Interannual and long term variability of low level jetstream of the Asian summer monsoon

Interannual and long-term variability of the low level jetstream (LLJ) of the Asian summer monsoon during June to September was studied using reanalysis wind data. In order to study the variability, the domain of the LLJ covering the Indian and west Pacific Oceans was divided into six regions (boxes...
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Autor*in:	Shinu Sheela Wilson [verfasserIn] P. V. Joseph [verfasserIn] K. Mohanakumar [verfasserIn] Ola M. Johannessen [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2018

Schlagwörter:	low level jetstream Indian Summer Monsoon Rainfall (ISMR) El Nino Index Inter-annual variability

Übergeordnetes Werk:	In: Tellus: Series A, Dynamic Meteorology and Oceanography - Stockholm University Press, 2012, 70(2018), 1, Seite 9
Übergeordnetes Werk:	volume:70 ; year:2018 ; number:1 ; pages:9

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.1080/16000870.2018.1445380

Katalog-ID:	DOAJ024741671

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allfields	10.1080/16000870.2018.1445380 doi (DE-627)DOAJ024741671 (DE-599)DOAJ6dc4cfef288a499ab4abc23e06f54b08 DE-627 ger DE-627 rakwb eng GC1-1581 QC851-999 Shinu Sheela Wilson verfasserin aut Interannual and long term variability of low level jetstream of the Asian summer monsoon 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Interannual and long-term variability of the low level jetstream (LLJ) of the Asian summer monsoon during June to September was studied using reanalysis wind data. In order to study the variability, the domain of the LLJ covering the Indian and west Pacific Oceans was divided into six regions (boxes) based on their physical characteristics. The long term variability of LLJ and its relation with Indian monsoon rainfall and El Nino index were analysed. The low level circulation over Indian Ocean becomes weak during the positive phase of El Nino Southern Oscillation leads to warmer sea surface temperature over Indian Ocean. The strength of the low level jet over India depends on the convective heating of the atmosphere and not on the strength of the south Indian Ocean trade wind (ITz) which remains a passive component of the LLJ. The LLJ flow through peninsular India is weaker and the flow south of peninsular India is stronger during the recent decades in association with increasing number of break monsoon days. The cross equatorial flow over west Pacific Ocean has statistically significant increasing trend related to the increasing convection in the west Pacific Ocean. low level jetstream Indian Summer Monsoon Rainfall (ISMR) El Nino Index Inter-annual variability Oceanography Meteorology. Climatology P. V. Joseph verfasserin aut K. Mohanakumar verfasserin aut Ola M. Johannessen verfasserin aut In Tellus: Series A, Dynamic Meteorology and Oceanography Stockholm University Press, 2012 70(2018), 1, Seite 9 (DE-627)324455895 (DE-600)2026987-0 16000870 nnns volume:70 year:2018 number:1 pages:9 https://doi.org/10.1080/16000870.2018.1445380 kostenfrei https://doaj.org/article/6dc4cfef288a499ab4abc23e06f54b08 kostenfrei http://dx.doi.org/10.1080/16000870.2018.1445380 kostenfrei https://doaj.org/toc/1600-0870 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2025 GBV_ILN_2031 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2061 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2190 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 70 2018 1 9
spelling	10.1080/16000870.2018.1445380 doi (DE-627)DOAJ024741671 (DE-599)DOAJ6dc4cfef288a499ab4abc23e06f54b08 DE-627 ger DE-627 rakwb eng GC1-1581 QC851-999 Shinu Sheela Wilson verfasserin aut Interannual and long term variability of low level jetstream of the Asian summer monsoon 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Interannual and long-term variability of the low level jetstream (LLJ) of the Asian summer monsoon during June to September was studied using reanalysis wind data. In order to study the variability, the domain of the LLJ covering the Indian and west Pacific Oceans was divided into six regions (boxes) based on their physical characteristics. The long term variability of LLJ and its relation with Indian monsoon rainfall and El Nino index were analysed. The low level circulation over Indian Ocean becomes weak during the positive phase of El Nino Southern Oscillation leads to warmer sea surface temperature over Indian Ocean. The strength of the low level jet over India depends on the convective heating of the atmosphere and not on the strength of the south Indian Ocean trade wind (ITz) which remains a passive component of the LLJ. The LLJ flow through peninsular India is weaker and the flow south of peninsular India is stronger during the recent decades in association with increasing number of break monsoon days. The cross equatorial flow over west Pacific Ocean has statistically significant increasing trend related to the increasing convection in the west Pacific