In:
Journal of Advances in Modeling Earth Systems, American Geophysical Union (AGU), Vol. 13, No. 9 ( 2021-09)
Abstract:
Over ocean, aerosol optical depth (AOD) bias contributes about 25% to the 60°S–60°N mean shortwave (SW) flux bias for the multi‐model mean (MMM) result Over land, AOD and land surface albedo biases contribute about 40% and 30% to the 60°S–60°N mean SW flux bias for the MMM result Observation‐based land surface albedo should be used by all models to accurately calculate the top‐of‐atmosphere (TOA) SW fluxes
Type of Medium:
Online Resource
ISSN:
1942-2466
,
1942-2466
DOI:
10.1029/2021MS002584
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2021
detail.hit.zdb_id:
2462132-8