Rapid northward shift of the Indian Monsoon on the Tibetan Plateau at the end of the Little Ice Age

@article{Zhang2017,
  Title = {Rapid northward shift of the Indian Monsoon on the Tibetan Plateau at the end of the Little Ice Age},
  Author = {Zhang, Xiaolong and Xu, Baiqing and Günther, Franziska and Witt, Roman and Wang, Mo and Xie, Ying and Zhao, Huabiao and Li, Jiule and Gleixner, Gerd},
  Editor = {},
  Journal = {Journal of Geophysical Research Atmospheres},
  Year = {2017},
  Pages = {9262-9279},
  Volume = {122},
  Doi = {10.1002/2017JD026849},
  Abstract = {Variations in the Indian Monsoon (IM) and Westerlies (WS) significantly affect the climate on the Tibetan Plateau (TP) and have widespread ecological and socioeconomic impacts on the whole of Asian society. So far, however, the rate and magnitude of changes in the IM have still remained unclear. Here we report for the first time that the IM rapidly shifted northward at the end of the Little Ice Age (LIA). We used sediment proxies for humidity and moisture sources from the Taro Co Lake, which is located in the transition zone between the WS and IM. Our comprehensive survey of climate records for the TP and its peripheral mountain ranges revealed that the northern boundary of the IM (i.e., the southern boundary of the WS) lay along the southern slope of the Gandise Range (~29.5°N) in the late LIA. In contrast, it passed quickly over the Gandise Range by at least 1.5° in latitude at the end of the LIA. Our results suggest that this rapid climatic shift was potentially triggered by the counteracting effects of blocking by the TP and its marginal orography, which hindered the northward movement of the IM, and the pulling thermal gradient of the TP.

Key Points

• The Indian Monsoon rapidly shifted northward at the end of the Little Ice Age
• The Indian Monsoon passed over the Gandise Range by at least 1.5° in latitude
• The counteracting effects of orographic blocking and thermal pulling of the Tibetan Plateau potentially triggered this rapid shift},
}

TY  - JOUR
AU  - Zhang, Xiaolong
AU  - Xu, Baiqing
AU  - Günther, Franziska
AU  - Witt, Roman
AU  - Wang, Mo
AU  - Xie, Ying
AU  - Zhao, Huabiao
AU  - Li, Jiule
AU  - Gleixner, Gerd
TI  - Rapid northward shift of the Indian Monsoon on the Tibetan Plateau at the end of the Little Ice Age
T2  - Journal of Geophysical Research Atmospheres
PY  - 2017
SP  - 9262-9279
VL  - 122
DO  - 10.1002/2017JD026849
AB  - Variations in the Indian Monsoon (IM) and Westerlies (WS) significantly affect the climate on the Tibetan Plateau (TP) and have widespread ecological and socioeconomic impacts on the whole of Asian society. So far, however, the rate and magnitude of changes in the IM have still remained unclear. Here we report for the first time that the IM rapidly shifted northward at the end of the Little Ice Age (LIA). We used sediment proxies for humidity and moisture sources from the Taro Co Lake, which is located in the transition zone between the WS and IM. Our comprehensive survey of climate records for the TP and its peripheral mountain ranges revealed that the northern boundary of the IM (i.e., the southern boundary of the WS) lay along the southern slope of the Gandise Range (~29.5°N) in the late LIA. In contrast, it passed quickly over the Gandise Range by at least 1.5° in latitude at the end of the LIA. Our results suggest that this rapid climatic shift was potentially triggered by the counteracting effects of blocking by the TP and its marginal orography, which hindered the northward movement of the IM, and the pulling thermal gradient of the TP.

Key Points

• The Indian Monsoon rapidly shifted northward at the end of the Little Ice Age
• The Indian Monsoon passed over the Gandise Range by at least 1.5° in latitude
• The counteracting effects of orographic blocking and thermal pulling of the Tibetan Plateau potentially triggered this rapid shift
ER  -