‘yancin kai daga Sudan, ta zama ƙasa ta goma sha ɗaya a kwarin Nilu. A rikice-rikicen ruwa na gaba, Sudan ta Kudu ta yi kawance da ƙasashen sama maimakon Sudan.[24]
A 2011, Habasha ta sanar da shirin gina babban dam a kan Blue Nile kusa da iyakar Sudan. Dam ɗin daga baya aka sanya masa suna Grand Ethiopian Renaissance Dam (GERD).[139] Habasha ta ɗauki GERD a matsayin muhimmin ginshiƙi na makomar ƙasar, saboda wutar lantarki da dam ɗin zai samar za ta inganta rayuwar jama’a. Masar ta damu cewa dam ɗin zai rage ruwan ban ruwa saboda tana amfani da kusan duk ruwan da ke shiga ƙasar, kuma ta yi fargabar zai haifar da ƙarancin ruwa. Sudan ta damu da tsaro da samar da ruwa.[140] Bayan sanarwar dam ɗin, shugaban Masar Mohamed Morsi ya yi nuni da yiwuwar kai hare-haren soja kan Habasha,[139] kuma Sudan da Masar suka gudanar da atisayen soja tare.[141]
An gudanar da tattaunawa da dama tsakanin Habasha, Sudan, da Masar yayin da ake gina dam ɗin da kuma lokacin da ake cika tafkin.[142] A 2015 ƙasashen suka rattaba hannu kan "Declaration of Principles" wanda ya ƙunshi yarjejeniyoyi na manyan manufofi kan amfani da ruwa da hanyoyin cika tafkin.[143] A 2019, Amurka ta jagoranci tattaunawa tsakanin ƙasashen.[143] A 2020, African Union ta fara jagorantar tattaunawa.[144] A wannan shekarar, Masar ta nemi Majalisar Tsaron Ƙungiyar Ƙasashen Duniya ta shiga, amma ta ƙi.[145] A 2021 da 2022, UAE ta jagoranci tattaunawa.[146] Gina dam ɗin GERD ya kammala a 2020, kuma a 2025 tafkin ya cika kuma yawancin injinan dam ɗin suna samar da wutar lantarki.[147]
Siyasar ruwa a zamanin murnar
[gyara sashe | gyara masomin]Kogin Nile yana ratsa iyakokin ƙasashe da dama, wanda hakan ya sa ya zama kogin da ya ratsa iyakoki kuma batun takaddamar siyasa.
Zamanin mulkin mallaka
[gyara sashe | gyara masomin]Bayan fara mulkin mallakar Birtaniya a Masar a shekarar 1882,[lower-alpha 25] sun fara ƙarin ayyukan ruwa don haɓaka samar da auduga da kuma tallafawa al'ummar Masar da ke haɓaka cikin sauri.[149][lower-alpha 23] Madatsar ruwa ta farko mafi girma da aka gina akan kogin Nile ita ce madatsar ruwa ta Aswan Low Dam, wadda aka kammala a shekarar 1902. An ɗaga tsawonta sau biyu: a shekarun 1912 da 1933.[150] Sauran madatsun ruwa da aka gina a ƙarƙashin tsarin mulkin mallaka sun haɗa da madatsar ruwa ta Sennar Dam, wadda aka gina tsakanin 1914 da 1925 a jikin kogin Blue Nile a Sudan, da kuma madatsar ruwa ta Jebel Aulia Dam, wadda aka kammala a shekarar 1937 kusa da Khartoum.[113] Babban dalilin gina madatsun ruwan a ƙarni na 20 shi ne don tallafawa ban ruwa; samar da wutar lantarki daga ruwa ya kasance manufa ta biyu ce kawai.[114]
A shekarar 1929, an cimma yarjejeniya tsakanin Masar da hadakar ƙasashen Anglo-Egyptian Sudan.[151] Yarjejeniyar ta tanadi cewa Masar da Sudan za su yi amfani da cubic meter biliyan 48 da biliyan 4 na gudanar ruwan Nile a kowace shekara, bi da bi. Masar ta tanadi haƙƙin sanya ido kan gudanar ruwan Nile a ƙasashen da ke sama, da gudanar da ayyukan da suka shafi kogin ba tare da amincewar ƙasashen da ke saman kogi ba, da kuma yin weto (ko hana) kowane irin aikin gine-gine da zai yi tasiri mara kyau ga Masar.[152]
Zamanin bayan mulkin mallaka
[gyara sashe | gyara masomin]
Masar da Sudan sun sami 'yancin kai daga Birtaniya a tsakiyar shekarun 1950.[118][lower-alpha 23] A shekarar 1959 Masar da Sudan sun sabunta yarjejeniyar raba ruwa ta shekarar 1929. Sabuwar yarjejeniyar ta raba ruwan da za a raba tsakanin Masar da Sudan zuwa cubic meter biliyan 55.5 da biliyan 18.5 bi da bi. [153] An cire ƙasashen da ke saman kogin na yankin magudanar ruwan Nile daga yarjejeniyar ta 1959—gami da Habasha, wadda ita ce tushen fiye da kashi biyu cikin uku na ruwan kogin Nile.[121]
Yarjejeniyar ta 1959 ta haɗa da sharullan da ke ba Masar da Sudan damar gina madatsun ruwa, wanda kuma suka yi: Masar ta gina madatsar ruwa ta Aswan High Dam (an kammala a shekarar 1970); Sudan ta gina madatsar ruwa ta Khashm el-Girba Dam (1964), Roseires Dam (1966), Merowe Dam (2009), da kuma rukunin madatsun ruwa na Upper Atbara and Setit Dam Complex (2017).[121][lower-alpha 26]
A shekarar 1960, Masar ta fara gina madatsar ruwa ta Aswan High Dam wacce ke tara kusan gudanar ruwan Nile na tsawon shekaru biyu.[154] Madatsar ruwan ta mayar da sashen kogin Nile na ƙasa (daga madatsar ruwan zuwa teku) ya zama wata babbar hanyar ban ruwa.[124] Madatsar ruwan tana da kyakkyawan tasiri: ana samun ƙarin ruwa don ban ruwa, kuma wutar lantarki daga ruwa ta samar da ƙarin wuta don masana'antun Masar. Mummunan tasirin madatsar ruwan sun haɗa da gurɓacewar ingancin ruwa, raguwar albarkar ƙasa saboda rashin sabon laka da ambaliyar ruwa ke ajiyewa, ƙaruwar gishirin ƙasa, cutar tsarki (schistosomiasis), asarar wuraren zama na tito da namun daji na asali, da kuma kwashe mutanen Nubia. [155]
Madatsar ruwa ta Aswan High Dam ta nutsar da wani babban yanki na kofatun kogin Nile, kuma ta kusan nutsar da tsofaffin abubuwan tarihi masu mahimmanci da dama. Wani kamfen na ƙasa da ƙasa don ceton abubuwan tarihin na Nubia daga nutsewa a cikin sabon tafkin ya yi nasarar ceton wasu abubuwan tarihin, ciki har da haikalan Abu Simbel.[117] Madatsar ruwa ta Aswan High Dam ta kuma tilasta ƙaurace wa mutanen Nubia da dama da ke zaune a kwarin da sabon tafkin ya mamaye. An fitar da mutanen Nubia daga ƙasashen kakanninsu, kuma da yawa an tilasta musu yin ƙaura zuwa birane a Masar da Sudan.[156]
Rashin jituwa da shawarwari a ƙarshen ƙarni na 20
[gyara sashe | gyara masomin]A tsawon ƙarni na 20, an sami rashin daidaituwa bayyananne a cikin ikon siyasa a cikin yankin magudanar ruwan Nile: Masar da Sudan a arewa sun fi mallakar iko fiye da sauran ƙasashe goma na hudu zuwa kudu.[126] Bayan Masar da Sudan sun ƙirƙiri yarjejeniyar ta 1959, da yawa daga cikin ƙasashen sama (gami da Kenya, Tanzania, Uganda, da Habasha) sun fara nuna rashin amincewa da sharullan yarjejeniyar, kuma sun yi gardamar cewa ba su da alaƙa da yarjejeniyar domin ba su kasance ɓangare na ta ba.[127] Gardamar ƙasashen na sama ita ce cewa madatsun ruwa da Masar da Sudan suka gina sun kare waɗannan ƙasashe biyu daga fari, yunwa, da ambaliyar ruwa, duk da haka ƙasashen sama kamar Habasha har yanzu suna fuskantar fari da yunwa.[128][lower-alpha 27] Alal misali, madatsar ruwa ta Aswan High Dam tana samar da kusan kilowatt-hours biliyan 10 a kowace shekara; kuma ta ba manoman Masar damar yin girbi sau uku a kowace shekara, idan aka kwatanta da girbi guda ɗaya kafin gina madatsar ruwan.[129] Shugabannin Masar galibi suna bayyana cewa a shirye suke su yi amfani da ƙarfin soja don kare haƙƙoƙinsu a ƙarƙashin yarjejeniyar ta 1959.[158]
A ƙarshen ƙarni na 20, ƙasashen Afirka sun shiga cikin ƙoƙarce-ƙoƙarce da dama don kafa manufofin raba ruwa—gami da Hukumar Undugu Commission (wadda ta yi aiki daga 1983 zuwa 1993) da kuma TECCONILE (wadda ta yi aiki daga 1993 zuwa 1998)—amma ba su yi nasarar ƙirƙirar yarjejeniyoyi na dogon lokaci ba.[131] A shekarar 1999, tara daga cikin ƙasashe goma[lower-alpha 28] na yankin magudanar ruwan Nile—Burundi, Jamhuriyar Demokradiyyar Kongo, Masar, Habasha, Kenya, Rwanda, Sudan, Tanzania da Uganda—sun kafa shirin Nile Basin Initiative don haɓaka tattaunawa ta lumana game da batutuwan da suka shafi yankin magudanar ruwan Nile. [160]
Juya ikon zuwa ƙasashen sama
