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This file was derived from: LFC-NCL.png

Mmẹkụwátá

Nkówá
English: Diagram showing the path of a convective parcel of moist air. It becomes satured when it reaches the Level of Condensation by Lifting (LCL) and reaches instability at the Level of Free Convection (LFC) when its temperature (T) becomes greater than the one from the environment. The CAPE is the area between the environment and the parcel path between the LFC and the Equilibrium level.
Ǹgụ́ụ̀bọ̀chị̀
Mkpọlọ́gwụ̀ File:LFC-NCL.png
Odé ákwụ́kwọ́ Pierre_cb, Grische
Nke ya ozor Meteorology_thermodynamic_fr.svg

Nkwényé

w:en:Creative Commons
í-kpó-áhà gbásàa kà
Edebere faịlụ a n'okpuru ikikeree Creative Commons Attribution-Share Alike 3.0 Unported license.
I wepulara nóru:
  • i nye – ikọpị,ikekasi na izịpụ ọru a
  • i dowaria – igbanwee ọrụ a
Ọ ga bụ na ọnọdụ ndi a:
  • í-kpó-áhà – Ị ga-enyerịrị ugo kwesịrị ekwesị, nye njikọ na ikikere ahụ, ma gosikwa ma emere mgbanwe. Ị nwere ike ime ya n'ụzọ ezi uche ọ bụla, mana ọ bụghị n'ụzọ ọ bụla na-egosi na onye nyere ikikere kwadoro gị maọbụ ojiji gị.
  • gbásàa kà – Ọ bụrụ na ị tụgharịgharịa, gbanwee, ma ọ bụ wulite n'elu ihe ahụ, ị ga-ekesa ndenye gị n'okpuru otu ma ọ bụ ikike dakọtara dị ka nke mbụ.

Nkowapụta

Tinye nkọwa otu ahịrị ihe faịlụ a na-anochi anya ya.
Path of a parcel of moist air lifted up to saturation at the LCL and reaching afterwards the LFC, where it becomes positively bouyant.

Ihe ndị egosiri na faịlụ a

depicts Bekee

Oge/afọ mmalite

8 Eprel 2014

MIME ụdị

image/svg+xml

Ịta nke usòrò

Bìri èhì/ogè k'ị hụ òtù ụ̀fa dị̀ m̀gbè ahụ̀.

Èhì/OgèMbọ-akaÓgólógó na asaáÒjìèmeNkwute
dị ùgbu â10:25, 8 Eprel 2014NvóÁká màkà otù ȯ dị nà 10:25, 8 Eprel 2014336 × 542 (15 KB)GrischeUser created page with UploadWizard

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