QR koda

Countergradient Momentum Transport in Clear Convective Atmospheric Boundary Layers

Abstract The vertical profiles of the wind speed and direction in atmospheric boundary layers are strongly controlled by turbulence. Most global weather forecast and climate models parameterize the vertical transport of horizontal momentum by turbulent eddies by means of a downgradient eddy diffusio...

Popoln opis

Shranjeno v:
Bibliografske podrobnosti
Principais autores: Stephan R. deRoode, Fredrik Jansson, Lydia Mak, Louise Nuijens
Format: Artigo
Jezik:Inglês
Izdano: American Geophysical Union (AGU) 2025-09-01
Serija:Journal of Advances in Modeling Earth Systems
Teme:
Online dostop:https://doi.org/10.1029/2024MS004579
Oznake: Označite
Brez oznak, prvi označite!