Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1007/s00382-019-04718-z |
A PMIP3 narrative of modulation of ENSO teleconnections to the Indian summer monsoon by background changes in the Last Millennium | |
Tejavath, Charan Teja1; Ashok, Karumuri1; Chakraborty, Supriyo2; Ramesh, Rengaswamy3 | |
2019-09-01 | |
发表期刊 | CLIMATE DYNAMICS |
ISSN | 0930-7575 |
EISSN | 1432-0894 |
出版年 | 2019 |
卷号 | 53页码:3445-3461 |
文章类型 | Article |
语种 | 英语 |
国家 | India |
英文摘要 | Using nine model simulations from the PMIP3, we study simulated mean Indian summer (June-September) climate and its variability during the Last Millennium (LM; CE0850-1849) with emphasis on the Medieval Warm Period (MWP; CE1000-1199) and Little Ice Age (LIA; CE1550-1749), after validation of the simulated 'current day (CE1850-2005)' climate and trends. We find that the simulated above (below) mean-LM summer temperatures during the MWP (LIA) are associated with relatively higher (lower) moisture, and relatively higher (lower) number of concurrent El Ninos (La Ninas). Importantly, the models simulate higher (lower) Indian summer monsoon rainfall (ISMR) during the MWP (LIA) compared to the LM-mean, notwithstanding a strong simulated negative correlation between NINO3.4 index and the area-averaged ISMR. Interestingly, the percentage of the simulated strong El Ninos (La Ninas) associated with negative (positive) ISMR anomalies is higher (lower) in the LIA (MWP). This nonlinearity is explained by the simulated background climate changes, as follows. Distribution of simulated anomalous 850 hPa boreal summer velocity potential during MWP in models indicates, relative to the mean LM conditions, a zone of anomalous convergence in the central tropical Pacific flanked by two zones of divergence, i.e. a westward shift in the Walker circulation. The anomalous divergence centre in the west during the MWP also extends into the equatorial eastern Indian Ocean, triggering in an anomalous convergence zone over India and relatively higher moisture transport therein and therefore excess rainfall during the MWP as compared to the LM-mean, and hence an apparent weakening in the El Nino impact. |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000483626900057 |
WOS关键词 | TROPICAL PACIFIC ; GLOBAL PRECIPITATION ; SOUTHWEST MONSOON ; OXYGEN-ISOTOPE ; CLIMATE-CHANGE ; OCEAN DIPOLE ; EL-NINO ; HOLOCENE ; TEMPERATURE ; VARIABILITY |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/186385 |
专题 | 气候变化 |
作者单位 | 1.Univ Hyderabad, Ctr Earth Ocean & Atmospher Sci, Hyderabad, India; 2.Indian Inst Trop Meteorol, Pune, Maharashtra, India; 3.NISER, Sch Earth & Planetary Sci, Bhubaneswar, India |
推荐引用方式 GB/T 7714 | Tejavath, Charan Teja,Ashok, Karumuri,Chakraborty, Supriyo,et al. A PMIP3 narrative of modulation of ENSO teleconnections to the Indian summer monsoon by background changes in the Last Millennium[J]. CLIMATE DYNAMICS,2019,53:3445-3461. |
APA | Tejavath, Charan Teja,Ashok, Karumuri,Chakraborty, Supriyo,&Ramesh, Rengaswamy.(2019).A PMIP3 narrative of modulation of ENSO teleconnections to the Indian summer monsoon by background changes in the Last Millennium.CLIMATE DYNAMICS,53,3445-3461. |
MLA | Tejavath, Charan Teja,et al."A PMIP3 narrative of modulation of ENSO teleconnections to the Indian summer monsoon by background changes in the Last Millennium".CLIMATE DYNAMICS 53(2019):3445-3461. |
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