So'ose paɛ yelezuo la

Climate models

Ze'ele Wikipiidiya

maala climate dela sɛla n de kalɛ wɛda models dikɛ la    sɔa tara sɔsiga ti la sugera nimu'urɛ sɔsiga magesɛ wuu 'atmosphere 'tiŋa zuo,kule katɛ, and sakuga. Ba tari ba ita la yɛla zo'e zo'e yɛsera la zamesego sɔ wɛda system ti la zɛkɛ ti beere wɛda. Wɛda models me ta'am dɛna zoore(I.e dagena kalɛ)models la tuusum me dela sɛla n lagum paasɛ beere

Wɛda maala kalɛ ze'eti la  pansɛka n  ze'eti wileŋa puan kini na la ti la dɛna 'electronmagnetic radiation wave gira.'chiefly yɛa la wave gira (du)'infrared, n la wave yese woko (zaɛ) infrared electromagnetic. A ka zu iŋetulegerɛ teesum.

Kalɛ  maala zo'e mɛ bɔna burabura.mw "a simple radiant heat transfer model treats tiŋa la wuu zugu yiŋa zia la averages paŋa sɛsiga.ina ta'am karigɛ woko puan (radiative -convective models) la zaleŋa.Coupled atmosphere - ocean - sea ice dunia maala models'' solve the full equations for mass la paŋa transfer la radiant exchange. Le pa'asɛ , modelling burabura ba sɛba ta'am ''interlinked, mw peelum tuunɛ, ''in Earth System models,basɛ ti viiseba tana bukera sɔsega climate la ecosystems[1][2][3]

Viisegɔ Lɔgerɔ[demese | demesego zia]

  1. Pubs.GISS: Wang and Stone 1980: Effect of ice-albedo feedback on global sensitivity in a one-dimensional.... nasa.gov.
  2. Wang, W.C. (1980). "Effect of ice-albedo feedback on global sensitivity in a one-dimensional radiative-convective climate model". J. Atmos. Sci. 37 (3): 545–52. DOI:<0545:EOIAFO>2.0.CO;2 10.1175/1520-0469(1980)037<0545:EOIAFO>2.0.CO;2.
  3. Climate Change 2001: The Scientific Basis. grida.no.