Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China.
University of Chinese Academy of Sciences, Beijing, China.
Sci Rep. 2018 Aug 8;8(1):11860. doi: 10.1038/s41598-018-30320-0.
In this study, the spatiotemporal distributions of monthly and annual temperature minima (T) and maxima (T), extreme T and T, the highest (lowest) T (T), frost day (FD), icing day (ID), summer day (SD) and tropical night (TR) at 112 stations and over the ten large river basins on the Tibetan Plateau and its surroundings (TPS) during 1963-2015 are examined. Mann-Kendall test is applied for the trends. The analyses show: the northwest experiences the hottest summer while the central TPS has the coldest winter and most frequent frost and icing days. The northwest (southeast) features the highest (lowest) monthly extreme temperature ranges. The northwest has the most frequent hot summer days, whereas the southeast has the least frequent frost and icing days. The entire TPS displays few tropical nights. Most stations show positive trends for all monthly and annual T and T variables. February displays the most positive trends for both monthly T and T variables while April shows the highest number of stations with decreasing trends in monthly T. The trends of FD and ID are negative, whereas the trends of SU and TR are positive. Over river basins, the trends of monthly T are all positive and statistically significant and the trends of monthly T are all positive except for one negative trend and around 1/3 of the positive trends are statistically significant. Relatively larger increases in monthly T and T are noted for the cold season than the warm. The monthly and annual T variables increase more than T variables.
在这项研究中,考察了青藏高原及其周边地区(TPS)的 112 个站点和 10 个大型流域在 1963-2015 年期间逐月和逐年的最低温度(T)和最高温度(T)、极端最低温度(T)和极端最高温度(T)、最高温度(T)和最低温度(T)、霜日(FD)、结冰日(ID)、夏日(SD)和热带夜(TR)的时空分布。采用 Mann-Kendall 检验进行趋势分析。结果表明,青藏高原西北部夏季最热,而中部冬季最冷,霜日和结冰日最频繁。西北(东南)地区月极端温差最大(小)。青藏高原西北部地区夏日炎热天数最多,而东南部地区霜日和结冰日最少。整个 TPS 地区热带夜较少。大多数站点的逐月和全年 T 和 T 变量均呈正趋势。2 月的逐月 T 和 T 变量均呈最显著的正趋势,而 4 月的逐月 T 减少趋势站点数最多。FD 和 ID 的趋势为负,而 SU 和 TR 的趋势为正。流域尺度上,逐月 T 的趋势均为正且显著,逐月 T 的趋势除了一个负趋势外均为正,约有 1/3的正趋势显著。与温暖季节相比,寒冷季节的逐月 T 和 T 增加更为明显。逐月和全年 T 变量的增加幅度大于 T 变量。