[gyara sashe | gyara masomin]
A farkon ƙarni na 21, iko ya koma ga ƙasashen sama yayin da suka fara gina madatsun ruwa ba tare da amincewar Masar ko Sudan ba.[126] A shekarar 2008, Habasha ta gina madatsar ruwa ta Tekezé Dam ba tare da neman izini daga Masar ko Sudan ba.[134] A shekarar 2010, ƙasashen sama guda biyar—Uganda, Habasha, Rwanda, Tanzania, da Kenya[lower-alpha 29]—sun sanya hannu kan wata sabuwar yarjejeniya—wato Cooperative Framework Agreement—wadda ke da nufin raba ruwa cikin adalci ga ƙasashen sama. Kenya ta sami kwarin gwiwar sanya hannu kan yarjejeniyar ne saboda tana da shirin hako ruwa daga tafkin Victoria don ban ruwa. Yarjejeniyar ta 2010 ta fuskanci adawa daga Masar da Sudan.[162] A shekarar 2011, Sudan ta Kudu ta sami 'yancin kai daga Sudan, inda ta zama ƙasa ta sha ɗaya a yankin magudanar ruwan Nile. A cikin takaddamar ruwa na gaba, Sudan ta Kudu ta haɗa kai da ƙasashen sama maimakon da Sudan.[24]
A shekarar 2011, Habasha ta sanar da shirin gina wata babbar madatsar ruwa a jikin kogin Blue Nile kusa da iyaka da Sudan. Daga baya aka sanya wa madatsar ruwan suna Grand Ethiopian Renaissance Dam (GERD).[139] Habasha ta ɗauki GERD a matsayin abu mai mahimmanci ga makomar ƙasar, saboda wutar lantarki da madatsar ruwan za ta samar zai ba ta damar haɓaka ingancin rayuwar al'ummarta sosai. Masar ta damu cewa madatsar ruwan za ta fuskanci barazana ga ban ruwan amfanin gonakanta saboda Masar ta riga ta yi amfani da kusan dukkanin ruwan kogin da ke shiga ƙasarta, kuma ta damu cewa sabuwar madatsar ruwan za ta haifar da ƙarancin ruwa. Sudan kuma ta damu da tsaro da wadatar ruwa.[163] Bayan an sanar da gina madatsar ruwan, shugaban Masar Mohamed Morsi ya ba da nuni da cewa hare-haren soja akan Habasha na iya zama zaɓi,[139] kuma Sudan da Masar sun gudanar da atisayen soja na haɗin gwiwa da dama.[141]
An gudanar da shawarwari masu yawa tsakanin Habasha, Sudan, da Masar yayin da ake gina madatsar ruwan kuma ake cika tafkin.[142] A shekarar 2015 ƙasashen sun sanya hannu kan "Declaration of Principles" (Sanarwar Ka'idoji) wadda ke ƙunshe da yarjejeniyoyi na babban mataki game da amfani da ruwa da hanyoyin cika tafkin ruwan.[143][lower-alpha 30] A shekarar 2019, Amurka ta karɓi bakuncin tattaunawa tsakanin ƙasashen da abin ya shafa.[143] A shekarar 2020, Ƙungiyar Tarayyar Afirka ta fara sauƙaƙe tattaunawa.[144] A shekarar nan, Masar ta buƙaci Kwamitin Tsaro na Majalisar Ɗinkin Duniya da ya tsoma baki, amma ya ƙi yin hakan.[145] A shekarun 2021 da 2022, UAE ta karɓi bakuncin tattaunawa.[146] An kammala gina madatsar ruwa ta GERD a shekarar 2020, kuma a shekarar 2025 tafkin ya cika kuma mafi yawan janatocin madatsar ruwan suna samar da wutar lantarki.[147]
Tattalin arziki
[gyara sashe | gyara masomin]Ayyukan Noma
[gyara sashe | gyara masomin]
Akwai babban bambanci a cikin ayyukan noma tsakanin ƙasashen arewa na yankin magudanar ruwan Nile (Masar, Sudan, da Sudan ta Kudu) da kuma ƙasashen kudu (Uganda, Habasha, da sauransu).[165] Arewa mafi yawanta hamada ce, fari ga shi kuma kudu tana samun ruwan sama mai yawa; amfanin gona a arewa ya dogara ne da farko kan ban ruwa, yayin da kudu ta dogara da ruwan sama da ke taruwa a cikin ƙasa (soil water); yawan amfanin gona ya fi yawa a arewa (saboda yawan amfani da takin zamani da magungunan kashe kwari) fiye da kudu; kuma arewa tana da manyan gine-ginen ban ruwa (madatsun ruwa, magudanar ruwa, da sauransu) waɗanda ke samun goyon bayan manufofin gwamnati da kafofin tallafi na ƙasa da ƙasa.[165] Adadin ruwan ƙasa da ake amfani da shi kowace shekara don amfanin gona a kudu ya kai cubic kilometer 229, wanda ya ninka jimillar gudanar ruwan Nile na shekara-shekara sau biyu (kusan cubic kilometer 100).[166] Yawan amfanin gona a kudu yana fuskantar cikas saboda nisan tazara zuwa kasuwa; sabanin arewa, inda kusan dukkanin gonaki ke tattare a cikin wani kunkuntar yanki a gefen koguna tare da wadatattun damammakin sufuri.[167]
Rashin ruwan sama da na ƙarƙashin ƙasa ya sa Masar ta dogara da kogin Nile don kusan dukkanin buƙatun ta na ruwa.[168] Manyan amfanin gona da ake nomawa a Masar sun haɗa da auduga, alkama, masara, shinkafa, dawa, da wake (fava beans).[168] Gabaɗaya akwai lokutan shuka guda biyu a Masar: lokacin rani (auduga) da lokacin sanyi (hatsi da kayan lambu).[169] Tun daga shekarun 1950, Masar ta daɗa yin amfani da dabarun noma na masana'antu (gami da amfani da takin zamani da magungunan kashe kwari) don haɓaka yawan amfanin gona.[170] Ƙasar Masar kashi 94% hamada ce, sumni kashi 3% kuma ƙasa ce mai kyau don noma.[169] Mafi yawan ƙasar noma ta Masar tana cikin yankin Nile Delta, sauran kuma suna gefen kogin Nile.[171]
Manyan amfanin gona a Sudan su ne gyaɗa, auduga, ridi, rake, da dawa. Sauran amfanin gona sun haɗa da maiwa, alkama, masara, da sha'ir.[172] Amfanin gonar Sudan yana samun ruwa ne daga kogunan Blue Nile da White Nile, tare da tallafin madatsun ruwa da dama da suka haɗa da Sennar Dam da Khashm el-Girba Dam.[172] Mafi yawan ƙasar da ake wa ban ruwa tana cikin tsarin Gezira Scheme, wani babban aikin ban ruwa da aka fara tun a shekarun 1920.[173]
Sufurin Kifi
[gyara sashe | gyara masomin]
Kogin Nile da tabkuna masu alaƙa da shi sun kasance muhimmiyar hanyar samun abinci ga mutanen da ke zaune kusa da ruwan tun zamanin da.[175] A shekarar 2000, yankin magudanar ruwan Nile ya samar da kusan tan miliyan 1.4 na kifi a kowace shekara, wanda ya kai fiye da rabin jimillar kifin ruwan sanyi da aka samu daga daukacin nahiyar Afirka (tan miliyan 2.2).[176] Tafkin Victoria kaɗai—tafki mafi girma a Afirka—ya samar da tan miliyan 1.[177] Kifin da ake samu daga tabkunan yankin magudanar ruwan Nile ya zarce adadin kifin da ake kamawa a cikin kogunansa.[175] Dukkanin ruwayen yankin magudanar ruwan Nile—banda yankin Sudd—suna nuna alamun fuskantar matsalar yawan kamun kifi da ya wuce kima.[178] A shekarun 1950, an shigar da kifin Nile perch da Nile tilapia cikin Tafkin Victoria a matsayin ƙoƙarin juyar da raguwar kifin asali na tafkin; ƙoƙarin ya yi nasara, amma ya haifar da raguwar nau'ikan kifin asali a cikin tafkin.[179] A halin yanzu, mafi yawan kifin da ake kamawa a Tafkin Victoria su ne Nile perch da Silver cyprinid (wato kifin sardine na Tafkin Victoria).[175] Wasu kamun kifi—musamman na kifin Nile perch—an fi fitar da su zuwa Turai, maimakon a cinye su a cikin gida.[114] Ana gudanar da noman kifi a wasu sassa na yankin magudanar ruwan.[180]
Wutar Lantarki daga Ruwa
[gyara sashe | gyara masomin]
Kogin Nile da rassan sa suna samar da wuta ga dazin tashoshin wutar lantarki daga ruwa, waɗanda gabaɗaya suke da ikon samar da sama da gigawatts 10 (GW) na wutar lantarki.[lower-alpha 31] Kafin shekarar 2000, akwai madatsun ruwa kaɗan a kogin Nile, amma bayan haka, gwamnatoci sun hanzarta gina madatsun ruwa.[181] Tashoshin wutar lantarki daga ruwa waɗanda ke da ikon samar da wuta sama da 100 MW an lissafa su a cikin teburin da ke ƙasa.[lower-alpha 32]
| Tashar Wutar Lantarki |
Wuri na Kusa |
Shekarar Kammalawa |
Ikon Samar da Wuta (MW, a 2025) |
Reshen Kogi |
|---|---|---|---|---|
| Aswan Low Dam | Samfuri:Operational | 1902, 1912, 1933, 1985 | 550[182] | Babban Nile |
| Aswan High Dam | Samfuri:Operational | 1970 | 2,100[34] | Babban Nile |
| Merowe Dam | Samfuri:WinDL | 2009 | 1,250[183] | Babban Nile |
