Why does the temperature rise faster in the arid region of northwest China

[1] During 1960–2010, the air temperature in the arid region of northwest China had a significant rising trend (P < 0.001), at a rate of 0.343°C/decade, higher than the average of China (0.25°C/decade) and that of the entire globe (0.13°C/decade) for the same period. Based on the analysis of the data from 74 meteorological stations in the region for 1960–2010, we found that among the four seasons the temperature change of winter has been playing the most important role in the yearly change in this region. We also found that the winter temperature in this region has a strong association with the Siberian High (correlation coefficient: R = −0.715) and the greenhouse gas emission (R = 0.51), and between the two the former is stronger. We thus suggest that the weakening of the Siberian High during the 1980s to 1990s on top of the steady increasing of the greenhouse emission is the main reason for the higher rate of the temperature rise in the arid region of the northwest China.

[1]  Ke Fan,et al.  Antarctic oscillation and the dust weather frequency in North China , 2004 .

[2]  James W. Hurrell,et al.  North Atlantic climate variability: The role of the North Atlantic Oscillation , 2009 .

[3]  Fubao Sun,et al.  Partitioning the variance between space and time , 2010 .

[4]  F. Joos,et al.  Global warming and marine carbon cycle feedbacks on future atmospheric CO2 , 1999, Science.

[5]  Ren Guo,et al.  Changes of Surface Air Temperature in China During 1951—2004 , 2005 .

[6]  D. Gong,et al.  Definition of Antarctic Oscillation index , 1999 .

[7]  H. B. Mann.  Nonparametric Tests Against Trend , 1945 .

[8]  A. Barnston,et al.  Classification, seasonality and persistence of low-frequency atmospheric circulation patterns , 1987 .

[9]  O. Edenhofer,et al.  Intergovernmental Panel on Climate Change (IPCC) , 2013 .

[10]  Corinne Le Quéré,et al.  Climate Change 2013: The Physical Science Basis , 2013 .

[11]  Zhao Hongyan.  New Development of Climate Change in Northwest China and Its Impact on Arid Environment , 2010 .

[12]  A reconstructed Siberian High index since A.D. 1599 from Eurasian and North American tree rings , 2005 .

[13]  Chang‐Hoi Ho,et al.  Possible influence of the Antarctic Oscillation on tropical cyclone activity in the western North Pacific , 2005 .

[14]  Richard L. Smith,et al.  Quantifying Uncertainty in Projections of Regional Climate Change: A Bayesian Approach to the Analysis of Multimodel Ensembles , 2005 .

[15]  D. Stephenson,et al.  Observed Trends and Teleconnections of the Siberian High: A Recently Declining Center of Action , 2005 .

[16]  Chang‐Hoi Ho,et al.  The Siberian High and climate change over middle to high latitude Asia , 2002 .

[17]  IMPACT OF CLIMATE-CHANGE ON SURFACE-WATER RESOURCE AND TENDENCY, IN THE FUTURE IN THE ARID ZONE OF NORTHWESTERN CHINA (SCI) , 1995 .

[18]  S. Yue,et al.  Power of the Mann–Kendall and Spearman's rho tests for detecting monotonic trends in hydrological series , 2002 .

[19]  H. Tian,et al.  Net exchanges of CO2, CH4, and N2O between China's terrestrial ecosystems and the atmosphere and their contributions to global climate warming , 2011 .

[20]  M. Kendall,et al.  Rank Correlation Methods , 1949 .

[21]  W. G. Strand,et al.  How Much More Global Warming and Sea Level Rise? , 2005, Science.

[22]  S. Yue,et al.  Corrigendum to ``Power of the Mann-Kendall and Spearman's rho tests for detecting monotonic trends in hydrological series'' [J. Hydrol. 259 (2002) 254 271] , 2002 .

[23]  J. Wallace,et al.  Annular Modes in the Extratropical Circulation. Part I: Month-to-Month Variability* , 2000 .

[24]  B. Santer,et al.  Selecting global climate models for regional climate change studies , 2009, Proceedings of the National Academy of Sciences.

[25]  Deliang Chen,et al.  Recent Recovery of the Siberian High Intensity , 2011 .

[26]  Vincent R. Gray.  Climate Change 2007: The Physical Science Basis Summary for Policymakers , 2007 .

[27]  Roger A. Pielke,et al.  Analysis of the impacts of station exposure on the U.S. Historical Climatology Network temperatures and temperature trends , 2011 .

[28]  Jianfeng Li,et al.  Observed changes of temperature extremes during 1960–2005 in China: natural or human-induced variations? , 2011 .

[29]  Chang‐Hoi Ho,et al.  Influences of Arctic Oscillation and Madden-Julian Oscillation on cold surges and heavy snowfalls over Korea: A case study for the winter of 2009–2010 , 2010 .

[30]  K. Shine.  Radiative Forcing of Climate Change , 2000 .

[31]  A. Taylor,et al.  Multi-century variability in the Pacific North American circulation pattern reconstructed from tree rings , 2010 .

[32]  R. Knutti,et al.  Regional climate change patterns identified by cluster analysis , 2010 .

[33]  O. Edenhofer,et al.  Mitigation from a cross-sectoral perspective , 2007 .

[34]  D. Yihui.  Build-up, air mass transformation and propagation of Siberian high and its relations to cold surge in East Asia , 1990 .

[35]  A. Lynch,et al.  Estimating the Uncertainty in a Regional Climate Model Related to Initial and Lateral Boundary Conditions , 2005 .

[36]  R. Allan,et al.  A new globally complete monthly historical gridded mean sea level pressure dataset (HadSLP2): 1850-2004 , 2006 .

[37]  P. Jones,et al.  Uncertainty estimates in regional and global observed temperature changes: A new data set from 1850 , 2006 .

[38]  Crowley,et al.  Atmospheric science: Methane rises from wetlands , 2011, Nature.

[39]  Chen Yaning,et al.  Plausible impact of global climate change on water resources in the Tarim River Basin , 2005 .

[40]  F. Giorgi,et al.  Regional climate model simulation of projected 21st century climate change over an all‐Africa domain: Comparison analysis of nested and driving model results , 2011 .

[41]  M. Kendall.  Rank Correlation Methods , 1949 .