Boreal Summer Extratropical Intraseasonal Waves over the Eurasian Continent and Real-Time Metrics

被引:22
作者
Zhu, Tao [1 ]
Yang, Jing [1 ,2 ]
Wang, Bin [3 ,4 ]
Bao, Qing [5 ]
机构
[1] Beijing Normal Univ, Fac Geog Sci, State Key Lab Earth Surface Proc & Resource Ecol, Key Lab Environm Change & Nat Disaster, Beijing, Peoples R China
[2] Beijing Normal Univ, Fac Geog Sci, Beijing, Peoples R China
[3] Univ Hawaii Manoa, Dept Atmospher Sci, Honolulu, HI USA
[4] Univ Hawaii Manoa, Int Pacific Res Ctr, Honolulu, HI USA
[5] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geoph, Beijing, Peoples R China
基金
中国国家自然科学基金;
关键词
MADDEN-JULIAN OSCILLATION; NORTH-ATLANTIC OSCILLATION; POLAR FRONT JET; PART I; GEOPOTENTIAL HEIGHT; TELECONNECTION PATTERN; ATMOSPHERIC BLOCKING; WESTERN PACIFIC; ROSSBY WAVES; VARIABILITY;
D O I
10.1175/JCLI-D-22-0788.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Boreal summer extratropical intraseasonal oscillation (EISO) is crucial in modulating regional subseasonal variation and particularly causing extreme meteorological events, but it has yet to be well clarified and operationally moni-tored. This study first objectively sorts out three dominant EISOs trapped along two extratropical westerly jet streams over Eurasia, and then proposes the corresponding real-time metrics. The three dominant EISOs are (i) an 8-25-day eastward-propagating wave along the subtropical westerly jet (EISO-SJE) initiating at the exit of the North America-North Atlantic jet and strengthening over the Black Sea-Caspian Sea-arid central Asia region; (ii) a 10-30-day eastward-traveling wave along the polar front jet (EISO-PJE), starting near Scandinavia and enhancing from the East European Plain to the West Siberian Plain and then decaying over the Okhotsk region; (iii) a 10-40-day westward-migrating wave along the polar front jet (EISO-PJW), which enhances near the Ural Mountains and weakens over Scandinavia. The real-time metrics then, following the three EISOs, have been constructed, and they are able to capture the spatiotemporal features of three EISOs in application. Moreover, the close linkages between these EISOs and the regional extremes/the blocking occurrence have been clearly demonstrated, confirming the importance of real-time EISO metrics. Together with tropical intraseasonal oscillation, this study provides the subseasonal-to-seasonal (S2S) community with a well-portrayed unified picture of extra-tropical intraseasonal waves and the real-time metrics for monitoring boreal summer intraseasonal signals over Eurasia and facilitate subseasonal predictions.
引用
收藏
页码:3971 / 3991
页数:21
相关论文
共 162 条
[1]   Active/break cycles: diagnosis of the intraseasonal variability of the Asian Summer Monsoon [J].
Annamalai, H ;
Slingo, JM .
CLIMATE DYNAMICS, 2001, 18 (1-2) :85-102
[2]  
[Anonymous], J CLIMATE, V33, P2183, DOI [10.1175/JCLI-D-19-0458.1, DOI 10.1175/JCLI-D-19-0458.1]
[3]  
[Anonymous], J GEOPHYS RES-ATMOS, V124, P3110, DOI [10.1029/2018JD029868, DOI 10.1029/2018JD029868]
[4]   Tropospheric and Stratospheric Causal Pathways Between the MJO and NAO [J].
Barnes, Elizabeth A. ;
Samarasinghe, Savini M. ;
Ebert-Uphoff, Imme ;
Furtado, Jason C. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2019, 124 (16) :9356-9371
[5]   The Hot Summer of 2010: Redrawing the Temperature Record Map of Europe [J].
Barriopedro, David ;
Fischer, Erich M. ;
Luterbacher, Juerg ;
Trigo, RicardoM. ;
Garcia-Herrera, Ricardo .
SCIENCE, 2011, 332 (6026) :220-224
[6]   The 2003 heat wave as an example of summers in a greenhouse climate? Observations and climate model simulations for Basel, Switzerland [J].
Beniston, M ;
Diaz, HF .
GLOBAL AND PLANETARY CHANGE, 2004, 44 (1-4) :73-81
[7]  
Branstator G, 2002, J CLIMATE, V15, P1893, DOI 10.1175/1520-0442(2002)015<1893:CTTJSW>2.0.CO
[8]  
2
[9]  
BRANSTATOR G, 1987, J ATMOS SCI, V44, P2310, DOI 10.1175/1520-0469(1987)044<2310:ASEOTA>2.0.CO
[10]  
2