scholarly journals Chinese cave δ18O records do not represent northern East Asian summer monsoon rainfall

2017 ◽  
Vol 114 (15) ◽  
pp. E2987-E2988 ◽  
Author(s):  
Jianbao Liu ◽  
Shengqian Chen ◽  
Jianhui Chen ◽  
Zhiping Zhang ◽  
Fahu Chen
2015 ◽  
Vol 28 (7) ◽  
pp. 2623-2634 ◽  
Author(s):  
Wei Wei ◽  
Renhe Zhang ◽  
Min Wen ◽  
Baek-Jo Kim ◽  
Jae-Cheol Nam

Abstract A diagnostic analysis reveals that on the interannual time scale the southeast–northwest movement is a dominant feature of the South Asian high (SAH), and it is closely related to the Indian and East Asian summer monsoon rainfall. The southeastward (northwestward) shift of the SAH is closely related to less (more) Indian summer monsoon rainfall and more (less) rainfall in the Yangtze River valley (YRV) over the East Asian summer monsoon region. An anomalous AGCM is utilized to examine the effect of latent heat anomalies associated with the Asian summer monsoon rainfall on the SAH. The negative latent heat anomalies over the northern Indian Subcontinent associated with a weak Indian summer monsoon stimulates an anomalous cyclone to its northwest and an anticyclone to its northeast over the eastern Tibetan Plateau and eastern China in the upper troposphere, which is responsible for the east–west shift of the SAH and more rainfall in the YRV. The positive latent heat release associated with rainfall anomalies in the YRV excites a southward-located anticyclone over eastern China, exerting a feedback effect on the SAH and leading to a southeast–northwest shift of the SAH.


2017 ◽  
Vol 114 (15) ◽  
pp. E2989-E2990 ◽  
Author(s):  
Yonaton Goldsmith ◽  
Wallace S. Broecker ◽  
Hai Xu ◽  
Pratigya J. Polissar ◽  
Peter deMenocal ◽  
...  

2018 ◽  
Vol 52 (11) ◽  
pp. 6989-7011 ◽  
Author(s):  
S. N. Raj Deepak ◽  
Jasti S. Chowdary ◽  
A. Ramu Dandi ◽  
G. Srinivas ◽  
Anant Parekh ◽  
...  

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