Possible Causes of the Interdecadal Transition of the Somali Jet Around the Late 1990s
This observational study demonstrates that the Somali jet（SMJ） experienced a notable interdecadal transition in not only its lower-level parts（〈 850 hP a） but also its higher-level parts（850-600 h Pa） in the late 1990 s. The results also show that the jet at higher level is more significantly relate...
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| Published in | Acta meteorologica Sinica Vol. 29; no. 2; pp. 214 - 227 |
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| Main Author | |
| Format | Journal Article |
| Language | English |
| Published |
Beijing
The Chinese Meteorological Society
01.04.2015
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| Subjects | |
| Online Access | Get full text |
| ISSN | 2095-6037 0894-0525 2198-0934 2191-4788 |
| DOI | 10.1007/s13351-015-4103-1 |
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| Abstract | This observational study demonstrates that the Somali jet（SMJ） experienced a notable interdecadal transition in not only its lower-level parts（〈 850 hP a） but also its higher-level parts（850-600 h Pa） in the late 1990 s. The results also show that the jet at higher level is more significantly related to East Asian monsoon rainfall than that at lower level. Thus, a new whole-layer SMJ（WSMJ） index which includes variations of the higher-level jet is defined based on the average meridional wind speed at five levels（1000-600 h Pa）. The interdecadal transition of the SMJ can be mainly attributed to the meridional thermal contrast anomalies near the equator which are associated with the three-pole pattern of the southern Indian Ocean. |
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| AbstractList | This observational study demonstrates that the Somali jet (SMJ) experienced a notable interdecadal transition in not only its lower-level parts (< 850 hPa) but also its higher-level parts (850-600 hPa) in the late 1990s. The results also show that the jet at higher level is more significantly related to East Asian monsoon rainfall than that at lower level. Thus, a new whole-layer SMJ (WSMJ) index which includes variations of the higher-level jet is defined based on the average meridional wind speed at five levels (1000-600 hPa). The interdecadal transition of the SMJ can be mainly attributed to the meridional thermal contrast anomalies near the equator which are associated with the three-pole pattern of the southern Indian Ocean. This observational study demonstrates that the Somali jet (SMJ) experienced a notable interdecadal transition in not only its lower-level parts (< 850 hPa) but also its higher-level parts (850–600 hPa) in the late 1990s. The results also show that the jet at higher level is more signifi cantly related to East Asian monsoon rainfall than that at lower level. Thus, a new whole-layer SMJ (WSMJ) index which includes variations of the higher-level jet is defi ned based on the average meridional wind speed at fi ve levels (1000–600 hPa). The interdecadal transition of the SMJ can be mainly attributed to the meridional thermal contrast anomalies near the equator which are associated with the three-pole pattern of the southern Indian Ocean. This observational study demonstrates that the Somali jet（SMJ） experienced a notable interdecadal transition in not only its lower-level parts（〈 850 hP a） but also its higher-level parts（850-600 h Pa） in the late 1990 s. The results also show that the jet at higher level is more significantly related to East Asian monsoon rainfall than that at lower level. Thus, a new whole-layer SMJ（WSMJ） index which includes variations of the higher-level jet is defined based on the average meridional wind speed at five levels（1000-600 h Pa）. The interdecadal transition of the SMJ can be mainly attributed to the meridional thermal contrast anomalies near the equator which are associated with the three-pole pattern of the southern Indian Ocean. |
| Author | 肖子牛 石文静 杨萍 |