Ocean. low level jetstream Indian Summer Monsoon Rainfall (ISMR) El Nino Index Inter-annual variability Oceanography Meteorology. Climatology P. V. Joseph verfasserin aut K. Mohanakumar verfasserin aut Ola M. Johannessen verfasserin aut In Tellus: Series A, Dynamic Meteorology and Oceanography Stockholm University Press, 2012 70(2018), 1, Seite 9 (DE-627)324455895 (DE-600)2026987-0 16000870 nnns volume:70 year:2018 number:1 pages:9 https://doi.org/10.1080/16000870.2018.1445380 kostenfrei https://doaj.org/article/6dc4cfef288a499ab4abc23e06f54b08 kostenfrei http://dx.doi.org/10.1080/16000870.2018.1445380 kostenfrei https://doaj.org/toc/1600-0870 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2025 GBV_ILN_2031 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2061 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2190 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 70 2018 1 9
allfields_unstemmed	10.1080/16000870.2018.1445380 doi (DE-627)DOAJ024741671 (DE-599)DOAJ6dc4cfef288a499ab4abc23e06f54b08 DE-627 ger DE-627 rakwb eng GC1-1581 QC851-999 Shinu Sheela Wilson verfasserin aut Interannual and long term variability of low level jetstream of the Asian summer monsoon 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Interannual and long-term variability of the low level jetstream (LLJ) of the Asian summer monsoon during June to September was studied using reanalysis wind data. In order to study the variability, the domain of the LLJ covering the Indian and west Pacific Oceans was divided into six regions (boxes) based on their physical characteristics. The long term variability of LLJ and its relation with Indian monsoon rainfall and El Nino index were analysed. The low level circulation over Indian Ocean becomes weak during the positive phase of El Nino Southern Oscillation leads to warmer sea surface temperature over Indian Ocean. The strength of the low level jet over India depends on the convective heating of the atmosphere and not on the strength of the south Indian Ocean trade wind (ITz) which remains a passive component of the LLJ. The LLJ flow through peninsular India is weaker and the flow south of peninsular India is stronger during the recent decades in association with increasing number of break monsoon days. The cross equatorial flow over west Pacific Ocean has statistically significant increasing trend related to the increasing convection in the west Pacific Ocean. low level jetstream Indian Summer Monsoon Rainfall (ISMR) El Nino Index Inter-annual variability Oceanography Meteorology. Climatology P. V. Joseph verfasserin aut K. Mohanakumar verfasserin aut Ola M. Johannessen verfasserin aut In Tellus: Series A, Dynamic Meteorology and Oceanography Stockholm University Press, 2012 70(2018), 1, Seite 9 (DE-627)324455895 (DE-600)2026987-0 16000870 nnns volume:70 year:2018 number:1 pages:9 https://doi.org/10.1080/16000870.2018.1445380 kostenfrei https://doaj.org/article/6dc4cfef288a499ab4abc23e06f54b08 kostenfrei http://dx.doi.org/10.1080/16000870.2018.1445380 kostenfrei https://doaj.org/toc/1600-0870 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2025 GBV_ILN_2031 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2061 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2190 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 70 2018 1 9
allfieldsGer	10.1080/16000870.2018.1445380 doi (DE-627)DOAJ024741671 (DE-599)DOAJ6dc4cfef288a499ab4abc23e06f54b08 DE-627 ger DE-627 rakwb eng GC1-1581 QC851-999 Shinu Sheela Wilson verfasserin aut Interannual and long term variability of low level jetstream of the Asian summer monsoon 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Interannual and long-term variability of the low level jetstream (LLJ) of the Asian summer monsoon during June to September was studied using reanalysis wind data. In order to study the variability, the domain of the LLJ covering the Indian and west Pacific Oceans was divided into six regions (boxes) based on their physical characteristics. The long term variability of LLJ and its relation with Indian monsoon rainfall and El Nino index were analysed. The low level circulation over Indian Ocean becomes weak during the positive phase of El Nino Southern Oscillation leads to warmer sea surface temperature over Indian Ocean. The strength of the low level jet over India depends on the convective heating of the atmosphere and not on the strength of the south Indian Ocean trade wind (ITz) which remains a passive component of the LLJ. The LLJ flow through peninsular India is weaker and the flow south of peninsular India is stronger during the recent decades in association with increasing number of break monsoon days. The cross equatorial flow over west Pacific Ocean has statistically significant increasing trend related to the increasing convection in the west Pacific Ocean. low level jetstream Indian Summer Monsoon Rainfall (ISMR) El Nino Index Inter-annual variability Oceanography Meteorology. Climatology P. V. Joseph verfasserin aut K. Mohanakumar verfasserin aut Ola M. Johannessen verfasserin aut In Tellus: Series A, Dynamic Meteorology and Oceanography Stockholm University Press, 2012 70(2018), 1, Seite 9 (DE-627)324455895 (DE-600)2026987-0 16000870 nnns volume:70 year:2018 number:1 pages:9 https://doi.org/10.1080/16000870.2018.1445380 kostenfrei https://doaj.org/article/6dc4cfef288a499ab4abc23e06f54b08 kostenfrei http://dx.doi.org/10.1080/16000870.2018.1445380 kostenfrei https://doaj.org/toc/1600-0870 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2025 GBV_ILN_2031 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2061 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2190 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 70 2018 1 9
