Advection na danshi
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Advection na danshi shine jigilar tururi ta iska. Aunawa da ilimin tururin ruwa na yanayi, ko "ruwa", yana da mahimmanci a cikin tsinkaya na duk abubuwan yanayi, musamman girgije, hazo, zafin jiki, zafi, ƙididdigar ta'aziyya da hazo. Yankunan advection na danshi galibi suna tare da yankuna na advection mai dumi.[1]
Ma'anar
[gyara sashe | gyara masomin]Yin amfani da ma'anar gargajiya na advection, an bayyana advection na danshi kamar haka:
inda V shine iska mai laushi, kuma
ρ
m
{\displaystyle \rho _{m}}
shine yawan tururi na ruwa. Koyaya, yawanci ana auna abun cikin tururi na ruwa dangane da haɗuwa (ƙananan taro) a cikin satar-linkid="22" href="./Meteorological_reanalysis" id="mwGQ" rel="mw:WikiLink" title="Meteorological reanalysis">sake nazarin ko raɓa (zafin jiki zuwa matsin matsin tururi, watau zafi na dangi zuwa 100%) a cikin hasashen aiki. Za'a iya tunanin advection na raɓa kanta a matsayin advection mai danshi:
Ruwa mai guba
[gyara sashe | gyara masomin]Dangane da haɗuwa, ana iya wakiltar jigilar kaya / advection a kwance dangane da kwararar danshi:
inda q shine rabo na gauraya. Ana iya haɗa darajar a duk faɗin yanayi don jimlar jigilar danshi ta hanyar tsaye:
inda
ρ
{\displaystyle \rho }
shine yawan iska, kuma P shine matsin lamba a ƙasa. Don ma'anar dama mai nisa, mun yi amfani da kusanci na daidaitattun Hydrostatic.
Kuma bambancinsa (haɗuwa) yana nuna evapotranspiration (ruwa) kamar ƙarawa (cirewa) danshi daga shafi:
inda P, E, da cikakkiyar kalma sune - hazo, evapotranspiration, da kuma lokacin canjin ruwan sama, duk an wakilta su dangane da taro / (yanki * lokaci na raka'a). Mutum na iya canzawa zuwa wasu raka'a na yau da kullun a tsawon kamar mm ta hanyar ninka yawan ruwa mai ruwa da kuma ma'aunin juyawa na tsawon lokaci.
Dubi kuma
[gyara sashe | gyara masomin]- Haar (fog)
- Tsarin ruwa
- Advection mai kyau
Manazarta
[gyara sashe | gyara masomin]- ↑ "Moisture Advection: along the 850 mb surface". ww2010.atmos.uiuc.edu. Retrieved 2019-02-07.