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Variability of global upper-tropospheric water vapor derived from satellite infrared observations

机译:来自卫星红外观测的全球对流层高层水汽的变异性

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Uncertainties in the amount and variability of global atmospheric water vapor content weaken our ability to define the present climate system and lessens our confidence in future predictions of climate change. In particular, the small amount of water vapor in the upper troposphere contributes disproportionately to the Earth's radiation budget. In this paper, infrared observations of global upper tropospheric water vapor are analyzed to examine variability on seasonal and interannual time scales. Particular attention is given to the intersatellite calibration of the seven instruments used to piece together the time series of observations from 1981-1990 (and extending the record through 1993 by IGARSS). A method for identifying and removing the intersatellite biases is discussed and implemented. Analysis of the adjusted time series shows upper troposphere water vapor variability related to the seasonal cycle of the monsoon circulations and interannual variability related to El Nino/Southern Oscillation warm and cold events.
机译:全球大气中水汽含量的数量和变异性的不确定性削弱了我们定义当前气候系统的能力,并削弱了我们对未来气候变化预测的信心。特别是,对流层高层中少量的水蒸气对地球的辐射预算造成了不成比例的贡献。在本文中,对全球对流层高层水蒸气的红外观测进行了分析,以检查季节和年际时间尺度的变化。特别关注了七种仪器的星际校准,这些仪器用于将1981-1990年的观测时间序列拼凑在一起(并由IGARSS将记录扩展到1993年)。讨论并实现了一种识别和消除星际偏差的方法。对调整后的时间序列的分析表明,与季风环流的季节周期有关的对流层高层水汽变化和与厄尔尼诺现象/南方涛动的冷热事件有关的年际变化。

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