Evaluations of retrieved cloud liquid water from AMSR-E, and impacts on numerical weather prediction

T. Egawa, M. Kazumori
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Abstract

Japan Meteorological Agency (JMA) uses the observations from the Advanced Microwave Scanning Radiometer for Earth Observing System (AMSR-E) in the data assimilation systems for the numerical weather prediction (NWP). In the JMA mesoscale model (MSM), retrievals of total column precipitable water (TCPW) and precipitation (PR) are assimilated. A MSC (Meteorological Satellite Center) algorithm is used to retrieve them. In the global spectral model (GSM), radiances of vertically polarized channels in less-cloudy area are assimilated. But cloud-affected radiances are also used. In our NWP experiments, retrievals of cloud liquid water (CLW) from AMSR-E with the MSC algorithm were used to remove the strongly cloud-affected data and to correct the bias which is derived from the thin cloud. The most significant impact on the forecast experiment was the improvement of the temperature at 850 hPa in the tropics.
AMSR-E反演云液态水的评价及其对数值天气预报的影响
日本气象厅(JMA)在数值天气预报(NWP)的资料同化系统中使用先进微波扫描地球观测系统(AMSR-E)的观测资料。在JMA中尺度模式(MSM)中,总柱可降水量(TCPW)和降水量(PR)被同化。采用MSC(气象卫星中心)算法检索。在全球光谱模式(GSM)中,吸收了少云地区垂直极化信道的辐射度。但也使用了受云影响的辐射。在我们的NWP实验中,使用MSC算法从AMSR-E检索云液态水(CLW)来去除强云影响数据并纠正来自薄云的偏差。对预报试验影响最显著的是热带地区850 hPa温度的改善。
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