期刊文献+

Changes in temperature extremes in the Yangtze River Basin, 1962-2011 被引量:15

Changes in temperature extremes in the Yangtze River Basin, 1962-2011
原文传递
导出
摘要 Based on daily maximum and minimum temperature observed by the China Mete- orological Administration at 115 meteorological stations in the Yangtze River Basin from 1962 to 2011, the methods of linear regression, principal component analysis and correlation analysis are employed to investigate the temporal variability and spatial distribution of tem- perature extremes. Sixteen indices of extreme temperature are selected. The results are as follows: (1) The occurrence of cold days, cold nights, ice days, frost days and cold spell du- ration indicator has significantly decreased by -0.84, -2.78, -0.48, -3.29 and -0.67 days per decade, respectively. While the occurrence of warm days, warm nights, summer days, tropi- cal nights, warm spell duration indicator and growing season length shows statistically sig- nificant increasing trends at rates of 2.24, 2.86, 2.93, 1.80, 0.83 and 2.30 days per decade, respectively. The tendency rate of the coldest day, coldest night, warmest day, warmest night and diurnal temperature range is 0.33, 0.47, 0.16, 0.19 and -0.07~C per decade, respectively (2) The magnitudes of changes in cold indices (cold nights, coldest day and coldest night) are obviously greater than those of warm indices (warm nights, warmest day and warmest night). The change ranges of night indices (warm nights and cold nights) are larger than those of day indices (warm days and cold days), which indicates that the change of day and night tem- perature is asymmetrical. (3) Spatially, the regionally averaged values of cold indices in the upper reaches of the Yangtze River Basin are larger than those in the middle and lower reaches. However, the regionally averaged values of most warm indices (except warm spell duration indicator) and growing season length in the middle and lower reaches are larger than those in the upper reaches. (4) The extreme temperature indices are well correlated with each other except diurnal temperature range. Based on daily maximum and minimum temperature observed by the China Mete- orological Administration at 115 meteorological stations in the Yangtze River Basin from 1962 to 2011, the methods of linear regression, principal component analysis and correlation analysis are employed to investigate the temporal variability and spatial distribution of tem- perature extremes. Sixteen indices of extreme temperature are selected. The results are as follows: (1) The occurrence of cold days, cold nights, ice days, frost days and cold spell du- ration indicator has significantly decreased by -0.84, -2.78, -0.48, -3.29 and -0.67 days per decade, respectively. While the occurrence of warm days, warm nights, summer days, tropi- cal nights, warm spell duration indicator and growing season length shows statistically sig- nificant increasing trends at rates of 2.24, 2.86, 2.93, 1.80, 0.83 and 2.30 days per decade, respectively. The tendency rate of the coldest day, coldest night, warmest day, warmest night and diurnal temperature range is 0.33, 0.47, 0.16, 0.19 and -0.07~C per decade, respectively (2) The magnitudes of changes in cold indices (cold nights, coldest day and coldest night) are obviously greater than those of warm indices (warm nights, warmest day and warmest night). The change ranges of night indices (warm nights and cold nights) are larger than those of day indices (warm days and cold days), which indicates that the change of day and night tem- perature is asymmetrical. (3) Spatially, the regionally averaged values of cold indices in the upper reaches of the Yangtze River Basin are larger than those in the middle and lower reaches. However, the regionally averaged values of most warm indices (except warm spell duration indicator) and growing season length in the middle and lower reaches are larger than those in the upper reaches. (4) The extreme temperature indices are well correlated with each other except diurnal temperature range.
出处 《Journal of Geographical Sciences》 SCIE CSCD 2014年第1期59-75,共17页 地理学报(英文版)
基金 l National Basic Research Program of China (973 Program), No.2013CBA01801 National Natural Science Foundation of China, No.41161012, No.41240001 Basic Scientific Research Foundation in University of Gansu Province
关键词 Yangtze River Basin temperature extremes warm indices cold indices variation tendency Yangtze River Basin temperature extremes warm indices cold indices variation tendency
  • 相关文献

参考文献42

  • 1Aguilar E, Barry A, Brunet Met al., 2009. Changes in temperature and precipitation extremes in western Central Africa, Guinea Conakry, and Zimbabwe, 1955-2006. Journal of Geophysical Research, 114, D02115, doi: 10.1029/2008JD011010.
  • 2Aguilar E, Peterson T C, Obando P R et al., 2005. Changes in precipitation and temperature extremes in Central America and northern South America, 1961-2003. Journal of Geophysical Research, 110, D23107, doi: 10.1029/2005JD006119.
  • 3Alexander L V, Zhang X, Peterson T C et al., 2006. Global observed changes in daily climate extremes of tem- perature and precipitation. Journal of Geophysical Research, 111, D05109, doi: 10.1029/2005JD006290.
  • 4Changnon S A, Pielke Jr R A, Changnon D et al., 2000. Human factors explain the increased losses from weather and climate extremes. Bulletin of American Meteorological Society, 81:437-442.
  • 5Cheng Xiaoguang, Declan C, Zheng Guangfen et al., 2008. Trends of extreme temperature in Ningxia during 1961-2004. Advances in Climate Change Research, 4(2): 73-77. (in Chinese).
  • 6Choi G, Collins D, Ren G Yet al., 2009. Changes in means and extreme events of temperature and precipitation in the Asia-Pacific Network region, 1955-2007. International Journal of Climatology, 29:1906-1925.
  • 7Ding Bin, Gu Xianyue, Liao Qilong, 2006. Characteristics in the variation of temperature over the Yangtze River valley over last 50 years. Resources and Environment in the Yangtze Basin, 15(4): 531-536. (in Chinese).
  • 8Ding Yihui, Ren Guoyu, Shi Guangyu et al., 2006. National Assessment Report of Climate Change (I): Climate change in China and its future trend. Advances in Climate Change Research, 2(1): 3-8. (in Chinese).
  • 9Easterling D R, Evans J L, Grolsman P Ya et al., 2000. Observed variability and trends in extreme climate events: A brief review. Bulletin of American Meteorological Society, 81 (3): 417-425.
  • 10Editorial Committee of China's National Assessment Report (ECCNAR) on Climate Change, 2007. The China's National Assessment Report on Climate Change. Beijing: Science Press, 18-40. (in Chinese).

同被引文献200

引证文献15

二级引证文献110

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部