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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...

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שמור ב:
Principais autores: Stephan R. deRoode, Fredrik Jansson, Lydia Mak, Louise Nuijens
פורמט: Artigo
שפה:Inglês
יצא לאור: American Geophysical Union (AGU) 2025-09-01
סדרה:Journal of Advances in Modeling Earth Systems
נושאים:
atmospheric boundary layers
wind
parameterizations
turbulence
large‐eddy simulations
גישה מקוונת:https://doi.org/10.1029/2024MS004579
תגים: הוספת תג
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