Distinct impacts of the Mongolian and Tibetan Plateaus on the evolution of the East Asian monsoon

The Mongolian Plateau (MP), which is relatively lower in altitude and smaller in extent than the Tibetan Plateau (TP), has received little attention about its climate effect. Building upon previous work in which we highlighted the role of the MP on the high‐level westerly jet stream, the response of surface‐level features of the Asian climate is examined in this study. The results show that the Indian and East Asian summer monsoonal and inland precipitation are mainly enhanced by the uplift of the TP. The precipitation during the onset of the summer monsoon is also intensified over India and eastern China. In addition, the East Asian monsoon domain is significantly expanded with the uplift of the TP, while the Indian summer monsoon domain does not change obviously. The MP plays a significant role in the strengthening of the East Asian winter monsoon, which is larger than the TP. With the uplift of the MP, the cold northerly wind in winter intensifies significantly in East Asia from higher latitudes to the South China Sea. The Siberian high is also enhanced and moves remarkably northward to its modern location. The strengthening of the Asian winter monsoon is related to the MP‐induced diversion of westerly wind. The bypassing flows around the plateau modify the temperature advections over middle latitudes and the atmosphere thermal structure in winter, which leads to the strengthening of the East Asian winter monsoon.

[1]  Liu Yimin,et al.  Global Monsoon Dynamics and Climate Change , 2015 .

[2]  Weijian Zhou,et al.  Variability of stalagmite-inferred Indian monsoon precipitation over the past 252,000 y , 2015, Proceedings of the National Academy of Sciences.

[3]  Xiao-dong Liu,et al.  Impact of Mongolian Plateau versus Tibetan Plateau on the westerly jet over North Pacific Ocean , 2015, Climate Dynamics.

[4]  C. Chamberlain,et al.  Aridification of Central Asia and uplift of the Altai and Hangay Mountains, Mongolia: Stable isotope evidence , 2014, American Journal of Science.

[5]  Chengshan Wang,et al.  Outward-growth of the Tibetan Plateau during the Cenozoic: A review ☆ , 2014 .

[6]  Weijian Zhou,et al.  Global Monsoon Dynamics and Climate Change-annurev-earth-pdf , 2014 .

[7]  B. Dong,et al.  Influence of the Tibetan Plateau uplift on the Asian monsoon-arid environment evolution , 2013 .

[8]  Gaojun Li,et al.  Evolving sources of eolian detritus on the Chinese Loess Plateau since early Miocene: Tectonic and climatic controls , 2013 .

[9]  Michele M. Rienecker,et al.  Decadal prediction skill in the GEOS-5 forecast system , 2013, Climate Dynamics.

[10]  M. Fortelius,et al.  Asynchronous responses of East Asian and Indian summer monsoons to mountain uplift shown by regional climate modelling experiments , 2013, Climate Dynamics.

[11]  F. Oldfield,et al.  Delayed build-up of Arctic ice sheets during 400,000-year minima in insolation variability , 2012, Nature.

[12]  Qing Bao,et al.  Thermal Controls on the Asian Summer Monsoon , 2012, Scientific Reports.

[13]  Peter J. Webster,et al.  Recent change of the global monsoon precipitation (1979–2008) , 2012, Climate Dynamics.

[14]  N. Mahowald,et al.  Simulated variations of eolian dust from inner Asian deserts at the mid-Pliocene, last glacial maximum, and present day: contributions from the regional tectonic uplift and global climate change , 2011 .

[15]  Weijian Zhou,et al.  New eolian red clay sequence on the western Chinese Loess Plateau linked to onset of Asian desertification about 25 Ma ago , 2011 .

[16]  Xiaodong Liu,et al.  Distinguishing the provenance of fine-grained eolian dust over the Chinese Loess Plateau from a modelling perspective , 2011 .

[17]  X. Fang,et al.  Miocene pollen record of KC-1 core in the Qaidam Basin, NE Tibetan Plateau and implications for evolution of the East Asian monsoon , 2011 .

[18]  Xijun Ni,et al.  Late Oligocene-Miocene mid-latitude aridification and wind patterns in the Asian interior , 2010 .

[19]  W. Boos,et al.  Orographic controls on climate and paleoclimate of Asia: thermal and mechanical roles for the Tibetan Plateau. , 2010 .

[20]  S. Clemens,et al.  Non-stationary response of Plio-Pleistocene East Asian winter monsoon variation to ice volume forcing , 2010 .

[21]  Huayu Lu,et al.  Aeolian sediment evidence that global cooling has driven late Cenozoic stepwise aridification in central Asia , 2010 .

[22]  Tomonori Sato.  Influences of subtropical jet and Tibetan Plateau on precipitation pattern in Asia: Insights from regional climate modeling , 2009 .

[23]  J. Metcalf,et al.  Multi-method chronometry of the Teletskoye graben and its basement, Siberian Altai Mountains: new insights on its thermo-tectonic evolution , 2009 .

[24]  Q. Hao,et al.  A major reorganization of Asian climate by the early Miocene , 2008 .

[25]  Wan,et al.  The Influence of Mechanical and Thermal Forcing by the Tibetan Plateau on Asian Climate , 2007 .

[26]  C. Sue,et al.  Uplift age and rates of the Gurvan Bogd system (Gobi-Altay) by apatite fission track analysis , 2007 .

[27]  N. Harris.  The elevation history of the Tibetan Plateau and its implications for the Asian monsoon , 2006 .

[28]  W. Liu,et al.  Role of Narrow Mountains in Large-Scale Organization of Asian Monsoon Convection* , 2006 .

