Omens of coupled model biases in the CMIP5 AMIP simulations

被引:0
|
作者
Alina Găinuşă-Bogdan
Frédéric Hourdin
Abdoul Khadre Traore
Pascale Braconnot
机构
[1] Laboratoire de Météorologie Dynamique/IPSL/UPMC Univ Paris 06/Sorbone Universités/CNRS,
[2] Environnements et Paléoenvironnements Océaniques et Continentaux/OASU/Université de Bordeaux/CNRS,undefined
[3] Laboratoire des Sciences du Climat et de l’Environnement,undefined
[4] IPSL,undefined
[5] unité mixte CEA-CNRS-UVSQ,undefined
来源
Climate Dynamics | 2018年 / 51卷
关键词
Climate model biases; AMIP simulations; Coupled simulations; Latent heat flux; Sea surface temperature; Sensitivity tests;
D O I
暂无
中图分类号
学科分类号
摘要
Despite decades of efforts and improvements in the representation of processes as well as in model resolution, current global climate models still suffer from a set of important, systematic biases in sea surface temperature (SST), not much different from the previous generation of climate models. Many studies have looked at errors in the wind field, cloud representation or oceanic upwelling in coupled models to explain the SST errors. In this paper we highlight the relationship between latent heat flux (LH) biases in forced atmospheric simulations and the SST biases models develop in coupled mode, at the scale of the entire intertropical domain. By analyzing 22 pairs of forced atmospheric and coupled ocean-atmosphere simulations from the CMIP5 database, we show a systematic, negative correlation between the spatial patterns of these two biases. This link between forced and coupled bias patterns is also confirmed by two sets of dedicated sensitivity experiments with the IPSL-CM5A-LR model. The analysis of the sources of the atmospheric LH bias pattern reveals that the near-surface wind speed bias dominates the zonal structure of the LH bias and that the near-surface relative humidity dominates the east–west contrasts.
引用
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页码:2927 / 2941
页数:14
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