| Upper Atbara and Setit Dam Complex | Samfuri:WinDL | 2017 | 320[184] | Atbarah da Tekezé |
| Roseires Dam | Samfuri:WinDL | 1966, 2013 | 280[185] | Blue Nile |
| Tana Beles | Samfuri:Partial | 2010 | 460[186] | Kogin Beles, Blue Nile |
| Tekezé Dam | Samfuri:Partial | 2009 | 300[186] | Tekezé, Atbarah |
| Grand Ethiopian Renaissance Dam | Samfuri:Partial | 2020 | 5,150[133] | Blue Nile |
| Fincha | Samfuri:Partial | 1973 | 134[186] | Blue Nile (Chomen Lake) |
| Karuma | Karuma Falls, Uganda | 2024 | 600[187] | Victoria Nile |
| Isimba | Kamuli District, Uganda | 2019 | 183[188] | Victoria Nile |
| Bujagali | Bujagali Falls, Uganda | 2012 | 250[189] | Victoria Nile |
| Kiira | Kimaka, Uganda | 2003 | 200[190] | Victoria Nile |
| Nalubaale | Jinja, Uganda | 1954 | 180[191] | Victoria Nile |
Sufuri
[gyara sashe | gyara masomin]
Kogin Nile yana da sassauƙan gangare a arewa idan aka kwatanta da yankin kudu mai tuddai—sakamakon haka ƙasashen arewa (Masar, Sudan, da Sudan ta Kudu) suna da sassan ruwa da za a iya yin amfani da su don sufuri cikin sauƙi.[192] A Masar, kogin ba shi da wani babban cikas tsakanin delta da katarat ta farko a Aswan, kuma a sakamakon haka an yi amfani da wannan sashe sosai don sufuri.[193] Ana iya amfani da wannan sashe tun ma kafin zuwan jiragen ruwa masu amfani da tururi, saboda gudanar ruwa na iya ɗaukar jiragen ruwa zuwa ƙasa, kuma iskoki daga arewa galibi suna taimaka wa jiragen ruwa na madauki tafiya zuwa sama.[194] Kogin Blue Nile gabaɗaya ba shi da sauƙin sufuri a mafi yawan wurare. Maimakon kogin, mutanen Habasha da turawan mulkin mallaka na Italiya sun yi amfani da hanyar ƙasa—wato Strada Imperiale—don sufuri daga arewa zuwa kudu a Habasha.[195] Kamar yadda yake a shekarar 1903, masu bincike har yanzu suna binciken kogin Blue Nile don gani ko za a iya amfani da shi don sufuri tsakanin Habasha da Sudan, amma ba su yi nasara ba.[196]
A tsohuwar Masar, kogin shi ne babban tsarin sufuri, kuma an gina jiragen ruwa iri-iri—na yau da kullum da na bukukuwa.[81] Jiragen ruwan Masar sun kasance masu ƙarfi sosai don ɗaukar manyan ginshiƙan dutse (obelisks) da duwatsu don gina dala da haikali.[197][lower-alpha 34] A zamanin murnar, ana ci gaba da amfani da kogin don sufuri, musamman a Masar, wadda ke da hanyoyin ruwa guda huɗu da suka dace da manyan jiragen ruwa: guda biyu a delta, guda ɗaya tsakanin delta da Aswan High Dam, da kuma guda ɗaya a Lake Nasser. Masar tana jigilar tan miliyan 500 na kaya a kan kogin kowace shekara, wanda hakan ya kai kusan kashi 0.8% kacal na jimillar jigilar kayayyaki na Masar (mafi yawan kayayyaki ana jigilar su ne ta hanya ko layin dogo).[lower-alpha 35] Kayayyakin da ake jigilar su a kan kogin sun haɗa da siminti, farandutse (limestone), gawayi, kayayyakin man fetur, da phosphates.[200]
Daga sama da Lake Nasser, kogin Nile da rassan sa suna ɗauke da maɓuɓɓugar ruwa, katarat, rapids, da madatsun ruwa waɗanda ke sa sufuri na nisa mai tsawo ya zama mai wahala.[201] Wani cikas ga sufuri shi ne Sudd, wani babban dausayi mai dausayi a kan kogin White Nile a Sudan ta Kudu. Shirye-shiryen gina magudanar ruwa ta cikin dausayin—da ake kira Jonglei Canal—an fara su ne a farkon ƙarni na 20 da nufin samar da ƙarin ruwa don shuka auduga a Masar. An fara ginin na ɗan lokaci a shekarar 1978, amma ba da daɗewa ba aka dakatar da aikin.[202]
Bude Ido da Shakatawa
[gyara sashe | gyara masomin]
Kogin Nile—musamman sashin da ke Masar—ya kasance ɗaya daga cikin wuraren buɗe ido mafi shahara a duniya na tsawon dubunnan shekaru, kuma ya kasance jigon rubuce-rubucen tafiye-tafiye masu yawa.[203][lower-alpha 36] Ɗaya daga cikin wuraren da aka fi ziyarta a gefen kogin Nile shi ne rukunin dala na Giza pyramid complex—kusan kilomita 9 daga ainihin hanyar kogin Nile na yanzu a birnin Alkahira—wanda ya kasance wurin buɗe ido tun zamanin Helenawa.[204][lower-alpha 34]
Sashen kogin Nile tsakanin Alkahira da Aswan ya daɗe yana zama sanannen wuri ga masu buɗe ido: lokacin bukukuwan da suka shafi buɗe Suez Canal a shekarar 1870, wani babban rukunin masu buɗe ido ya yi tafiyar jirgin ruwa a wannan sashe na kogin kuma sun ziyarci Luxor, Dendera, Saqqara, Edfu, da Philae.[203] Ɗaya daga cikin hukumomin balaguro na farko a duniya, wato Thomas Cook & Son, ya fara ba da rangadin kogin a shekarar 1870 lokacin da aka buɗe Suez Canal, kuma ya fara balaguron jiragen ruwa na tururi a kai a shekarar 1875.[205] Tun lokacin da aka gina madatsar ruwa ta Aswan High Dam a shekarar 1970, madatsar ruwan da kanta ta zama wurin jan hankalin masu buɗe ido, tare da haikalan da ke kusa da aka kwashe lokacin ginin don guje wa nutsewa.[206] Madatsar ruwa ta Aswan High Dam ta kuma amfani masana'antun jiragen ruwan shakatawa saboda kogin daga Aswan zuwa delta ya zama mai sauƙin sufuri cikin aminci a duk tsawon shekara.[207]
Yankin magudanar ruwan Nile gida ne ga gidan shakatawa da wuraren kiyaye halittu da dama, gami da Murchison Falls National Park na Uganda[208] da kuma Salouga and Ghazal Protected Area na Masar.[209] Maɓuɓɓugar ruwa ta Bujagali Falls ta taɓa kasancewa ɗaya daga cikin fitattun wuraren shawagin kwal jirgin ruwa (rafting) na Afirka, amma ta nutse sakamakon gina tashar wutar lantarki ta Bujagali Power Station.[210]
A cikin al'ada
[gyara sashe | gyara masomin]Fasaha da adabi
[gyara sashe | gyara masomin]Kogin ya kasance ana nuna shi akai-akai a cikin fasahar tsohuwar Masar, sau da yawa tare da sarakuna suna kamun kifi ko kuma suna harbawa dorina mashin.[212] Ayyukan fasaha na yanayin ƙasa da ke nuna kogin Nilu – ko dai kai tsaye ko a fakaice – ana kiran su yanayin ƙasar Nilu. Yanayin ƙasar Nilu yana da siffar hoton kogi da ke nuna rayuwar shuke-shuke da dabbobi, wanda yawancinsu na asalin ƙasar Masar ne. Abubuwan da aka saba gani sun haɗa da ganyen papyrus, itacen dabino, kifi da tsuntsayen ruwa, kuma – da kashin-da-tari – dabbobi irin su kyanwar daji, birai, da kada.[212]
Hakanan ana wakiltar yanayin ƙasar Nilu a cikin ayyukan fasaha daga tsohuwar Girka da tsohuwar Rome.[214] Fasahar Nilu ta Daular Romawa ta fi ba da muhimmanci ga dabbobi masu zafi, yawanci sun haɗa da kadoji da dorina.[214] Wani shahararren wakilci na Nilu a cikin fasaha shi ne Kamannin Kogin Nilu, babban mutum-mutumi na marmara daga wajen ƙarni na 2 CE na Rome – yanzu yana cikin Gidan Tarihi na Vatican.[lower-alpha 38] Ana wakiltar Nilu a matsayin mutum mai kishingida riƙe da damammakin alkama a hannunsa. A gefensa akwai sphinx – wanda ke wakiltar Masar – da yara goma sha shida waɗanda ke nuni ga kamu goma sha shida (kyakkyawan tsayin ambaliyar ruwa na shekara-shekara). A gindinsa akwai kadoji, pigmies (mutane gajeru), da dorina.[213]
Ana ganin Nilu a cikin ayyukan fasaha da ke nuna manyan koguna guda huɗu na duniya: Nilu (Afirka), Danube (Turai), Ganges (Asiya), da Río de la Plata (Amurka). Misalai sun haɗa da zanen Koguna Huɗu na Aljanna na Peter Paul Rubens (1615)[216] da kuma maɓuɓɓugar ruwa a Rome Fontana dei Quattro Fiumi wanda Gian Lorenzo Bernini ya tsara (1651).[217] A cikin maɓuɓɓugar ruwa ta Bernini, an nuna Nilu a matsayin mutum mai kansa a rufe da tufa, wanda ke nuna alamun sirrin asalin kogin Nilu da ba a sani ba.[218]