| AuthorAffiliation | Department of Atmospheric Science, Nanjing University of Information Science ＆ Technology, Nanjing 210044, China State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China China Meteorological Administration Training Center, Beijing 100081, China Cooperative Institute for Meteorological Satellite Studies, University of Wisconsin-Madison, Madison, WI 53706, USA |
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| Cites_doi | 10.1175/1520-0469(1979)036<2153:OTDOTE>2.0.CO;2 10.1175/1520-0493(1981)109<0182:ACSOAF>2.0.CO;2 10.1175/1520-0493(1999)127<1157:TMEAVO>2.0.CO;2 10.1002/qj.49709540412 10.1002/qj.388 10.1007/978-3-642-79268-7_10 10.1175/1525-7541(2002)003<0249:GLPAYM>2.0.CO;2 10.1175/1520-0469(1976)033<2350:NSOTSJ>2.0.CO;2 10.1007/s00376-011-1120-6 10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2 10.1007/BF00874408 10.1175/2010JCLI3648.1 10.1175/1520-0442(2001)014<0434:SJITAS>2.0.CO;2 10.1175/1520-0493(1970)098<0423:OTAVOT>2.3.CO;2 10.1175/1520-0469(1979)036<2139:OTDOTE>2.0.CO;2 10.1175/1520-0442(2004)017<3866:OTIORP>2.0.CO;2 10.1175/1520-0469(1982)039<2267:OTDOTE>2.0.CO;2 10.1002/qj.49709540409 10.1175/JCLI-D-11-00394.1 10.1175/JCLI-D-12-00524.1 10.1175/1520-0469(1995)052<1341:AMOTAS>2.0.CO;2 10.1007/BF00874409 10.1007/s00376-009-9045-z 10.1002/joc.1720 10.1007/s00376-011-1076-6 10.1175/1520-0442(2004)017<2466:IEROS>2.0.CO;2 10.3402/tellusa.v64i0.18590 10.1175/1520-0469(1979)036<1895:APBLMF>2.0.CO;2 10.1029/2008GL037079 |
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| Copyright | The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2015 Copyright © Wanfang Data Co. Ltd. All Rights Reserved. |
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| DocumentTitleAlternate | Possible Causes of the Interdecadal Transition of the Somali Jet Around the Late 1990s |
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| GeographicLocations | ISW, Arabian Sea, Somali Jet ISW, Indian Ocean |
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| Keywords | Asian summer monsoon index southern Indian Ocean Somali jet interdecadal transition sea surface temperature |
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| Notes | 11-2277/P This observational study demonstrates that the Somali jet（SMJ） experienced a notable interdecadal transition in not only its lower-level parts（〈 850 hP a） but also its higher-level parts（850-600 h Pa） in the late 1990 s. The results also show that the jet at higher level is more significantly related to East Asian monsoon rainfall than that at lower level. Thus, a new whole-layer SMJ（WSMJ） index which includes variations of the higher-level jet is defined based on the average meridional wind speed at five levels（1000-600 h Pa）. The interdecadal transition of the SMJ can be mainly attributed to the meridional thermal contrast anomalies near the equator which are associated with the three-pole pattern of the southern Indian Ocean. interdecadal transition,Somali jet,index,Asian summer monsoon,southern Indian Ocean,sea surface temperature XIAO Ziniu, SHI Wenjing and YANG Ping（ I Department of Atmospheric Science, Nanjing University of Information Science ＆ Technology, Nanjing 210044, China 2 State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China 3 China Meteorological Administration Training Center, Beijing 100081, China 4 Cooperative Institute for Meteorological Satellite Studies, University of Wisconsin-Madison, Madison, WI 53706, USA） ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
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| Snippet | This observational study demonstrates that the Somali jet（SMJ） experienced a notable interdecadal transition in not only its lower-level parts（〈 850 hP a） but... This observational study demonstrates that the Somali jet (SMJ) experienced a notable interdecadal transition in not only its lower-level parts (< 850 hPa) but... |
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| SubjectTerms | Atmospheric Protection/Air Quality Control/Air Pollution Atmospheric Sciences Earth and Environmental Science Earth Sciences Geophysics and Environmental Physics Marine Meteorology 东亚季风 南印度洋 原因 年代际 水平射流 索马里急流 风速 |
| Title | Possible Causes of the Interdecadal Transition of the Somali Jet Around the Late 1990s |
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