The decadal variability of the tropical Indian Ocean SST-the South Asian High relation: CMIP5 model study
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| 024 | 7 | 0 | |a 10.1007/s00382-014-2285-3 |2 doi |
| 035 | |a (NATIONALLICENCE)springer-10.1007/s00382-014-2285-3 | ||
| 245 | 0 | 4 | |a The decadal variability of the tropical Indian Ocean SST-the South Asian High relation: CMIP5 model study |h [Elektronische Daten] |c [X. Qu, G. Huang] |
| 520 | 3 | |a Based on Coupled Model Intercomparison Project phase 5 (CMIP5) models, present study investigates the decadal variability of the tropical Indian Ocean (TIO) sea surface temperature (SST)-the South Asian High (SAH) relation (hereafter TSR) as well as its responses to the global warming. Out of the 17 CMIP5 models, only one (GFDL-CM3) reproduces reasonably the influence of the TIO SST on the SAH. In the historical simulations of GFDL-CM3, the TSR features fluctuations modulated by the western Pacific SST and the Indian subcontinent precipitation. When the TIO warming is accompanied by warm western Pacific, the western Pacific SST-induced tropospheric warming propagates westwards, warms the troposphere surrounding the Indian Ocean, enhances SAH and leads to higher TSR; when accompanied by not so warmed western Pacific, the TSR is lower. While, if the TIO warming is accompanied by negative rainfall anomalies over the Indian subcontinent, the rainfall-induced upper-troposphere cyclone over the subtropical Asia weakens the response of the SAH and leads to lower TSR; if not accompanied by negative rainfall anomalies, the TSR is higher. The decadal variability of the TSR is not subject to the global warming. In RCP45 and RCP85 scenarios, the TSR is also not directly affected by global warming. The rainfall over the Indian subcontinent is still a factor modulating the TSR. While, the western Pacific SST is invalid in the influences of the TIO SST on the SAH. | |
| 540 | |a Springer-Verlag Berlin Heidelberg, 2014 | ||
| 690 | 7 | |a The tropical Indian Ocean |2 nationallicence | |
| 690 | 7 | |a The South Asian High |2 nationallicence | |
| 690 | 7 | |a Tropospheric temperature |2 nationallicence | |
| 690 | 7 | |a Decadal variability |2 nationallicence | |
| 700 | 1 | |a Qu |D X. |u Center for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences, 100029, Beijing, China |4 aut | |
| 700 | 1 | |a Huang |D G. |u Key Laboratory of Regional Climate-Environment Research for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, P. O. Box 9804, 100029, Beijing, China |4 aut | |
| 773 | 0 | |t Climate Dynamics |d Springer Berlin Heidelberg |g 45/1-2(2015-07-01), 273-289 |x 0930-7575 |q 45:1-2<273 |1 2015 |2 45 |o 382 | |
| 856 | 4 | 0 | |u https://doi.org/10.1007/s00382-014-2285-3 |q text/html |z Onlinezugriff via DOI |
| 898 | |a BK010053 |b XK010053 |c XK010000 | ||
| 900 | 7 | |a Metadata rights reserved |b Springer special CC-BY-NC licence |2 nationallicence | |
| 908 | |D 1 |a research-article |2 jats | ||
| 949 | |B NATIONALLICENCE |F NATIONALLICENCE |b NL-springer | ||
| 950 | |B NATIONALLICENCE |P 856 |E 40 |u https://doi.org/10.1007/s00382-014-2285-3 |q text/html |z Onlinezugriff via DOI | ||
| 950 | |B NATIONALLICENCE |P 700 |E 1- |a Qu |D X. |u Center for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences, 100029, Beijing, China |4 aut | ||
| 950 | |B NATIONALLICENCE |P 700 |E 1- |a Huang |D G. |u Key Laboratory of Regional Climate-Environment Research for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, P. O. Box 9804, 100029, Beijing, China |4 aut | ||
| 950 | |B NATIONALLICENCE |P 773 |E 0- |t Climate Dynamics |d Springer Berlin Heidelberg |g 45/1-2(2015-07-01), 273-289 |x 0930-7575 |q 45:1-2<273 |1 2015 |2 45 |o 382 | ||