Bayan gaisuwa ga Nilu an tsara shi kuma mutanen tsohuwar Masar sun rera shi; ya yi bikin ambaliyar ruwan Nilu da fa'idodin da ya kawo wa wayewar Masar.[219] Isma'il Pasha ya ba Giuseppe Verdi aikin tsara wasan opera don bikin buɗe Kogin Suez. Wasan operan, Aida, an nuna shi a sabon gidan wasan kwaikwayo na masarautar Masar (Egyptian Royal Opera House) a cikin shekarar 1871. Kashi na uku na wasan operan an shirya shi ne a gabar kogin Nilu.[220] Tun lokacin da aka fara ginin Babban Madatsar Ruwa ta Habasha (Grand Ethiopian Renaissance Dam), mawakan Habasha sun fitar da wakoki da ke yabo da ɗaukaka kogin Nilu da madatsar ruwan.[221]
William Shakespeare ya sa jarumi Marc Antony ya kwatanta ambaliyar ruwan Nilu a cikin wasan kwaikwayo na Antony and Cleopatra: "Haka suke yi, yallabai: suna auna kwararar Nilu ta wasu ma'aunai a cikin dala; sun sani, ta tsayi, ko ƙanƙanta, ko matsakaici, idan fari ko yalwar girbi zai biyo baya: yayin da Nilus ke ƙaruwa sosai, haka yake ƙara alkawari: yayin da yake raguwa, mai shuka iri a kan laka da ta rube yake watsa hatsinsa, kuma ba da jimawa ba girbi zai zo."[222][lower-alpha 39]
Agatha Christie ta rubuta shahararren littafin nan na binciken sirri na shekarar 1937 mai suna Death on the Nile, game da kisan kai a cikin jirgin ruwan tururi na Nilu, wanda ya yi tasiri ga sauye-sauye da yawa na wasan kwaikwayo.[223] Adrift on the Nile wani labari ne na shekarar 1966 na marubucin Masar kuma wanda ya lashe kyautar Nobel, Naguib Mahfouz, game da wani saurayi da ke zaune a cikin jirgin ruwa na gida a kan kogin Nilu. Kogin wani misali ne na rayuwar da ba zai iya sarrafawa ba, wanda ya sa shi juya wa al'umma baya.[224] Kogin Nilu yana taka muhimmiyar rawa a wasannin bidiyo da yawa, gami da Civilization VI.[225]
Tatsuniya da addini
[gyara sashe | gyara masomin]

Ilimin sararin samaniya na tsoffin Masarawa ya kasance mai dorewa a dabi'ance: maimakon kallon rayuwa a matsayin mai farawa da ƙarshe, ana kallon ta ne a matsayin da'ira mai dorewa. Wannan mahangar rayuwa ta da'ira ta samo asali ne daga duniyar dabi'a da ta kewaye Masarawa, hanyar wucewar rana ta yau da kullum, da kuma ambaliyar ruwan Nilu na shekara-shekara.[228] Allahn rana Ra yana ratsa sararin sama kowace rana daga gabas zuwa yamma, kuma matakai uku na ranar (fitowar rana, rana, da faɗuwar rana) sun dace da tsarin rayuwar ɗan adam: haihuwa, rayuwa, da mutuwa. Don wannan dalili, yawancin wuraren binne mutane an sanya su a gabar yammacin kogin Nilu, inda zasu kasance kusa da ranar da ke faɗuwa.[229] [lower-alpha 40]
A cikin addinin tsohuwar Masar, babu wani allah guda ɗaya da ya siffata kogin Nilu kamar yadda allah Ra ya siffata rana.[230] Allolin da ke da alaƙa da kogin sun haɗa da Hapy (allahn ambaliyar ruwa na shekara-shekara) da Khnum (allahn magudanan ruwa na farko na Nilu), waɗanda ke da alhakin samar da ambaliyar ruwan Nilu na shekara-shekara wanda ke takaita ƙasar noma ta ƙasar. [226] Addinin Masar ya sanya tushen ambaliyar ruwan Nilu na shekara-shekara a Tsibirin Elephantine (a madaidaicin ruwa na farko) inda aka yi imanin cewa ruwan ambaliyar yana kwarara ne daga duniyar matattu.[231]
Isis ta kasance babbar dangi a addinin Masar, tana da alaƙa mai ƙarfi da Nilu. Kungiyoyin asiri da ke da tushe a kan Isis sun bazu daga Masar zuwa Turai a ƙarni na biyu BCE.[232] Misali na tasirin ƙungiyar asiri ta Isis a Turai shi ne mosaic na Nilu na Palestrina, wanda ke Rome kuma ya kasance na ƙarni na farko BCE: mosaic mai girman mita 4 zuwa 3 yana nuna cikakken yanayin ƙasar Nilu.[233]
A cikin tatsuniyoyin Girka, Nilus shi ne allahn Nilu, ɗaya daga cikin dubban allolin kogi yaran Titans Oceanus da 'yar'uwarsa-matarsa Tethys. Nilus shi ne mahaifin naiad Memphis, wanda ya kafa birnin Memphis na tatsuniya a Masar.[234]
An ambaci sunan Nilu a cikin Littafi Mai Tsarki sau da yawa, ciki har da labari a cikin Littafin Fitowa game da jariri Musa da aka sanya shi a cikin kwando a cikin kogin.[227] Wasu mahukunta sun gano kogin Gihon – wanda aka ambata a cikin Littafin Farawa a matsayin ɗaya daga cikin Koguna Huɗu na Aljanna – a matsayin Nilu.[227] Labari mafi mahimmanci ga mutanen Coptic na Masar ana samun shi a cikin Littafin Matiyu: yana ba da labarin yadda kakan Yusufu da Maryamu mahaifiyar Yesu suka gudu zuwa Masar kuma suka zauna kusa da Nilu na shekaru da yawa, don haka suka guje wa Hiridus Mai Girma.[227]
Manazarta
[gyara sashe | gyara masomin]- 1 2 3 4 5 6 7 8 9 10 11 12 Hurst 2025.
- ↑ Allen 2000, pp. 21,101.
- ↑ Allen 2000, p. 339, 470.
- ↑ Samfuri:Multiref
- 1 2 Dumont 2009, p. 6.
- ↑ Hamilton 2016, p. 66.
- ↑ Murray 1923, p. 8.
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Sutcliffe 2009, pp. 338,345.
- 1 2 Dumont 2009, p. 4.
- ↑ Talling 2009, p. 390.
- ↑ Dumont 2009, p. 5.
- 1 2 3 4 5 6 7 8 9 10 Samfuri:Multiref
- 1 2 Samfuri:Multiref
- 1 2 Samfuri:Multiref
- ↑ "Source Du Nil", Google Maps.
- ↑ Tvedt 2021, p. 6.
- ↑ Walubiri 2018.
- ↑ Samfuri:Multiref
- 1 2 Tvedt 2021, pp. 323–324.
- ↑ Cite error: Invalid
<ref>tag; no text was provided for refs named "basinSize". - ↑ Allan 2009, p. 753.
- 1 2 3 4 Ranjan 2024, p. 18.
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Tvedt 2021, p. 214.
- 1 2 3 4 Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Collins 2002, pp. 47-69.
- ↑ Bunbury 2023, pp. 44-45.
- ↑ Shahin 2002, p. 276.
- 1 2 El-Shabrawy 2009, p. 149.
- ↑ Samfuri:Multiref
- ↑ Bunbury 2023, p. 45.
- ↑ Hamza 2009, p. 75.
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- 1 2 Senay 2014, p. 8639, Table 3.
- 1 2 Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ "Nile Basin Dongola", Global Runoff Data Center.
- ↑ Samfuri:Multiref
- ↑ Senay 2014, p. 8639, Table 4. Based on annual discharge figures: Blue Nile 48 km³; White Nile 28 km³; Atbarah 12 km³.
- ↑ Sutcliffe 2009, p. 357.
- ↑ Sutcliffe 2009, p. 346.
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Tvedt 2021, p. 5.
- ↑ Collins 2002, pp. 20-26.
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Lemma 2019, p. 1.
- ↑ Talbot & Williams 2009, p. 38.
- ↑ Talbot & Williams 2009, p. 37.
- 1 2 Samfuri:Multiref
- ↑ Witte 2009, p. 647.
- 1 2 3 Samfuri:Multiref
- ↑ Green 2009, p. 205.
- 1 2 Green 2009a, p. 705.
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Talling 2009a, p. 368.
- ↑ Samfuri:Multiref
- ↑ "Nile Basin National Water Quality", Nile Basin Initiative, pp. 12-22.
- ↑ Samfuri:Multiref
- ↑ Abotalib 2023.
- 1 2 3 Samfuri:Multiref
- 1 2 Williams 2009a, p. 771.
- ↑ Tvedt 2021, pp. 246,346
- ↑ Plummer 2023
- ↑ Abdelsalam 2018, pp. 742,768, Figures 30A, 30B, 30C, 30D
- ↑ Samfuri:Multiref
- 1 2 Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Assmann 2001, p. 59
- 1 2 Samfuri:Multiref
- 1 2 Samfuri:Multiref
- ↑ Shoup 2017, Article: "Culture of the Nile"
- ↑ Shoup 2017, Article: "History of Sudan: Arrival of Christianity and Islam"
- ↑ Shoup 2017, Article: "Ethiopia (Abyssinia)"
- ↑ Samfuri:Multiref
- ↑ Shoup 2017, Article: "Ethiopia (Abyssinia)"
- ↑ Stokes 2009, pp. 499-500, Article: "Nilotes"
- ↑ Samfuri:Multiref
- 1 2 3 Samfuri:Multiref
- ↑ Tvedt 2021, pp. 19-20
- ↑ Bunbury 2023, p. 50
- ↑ Collins 2002, p. 21
- ↑ Collins 2002, p. 21
- ↑ Bunbury 2023, pp. 50-52
- ↑ Samfuri:Multiref
- ↑ Tvedt 2021, pp. 177-179
- ↑ Tvedt 2021, p. 2
- ↑ Williams 2009, p. 70
- ↑ Tvedt 2021, pp. 177-179
- ↑ Tvedt 2021, p. 324
- ↑ Tvedt 2021, pp. 174–175
- ↑ Collins 2002, p. 36
- ↑ Allan 2009, pp. 749-751.
