Multi-centennial scale SST and Indian summer monsoon precipitation variability since the mid-Holocene and its nonlinear response to solar activity

The Holocene ◽  
2015 ◽  
Vol 25 (9) ◽  
pp. 1415-1424 ◽  
Author(s):  
Manish Tiwari ◽  
Siddhesh S Nagoji ◽  
Raja S Ganeshram
Keyword(s):  
Solar Activity ◽  
Summer Monsoon ◽  
Indian Summer Monsoon ◽  
Nonlinear Response ◽  
Precipitation Variability ◽  
Monsoon Precipitation

The leading mode of Indian Summer Monsoon precipitation variability during the last millennium

2011 ◽  
Vol 38 (15) ◽  
Author(s):  
Ashish Sinha ◽  
Max Berkelhammer ◽  
Lowell Stott ◽  
Manfred Mudelsee ◽  
Hai Cheng ◽  
...  
Keyword(s):  
Summer Monsoon ◽  
Indian Summer Monsoon ◽  
Precipitation Variability ◽  
Last Millennium ◽  
Monsoon Precipitation ◽  
Leading Mode

VARIABILITY IN THE INDIAN SUMMER MONSOON PRECIPITATION AND LAKE LEVELS IN EASTERN TIBET

2016 ◽  
Author(s):  
Melanie Perello ◽  
◽  
Broxton W. Bird ◽  
Yanbin Lei ◽  
Pratigya J. Polissar ◽  
...  
Keyword(s):  
Summer Monsoon ◽  
Indian Summer Monsoon ◽  
Monsoon Precipitation ◽  
Lake Levels ◽  
Eastern Tibet

scholarly journals Nonlinear Response of Asian Summer Monsoon Precipitation to Emission Reductions in India and China

2021 ◽  
Author(s):  
Ross Herbert ◽  
Laura J Wilcox ◽  
Manoj Joshi ◽  
Ellie Highwood ◽  
Dave Frame
Keyword(s):  
Summer Monsoon ◽  
Nonlinear Response ◽  
Asian Summer Monsoon ◽  
Monsoon Precipitation ◽  
Emission Reductions ◽  
Asian Summer ◽  
India And China

Strengthened Indian Summer Monsoon Precipitation Susceptibility Linked to Dust‐Induced Ice Cloud Modification

2019 ◽  
Vol 46 (14) ◽  
pp. 8431-8441 ◽  
Author(s):  
Piyushkumar N. Patel ◽  
Ritesh Gautam ◽  
Takuro Michibata ◽  
Harish Gadhavi
Keyword(s):  
Summer Monsoon ◽  
Indian Summer Monsoon ◽  
Monsoon Precipitation ◽  
Ice Cloud

scholarly journals Tree-ring-inferred glacier mass balance variation in southeastern Tibetan Plateau and its linkage with climate variability

2013 ◽  
Vol 9 (6) ◽  
pp. 2451-2458 ◽  
Author(s):  
J. Duan ◽  
L. Wang ◽  
L. Li ◽  
Y. Sun
Keyword(s):  
Tibetan Plateau ◽  
Climate Variability ◽  
Mass Balance ◽  
Tree Ring ◽  
Summer Monsoon ◽  
Indian Summer Monsoon ◽  
Dominant Factor ◽  
Glacier Mass Balance ◽  
Monsoon Precipitation

Abstract. A large number of glaciers in the Tibetan Plateau (TP) have experienced wastage in recent decades. And the wastage is different from region to region, even from glacier to glacier. A better understanding of long-term glacier variations and their linkage with climate variability requires extending the presently observed records. Here we present the first tree-ring-based glacier mass balance (MB) reconstruction in the TP, performed at the Hailuogou Glacier in southeastern TP during 1868–2007. The reconstructed MB is characterized mainly by ablation over the past 140 yr, and typical melting periods occurred in 1910s–1920s, 1930s–1960s, 1970s–1980s, and the last 20 yr. After the 1900s, only a few short periods (i.e., 1920s–1930s, the 1960s and the late 1980s) were characterized by accumulation. These variations can be validated by the terminus retreat velocity of Hailuogou Glacier and the ice-core accumulation rate in Guliya and respond well to regional and Northern Hemisphere temperature anomaly. In addition, the reconstructed MB is significantly and negatively correlated with August–September all-India monsoon rainfall (AIR) (r1871-2008 = −0.342, p < 0.0001). These results suggest that temperature variability is the dominant factor for the long-term MB variation at the Hailuogou Glacier. Indian summer monsoon precipitation does not affect the MB variation, yet the significant negative correlation between the MB and the AIR implies the positive effect of summer heating of the TP on Indian summer monsoon precipitation.

Abrupt Holocene Indian Summer Monsoon failures: A primary response to solar activity?

The Holocene ◽  
2015 ◽  
Vol 25 (4) ◽  
pp. 677-685 ◽  
Author(s):  
Hai Xu ◽  
Kevin M Yeager ◽  
Jianghu Lan ◽  
Bin Liu ◽  
Enguo Sheng ◽  
...  
Keyword(s):  
Solar Activity ◽  
Summer Monsoon ◽  
Indian Summer Monsoon ◽  
Primary Response
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