Changes in daily climate extremes in the eastern and central Tibetan Plateau during 1961–2005

[1] Changes in indices of climate extremes are analyzed on the basis of daily maximum and minimum surface air temperature and precipitation at 71 meteorological stations with elevation above 2000 m above sea level in the eastern and central Tibetan Plateau (TP) during 1961–2005. Twelve indices of extreme temperature and nine indices of extreme precipitation are examined. Temperature extremes show patterns consistent with warming during the studied period, with a large proportion of stations showing statistically significant trends for all temperature indices. Stations in the northwestern, southwestern, and southeastern TP have larger trend magnitudes. The regional occurrence of extreme cold days and nights has decreased by −0.85 and −2.38 d/decade, respectively. Over the same period, the occurrence of extreme warm days and nights has increased by 1.26 and 2.54 d/decade, respectively. The number of frost days and ice days shows statistically significant decreasing at the rate of −4.32 and −2.46 d/decade, respectively. The length of growing season has statistically increased by 4.25 d/decade. The diurnal temperature range exhibits a statistically decreasing trend at a rate of −0.20°C per decade. The extreme temperature indices also show statistically significant increasing trends, with larger values for the index describing variations in the lowest minimum temperature. In general, warming trends in minimum temperature indices are of greater magnitude than those for maximum temperature. Most precipitation indices exhibit increasing trends in the southern and northern TP and show decreasing trends in the central TP. On average, regional annual total precipitation, heavy precipitation days, maximum 1-day precipitation, average wet days precipitation, and total precipitation on extreme wet days show nonsignificant increases. Decreasing trends are found for maximum 5-day precipitation, consecutive wet days, and consecutive dry days, but only the last is statistically significant.

[1]  W. Hoeffding,et al.  Rank Correlation Methods , 1949 .

[2]  Chengfeng Li,et al.  Seasonal Heating of the Tibetan Plateau and Its Effects on the Evolution of the Asian Summer Monsoon , 1992 .

[3]  Thomas C. Peterson,et al.  Changes in precipitation and temperature extremes in Central America and northern South America, 1961–2003 , 2005 .

[4]  Yuqing Wang,et al.  Observed trends in extreme precipitation events in China during 1961–2001 and the associated changes in large‐scale circulation , 2005 .

[5]  Ming Xu,et al.  Observed trends of precipitation amount, frequency, and intensity in China, 1960–2000 , 2005 .

[6]  T. Niu,et al.  The characteristics of climate change over the Tibetan Plateau in the last 40 years and the detection of climatic jumps , 2004 .

[7]  Xuebin Zhang,et al.  Temperature and precipitation trends in Canada during the 20th century , 2000, Data, Models and Analysis.

[8]  Guoxiong Wu,et al.  New proofs of the recent climate warming over the Tibetan Plateau as a result of the increasing greenhouse gases emissions , 2006 .

[9]  Yuqing Wang,et al.  Correction to “Observed trends in extreme precipitation events in China during 1961–2001 and the associated changes in large‐scale circulation” , 2005 .

[10]  Carlos A. Coelho,et al.  Evidence of trends in daily climate extremes over southern and west Africa , 2006 .

[11]  Francis W. Zwiers,et al.  Avoiding Inhomogeneity in Percentile-Based Indices of Temperature Extremes , 2005 .

[12]  H. L. Miller,et al.  Climate Change 2007: The Physical Science Basis , 2007 .

[13]  Xiao-dong Liu,et al.  Climatic warming in the Tibetan Plateau during recent decades , 2000 .

[14]  Roger A. Pielke,et al.  Temporal Fluctuations in Weather and Climate Extremes That Cause Economic and Human Health Impacts: A Review , 1999 .

[15]  Zhi-Yong Yin,et al.  Temporal trends and variability of daily maximum and minimum, extreme temperature events, and growing season length over the eastern and central Tibetan Plateau during 1961-2003 , 2006 .

[16]  Zhi-Yong Yin,et al.  Spatial and Temporal Variation of Summer Precipitation over the Eastern Tibetan Plateau and the North Atlantic Oscillation , 2001 .

[17]  M. Rusticucci,et al.  Observed Trends in Indices of Daily Temperature Extremes in South America 1960–2000 , 2005 .

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

[19]  Thomas C. Peterson,et al.  Recent changes in climate extremes in the Caribbean region , 2002 .

[20]  Liu Yimin,et al.  New proofs of the recent climate warming over the Tibetan Plateau as a result of the increasing greenhouse gases emissions , 2006 .

[21]  Lin Zhenyao,et al.  Spatial characteristics of changes in temperature and precipitation of the Qinghai-Xizang (Tibet) Plateau , 1996 .

[22]  Thomas C. Peterson,et al.  Changes in daily temperature and precipitation extremes in central and south Asia , 2006 .

[23]  Wu Shaohong,et al.  Climatic trends over the Tibetan Plateau during 1971-2000 , 2007 .

[24]  Xiaolan L. Wang Comments on “Detection of Undocumented Changepoints: A Revision of the Two-Phase Regression Model” , 2003 .

[25]  Xiaolan L. Wang,et al.  Changes of Extreme Wave Heights in Northern Hemisphere Oceans and Related Atmospheric Circulation Regimes , 2001 .

[26]  G. Meehl,et al.  Climate extremes: observations, modeling, and impacts. , 2000, Science.

[27]  J. V. Revadekar,et al.  Global observed changes in daily climate extremes of temperature and precipitation , 2006 .

[28]  M. J. MANTONa,et al.  TRENDS IN EXTREME DAILY RAINFALL AND TEMPERATURE IN SOUTHEAST ASIA AND THE SOUTH PACIFIC : 1961 – 1998 , 2001 .

[29]  R. W. Vachon,et al.  Stable isotopic variations in west China: A consideration of moisture sources , 2007 .

[30]  Shi-chang Kang,et al.  Relationship between trends in temperature extremes and elevation in the eastern and central Tibetan Plateau, 1961–2005 , 2008 .

[31]  Qiang Zhang,et al.  Changes of Climate Extremes in China , 1999 .

[32]  Xuebin Zhang,et al.  Trends in Middle East climate extreme indices from 1950 to 2003 , 2005 .

[33]  Russell S. Vose,et al.  Maximum and minimum temperature trends for the globe: An update through 2004 , 2005 .

[34]  B. Chen,et al.  Enhanced climatic warming in the Tibetan Plateau due to doubling CO2: a model study , 2003 .

[35]  M. Haylock,et al.  Change in mean temperature as a predictor of extreme temperature change in the Asia–Pacific region , 2005 .

[36]  R. Katz,et al.  Extreme events in a changing climate: Variability is more important than averages , 1992 .

[37]  M. Rusticucci,et al.  Trends in Total and Extreme South American Rainfall in 1960–2000 and Links with Sea Surface Temperature , 2006 .

[38]  M. Haylock,et al.  Observed coherent changes in climatic extremes during the second half of the twentieth century , 2002 .

[39]  Zheng Du,et al.  A discussion on the boundary and area of the Tibetan Plateau in China , 2002 .

[40]  D. Qin,et al.  Recent temperature increase recorded in an ice core in the source region of Yangtze River , 2007 .

[41]  P. Sen Estimates of the Regression Coefficient Based on Kendall's Tau , 1968 .

[42]  G. Wu,et al.  Role of the Tibetan Plateau thermal forcing in the summer climate patterns over subtropical Asia , 2005 .

[43]  Review of the studies on climate change since the last inter-glacial period on the Tibetan Plateau , 2006 .

[44]  Guoxiong Wu,et al.  Change of cloud amount and the climate warming on the Tibetan Plateau , 2006 .