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- 1 2 Ranjan 2024, p. 22.
- 1 2 3 Dumont 2009, p. 17.
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- 1 2 3 Fleming & Lothian 1997, pp. 135-136.
- 1 2 Ranjan 2024, pp. 22-23.
- ↑ Tvedt 2021, pp. 63-68.
- ↑ Samfuri:Multiref
- 1 2 3 4 Ranjan 2024, p. 24.
- 1 2 Ranjan 2024, pp. 22-24.
- ↑ Samfuri:Multiref
- 1 2 Dumont 2009, p. 16.
- ↑ Samfuri:Multiref
- 1 2 3 4 Samfuri:Multiref
- 1 2 Ranjan 2024, pp. 24-25.
- 1 2 Tvedt 2021, pp. 71, 339-344.
- 1 2 Tvedt 2021, p. 70.
- ↑ Samfuri:Multiref
- 1 2 Ranjan 2024, pp. 26-27.
- ↑ Samfuri:Multiref
- 1 2 3 Endeshaw 2025.
- 1 2 Tvedt 2021, pp. 336-337.
- ↑ Tvedt 2021, pp. 244–245.
- ↑ Ranjan 2024, pp. 25–26.
- ↑ Roussi 2020.
- ↑ Bunbury 2023, p. 70.
- 1 2 3 4 Ranjan 2024, p. 27.
- ↑ Samfuri:Multiref
- 1 2 İlkbahar & Mercan 2023, pp. 1165-1166.
- 1 2 Roach 2025, pp. 1-2.
- 1 2 3 4 5 Ranjan 2024, p. 28.
- 1 2 Ranjan 2024, pp. 29-31.
- 1 2 Ranjan 2024, pp. 30-32.
- 1 2 Ranjan 2024, pp. 30,33.
- 1 2 Mureithi 2025.
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Waslekar 2009, p. 2.
- ↑ Samfuri:Multiref
- ↑ Tvedt 2021, p. 312.
- ↑ Samfuri:Multiref
- ↑ Tvedt 2021, pp. 244-245.
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- ↑ Samfuri:Multiref
- 1 2 Allan 2009, pp. 754-758.
- ↑ Allan 2009, pp. 754-755.
- ↑ Allan 2009, p. 758.
- 1 2 Samfuri:Multiref
- 1 2 Holt 2026.
- ↑ Samfuri:Multiref
- ↑ Hamza 2009, pp. 75, 84.
- 1 2 Sabr 2026.
- ↑ Samfuri:Multiref
- ↑ Cite error: Invalid
<ref>tag; no text was provided for refs named "perch". - 1 2 3 Witte 2009a, pp. 723-724.
- ↑ Witte 2009a, pp. 724-725.
- ↑ Witte 2009a, pp. 724-725, 742.
- ↑ Samfuri:Multiref
- ↑ Witte 2009a, p. 723.
- ↑ Samfuri:Multiref
- ↑ Tvedt 2021, p. 348.
- ↑ "Aswan Low Dam", Egypt MOEE.
- ↑ "Merowe Dam - Sudan", Abu Dhabi Fund for Development.
- ↑ "Upper Atbara Dam", OPEC Fund for International Development.
- ↑ "Roseires Dam", IHA.
- 1 2 3 Hailu 2022, Table 4.
- ↑ "Karuma", Uganda Radio Network.
- ↑ "Isimba Power Station", UEGCL.
- ↑ Griffin 2018.
- ↑ Angurini 2021.
- ↑ Tumwesigye 2011, p. 10.
- ↑ Sutcliffe 2009, p. 336.
- ↑ Tvedt 2021, p. 12.
- ↑ Samfuri:Multiref
- ↑ Tvedt 2021, p. 317.
- ↑ Tvedt 2021, pp. 115-117, 317.
- ↑ Samfuri:Multiref
- ↑ Younes 2024.
- ↑ "Private Sector in River Transport", EnterpriseAM.
- ↑ Samfuri:Multiref
- ↑ Dumont 2009, pp. 6-7.
- ↑ Samfuri:Multiref
- 1 2 3 Tvedt 2021, p. 47.
- ↑ Tvedt 2021, p. 54.
- ↑ Tvedt 2021, p. 77.
- ↑ Tvedt 2021, pp. 85-87.
- ↑ Tvedt 2021, p. 71.
- ↑ Tvedt 2021, p. 189.
- ↑ Bunbury 2023, p. 53.
- ↑ Tvedt 2021, p. 219.
- 1 2 3 Siliotti 1997, pp. 154-155.
- 1 2 3 Samfuri:Multiref
- 1 2 Samfuri:Multiref
- 1 2 Samfuri:Multiref
- ↑ "Colossal", The Concise Oxford Dictionary.
- ↑ Rosenthal 2005, pp. 41-42.
- ↑ Schama 1995, pp. 289-305.
- ↑ Samfuri:Multiref
- ↑ "Hymn to the Nile Flood", University College London.
- ↑ Tvedt 2021, p. 43.
- ↑ Ayenalem 2023.
- ↑ Tvedt 2021, p. 59.
- ↑ Tvedt 2021, pp. 77-78.
- ↑ Tvedt 2021, pp. 72-73.
- ↑ Tian 2025, pp. 95,100-102.
- 1 2 Samfuri:Multiref
- 1 2 3 4 Tvedt 2021, pp. 20-22.
- ↑ Samfuri:Multiref
- 1 2 Samfuri:Multiref
- ↑ Hornung 1982, pp. 77–79.
- ↑ Assmann 2001, pp. 54-55, 63.
- ↑ Tvedt 2021, p. 1.
- ↑ Tvedt 2021, p. 2.
- ↑ Smith 1878, pp. 499, 553-554, 564, 866.
Majiya
[gyara sashe | gyara masomin]Litattafai
[gyara sashe | gyara masomin]- Allan, John (2009). "Nile Basin Asymmetries: A Closed Fresh Water Resource, Soil Water Potential, the Political Economy and Nile Transboundary Hydropolitics". In Dumont, Henri (ed.). The Nile: Origin, Environments, Limnology and Human Use. Springer Netherlands. pp. 749–770. ISBN 9781402097263. Retrieved 1 December 2025.
- Allen, James P (2000). Middle Egyptian: An Introduction to the Language and Culture of Hieroglyphs. Cambridge University Press. ISBN 0521774837.
- Appiah, A.; Gates, H.L., eds. (2005). Africana: The Encyclopedia of the African and African American Experience. Oxford University Press. ISBN 9780195170559.
- Assmann, Jan (2001) [1984]. The Search for God in Ancient Egypt. Lorton, David transl. Cornell University Press. ISBN 0801487293.
- Badawi, Mohammad, ed. (2003). Al-Muhit Oxford Study Dictionary: English-Arabic. Academia. ISBN 995330050X. Retrieved 31 January 2026.
- Beaumont, Peter (1993). Drylands: Environmental Management and Development. Routledge. ISBN 0415004578. Retrieved 13 March 2026.
- Betancourt, P.P (2007). Introduction to Aegean Art. Institute for Aegean Prehistory. ISBN 9781623030841. Retrieved 1 January 2026.
- Bunbury, Judith; et al. (2023). "The Egyptian Nile". In Wantzen, Karl M. (ed.). River Culture. UNESCO. pp. 43–78. doi:10.54677/HHMI3947 Check
|doi=value (help). ISBN 9789231005404. Retrieved 10 March 2026.
- Camberlin, Pierre; et al. (2009). "Nile Basin Climates". In Dumont, Henri (ed.). The Nile: Origin, Environments, Limnology and Human Use. Springer Netherlands. pp. 307–333. ISBN 9781402097263. Retrieved 1 December 2025.
- Collins, Robert (2002). The Nile. Yale University Press. ISBN 9780300097641. Retrieved 16 March 2026. The "Bibliographical Essay" (pp. 245–248) lists books about the Nile River.
- Dumont, Henri (2009). "A Description of the Nile Basin, and a Synopsis of Its History, Ecology, Biogeography, Hydrology, and Natural Resources". In Dumont, Henri (ed.). The Nile: Origin, Environments, Limnology and Human Use. Springer Netherlands. pp. 1–22. ISBN 9781402097263. Retrieved 1 December 2025.
- Eggermont, Hilde; et al. (2009). "Rwenzori Mountains (Mountains of the Moon): Headwaters of the Nile". In Dumont, Henri (ed.). The Nile: Origin, Environments, Limnology and Human Use. Springer Netherlands. pp. 243–262. ISBN 9781402097263. Retrieved 1 December 2025.
- El-Shabrawy, Gamal; Dumont, Henri (2009). "The Fayum Depression". In Dumont, Henri (ed.). The Nile: Origin, Environments, Limnology and Human Use. Springer Netherlands. pp. 95–124. ISBN 9781402097263. Retrieved 1 December 2025.
- El-Shabrawy, Gamal (2009). "Lake Nasser-Nubia". In Dumont, Henri (ed.). The Nile: Origin, Environments, Limnology and Human Use. Springer Netherlands. pp. 125–156. ISBN 9781402097263. Retrieved 1 December 2025.
- El-Sheekh, Mostafa (2009). "River Nile Pollutants and Their Effect on Life Forms and Water Quality". In Dumont, Henri (ed.). The Nile: Origin, Environments, Limnology and Human Use. Springer Netherlands. pp. 395–406. ISBN 9781402097263. Retrieved 1 December 2025.
