Tsarin rana

Tsarin rana
	ƙunshiya
Bayanai
Ƙaramin ɓangare na	biological rhythm (en)

Tsarin rana (ko sake zagayowar diele) kowane tsari ne wanda ke sake dawowa kowane sa'o'i 24 sakamakon cikakken juyawa na Duniya Duniya a kusa da axis dinta.^[1] Juyawa na duniya yana haifar da sauye-sauyen zafin jiki a ko'ina cikin rana da dare, da kuma sauye-shiryen yanayi a ko'in shekara. Tsarin rana ya dogara da radiation na rana.^[2]

Yanayi da yanayi

A cikin ilimin yanayi, sake zagayowar rana tana ɗaya daga cikin siffofin asali na Yanayin yanayi, gami da bambance-bambance a cikin zafin rana da ruwan sama.^[1] Hanyoyin yau da kullun na iya zama kusan sinusoid" id="mwJw" rel="mw:WikiLink" title="Sinusoidal">sinusoidal ko kuma sun haɗa da abubuwan da ke cikin sinusoid mai raguwa (saboda fitowar Sun da saitawa) da kuma shakatawa na zafi (Newton cooling) da dare.^[1] Tsarin rana kuma yana da babban tasiri a kan matakan carbon dioxide a cikin yanayi, saboda matakai kamar photosynthesis da numfashi na salula.^[3]

Tasirin halittu

Tsarin rana na haske da zafin jiki na iya haifar da irin wannan sake zagayowar a cikin hanyoyin halittu, kamar photosynthesis a cikin shuke-shuke [1] da kuma bakin ciki a cikin mutane. [2] Sakamakon shuke-shuke ga sake zagayowar muhalli na iya haifar da sake zagayowan kai tsaye a cikin ayyukan microbial na Rhizosphere, gami da daidaita nitrogen.[3]

Tsarin rabin rana

Akwai nau'ikan raƙuman ruwa daban-daban guda uku: na rana, wanda ke da babban ruwa guda ɗaya da ƙananan ruwa guda ɗaya a kowace rana; na rabin rana, wanda yake da manyan raƙuman mmiri guda biyu da ƙananan raƙuman ƙasa guda biyu a kowace rana, da kuma gauraye, wanda ke leɓuɓɓugar ruwa guda biyu da manyan raɗauka biyu a kowace ƙasa tare da tsawo daban-daban.

Tsarin rabin rana yana nufin tsari wanda ke faruwa kusan kowane sa'o'i goma sha biyu ko kusan sau biyu a rana. Sau da yawa waɗannan za a iya danganta su da hawan wata, a wannan yanayin lokacin ya kusa da awanni 12 da minti 25.

Dubi kuma

Tarihin Tarihi
Sautin Circadian
Gudun kai tsaye na Diel
Rashin rana
Diurnal climate [de]

Manazarta

↑ ^1.0 ^1.1 ^1.2 Betts, A (2015). "Boundary layer (atmospheric) and air polution | Diurnal Cycle". Encyclopedia of Atmospheric Sciences (in Turanci) (2nd ed.): 319–23. doi:10.1016/B978-0-12-382225-3.00135-3. ISBN 9780123822253.
↑ Hartmann, Dennis L. (1994). "The Energy Balance of the Surface". International Geophysics (in Turanci). 56: 81–114. doi:10.1016/S0074-6142(08)60561-6. ISSN 0074-6142.
↑ Matthews, Jack S.A.; Vialet-Chabrand, Silvere R.M.; Lawson, Tracy (2017). "Diurnal Variation in Gas Exchange: The Balance between Carbon Fixation and Water Loss". Plant Physiology. 174 (2): 614–623. doi:10.1104/pp.17.00152. ISSN 0032-0889. PMC 5462061. PMID 28416704.

[:0-1] 1.0 ^1.1 ^1.2 Betts, A (2015). "Boundary layer (atmospheric) and air polution | Diurnal Cycle". Encyclopedia of Atmospheric Sciences (in Turanci) (2nd ed.): 319–23. doi:10.1016/B978-0-12-382225-3.00135-3. ISBN 9780123822253.

[2] Hartmann, Dennis L. (1994). "The Energy Balance of the Surface". International Geophysics (in Turanci). 56: 81–114. doi:10.1016/S0074-6142(08)60561-6. ISSN 0074-6142.

[:1-3] Matthews, Jack S.A.; Vialet-Chabrand, Silvere R.M.; Lawson, Tracy (2017). "Diurnal Variation in Gas Exchange: The Balance between Carbon Fixation and Water Loss". Plant Physiology. 174 (2): 614–623. doi:10.1104/pp.17.00152. ISSN 0032-0889. PMC 5462061. PMID 28416704.

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