近45年雅鲁藏布江流域极端气候事件趋势分析
Trends in Daily Temperature and Precipitation Extremes over the Yarlung Zangbo River Basin during 1961-2005
查看参考文献16篇
文摘
|
利用雅鲁藏布江流域10个气象台站1961-2005年逐日最高气温、最低气温和日降水量资料,分析了该流域气温和降水等气候极端事件的变化趋势.研究表明:近45年以来,雅鲁藏布江流域夜间和白天极端低温日数分别以1.94和0.97天/10年的趋势在显著减少,夜间极端低温日数减少在冬季最明显,白天极端低温日数在秋季减少最明显:夜间极端高温日数和白天极端高温日数分别以3.03和1.26天/10年的速度显著增加,夜间极端高温日数增加在夏季最明显,白天极端高温日数增加在冬季最明显;日较差以0.11℃/10a的速度在显著减少,主要发生在冬季:最大的1天降水总量和逐年连续无降水天数有减少趋势,最大的5天降水总量、中雨天数、逐年平均降水强度和逐年连续降水天数有增加趋势,90年代以来增加趋势明显,与该地区经向风与水汽通量增加有关. |
其他语种文摘
|
Based on daily temperature (maximum and minimum) and daily precipitation at 10 meteorological stations over the Yarlung Zangbo River Basin observed by the China Meteorological Administration during the 1961-2005 period, the spatial and temporal variations in climate extremes are analyzed. The results are as follows: Over the 1961-2005 period, the regionally averaged occurrence of extreme cold days and nights has significantly decreased by-0.97 and -1.94 days/decade, respectively. Over the same period, the occurrence of extreme warm days and nights has significantly increased by 1.26 and 3.03 days/decade, respectively. The diurnal temperature range (DTR) exhibits a decreasing trend (0.11℃/decade), especially in winter, coinciding with the fact that there is a greater rise in the minimum temperature than in the maximum temperature. The decrease in the number of cold days mostly occurs in winter and autumn, while the increase in the number of warm nights and days mainly happens in summer and winter. Precipitation indices, due to the large and expected spatial variability, indicate that regionally averaged annual maximum with 1-day precipitation and consecutive dry days have no statistically significant decreasing trends. At the same time, there is no significant increase in regionally averaged daily rainfall intensity, consecutive wet days, number of heavy precipitation days and maximum annual amount for 5-day precipitation. |
来源
|
地理学报
,2009,64(5):592-600 【核心库】
|
关键词
|
雅鲁藏布江流域
;
极端气候
;
趋势
|
地址
|
1.
中国科学院青藏高原研究所, 北京, 100085
2.
国家气候中心, 北京, 100081
|
语种
|
中文 |
文献类型
|
研究性论文 |
ISSN
|
0375-5444 |
学科
|
大气科学(气象学) |
基金
|
国家自然科学基金
;
国家973计划
;
中国科学院知识创新工程重要方向项目
;
欧盟第六框架项目
|
文献收藏号
|
CSCD:3570025
|
参考文献 共
16
共1页
|
1.
IPCC.
Summary for Policymakcrs of Climate Change 2007:The Physical Science Basis.Contribution of Working Group I to the Fourth Assessment Report of the Intergovemmental Panel on Climate Change,2007
|
CSCD被引
2
次
|
|
|
|
2.
翟盘茂. 中国近四十年最高最低温度变化.
气象学报,1997,55(4):418-429
|
CSCD被引
213
次
|
|
|
|
3.
任福民. 1951—1990年中国极端气温变化分析.
大气科学,1998,22(2):217-227
|
CSCD被引
185
次
|
|
|
|
4.
You Qinglong. Changes in daily climate extremes in the eastem and central Tibetan Plateau during 1961-2005.
Journal of Geophysical Research D:Atmospheres,2008,113:D07101
|
CSCD被引
3
次
|
|
|
|
5.
游庆龙. 三江源地区1961~2005年气温极端事件变化.
长江流域资源与环境,2008,17(2):232-236
|
CSCD被引
23
次
|
|
|
|
6.
唐红玉. 1951-2002年中国平均最高、最低气温及日较差变化.
气候与环境研究,2005,10(4):728-735
|
CSCD被引
81
次
|
|
|
|
7.
刘学华. 中国近40年极端气温和降水的分布特征及年代际差异.
热带气象学报,2006,22(6):618-624
|
CSCD被引
79
次
|
|
|
|
8.
Zhai P M. Change of cliraate extfes in China.
Climatic Change,1999,42:203-218
|
CSCD被引
111
次
|
|
|
|
9.
翟盘茂. 中国降水极值变化趋势检测.
气象学报,1999,57(2):208-216
|
CSCD被引
222
次
|
|
|
|
10.
汤奇成.
中国河流水文,1998
|
CSCD被引
22
次
|
|
|
|
11.
边多. 近40年西藏“一江两河”流域气候变化特征.
应用气象学报,2006,17(2):169-175
|
CSCD被引
38
次
|
|
|
|
12.
杜军. 雅鲁藏布江中游地表湿润状况的趋势分析.
自然资源学报,2006,21(2):196-203
|
CSCD被引
13
次
|
|
|
|
13.
You Qinglong. Climate change over the Yarlung Zangbo River Basin during 1961-2005.
Journal of Geographical Sciences,2007,17(4):409-420
|
CSCD被引
15
次
|
|
|
|
14.
Alexander L V. Global observed changes in daily climate exffcmes of temperature and precipitation.
Journal of Geophysical Research D:Atmospheres,2006,111:D05109
|
CSCD被引
18
次
|
|
|
|
15.
Aguilar E. Changes in precipitation and temperature extremes in Central America and northern South America,1961-2003.
Journal of Geophysical Research D:Atmospheres,2005,110:23107
|
CSCD被引
1
次
|
|
|
|
16.
Kalnay,E. The NCEP/NCAR 40-year reanalysis project.
Bulletin of the American Meteorological Society,1996,77(3):437-471
|
CSCD被引
2274
次
|
|
|
|
|