allfieldsSound	10.1080/16000870.2018.1445380 doi (DE-627)DOAJ024741671 (DE-599)DOAJ6dc4cfef288a499ab4abc23e06f54b08 DE-627 ger DE-627 rakwb eng GC1-1581 QC851-999 Shinu Sheela Wilson verfasserin aut Interannual and long term variability of low level jetstream of the Asian summer monsoon 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Interannual and long-term variability of the low level jetstream (LLJ) of the Asian summer monsoon during June to September was studied using reanalysis wind data. In order to study the variability, the domain of the LLJ covering the Indian and west Pacific Oceans was divided into six regions (boxes) based on their physical characteristics. The long term variability of LLJ and its relation with Indian monsoon rainfall and El Nino index were analysed. The low level circulation over Indian Ocean becomes weak during the positive phase of El Nino Southern Oscillation leads to warmer sea surface temperature over Indian Ocean. The strength of the low level jet over India depends on the convective heating of the atmosphere and not on the strength of the south Indian Ocean trade wind (ITz) which remains a passive component of the LLJ. The LLJ flow through peninsular India is weaker and the flow south of peninsular India is stronger during the recent decades in association with increasing number of break monsoon days. The cross equatorial flow over west Pacific Ocean has statistically significant increasing trend related to the increasing convection in the west Pacific Ocean. low level jetstream Indian Summer Monsoon Rainfall (ISMR) El Nino Index Inter-annual variability Oceanography Meteorology. Climatology P. V. Joseph verfasserin aut K. Mohanakumar verfasserin aut Ola M. Johannessen verfasserin aut In Tellus: Series A, Dynamic Meteorology and Oceanography Stockholm University Press, 2012 70(2018), 1, Seite 9 (DE-627)324455895 (DE-600)2026987-0 16000870 nnns volume:70 year:2018 number:1 pages:9 https://doi.org/10.1080/16000870.2018.1445380 kostenfrei https://doaj.org/article/6dc4cfef288a499ab4abc23e06f54b08 kostenfrei http://dx.doi.org/10.1080/16000870.2018.1445380 kostenfrei https://doaj.org/toc/1600-0870 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2025 GBV_ILN_2031 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2061 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2190 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 70 2018 1 9
language	English
source	In Tellus: Series A, Dynamic Meteorology and Oceanography 70(2018), 1, Seite 9 volume:70 year:2018 number:1 pages:9
sourceStr	In Tellus: Series A, Dynamic Meteorology and Oceanography 70(2018), 1, Seite 9 volume:70 year:2018 number:1 pages:9
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	low level jetstream Indian Summer Monsoon Rainfall (ISMR) El Nino Index Inter-annual variability Oceanography Meteorology. Climatology
isfreeaccess_bool	true
container_title	Tellus: Series A, Dynamic Meteorology and Oceanography
authorswithroles_txt_mv	Shinu Sheela Wilson @@aut@@ P. V. Joseph @@aut@@ K. Mohanakumar @@aut@@ Ola M. Johannessen @@aut@@
publishDateDaySort_date	2018-01-01T00:00:00Z
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language_de	englisch
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callnumber-first	G - Geography, Anthropology, Recreation
author	Shinu Sheela Wilson
spellingShingle	Shinu Sheela Wilson misc GC1-1581 misc QC851-999 misc low level jetstream misc Indian Summer Monsoon Rainfall (ISMR) misc El Nino Index misc Inter-annual variability misc Oceanography misc Meteorology. Climatology Interannual and long term variability of low level jetstream of the Asian summer monsoon
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topic_title	GC1-1581 QC851-999 Interannual and long term variability of low level jetstream of the Asian summer monsoon low level jetstream Indian Summer Monsoon Rainfall (ISMR) El Nino Index Inter-annual variability
topic	misc GC1-1581 misc QC851-999 misc low level jetstream misc Indian Summer Monsoon Rainfall (ISMR) misc El Nino Index misc Inter-annual variability misc Oceanography misc Meteorology. Climatology
topic_unstemmed	misc GC1-1581 misc QC851-999 misc low level jetstream misc Indian Summer Monsoon Rainfall (ISMR) misc El Nino Index misc Inter-annual variability misc Oceanography misc Meteorology. Climatology
