Forced response of the East Asian summer rainfall over the past millennium: results from a coupled model simulation

2009 ◽  
Vol 36 (1-2) ◽  
pp. 323-336 ◽  
Author(s):  
Jian Liu ◽  
Bin Wang ◽  
Hongli Wang ◽  
Xueyuan Kuang ◽  
Ruyuan Ti
Keyword(s):  
Model Simulation ◽  
East Asian ◽  
Coupled Model ◽  
Summer Rainfall ◽  
Forced Response ◽  
The Past ◽  
East Asian Summer Rainfall ◽  
Asian Summer ◽  
Past Millennium

scholarly journals How much of the interannual variability of East Asian summer rainfall is forced by SST?

2015 ◽  
Vol 47 (1-2) ◽  
pp. 555-565 ◽  
Author(s):  
Chao He ◽  
Bo Wu ◽  
Chunhui Li ◽  
Ailan Lin ◽  
Dejun Gu ◽  
...  
Keyword(s):  
Interannual Variability ◽  
East Asian ◽  
Summer Rainfall ◽  
East Asian Summer Rainfall ◽  
Asian Summer

Decadal- to Centennial-Scale East Asian Summer Monsoon Variability Over the Past Millennium: An Oceanic Perspective

2018 ◽  
Vol 45 (15) ◽  
pp. 7711-7718 ◽  
Author(s):  
Richard Ching Wa Cheung ◽  
Moriaki Yasuhara ◽  
Briony Mamo ◽  
Kota Katsuki ◽  
Koji Seto ◽  
...  
Keyword(s):  
Summer Monsoon ◽  
East Asian Summer Monsoon ◽  
Asian Summer Monsoon ◽  
East Asian ◽  
The Past ◽  
Monsoon Variability ◽  
Asian Summer ◽  
Past Millennium

Understanding Changes in the Asian Summer Monsoon over the Past Millennium: Insights from a Long-Term Coupled Model Simulation*

2009 ◽  
Vol 22 (7) ◽  
pp. 1736-1748 ◽  
Author(s):  
Fangxing Fan ◽  
Michael E. Mann ◽  
Caspar M. Ammann
Keyword(s):  
Summer Monsoon ◽  
Radiative Forcing ◽  
Asian Summer Monsoon ◽  
Coupled Model ◽  
Climate System Model ◽  
The Past ◽  
Asian Summer ◽  
Simulation Results ◽  
Past Millennium

Abstract The Asian summer monsoon (ASM) and its variability were investigated over the past millennium through the analysis of a long-term simulation of the NCAR Climate System Model, version 1.4 (CSM 1.4) coupled model driven with estimated natural and anthropogenic radiative forcing during the period 850–1999. Analysis of the simulation results indicates that certain previously proposed mechanisms, such as warmer large-scale temperatures favoring a stronger monsoon through their effect on Eurasian snow cover, appear inconsistent with the mechanisms active in the simulation. Forced changes in tropical Pacific sea surface temperatures play an apparent role in the long-term changes in the ASM. Analyses of the simulation results suggest that the direct radiative effect of solar forcing variations on the ASM is quite weak and that dynamical responses may be far more important. Volcanic radiative forcing leads to a clearly detectable short-term reduction in the strength of the ASM. Comparisons with long-term proxy reconstructions of the ASM are attempted but are limited by the divergent behavior among different reconstructions as well as the limitations in the model’s coupled dynamics.

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