Ageostrophy

Ageostrophy ma ọ bụ (ageostrophic flow) bụ ọdịiche dị n'etiti ikuku ma ọ bụ mmiri na ikuku geostrophic ma ọ bụ ikuku geostrophhic.^[1]^[2] Ébé ọ bụ na geostrophy bụ ezi nguzozi n'etiti ike Coriolis na ike gradient nrụgide, ọganihu ageostrophic na-egosipụta enweghị nguzozi, ya mèrè a na-emetụtakarị na nsogbụ, mmegharị kwụ ọtọ (dị mkpa màkà ihu igwe), na mgbanwe ngwa ngwa na ógè. Ageostrophic flow na-egosipụta ịdị adị nkè okwu ndị ọzọ niile na usoro nhazi nke a leghaara ányà na echiche ahụ, gụnyere friction na ngwa ngwá ngwá ngwa Dv / Dt, nké gụnyere ike centrifugal na-agbagharị agbagharị.

Hụkwa[dezie | dezie ebe o si]

geostrophic
ifufe nke ala

Edensibia[dezie | dezie ebe o si]

↑ Douglass (March 2015). "Analysis of ageostrophy in strong surface eddies in the Atlantic Ocean" (in en). Journal of Geophysical Research: Oceans 120 (3): 1490–1507. DOI:10.1002/2014JC010350.
↑ Kontoyiannis (1990). "Ageostrophy and pressure work in the Gulf Stream at 73°W" (in en). Journal of Geophysical Research 95 (C12): 22209. DOI:10.1029/JC095iC12p22209. ISSN 0148-0227.

[1] Douglass (March 2015). "Analysis of ageostrophy in strong surface eddies in the Atlantic Ocean" (in en). Journal of Geophysical Research: Oceans 120 (3): 1490–1507. DOI:10.1002/2014JC010350.

[2] Kontoyiannis (1990). "Ageostrophy and pressure work in the Gulf Stream at 73°W" (in en). Journal of Geophysical Research 95 (C12): 22209. DOI:10.1029/JC095iC12p22209. ISSN 0148-0227.

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