- Embabi, N.S. (2018). Landscapes and Landforms of Egypt. Springer Nature. doi:10.1007/978-3-319-65661-8_4. ISBN 9783319656595. Archived from the original on 4 February 2020. Retrieved 4 February 2020.
- Faulkner, Raymond (1964) [1962]. A Concise Dictionary of Middle Egyptian. Griffith Institute. Retrieved 26 March 2026.
- Fierro, Pedro; Nyer, Evan K. (2007). The Water Encyclopedia: Hydrologic Data and Internet Resources. CRC Press. ISBN 9781420012583. Retrieved 24 March 2026.
- Fleming, Fergus; Lothian, Alan (1997). The Way to Eternity: Egyptian Myth. Duncan Baird. ISBN 0705435032.
- Gardiner, Alan (1964) [1927]. Egyptian Grammar (3rd ed.). Oxford University Press . Retrieved 26 March 2026.
- Ghabbour, Samir (2009). "The Oligochaeta of the Nile Basin Revisited". In Dumont, Henri (ed.). The Nile: Origin, Environments, Limnology and Human Use. Springer Netherlands. pp. 499–520. ISBN 9781402097263. Retrieved 1 December 2025.
- Green, Jim (2009). "The Kyoga Catchment". In Dumont, Henri (ed.). The Nile: Origin, Environments, Limnology and Human Use. Springer Netherlands. pp. 205–214. ISBN 9781402097263. Retrieved 1 December 2025.
- Green, Jim (2009a). "Birds of the Nile". In Dumont, Henri (ed.). The Nile: Origin, Environments, Limnology and Human Use. Springer Netherlands. pp. 705–720. ISBN 9781402097263. Retrieved 1 December 2025.
- Green, Jim; El-Moghraby, Asim (2009). "Swamps of the Upper White Nile". In Dumont, Henri (ed.). The Nile: Origin, Environments, Limnology and Human Use. Springer Netherlands. pp. 193–204. ISBN 9781402097263. Retrieved 1 December 2025.
- Hamilton, Alan (2016). Luganda Dictionary and Grammar. Alan Hamilton. ISBN 9780954149611. Retrieved 31 January 2026.
- Hamza, Waleed (2009). "The Nile Delta". In Dumont, Henri (ed.). The Nile: Origin, Environments, Limnology and Human Use. Springer Netherlands. pp. 75–94. ISBN 9781402097263. Retrieved 1 December 2025.
- Hart, George (2005). The Routledge Dictionary of Egyptian Gods and Goddesses (Second ed.). Routledge. ISBN 0415344956. Retrieved 15 January 2026.
- Hornung, Erik (1982) [1971]. Conceptions of God in Egypt: The One and the Many. Translated by Baines, John. Original in German. Cornell University Press. ISBN 9780801412233. Retrieved 15 January 2026.
- Hughes, Ralph H.; et al. (1992). IUCN Directory of African Wetlands (PDF). International Union for Conservation of Nature. ISBN 9782880329495. Retrieved 2013-03-25.
- Lehman, John (2009). "Lake Victoria". In Dumont, Henri (ed.). The Nile: Origin, Environments, Limnology and Human Use. Springer Netherlands. pp. 215–242. ISBN 9781402097263. Retrieved 1 December 2025.
- Murray, G. W. (1923). An English-Nubian Comparative Dictionary. Humphrey Milford, Oxford University Press. Retrieved 15 January 2026.
- Okidi, C. O. (1994). "History of the Nile and Lake Victoria Basins through Treaties". In Howell, P.P.; Alan, J. J. (eds.). The Nile: Sharing a Scarce Resource. Cambridge University Press. pp. 321–350. ISBN 9780521450409. Retrieved 12 January 2026.
- Redford, Donald B., ed. (2001). Oxford Encyclopedia of Ancient Egypt. 2. Oxford University Press. ISBN 0195138228. Retrieved 26 March 2026.
- Redford, Donald B., ed. (2001a). Oxford Encyclopedia of Ancient Egypt. 3. Oxford University Press. ISBN 0195138236. Retrieved 26 March 2026.
- Roach, Steven (2025). "Introduction: Nile Basin Politics and its Challenges". In Roach, Steven; Hudson, Derrick (eds.). Nile Basin Politics: From Coordinated to Cooperative Peace. Edward Elgar Publishing. pp. 1–16. doi:10.4337/9781803927176. ISBN 9781803927176. Retrieved 15 January 2026.
- Robins, Gay (2008) [1997]. The Art of Ancient Egypt. Harvard University Press. ISBN 9780674030657. Retrieved 24 February 2026.
- Rosenthal, Lisa (2005). Gender, Politics, and Allegory in the Art of Rubens. Cambridge University Press. ISBN 9780521842440. Retrieved 15 December 2025.
- Said, Rushdi (1993). The River Nile: Geology, Hydrology, and Utilization. Pergamon Press. ISBN 0080418864. Retrieved 11 February 2026.
- Schama, Simon (1995). Landscape and Memory. A.A. Knopf. ISBN 9780679402558. Retrieved 15 December 2025.
- Shahin, Mamdouh (2002). Hydrology and Water Resources of Africa. Springer Netherlands. ISBN 9781402008665. Retrieved 7 January 2026.
- Shoup, John A.; et al. (2017). The Nile: An Encyclopedia of Geography, History, and Culture. Bloomsbury Publishing / ABC-CLIO. ISBN 9798216123323. Retrieved 14 February 2026. EBook. The hardcover is ISBN 9781440840401.
- Siliotti, Alberto (1997). Guide to the Valley of the Kings. Barnes & Noble . ISBN 9780760733257. Retrieved 24 February 2026.
- Smith, William (1878). A New Classical Dictionary of Greek and Roman Biography, Mythology And Geography. Harper & Brothers. LCCN 04035163. Retrieved 7 January 2026.
- Stokes, Jamie (2009). Encyclopedia of the Peoples of Africa and the Middle East. 2. Facts On File. ISBN 9781438126760. Retrieved 13 March 2026.
- Sutcliffe, John; et al. (2009). "The Hydrology of the Nile Basin". In Dumont, Henri (ed.). The Nile: Origin, Environments, Limnology and Human Use. Springer Netherlands. pp. 334–364. ISBN 9781402097263. Retrieved 1 December 2025.
- Talbot, Michael; Williams, Martin (2009). "Cenozoic Evolution of the Nile Basin". In Dumont, Henri (ed.). The Nile: Origin, Environments, Limnology and Human Use. Springer Netherlands. pp. 37–60. ISBN 9781402097263. Retrieved 1 December 2025.
- Talling, Jack (2009). "History of Scientific Research". In Dumont, Henri (ed.). The Nile: Origin, Environments, Limnology and Human Use. Springer Netherlands. pp. 23–34. ISBN 9781402097263. Retrieved 1 December 2025.
- Talling, Jack (2009a). "Physical and Chemical Water Characteristics". In Dumont, Henri (ed.). The Nile: Origin, Environments, Limnology and Human Use. Springer Netherlands. pp. 367–394. ISBN 9781402097263. Retrieved 1 December 2025.
- {{cite book
| title =Ancient Egypt in Video Games |editor-first=Jennifer |editor-last= Cromwell | isbn = 9783111534022 |year=2025 | publisher = de Gruyter Oldenbourg | chapter = Pharaohs, Labourers and Wonder Builders: Illustrating Ancient Egypt with Game Mechanics in Strategy Games | pages = 87–110 | last= Tian |first=Tian
Unknown author
[gyara sashe | gyara masomin]- "Abyssinia, Or the Empire of Prester John". Library of Congress. Jodocus Hondius. 1619. Retrieved 11 February 2026.
- "A Look into the Current State of the River Transport Sector". EnterpriseAM. 16 July 2025. Retrieved 11 February 2026.
- "Aswan Dam (1,2) Electric Hydro Power Plant". Ministry of Electricity and Renewable Energy. 2011. Archived from the original on 20 July 2011. Retrieved 2 January 2011.
- "Baḥr Al-Ghazāl". Britannica. 2025. Retrieved 7 January 2026.
- "Colossal". Concise Oxford English Dictionary. Oxford University Press. 2001. p. 282. ISBN 0198604386. Retrieved 27 December 2025.
- "Desert Agriculture in Egypt". Copernicus: Europe's Eyes on Earth. European Union Space Programme. 3 February 2024. Retrieved 12 February 2026.
- "Gov't Wants the Private Sector to Get in on Developing Egypt's River Transport". EnterpriseAM. 5 April 2023. Retrieved 11 February 2026.
- "Hymn to the Nile Flood". Digital Egypt for Universities. University College London. 2000. Retrieved 27 March 2026.
- "Isimba Hydropower Station". Uganda Electricity Generation Company Limited . 1 February 2026. Retrieved 7 February 2026.
- "The 600 MW Karuma Hydropower Plant Commissioned". The Independent (Uganda). Uganda Radio Network. 26 September 2024. Retrieved 3 August 2025.
- "Merowe Dam - Sudan". Abu Dhabi Fund for Development. 2024. Retrieved 13 April 2026.
- "Nile". Vatican Museum. Retrieved 14 January 2026.
- "Nile Basin - Station: Dongola". Global Runoff Data Center. University of New Hampshire. Retrieved 12 February 2026.
- "Nile Basin National Water Quality Monitoring Baseline Study Report for Egypt". Nile Basin Initiative. 2005. Retrieved 31 December 2025.
- "Personification of the River Nile". Yale Peabody Museum. Retrieved 14 January 2026.
- "Sudan - Roseires". International Hydropower Association. 2022. Retrieved 9 February 2026.
- "Source Du Nil". Google Maps. 18 March 2026. Retrieved 18 March 2026.
