Precipitation and temperature changes in the major Chinese river basins during 1957-2013 and links to sea surface temperature

被引:64
作者
Tian, Qing [1 ]
Prange, Matthias [2 ]
Merkel, Ute [2 ]
机构
[1] E China Normal Univ, State Key Lab Estuarine & Coastal Res, 3663 N Zhongshan Rd, Shanghai 200062, Peoples R China
[2] Univ Bremen, Dept Geosci, MARUM Ctr Marine Environm Sci, D-28334 Bremen, Germany
关键词
Chinese rivers; Precipitation; Temperature; SST; Mann-Kendall test; MCA; CLIMATE-CHANGE; WATER DISCHARGE; TEMPORAL VARIATION; PAN EVAPORATION; SUMMER RAINFALL; PACIFIC-OCEAN; SEDIMENT LOAD; IMPACTS; VARIABILITY; TRENDS;
D O I
10.1016/j.jhydrol.2016.02.048
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The variation characteristics of precipitation and temperature in the three major Chinese river basins (Yellow River, Yangtze River and Pearl River) in the period of 1957-2013 were analyzed on an annual and seasonal basis, as well as their links to sea surface temperature (SST) variations in the tropical Pacific and Indian Ocean on both interannual and decadal time scales. Annual mean temperature of the three river basins increased significantly overall since 1957, with an average warming rate of about 0.19 degrees C/10a, but the warming was characterized by a staircase form with steps around 1987 and 1998. The significant increase of annual mean temperature could mostly be attributed to the remarkable warming trend in spring, autumn and winter. Warming rates in the northern basins were generally much higher than in the southern basins. However, both the annual precipitation and seasonal mean precipitation of the three river basins showed little change in the study area average, but distinct interannual variations since 1957 and clear regional differences. An overall warming-wetting tendency was found in the northwestern and southeastern river basins in 1957-2013, while the central regions tended to become warmer and drier. Results from a Maximum Covariance Analysis (MCA) showed that the interannual variations of seasonal mean precipitation and surface air temperature over the three river basins were both associated with the El Nino-Southern Oscillation (ENSO) since 1957. ENSO SST patterns affected precipitation and surface air temperature variability throughout the year, but with very different response patterns in the different seasons. For instance, temperature in most of the river basins was positively correlated with central-eastern equatorial Pacific SST in winter and spring, but negatively correlated in summer and autumn. On the decadal time scale, the seasonal mean precipitation and surface air temperature variations were strongly associated with the Pacific Quasi-Decadal Oscillation. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:208 / 221
页数:14
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