Understanding the Abrupt Climate Change in the Mid-1970s from a Phase-Space Transform Perspective

被引:13
作者
Dai, Tanlong [1 ]
Dong, Wenjie [2 ,3 ]
Guo, Yan [1 ]
Hong, Tao [1 ]
Ji, Dong [1 ]
Yang, Shili [1 ]
Tian, Di [4 ]
Wen, Xiaohang [5 ]
Zhu, Xian [1 ,3 ]
机构
[1] Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource Ecol, Beijing, Peoples R China
[2] Sun Yat Sen Univ, Sch Atmospher Sci, Guangzhou, Guangdong, Peoples R China
[3] Beijing Normal Univ, Future Earth Res Inst, Zhuhai Joint Innovat Ctr Climate Environm Ecosyst, Zhuhai, Peoples R China
[4] Second Inst Oceanog, State Key Lab Satellite Ocean Environm Dynam, Hangzhou, Zhejiang, Peoples R China
[5] Chengdu Univ Informat Technol, Coll Atmospher Sci, Plateau Atmosphere & Environm Key Lab Sichuan Pro, Chengdu, Sichuan, Peoples R China
基金
中国国家自然科学基金;
关键词
Climate classification; regimes; Climate variability; Climatology; ASIAN SUMMER MONSOON; MULTI-DECADAL VARIABILITY; ARCTIC OSCILLATION; SURFACE-TEMPERATURE; GLOBAL MONSOON; PRECIPITATION; 20TH-CENTURY; ENSO;
D O I
10.1175/JAMC-D-17-0345.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Abrupt climate change may cause heat, drought, and flood disasters. In this study, we find that many climate factors [e.g., the East Asian summer monsoon (EASM), the Arctic Oscillation (AO) and the Pacific decadal oscillation (PDO)] show a decadal-scale abrupt change in the 1970s. To analyze this phenomenon thoroughly, a new method of pedigree clustering combined with phase-space analysis (PCPSA) is used to establish two-dimensional phase-space coordinate systems of EASM-AO, EASM-PDO, and AO-PDO and the three-dimensional phase-space coordinate system of EASM-AO-PDO. By using the PCPSA method, it is found that all of the phase-space coordinate systems have a significant abrupt change in the mid-1970s, with a transition period, and the fit to the abrupt change of the phase-space coordinate system is better than 80%, which indicates excellent fit. By analyzing the correlation of EASM, AO, and PDO with sea level pressure (SLP) and sea surface temperature (SST), it is found that SLP has an obvious weakening trend in the high latitudes and an increasing trend in the tropics while SST has an increasing trend in most of the Southern Hemisphere waters and a minor weakening trend in the North Pacific Ocean waters between 30 degrees and 40 degrees N. Therefore, the abrupt climate change of the 1970s may well be a global abrupt change of the climatic system.
引用
收藏
页码:2551 / 2560
页数:10
相关论文
共 45 条
[21]  
2
[22]   Multidecadal Variability of North China Aridity and Its Relationship to PDO during 1900-2010 [J].
Qian, Cheng ;
Zhou, Tianjun .
JOURNAL OF CLIMATE, 2014, 27 (03) :1210-1222
[23]  
Shi N, 1996, INT J CLIMATOL, V16, P757, DOI 10.1002/(SICI)1097-0088(199607)16:7<757::AID-JOC50>3.0.CO
[24]  
2-5
[25]   Improvements to NOAA's historical merged land-ocean surface temperature analysis (1880-2006) [J].
Smith, Thomas M. ;
Reynolds, Richard W. ;
Peterson, Thomas C. ;
Lawrimore, Jay .
JOURNAL OF CLIMATE, 2008, 21 (10) :2283-2296
[26]   Relationship between Arctic Oscillation and Pacific Decadal Oscillation on decadal timescale [J].
Sun, JQ ;
Wang, HJ .
CHINESE SCIENCE BULLETIN, 2006, 51 (01) :75-79
[27]  
Tao S., 1987, MONSOON METEOROLOGY, P60
[28]   The Arctic Oscillation signature in the wintertime geopotential height and temperature fields [J].
Thompson, DWJ ;
Wallace, JM .
GEOPHYSICAL RESEARCH LETTERS, 1998, 25 (09) :1297-1300
[29]   Interdecadal changes in the major modes of Asian-Australian monsoon variability: Strengthening relationship with ENSO since the late 1970s [J].
Wang, Bin ;
Yang, Jing ;
Zhou, Tianjun .
JOURNAL OF CLIMATE, 2008, 21 (08) :1771-1789
[30]  
Wang HJ, 2001, ADV ATMOS SCI, V18, P376