- "The Nile Basin Trust Fund". World Bank Group. 14 January 2016. Retrieved 20 January 2026.
- "Upper Atbara Dam Complex Project". OPEC Fund for International Development. 2026. Retrieved 12 April 2026.
- Water Accounting in the Nile River Basin. Food and Agriculture Organization - United Nations. 2020. doi:10.4060/ca9895en. ISBN 9789251329825. Retrieved 11 December 2025.
Journals and websites
[gyara sashe | gyara masomin]- Abdelsalam, Mohamed G. (February 2018). "The Nile's journey through space and time: A geological perspective". Earth-Science Reviews. 177: 742–773. Bibcode:2018ESRv..177..742A. doi:10.1016/j.earscirev.2018.01.010.
- Abotalib, Abotalib Z.; et al. (March 2023). "Irreversible and Large-Scale Heavy Metal Pollution Arising From Increased Damming and Untreated Water Reuse in the Nile Delta". Earth's Future. 11 (3). Bibcode:2023EaFut..1102987A. doi:10.1029/2022EF002987. Unknown parameter
|article-number=ignored (help)
- Angurini, Tom (2021). "Eskom Invests in Kiira Dam Water Controllers". Daily Monitor. Uganda. OCLC 44216472. Retrieved 8 February 2026.
- Ayenalem, Abebe Yirga; et al. (28 December 2023). "Popular culture and Nile hydropolitics: Amharic songs about the Grand Ethiopian Renaissance Dam". International Journal of Water Governance. 10 (1). doi:10.59490/ijwg.10.2023.7359 Check
|doi=value (help).
- Beck, Hylke E.; et al. (30 October 2018). "Present and future Köppen-Geiger climate classification maps at 1-km resolution". Scientific Data. 5 (1). Bibcode:2018NatSD...580214B. doi:10.1038/sdata.2018.214. PMC 6207062. PMID 30375988. Unknown parameter
|article-number=ignored (help)
- Creasman, Pearce Paul; et al. (16 September 2010). "Overland Boat Transportation During the Pharaonic Period: Archaeology and Iconography". Journal of Ancient Egyptian Interconnections. 2 (3). doi:10.2458/azu_jaei_v02i3_creasman.
- Driouech, Fatima; et al. (September 2020). "Assessing Future Changes of Climate Extreme Events in the CORDEX-MENA Region Using Regional Climate Model ALADIN-Climate". Earth Systems and Environment. 4 (3): 477–492. Bibcode:2020ESE.....4..477D. doi:10.1007/s41748-020-00169-3.
- El Mahmoudi, A.; Gabr, A. (2008). "Geophysical Surveys to Investigate the Relation Between the Quaternary Nile Channels and the Messinian Nile Canyon at East Nile Delta, Egypt". Arabian Journal of Geosciences. Springer Nature. 2 (1): 53–67. doi:10.1007/s12517-008-0018-9. ISSN 1866-7511.
- Endeshaw, Dawit (2025). "Ethiopia Opens Africa's Largest Hydroelectric Dam to Egyptian Protest". Reuters. Retrieved 20 January 2026.
- Griffin, Dan (2018). "Nearly Completed Dam on White Nile Casts a Long Shadow". The Irish Times. Dublin, Ireland. ISSN 0791-5144. Retrieved 28 December 2021.
- Hafez, Ahmed M.; et al. (December 2024). "Assessing the influences of future water development projects in Tekeze-Atbara-Setit basin on the Nile River inflow at Aswan, Egypt". Journal of Hydrology: Regional Studies. 56. Bibcode:2024JHyRS..5602007H. doi:10.1016/j.ejrh.2024.102007. Unknown parameter
|article-number=ignored (help)
- Hailu, Ashebir Dingeto (2022). "Ethiopia hydropower development and Nile basin hydro politics". AIMS Energy. 10 (1): 87–101. doi:10.3934/energy.2022006.
- Hassan, Fekri A. (December 2007). "The Aswan High Dam and the International Rescue Nubia Campaign". African Archaeological Review. 24 (3–4): 73–94. doi:10.1007/s10437-007-9018-5. JSTOR 40743449.
- Haupt, Paul (1926). "Etymological and Critical Notes". The American Journal of Philology. 47 (4): 305–318. doi:10.2307/289993. JSTOR 289993.
- Healy, R. W.; et al. (2007). "Water Budgets: Foundations for Effective Water-Resources and Environmental Management" (PDF). U.S. Geological Survey. Retrieved 14 January 2026.
- Hegab, Mahmoud H.; et al. (4 March 2025). "Evaluating the spatial pattern of water quality of the Nile River, Egypt, through multivariate analysis of chemical and biological indicators". Scientific Reports. 15 (1). Bibcode:2025NatSR..15.7626H. doi:10.1038/s41598-025-89982-2. PMC 11880377 Check
|pmc=value (help). PMID 40038343 Check|pmid=value (help). Unknown parameter|article-number=ignored (help)
- Holt, Peter; et al. (2026). "Egypt: Agriculture and Fishing". Britannica. Retrieved 7 February 2026.
- Hurst, Harold Edwin; et al. (2025). "Nile River". Britannica. Retrieved 11 December 2025.
- Huyge, Dirk; et al. (November 2011). "First evidence of Pleistocene rock art in North Africa: securing the age of the Qurta petroglyphs (Egypt) through OSL dating". Antiquity. 85 (330): 1184–1193. doi:10.1017/S0003598X00061998.
- İlkbahar, Hasan; Mercan, Muhammed Hüseyin (2023). "Hydro-Hegemony, Counter-Hegemony And Neoclassical Realism on the Nile Basin: An Analysis of Egypt's Response to the Grand Ethiopian Renaissance Dam (Gerd)". Journal of Asian and African Studies (in Turanci). Sage Publishing. 60 (2): 7–8. doi:10.1177/00219096231188953. ISSN 0021-9096.
- Kuper, Rudolph; Kröpelin, Stefan (11 August 2006). "Climate-Controlled Holocene Occupation in the Sahara: Motor of Africa's Evolution". Science. 313 (5788): 803–807. Bibcode:2006Sci...313..803K. doi:10.1126/science.1130989. PMID 16857900.
- Lemma, Hanibal; et al. (October 2019). "Bedload transport measurements in the Gilgel Abay River, Lake Tana Basin, Ethiopia". Journal of Hydrology. 577. Bibcode:2019JHyd..57723968L. doi:10.1016/j.jhydrol.2019.123968. Unknown parameter
|article-number=ignored (help)
- Leplongeon, Alice (27 December 2017). "Technological variability in the Late Palaeolithic lithic industries of the Egyptian Nile Valley: The case of the Silsilian and Afian industries". PLOS ONE. 12 (12). Bibcode:2017PLoSO..1288824L. doi:10.1371/journal.pone.0188824. PMC 5744920. PMID 29281660. Unknown parameter
|article-number=ignored (help)
- Liu, S.; et al. (March 2009). "Pinpointing the sources and measuring the lengths of the principal rivers of the world". International Journal of Digital Earth. 2 (1): 80–87. Bibcode:2009IJDE....2...80L. doi:10.1080/17538940902746082.
- Marshall, Brian E. (September 2018). "Guilty as charged: Nile perch was the cause of the haplochromine decline in Lake Victoria". Canadian Journal of Fisheries and Aquatic Sciences. 75 (9): 1542–1559. Bibcode:2018CJFAS..75.1542M. doi:10.1139/cjfas-2017-0056.
- McCoy, Terrence; et al. (20 June 2023). "The Nile is the World's Longest River? The Amazon Would Like a Word". Washington Post. Retrieved 24 March 2026.
- McKenna, Amy; et al. (2025). "Blue Nile River". Britannica. Retrieved 31 December 2025.
- Mureithi, Carlos (9 September 2025). "Ethiopia Inaugurates Africa's Largest Hydroelectric Dam as Egypt Rift Deepens". The Guardian. Retrieved 15 February 2026.
- Plummer, Thomas W.; et al. (10 February 2023). "Expanded geographic distribution and dietary strategies of the earliest Oldowan hominins and Paranthropus". Science. 379 (6632): 561–566. Bibcode:2023Sci...379..561P. doi:10.1126/science.abo7452. PMID 36758076 Check
|pmid=value (help).
- Ranjan, Amit (2 January 2024). "Grand Ethiopian Renaissance Dam dispute: implications, negotiations, and mediations". Journal of Contemporary African Studies. 42 (1): 18–36. doi:10.1080/02589001.2023.2287425.
- Roussi, Antoaneta (23 July 2020). "Row over Africa's largest dam in danger of escalating, warn scientists". Nature. 583 (7817): 501–502. Bibcode:2020Natur.583..501R. doi:10.1038/d41586-020-02124-8. PMID 32669727.
- Sabr, Mohy el-Din; et al. (2026). "Sudan: Agriculture, Forestry, and Fishing". Britannica. Retrieved 7 February 2026.
- Senay, Gabriel B.; et al. (November 2014). "Understanding the hydrologic sources and sinks in the N ile B asin using multisource climate and remote sensing data sets". Water Resources Research. 50 (11): 8625–8650. Bibcode:2014WRR....50.8625S. doi:10.1002/2013WR015231.
- Tumwesigye, Robert; et al. (2011). Key Issues in Uganda's Energy Sector (PDF). International Institute for Environment and Development. ISBN 978-1-84369-831-9. Retrieved 7 February 2026.
- Van de Moortel, Aleydis (October 2007). "Book Review of Sacred and Secular: Ancient Egyptian Ships and Boats, by Cheryl A. Ward". American Journal of Archaeology. 111 (4). doi:10.3764/ajaonline1114.VandeMoortel.
- Walubiri, Moses (16 October 2018). "New Nile Bridge Is Fifth Longest of Its Kind in Africa". New Vision. Retrieved 16 October 2018.
