Spatiotemporal distribution characteristics and attribution of extreme regional low temperature event

Based on an objective identification technique for regional low temperature event(OITRLTE), the daily minimum temperature in China has been detected from 1960 to 2013. During this period, there were 60 regional extreme low temperature events(ERLTEs), which are included in the 690 regional low temper...

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Published inChinese physics B Vol. 24; no. 10; pp. 659 - 666
Main Author 封泰晨 张珂铨 苏海晶 王晓娟 龚志强 张文煜
Format Journal Article
LanguageEnglish
Published 01.10.2015
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ISSN1674-1056
2058-3834
1741-4199
DOI10.1088/1674-1056/24/10/109201

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Abstract Based on an objective identification technique for regional low temperature event(OITRLTE), the daily minimum temperature in China has been detected from 1960 to 2013. During this period, there were 60 regional extreme low temperature events(ERLTEs), which are included in the 690 regional low temperature events(RLTEs). The 60 ERLTEs are analyzed in this paper. The results show that in the last 50 years, the intensity of the ERLTEs has become weak; the number of lasted days has decreased; and, the affected area has become small. However, that situation has changed in this century.In terms of spatial distribution, the high intensity regions are mainly in Northern China while the high frequency regions concentrate in Central and Eastern China. According to the affected area of each event, the 60 ERLTEs are classified into six types. The atmospheric circulation background fields which correspond to these types are also analyzed. The results show that, influenced by stronger blocking highs of Ural and Lake Baikal, as well as stronger southward polar vortex and East Asia major trough at 500-h Pa geopotential height, cold air from high latitudes is guided to move southward and abnormal northerly winds at 850 h Pa makes the cold air blow into China along diverse paths, thereby forming different types of regional extreme low temperatures in winter.
AbstractList Based on an objective identification technique for regional low temperature event(OITRLTE), the daily minimum temperature in China has been detected from 1960 to 2013. During this period, there were 60 regional extreme low temperature events(ERLTEs), which are included in the 690 regional low temperature events(RLTEs). The 60 ERLTEs are analyzed in this paper. The results show that in the last 50 years, the intensity of the ERLTEs has become weak; the number of lasted days has decreased; and, the affected area has become small. However, that situation has changed in this century.In terms of spatial distribution, the high intensity regions are mainly in Northern China while the high frequency regions concentrate in Central and Eastern China. According to the affected area of each event, the 60 ERLTEs are classified into six types. The atmospheric circulation background fields which correspond to these types are also analyzed. The results show that, influenced by stronger blocking highs of Ural and Lake Baikal, as well as stronger southward polar vortex and East Asia major trough at 500-h Pa geopotential height, cold air from high latitudes is guided to move southward and abnormal northerly winds at 850 h Pa makes the cold air blow into China along diverse paths, thereby forming different types of regional extreme low temperatures in winter.
Based on an objective identification technique for regional low temperature event (OITRLTE), the daily minimum temperature in China has been detected from 1960 to 2013. During this period, there were 60 regional extreme low temperature events (ERLTEs), which are included in the 690 regional low temperature events (RLTEs). The 60 ERLTEs are analyzed in this paper. The results show that in the last 50 years, the intensity of the ERLTEs has become weak; the number of lasted days has decreased; and, the affected area has become small. However, that situation has changed in this century. In terms of spatial distribution, the high intensity regions are mainly in Northern China while the high frequency regions concentrate in Central and Eastern China. According to the affected area of each event, the 60 ERLTEs are classified into six types. The atmospheric circulation background fields which correspond to these types are also analyzed. The results show that, influenced by stronger blocking highs of Ural and Lake Baikal, as well as stronger southward polar vortex and East Asia major trough at 500-hPa geopotential height, cold air from high latitudes is guided to move southward and abnormal northerly winds at 850 hPa makes the cold air blow into China along diverse paths, thereby forming different types of regional extreme low temperatures in winter.
Author 封泰晨 张珂铨 苏海晶 王晓娟 龚志强 张文煜
AuthorAffiliation Department of Atmospheric Sciences, Lanzhou University, Lanzhou 730000, China College of Physics and Electronic Project, Changshu Institute of Technology, Changshu 215500, China Laboratory for Climate Prediction, National Climate Center, China Meteorological Administration, Beijing 100081, China
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Notes regional low temperature, extreme events, classification of low temperature events
Feng Tai-Chen, Zhang Ke-Quan, Su Hai-Jing,Wang Xiao-Juan,Gong Zhi-Qiang,Zhang Wen-Yu( a) Department of Atmospheric Sciences, Lanzhou University, Lanzhou 730000, China b) College of Physics and Electronic Project, Changshu Institute of Technology, Changshu 215500, China C) Laboratory for Climate Prediction, National Climate Center, China Meteorological Administration, Beijing 100081, China
11-5639/O4
Based on an objective identification technique for regional low temperature event(OITRLTE), the daily minimum temperature in China has been detected from 1960 to 2013. During this period, there were 60 regional extreme low temperature events(ERLTEs), which are included in the 690 regional low temperature events(RLTEs). The 60 ERLTEs are analyzed in this paper. The results show that in the last 50 years, the intensity of the ERLTEs has become weak; the number of lasted days has decreased; and, the affected area has become small. However, that situation has changed in this century.In terms of spatial distribution, the high intensity regions are mainly in Northern China while the high frequency regions concentrate in Central and Eastern China. According to the affected area of each event, the 60 ERLTEs are classified into six types. The atmospheric circulation background fields which correspond to these types are also analyzed. The results show that, influenced by stronger blocking highs of Ural and Lake Baikal, as well as stronger southward polar vortex and East Asia major trough at 500-h Pa geopotential height, cold air from high latitudes is guided to move southward and abnormal northerly winds at 850 h Pa makes the cold air blow into China along diverse paths, thereby forming different types of regional extreme low temperatures in winter.
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Snippet Based on an objective identification technique for regional low temperature event(OITRLTE), the daily minimum temperature in China has been detected from 1960...
Based on an objective identification technique for regional low temperature event (OITRLTE), the daily minimum temperature in China has been detected from 1960...
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SubjectTerms Atmospheric circulation
Blocking
China
Cold working
Extreme values
High frequencies
Regional
Spatial distribution
中国北方
事件
区域性
归因
时空分布特征
最低温度
目标识别技术
类型区
Title Spatiotemporal distribution characteristics and attribution of extreme regional low temperature event
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