首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Potential flaws of interdecadal changes over eastern China around the early 1990s in the National Centers for Environmental Prediction-National Center for Atmospheric Research reanalyses
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Potential flaws of interdecadal changes over eastern China around the early 1990s in the National Centers for Environmental Prediction-National Center for Atmospheric Research reanalyses

机译:1990年代初,中国国家环境预测中心-国家大气研究中心的年代际变化的潜在缺陷

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This study compares interdecadal changes in tropospheric temperature and geopotential height over eastern China in four reanalyses and upper air radiosonde (UAR) observations. It is found that the tropospheric temperature and geopotential height over eastern China during the period 1992-2000 were systematically lower in the National Centers for Environmental Prediction (NCEP)-National Center for Atmospheric Research (NCAR) reanalysis-1 and the NCEP-Department of Energy reanalysis-2 compared to the UAR observations. Accordingly, the tropospheric temperature and geopotential height over eastern China in the NCEP reanalyses showed a pronounced interdecadal decrease around 1992, while this decrease was not significant in the UAR observations, the 40 year European Centre for Medium-Range Weather Forecasts (ERA-40) reanalysis, and the 25 year Japanese Meteorological Agency (JRA-25) reanalysis. The overestimated interdecadal change in the NCEP reanalyses may lead to an inconsistent variation between tropospheric and surface climates. When summer surface air temperature increases (decreases) over southern China, summer tropospheric temperature over eastern China generally increases (decreases) in the ERA-40, JRA-25, and UAR data sets, which is physically supported by the NCAR Community Climate System Model version 3. However, this link between the troposphere and surface is not observed in the two NCEP reanalyses. The interdecadal bias in tropospheric temperature after 1992 in the NCEP reanalyses is possibly related to an operational change in the bias correction tables since 1992.
机译:本研究通过四个再分析和高空无线电探空仪(UAR)观测结果,比较了中国东部对流层温度和地势高度的年代际变化。结果发现,在1992-2000年期间,中国东部的对流层温度和地势高度在国家环境预测中心(NCEP)-国家大气研究中心(NCAR)重新分析-1和NCEP部门中均相对较低。能量再分析2与UAR观察结果相比。因此,在NCEP重新分析中,中国东部的对流层温度和地势高度显示1992年前后年代际显着下降,而这一下降在UAR观测(40年欧洲中距离天气预报中心(ERA-40))中并不显着。重新分析,以及25年的日本气象厅(JRA-25)重新分析。 NCEP重新分析中年代际变化的高估可能会导致对流层和地表气候之间不一致的变化。当华南地区夏季地面气温升高(降低)时,在ERA-40,JRA-25和UAR数据集中,华东地区夏季对流层温度总体上升高(降低),这在NCAR社区气候系统模型的支持下得到了物理支持。版本3。但是,在两次NCEP重新分析中未观察到对流层和表面之间的这种联系。 NCEP再分析中1992年以后对流层温度的年代际偏差可能与1992年以来偏差校正表的运行变化有关。

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