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Evaluation of the distribution of subtropical free tropospherichumidity in AMIP-2 simulations using METEOSAT water vaporchannel data

机译:利用METEOSAT水汽通道数据在AMIP-2模拟中评估亚热带自由对流层湿度的分布

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摘要

In the framework of the Atmospheric ModelIntercomparison Project (AMIP) phase 2, we haveestablished a diagnostic of the free tropospheric humidity(FTH) distribution using METEOSAT data over the 1984–1995 period for 14 climate models. The methodology ofevaluation follows a two step ‘‘model-to-satellite’’ approach.First the raw METEOSAT ‘‘Water Vapor’’ radiances aresimulated from the model profiles of temperature andhumidity using the RTTOV-7 radiative transfer model.Second, the radiances are converted into FTH using thesame coefficients as in the satellite product offering a directcomparison. The analysis is focused on the dry subtropicalareas observed by METEOSAT: the Eastern Mediterraneanand the tropical South Atlantic Ocean. Most of the modelsreproduce the observed seasonal cycle both in terms ofphasing and magnitude, despite an overall moist bias. A fewmodels are in close agreement with the satellite data. Themagnitude of the satellite estimated inter-annual variability isalso generally captured by models. Again, a small subsetof models shows close agreement with the observations.This comparison suggests general improvements of themodels with respect to the AMIP-1 simulations.
机译:在大气模型比较项目(AMIP)第二阶段的框架中,我们使用1984-1995年期间的METEOSAT数据对14个气候模型建立了对流层自由湿度(FTH)分布的诊断。评估方法遵循两步``从模型到卫星''的方法:首先使用RTTOV-7辐射传递模型从温度和湿度的模型剖面中模拟原始的METEOSAT``水蒸气''辐射率。使用与直接比较卫星产品相同的系数将其转换为FTH。该分析着重于METEOSAT观测到的干燥亚热带地区:东地中海和热带南大西洋。尽管总体上存在潮湿偏见,但大多数模型都从相位和幅度上再现了观察到的季节性周期。一些模型与卫星数据非常吻合。卫星估计的年际变化的幅度通常也由模型捕获。同样,一小部分模型显示出与观测值非常吻合。此比较表明,相对于AMIP-1模拟,该模型具有一般性改进。

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