[29]  David C. Smith,et al.  The Cenozoic palaeoenvironment of the Arctic Ocean , 2006, Nature.

[30]  C. Chamberlain,et al.  Earth science: The rise and growth of Tibet , 2006, Nature.

[31]  Bin Wang,et al.  Fundamental challenge in simulation and prediction of summer monsoon rainfall , 2005 .

[32]  Pinxian Wang,et al.  How old is the Asian monsoon system?—Palaeobotanical records from China , 2005 .

[33]  R. Wu,et al.  Roles of Indian and Pacific Ocean air–sea coupling in tropical atmospheric variability , 2005 .

[34]  Shuzhen Peng,et al.  Late Miocene–Pliocene development of Asian aridification as recorded in the Red-Earth Formation in northern China , 2004 .

[35]  A. Gupta,et al.  Late Oligocene–Miocene paleoceanographic evolution of the southeastern Indian Ocean: evidence from deep-sea benthic foraminifera (ODP Site 757) ☆ , 2004 .

[36]  A. Kitoh.  Effects of Mountain Uplift on East Asian Summer Climate Investigated by a Coupled Atmosphere–Ocean GCM , 2004 .

[37]  P. Peng,et al.  Changes in terrestrial ecosystem since 30 Ma in East Asia: Stable isotope evidence from black carbon in the South China Sea , 2003 .

[38]  T. Yasunari,et al.  An Evolution of the Asian Summer Monsoon Associated with Mountain Uplift—Simulation with the MRI Atmosphere-Ocean Coupled GCM— , 2003 .

[39]  Xiao-dong Liu,et al.  Sensitivity of East Asian monsoon climate to the uplift of the Tibetan Plateau , 2002 .

[40]  Bertrand Meyer,et al.  Oblique Stepwise Rise and Growth of the Tibet Plateau , 2001, Science.

[41]  J. Kutzbach,et al.  Evolution of Asian monsoons and phased uplift of the Himalaya–Tibetan plateau since Late Miocene times , 2001, Nature.

[42]  L. Sloan,et al.  Trends, Rhythms, and Aberrations in Global Climate 65 Ma to Present , 2001, Science.

[43]  An Yin,et al.  Geologic Evolution of the Himalayan-Tibetan Orogen , 2000 .

[44]  Z. Ding,et al.  Pedostratigraphy and paleomagnetism of a ̃7.0 Ma eolian loess-red clay sequence at Lingtai, Loess Plateau, north-central China and the implications for paleomonsoon evolution , 1999 .

[45]  D. Rea,et al.  Late Cenozoic eolian deposition in the North Pacific: Asian drying , 1998 .

[46]  Sandy P. Harrison,et al.  Climate and biome simulations for the past 21 , 1998 .

[47]  K. Hudnut,et al.  The Surface Rupture of the 1957 Gobi-Altay, Mongolia, Earthquake , 1997 .

[48]  D. Burbank,et al.  Reduced Himalayan sediment production 8 Myr ago despite an intensified monsoon , 1993, Nature.

[49]  L. Tungsheng,et al.  Stepwise coupling of monsoon circulations to global ice volume variations during the late Cenozoic , 1993 .

[50]  David Rind,et al.  Sensitivity of Asian and African climate to variations in seasonal insolation, glacial ice cover, sea surface temperature, and Asian orography , 1993 .

[51]  B. Windley,et al.  Mongolian plateau: Evidence for a late Cenozoic mantle plume under central Asia , 1993 .

[52]  J. Kutzbach,et al.  Sensitivity of Eurasian Climate to Surface Uplift of the Tibetan Plateau , 1993, The Journal of Geology.

[53]  S. Manabe,et al.  The Effects of Orography on Midlatitude Northern Hemisphere Dry Climates , 1992 .

[54]  V. Ittekkot,et al.  Foraminiferal production and monsoonal upwelling in the Arabian Sea: evidence from sediment traps , 1992, Geological Society, London, Special Publications.

[55]  J. Kutzbach,et al.  Sensitivity of climate to late Cenozoic uplift in southern Asia and the American west: Numerical experiments , 1989 .

[56]  Mike Shaltz.  Japan under pressure , 1989, Nature.

[57]  J. Quade,et al.  Development of Asian monsoon revealed by marked ecological shift during the latest Miocene in northern Pakistan , 1989, Nature.

[58]  Philip England,et al.  FINITE STRAIN CALCULATIONS OF CONTINENTAL DEFORMATION .2. COMPARISON WITH THE INDIA-ASIA COLLISION ZONE , 1986 .

[59]  G. Peltzer,et al.  On the mechanics of the collision between India and Asia , 1986, Geological Society, London, Special Publications.

[60]  J. Backman,et al.  Oxygen isotope calibration of the onset of ice-rafting and history of glaciation in the North Atlantic region , 1984, Nature.

[61]  Peter Molnar,et al.  Active faulting and cenozoic tectonics of the Tien Shan, Mongolia, and Baykal Regions , 1979 .

[62]  P. Molnar,et al.  Cenozoic Tectonics of Asia: Effects of a Continental Collision: Features of recent continental tectonics in Asia can be interpreted as results of the India-Eurasia collision. , 1975, Science.

[63]  S. Manabe,et al.  The Role of Mountains in the South Asian Monsoon Circulation , 1975 .

[64]  S. Manabe,et al.  The Effects of Mountains on the General Circulation of the Atmosphere as Identified by Numerical Experiments , 1974 .

[65]  H. Flohn,et al.  Large-scale aspects of the "summer monsoon" in South and East Asia , 1957 .

[66]  B. Bolin.  On the Influence of the Earth's Orography on the General Character of the Westerlies , 1950 .