| Weather and Climate |
|
|
|
|
| Analysis of High Temperature Climatic Characteristics in Ningxia and Atmospheric Circulation Anomaly |
| YANG Jian-ling1,2, FENG Jian-min1, YAN Jun1, WANG Jian-ying1, ZHENG Guang-fen1 |
1.Key Laboratory of Meteorological Disaster Preventing and Reducing in Ningxia, Yinchuan 750002, China;
2.Ningxia Climate Center, Yinchuan 750002, China |
|
|
|
|
Abstract Based on the daily maximum temperature data from 24 meteorological stations in Ningxia during 1960-2009 and the NCEP/NCAR reanalysis geopotential height data, the spatial distribution, inter-annual and inter-decadal variation trends of high temperature days in Ningxia, and the corresponding atmospheric circulation anomaly were analyzed. Results showed that the frequency of appearing high temperature was relatively high in mid-north area of Ningxia with Dawukou and Tongxin as two high frequency centers, and the highest frequency occurred in July. The number of high temperature days was most in 1971, 2000, 2001 and 2005, and no occurred in 1962, 1979 and 1989. Inter-decadal abrupt change of high temperature frequency occurred in the middle 1990s, and the average annual days with high temperature in Ningxia during 1997-2009 increased to 4.4 times that during 1960-1996. The inter-annual and inter-decadal anomalies of high temperature frequency are associated with wide range atmospheric circulation anomalies, namely a wave train distribution of high-level height anomaly field in a wide range from western Europe to the Bering Strait. If the meridional circulation in middle and high latitude of Asia is weak, the days with high temperature in Ningxia are most. On the contrary, if the meridional circulation is strong and the north cold air moves southward easily, the days with high temperature in Ningxia are less.
|
|
Received: 21 March 2012
Published: 20 September 2012
|
|
|
| [1]王绍武,叶谨林.近百年全球气候变暖的分析[J].大气科学,1995,19(5):545-553.[2]郭江勇,陈少勇,高蓉,等.气温变暖对西北西风带冬季气温的影响分析[J].中国沙漠,2010,30(1):175-181.[3]张洪芬,王劲松,黄斌.西北西风区与东部季风区年气温变化特征对比分析[J].中国沙漠,2009,29(6):1203-1206.[4]陈少勇,郭江勇,韩通,等.中国西北干旱半干旱区近46 a秋季气候变暖分析[J].中国沙漠,2009,29(3):544-550.[5]董满宇,江源,任斐鹏,等.近50 a来北方农牧交错带气温变化趋势及突变分析[J].中国沙漠,2010,30(4):926-932.[6]丁一汇,张锦,宋亚芳.天气和气候极端事件的变化及其与全球变暖的联系[J].气象,2002,28(3):3-7.[7]赵光平,杨淑萍,穆建华,等.全球变化对宁夏近40 a极端气温变化的影响[J].中国沙漠,2009,29(6):1207-1211.[8]王兴梅,张勃,戴声佩,等.甘肃省黄土高原区夏季极端降水的时空特征[J].中国沙漠,2011,31(1):223-229.[9]徐金芳,邓振镛,陈敏.中国高温热浪危害特征的研究综述[J].干旱气象,2009,27(2):163-167.[10]任福民,翟盘茂.1951-1990年中国极端气温变化分析[J].大气科学,1998,22(2):217-227.[11]邹瑾,冯晓云,胡桂芳,等.山东省夏季极端高温异常气候变化特征分析[J].气象科技,2004,32(3):182-186.[12]史军,丁一汇,崔林丽.华东极端高温气候特征及成因分析[J].大气科学,2009,33(2):347-358.[13]郭渠,孙卫国,程炳岩,等.重庆近48年来高温天气气候特征及其环流形势[J].长江流域资源与环境,2009,18(1):52-59.[14]林建,毕宝贵,何金海.2003年7月西太平洋副热带高压变异及中国南方高温形成机理研究[J].大气科学,2005,29(4):594-599.[15]尹洁,张传江,张超美.江西2003年夏季罕见高温气候诊断分析[J].南京气象学院学报,2005,28(6):855-861.[16]张尚印,张海东,徐祥德,等.我国东部三市夏季高温气候特征及原因分析[J].高原气象,2005,24(5):829-835.[17]王鹏祥,杨金虎.中国西北近45 a来极端高温事件及其对区域性增暖的响应[J].中国沙漠,2007,27(4):649-655.[18]赵庆云,赵红岩,王勇.甘肃省夏季异常高温及其环流特征分析[J].中国沙漠,2007,27(4):639-643.[19]王劲松,费晓玲,魏锋.中国西北近50 a来气温变化特征的进一步研究[J].中国沙漠,2008,28(4):724-732.[20]辛渝,陈洪武,李元鹏,等.新疆北部高温日数的时空变化特征及多尺度突变分析[J].干旱区研究,2008,25(3):438-446.[21]蔡新玲,高红燕,胡琳,等.陕西夏季高温的统计特征分析[J].陕西气象,2006(5):22-24.[22]桑建人,刘玉兰,邱旺.气候变暖对宁夏引黄灌区水稻生产的影响[J].中国沙漠,2006,26(6):953-958.[23]杨淑萍,赵光平,马力文,等.气候变暖对宁夏气候和极端天气事件的影响及防御对策[J].中国沙漠,2007,27(6):1072-1076.[24]桑建人,刘玉兰,舒志亮.近44 a宁夏严重干燥事件对气候变暖的响应[J].中国沙漠,2007,27(5):878-882.[25]陈楠,彭维耿.宁夏高温多、少年平均环流及OLR场特征分析[J].干旱气象,2004,22(2):23-27.[26]张智,林莉,梁培,等.宁夏年气温资料的均一性检验研究[J].气象,2009,35(10):79-83. |
| No Suggested Reading articles found! |
|
|
Viewed |
|
|
|
Full text
|
|
|
|
|
Abstract
|
|
|
|
|
Cited |
|
|
|
|
| |
Shared |
|
|
|
|
| |
Discussed |
|
|
|
|
2012, Vol. 32 