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title	Interannual and long term variability of low level jetstream of the Asian summer monsoon
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title_full	Interannual and long term variability of low level jetstream of the Asian summer monsoon
author_sort	Shinu Sheela Wilson
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author_browse	Shinu Sheela Wilson P. V. Joseph K. Mohanakumar Ola M. Johannessen
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author-letter	Shinu Sheela Wilson
doi_str_mv	10.1080/16000870.2018.1445380
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title_sort	interannual and long term variability of low level jetstream of the asian summer monsoon
callnumber	GC1-1581
title_auth	Interannual and long term variability of low level jetstream of the Asian summer monsoon
abstract	Interannual and long-term variability of the low level jetstream (LLJ) of the Asian summer monsoon during June to September was studied using reanalysis wind data. In order to study the variability, the domain of the LLJ covering the Indian and west Pacific Oceans was divided into six regions (boxes) based on their physical characteristics. The long term variability of LLJ and its relation with Indian monsoon rainfall and El Nino index were analysed. The low level circulation over Indian Ocean becomes weak during the positive phase of El Nino Southern Oscillation leads to warmer sea surface temperature over Indian Ocean. The strength of the low level jet over India depends on the convective heating of the atmosphere and not on the strength of the south Indian Ocean trade wind (ITz) which remains a passive component of the LLJ. The LLJ flow through peninsular India is weaker and the flow south of peninsular India is stronger during the recent decades in association with increasing number of break monsoon days. The cross equatorial flow over west Pacific Ocean has statistically significant increasing trend related to the increasing convection in the west Pacific Ocean.
abstractGer	Interannual and long-term variability of the low level jetstream (LLJ) of the Asian summer monsoon during June to September was studied using reanalysis wind data. In order to study the variability, the domain of the LLJ covering the Indian and west Pacific Oceans was divided into six regions (boxes) based on their physical characteristics. The long term variability of LLJ and its relation with Indian monsoon rainfall and El Nino index were analysed. The low level circulation over Indian Ocean becomes weak during the positive phase of El Nino Southern Oscillation leads to warmer sea surface temperature over Indian Ocean. The strength of the low level jet over India depends on the convective heating of the atmosphere and not on the strength of the south Indian Ocean trade wind (ITz) which remains a passive component of the LLJ. The LLJ flow through peninsular India is weaker and the flow south of peninsular India is stronger during the recent decades in association with increasing number of break monsoon days. The cross equatorial flow over west Pacific Ocean has statistically significant increasing trend related to the increasing convection in the west Pacific Ocean.
abstract_unstemmed	Interannual and long-term variability of the low level jetstream (LLJ) of the Asian summer monsoon during June to September was studied using reanalysis wind data. In order to study the variability, the domain of the LLJ covering the Indian and west Pacific Oceans was divided into six regions (boxes) based on their physical characteristics. The long term variability of LLJ and its relation with Indian monsoon rainfall and El Nino index were analysed. The low level circulation over Indian Ocean becomes weak during the positive phase of El Nino Southern Oscillation leads to warmer sea surface temperature over Indian Ocean. The strength of the low level jet over India depends on the convective heating of the atmosphere and not on the strength of the south Indian Ocean trade wind (ITz) which remains a passive component of the LLJ. The LLJ flow through peninsular India is weaker and the flow south of peninsular India is stronger during the recent decades in association with increasing number of break monsoon days. The cross equatorial flow over west Pacific Ocean has statistically significant increasing trend related to the increasing convection in the west Pacific Ocean.
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title_short	Interannual and long term variability of low level jetstream of the Asian summer monsoon
url	https://doi.org/10.1080/16000870.2018.1445380 https://doaj.org/article/6dc4cfef288a499ab4abc23e06f54b08 http://dx.doi.org/10.1080/16000870.2018.1445380 https://doaj.org/toc/1600-0870
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Interannual and long term variability of low level jetstream of the Asian summer monsoon

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