[Objective] The aim was to study the reasons for consecutive severe droughts in autumn and winter. [Method] By dint of precipitation in the observatory station and NCEP/NCAR reanalysis data in observatory station, the...[Objective] The aim was to study the reasons for consecutive severe droughts in autumn and winter. [Method] By dint of precipitation in the observatory station and NCEP/NCAR reanalysis data in observatory station, the circulation background, vertical movement, abnormal temperature and changes of water vapor conditions in Xuzhou from October 2008 to January 2009 were expounded to reveal the causes for consecutive drought in autumn and winter. [Result] Xuzhou was under stable situation for a long time in autumn and winter in 2008, being behind east coastal trough, the downward airstream prevailing; the south trough intensity was weak, and in addition to the east subtropical high and weak intensity, the water vapor transportation condition in Indian Ocean and South Sea was unfavorable. The autumn was warm and the cold air was weak; ever since winter, there were several cold air activities. But the influencing body was in the east, and the south warm and wet airstream was insufficient. Thus, they couldn’t met, which resulted into gale and lower temperature and less precipitation when under the influence of cold air. [Conclusion] The study provided theoretical basis for the prevention of drought in the area.展开更多
在近40年江苏降水异常机理分析的基础上,利用江苏月降水量资料和NCEP/NCAR逐月再分析资料对2010/2011年江苏秋冬春连旱与近40年的3次连旱过程进行了对比分析。结果表明,1980/1981年干旱持续时间最长,2010/2011年干旱程度最强。从气象要...在近40年江苏降水异常机理分析的基础上,利用江苏月降水量资料和NCEP/NCAR逐月再分析资料对2010/2011年江苏秋冬春连旱与近40年的3次连旱过程进行了对比分析。结果表明,1980/1981年干旱持续时间最长,2010/2011年干旱程度最强。从气象要素分析来看,2010/2011年干旱的对流层大气干燥程度、下沉运动的剧烈程度都较强,且持续时间较长。1980/1981年和2010/2011年北半球500 h Pa高度场上,亚洲中高纬地区主要表现为"东低西高"的距平分布型,贝加尔湖以西阻塞形势发展,东亚大槽加深且维持,东亚冬季风偏强,北方冷空气南下频繁,冷空气一方面阻碍了南方暖湿气流的输送,另一方面使得空气更干燥。海温异常分布为La Nina型,赤道中东太平洋和中国东部沿海附近海温表现为负异常,而中西太平洋海温表现为正异常,这样的海温分布特征有利于形成欧亚地区"东低西高"环流型。与上述两次连旱过程相比,1998/1999年和2008/2009年干旱程度略轻,大气背景场和海温异常分布存在差异。展开更多
基金Supported by Xuzhou Scientific Program (XM09B023)
文摘[Objective] The aim was to study the reasons for consecutive severe droughts in autumn and winter. [Method] By dint of precipitation in the observatory station and NCEP/NCAR reanalysis data in observatory station, the circulation background, vertical movement, abnormal temperature and changes of water vapor conditions in Xuzhou from October 2008 to January 2009 were expounded to reveal the causes for consecutive drought in autumn and winter. [Result] Xuzhou was under stable situation for a long time in autumn and winter in 2008, being behind east coastal trough, the downward airstream prevailing; the south trough intensity was weak, and in addition to the east subtropical high and weak intensity, the water vapor transportation condition in Indian Ocean and South Sea was unfavorable. The autumn was warm and the cold air was weak; ever since winter, there were several cold air activities. But the influencing body was in the east, and the south warm and wet airstream was insufficient. Thus, they couldn’t met, which resulted into gale and lower temperature and less precipitation when under the influence of cold air. [Conclusion] The study provided theoretical basis for the prevention of drought in the area.
文摘在近40年江苏降水异常机理分析的基础上,利用江苏月降水量资料和NCEP/NCAR逐月再分析资料对2010/2011年江苏秋冬春连旱与近40年的3次连旱过程进行了对比分析。结果表明,1980/1981年干旱持续时间最长,2010/2011年干旱程度最强。从气象要素分析来看,2010/2011年干旱的对流层大气干燥程度、下沉运动的剧烈程度都较强,且持续时间较长。1980/1981年和2010/2011年北半球500 h Pa高度场上,亚洲中高纬地区主要表现为"东低西高"的距平分布型,贝加尔湖以西阻塞形势发展,东亚大槽加深且维持,东亚冬季风偏强,北方冷空气南下频繁,冷空气一方面阻碍了南方暖湿气流的输送,另一方面使得空气更干燥。海温异常分布为La Nina型,赤道中东太平洋和中国东部沿海附近海温表现为负异常,而中西太平洋海温表现为正异常,这样的海温分布特征有利于形成欧亚地区"东低西高"环流型。与上述两次连旱过程相比,1998/1999年和2008/2009年干旱程度略轻,大气背景场和海温异常分布存在差异。
