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A statistical method to get surface level air-temperature from satellite observations of precipitable water

机译:一种从可观测水的卫星观测中获取地表气温的统计方法

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Ten-day mean surface level air-temperature from SSMI precipitable water (SSMI-Ta) has been derived and compared with the temperature from two ocean data buoys (Buoy-Ta) of Japan Meteorological Agency (JMA) for a period of six months (July–December, 1988). Statistical relations between air-temperature and mixing ratio, using data from ocean data buoys are used to derive air-temperature from mixing ratio, obtained from SSMI precipitable water. For getting the mixing ratio from precipitable water, regional mixing ratio-precipitable water relations have been used, instead of global relation proposed by Liu (1986). The rms errors (standard deviation of the difference between SSMI-Ta and Buoy-Ta) for two buoy locations are found to be 1.15 and 1.12°C, respectively. Surface level temperature for the two buoy locations are also derived using direct regression relation between Buoy-Ta and precipitable water. The rms errors of the SSMI-Ta, in this case are found to be reduced to 1.0°C.
机译:得出了SSMI可沉淀水(SSMI-Ta)的十天平均地面温度,并将其与日本气象厅(JMA)的两个海洋数据浮标(Buoy-Ta)的温度进行了六个月的比较( 1988年7月至12月)。空气温度与混合比之间的统计关系(使用海洋数据浮标的数据)用于从混合比得出空气温度,混合比是从SSMI可沉淀水获得的。为了从可降水量中获得混合比,使用了区域混合率-可沉淀水的关系,而不是Liu(1986)提出的全局关系。发现两个浮标位置的均方根误差(SSMI-Ta和浮标-Ta之差的标准偏差)分别为1.15和1.12°C。还使用浮标-Ta和可沉淀水之间的直接回归关系得出了两个浮标位置的表面温度。在这种情况下,SSMI-Ta的均方根误差已降至1.0°C。

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