- Warburg, Gabriel R. (2007). "The Search for the Sources of the White Nile and Egyptian-Sudanese Relations". Middle Eastern Studies. 43 (3): 475–486. doi:10.1080/00263200701246165. JSTOR 4284556.
- {{Cite web
|last= Waslekar |first= Sundeep |author-link= Sundeep Waslekar | url = http://www.strategicforesight.com/publication_pdf/11374Nile%20concise.pdf |title = Blue Peace fo
- ↑ Wasu daga cikin cataracts sun nutse saboda madatsun ruwa da aka gina.
- ↑ An fara gano wurin a 1969 ta masu bincike daga Waseda University.[14] A 2006, wasu masu yawon buɗe ido suka sake gano wurin, suka sanya alama a wani itace kusa (2°16′56″S 29°19′53″E / 2.28222°S 29.33139°E) wanda yanzu wurin yawon buɗe ido ne.[14] A 2009, masana suka yi amfani da hotunan tauraron dan adam don ƙara daidaita wurin, suka sanya shi a wani rijiya (2°19′35″S 29°21′30″E / 2.32639°S 29.35833°E) da ke nesa da wurin na 1969/2006.[14]
- ↑ Cite error: Invalid
<ref>tag; no text was provided for refs named "longest". - ↑ Abin tunawa yana a 3°54′54.0″S 29°50′16.5″E / 3.915000°S 29.837917°E.[17]
- ↑ Nilu yana fita daga Lake Victoria a Jinja, inda ake da wuraren yawon buɗe ido da ake kira "source of the Nile".[19]
- ↑ Asalin Bakin Nilu yana kusan km 75 kudu da Lake Tana, a 10°58′12″N 37°11′55″E / 10.9699°N 37.1986°E.[21]
- ↑ A shekara ta 2011, Sudan ta Kudu ta balle daga Sudan, ta zama ƙasa ta goma sha ɗaya a Kwarin Nilu.[24]
- ↑ Asalin Kogin Nilu yana kaiwa zuwa Kogin Rukarara, sannan zuwa Kogin Mwogo, wanda ke haɗuwa da Kogin Mbirurume ya zama Kogin Nyabarongo, wanda ke kaiwa zuwa Kogin Kagera, wanda kuma ke zubowa cikin Tafkin Victoria.[27]
- ↑ An auna ne ta fuskar faɗin ƙasa, ba girman ruwa ba.
- ↑ Yankin Farar Nilu, kamar yadda aka bayyana nan, yana dauke da karamin bangare na babban Kogin Farar Nilu.
- ↑ Bangaren Nilu tsakanin haduwar Bakar/Farar Nilu da Bahar Rum ana kiransa Babban Nilu ko Saharan Nilu.[35]
- 1 2 Cite error: Invalid
<ref>tag; no text was provided for refs named "exclGERD". - 1 2 Cite error: Invalid
<ref>tag; no text was provided for refs named "discharge". - ↑ An yi kwatancen ne da gudun Nilu da aka auna a Aswan. Gudun Nilu zuwa Tekun Bahar Rum ya fi ƙanƙanta.[lower-alpha 13]
- ↑ Yayin da gudun Blue Nile ke raguwa a lokacin sanyi, ruwan White Nile da aka tara yana ƙaruwa a Khartoum. A Afrilu da Mayu, White Nile yana bayar da kusan 80% na ruwan Nilu. Wannan ya ba da damar yin ban ruwa a duk shekara.[53]
- ↑ Ƙarfin ambaliyar Nilu na shekara-shekara yana iya bambanta sosai daga shekara zuwa shekara. Lokutan ƙarancin ambaliya na iya ɗaukar shekaru da dama ko ƙarni.[54]
- ↑ Gudun shekara-shekara na kogin a Aswan kusan 84 km³; kuma tafkin Aswan High Dam yana iya riƙe kusan 160 km³.[56]
- ↑ Jack Talling ya rubuta "Abubuwa biyu na ruwan Nilu na ƙasa sun jawo hankali – cewa yana da inganci don sha da ban ruwa, kuma cewa yana ɗauke da yawan laka a yanayi."[70]
- ↑ Kogin Nilu da Tafkin Victoria ba su kasance a irin wannan siffar ba a lokacin Australopithecus afarensis, Homo habilis, ko masana'antar Oldowan.[79]
- ↑ Wasu masana sun sanya iyakar arewacin Nubia a Ambaliya ta Farko;Appiah & Gates 2005, pp. 1447 wasu kuma a Ambaliya ta Biyu.Tvedt 2021, p. 93
- ↑ Kusan 642 Z.Z., mayaƙan Larabawa sun kawo addinin Musulunci zuwa Masar, suka maye gurbin addinin Masar na dā.[99]
- ↑ Turawan Yamma sun raba Afirka a wani tsari da ake kira Scramble for Africa, wanda aka tabbatar a taron Berlin na 1885. Bisa wannan yarjejeniya, Birtaniya ta samu mafi yawan kwarin Nilu.[110]
- 1 2 3 4 Masar ta samu ‘yancin kai na zahiri a 1922, amma Birtaniya ta ci gaba da iko da harkokin waje kuma ta ajiye sojoji kusa da Suez Canal. Cikakken ‘yanci ya samu a 1957 bayan rikicin Suez.[119] Cite error: Invalid
<ref>tag; name "EgyptIndep" defined multiple times with different content. - ↑ Yarjejeniyar ta 1959 ta kuma tanadi diyya daga Masar zuwa Sudan saboda korar Nubians daga wuraren su na asali sakamakon tafkin da Aswan High Dam ya haifar.[122]
- ↑ Turawan mulkin mallaka sun raba Afirka a lokacin wani tsari da ake kira tseren kwace Afirka, wanda aka amince da shi a taron Berlin na shekarar 1885. Karkashin wannan yarjejeniya, Birtaniya ta sami mafi yawan yankin magudanar ruwan Nile.[148]
- ↑ Yarjejeniyar ta 1959 ta kuma tanadi biyan diyya na kuɗi daga Masar zuwa Sudan don kwashe mutanen Nubia sakamakon sabon tafkin ruwa da aka samar a bayan madatsar ruwa ta Aswan High Dam.[122]
- ↑ A cewar Sundeep Waslekar, fari a yankin magudanar ruwan Nile a ƙarni na 20 ya shafi kusan mutane miliyan 170 kuma ya kashe mutane rabin miliyan. Daga cikin fari guda 70 da suka faru tsakanin 1900 da 2012, guda 55 sun faru ne a Habasha, Sudan, Sudan ta Kudu, Kenya da Tanzania.[157]
- ↑ Sudan ta Kudu ba ta zama ƙasa ba tukunna a shekarar 1999, amma ta shiga shirin Nile Basin Initiative a shekarar 2012.[24] Eritrea ta ƙi shiga cikin shirin Nile Basin Initiative.[159]
- ↑ Kenya ba tana ɗaya daga cikin waɗanda suka fara sanya hannu ba, amma ta sanya hannu jim kaɗan bayan ƙirƙirar ta.[161]
- ↑ Yarjejeniyar ta 2015 ta gindaya cewa ƙasashe ukun za su yi amfani da ruwan kogin Nile cikin adalci da dacewa; kuma sun amince kan wata hanya ta cika tafkin da kuma sarrafa madatsar ruwan.[143]
- ↑ An lissafa jimillar ikon samar da wuta na yankin magudanar ruwan Nile ta hanyar haɗa dakarun samar da wuta daga tebur mai taken "Manyan tashoshin wutar lantarki daga ruwa a yankin magudanar ruwan Nile". An gano hanyoyin samun bayanan ikon kowace tashar wutar lantarki a cikin wannan tebur ɗin.
- ↑ Wannan teburin ya haɗa da tashoshin wutar lantarki daga ruwa kawai waɗanda ke da ikon samar da wuta sama da 100 MW. Ba a haɗa da ƙananan tashoshi ba kamar su Assiut Barrage, Jebel Aulia Dam, Naga Hammadi dam, Esna Power Plant, da Tis Abay I, II. Ba a haɗa da tashoshin wutar lantarki na wajen yankin magudanar ruwan Nile ba, kamar su Gilgel Gibe Dams I, II, da III na Habasha.
- ↑ Launuka a cikin shashen "Wuri na Kusa" suna nuna ƙasar da tashar wutar lantarki take.
- 1 2 Ayyukan fasaha da ke nuna obelisk a kan jirgin ruwa yana nan a cikin haikalan jana'iza na Deir el-Bahari. Kogin Nile ya kasance mafi kusa da rukunin dala na Giza Pyramid Complex fiye da yadda yake a yau, wanda hakan ya ba jiragen ruwa damar kawo duwatsu kusa da wurin ginin.[198]
- ↑ Bayanai game da jigilar kayayyaki ta ruwa a Masar na shekarar 2023 ne.[199]
- ↑ A shekarar 1992, ma'aikacin laburare na Smithsonian Martin R. Kalfatovic ya tattara littattafai 1,150 da ke bayyana tafiye-tafiye a kogin Nile.[203]
- ↑ Cikakken bayani na babban aikin fasaha a cikin Kabarin Menna a cikin Makabartar Theban[211]
- ↑ Babban mutum-mutumi shi ne wanda ya ninka girman rayuwa na asali ko fiye da haka.[215]
- ↑ Zance daga Antony and Cleopatra (Kashi na 2, Shafi na 7). "Foison" yana nufin girbi mai albarka.
- ↑ Gefen yamma na kogin shi ne inda yawancin abubuwan tunawa na jana'izar Masar suke, gami da rukunin dala na Giza, Makabartar Memphite, da kwarin Sarakuna.[229]
<ref> tags exist for a group named "lower-alpha", but no corresponding <references group="lower-alpha"/> tag was found.