兰州大学学报(自然科学版)
蘭州大學學報(自然科學版)
란주대학학보(자연과학판)
JOURNAL OF LANZHOU UNIVERSITY(NATURAL SCIENCES)
2014年
1期
54-58
,共5页
张圆圆%李艳%付培健%李景鑫%董雷鹏
張圓圓%李豔%付培健%李景鑫%董雷鵬
장원원%리염%부배건%리경흠%동뢰붕
ENSO Modoki%极端低温%西北地区
ENSO Modoki%極耑低溫%西北地區
ENSO Modoki%겁단저온%서북지구
ENSO Modoki%extremely low temperature%Northwest China
利用1979-2008年的NCEP/NCAR再分析资料和中国西北地区136个台站的气象资料,研究了ENSO Modoki与春、秋季中国西北地区极端低温的关系。结果表明:当秋季发生El Ni?o Modoki事件时,次年春季新疆中部、西北部边缘地区及祁连山脉附近的极端低温事件较少,发生La Ni?a Modoki事件时则相反;当冬季发生El Ni?o Modoki事件时,次年秋季宁夏、陕西及甘肃中南部地区的极端低温事件较多,而发生La Ni?a Modoki事件时则相反。另外,500 hPa位势高度场合成分析显示,极端低温事件多发与否,与中国西北地区附近是否有发展旺盛的径向环流有着一定的关系。
利用1979-2008年的NCEP/NCAR再分析資料和中國西北地區136箇檯站的氣象資料,研究瞭ENSO Modoki與春、鞦季中國西北地區極耑低溫的關繫。結果錶明:噹鞦季髮生El Ni?o Modoki事件時,次年春季新疆中部、西北部邊緣地區及祁連山脈附近的極耑低溫事件較少,髮生La Ni?a Modoki事件時則相反;噹鼕季髮生El Ni?o Modoki事件時,次年鞦季寧夏、陝西及甘肅中南部地區的極耑低溫事件較多,而髮生La Ni?a Modoki事件時則相反。另外,500 hPa位勢高度場閤成分析顯示,極耑低溫事件多髮與否,與中國西北地區附近是否有髮展旺盛的徑嚮環流有著一定的關繫。
이용1979-2008년적NCEP/NCAR재분석자료화중국서북지구136개태참적기상자료,연구료ENSO Modoki여춘、추계중국서북지구겁단저온적관계。결과표명:당추계발생El Ni?o Modoki사건시,차년춘계신강중부、서북부변연지구급기련산맥부근적겁단저온사건교소,발생La Ni?a Modoki사건시칙상반;당동계발생El Ni?o Modoki사건시,차년추계저하、협서급감숙중남부지구적겁단저온사건교다,이발생La Ni?a Modoki사건시칙상반。령외,500 hPa위세고도장합성분석현시,겁단저온사건다발여부,여중국서북지구부근시부유발전왕성적경향배류유착일정적관계。
NCEP/NCAR reanalysis data and data from 136 weather station in Northwest China were used to establish the relationship between ENSO Modoki and extremely low temperature over Northwest China. A correlation analysis showed that when El Ni?o Modoki occurred in autumn, the number of occurrences of extremely low temperature events would decrease in central Xinjiang, northwest edge of the area and the Qilian Mountains area in the next spring. However, when La Ni?a Modoki occurred in autumn, the situation would be opposite. When El Ni?o Modoki occurred in winter, the number of occurrences of extremely low temperature events would increase in Ningxia, Shanxi, central and southern Gansu in next autumn; when La Ni?a Modoki occurred in winter, the situation would be opposite. Composting analysis of 500 hPa geopotential height field showed that the occurrence of extremely low temperature events relied heavily on exuberant radial circulation near Northwest China.