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河西走廊东部近50年气候变化特征及区内5站对比分析
引用本文:杨晓玲,丁文魁,杨金虎,周文霞.河西走廊东部近50年气候变化特征及区内5站对比分析[J].干旱地区农业研究,2011,29(5):259-268.
作者姓名:杨晓玲  丁文魁  杨金虎  周文霞
作者单位:1. 中国气象局兰州干旱气象研究所,甘肃省干旱气候变化与减灾重点实验室,中国气象局干旱气候变化与减灾重点开放实验室,甘肃兰州730020;甘肃省武威市气象局,甘肃武威733000
2. 甘肃省武威市气象局,甘肃武威,733000
3. 甘肃省定西市气象局,甘肃定西,743000
基金项目:甘肃省第五批“十人计划”资助
摘    要:利用河西走廊东部武威市五个气象站近50年气温、降水资料,运用统计学的方法,详细分析了当地气温、降水的时空变化特征,并进行了对比分析.结果表明,北部川区气温远大于南部山区,随海拔高度的升高气温逐渐降低;北部川区降水远小于南部山区,随海拔高度的升高降水逐渐增多.各地年平均气温呈上升趋势,20世纪90年代以来升温明显.从平均...

关 键 词:河西走廊东部  气候  变化特征  对比分析

Change characteristics and 5 stations contrastive analysis of climatein eastern Hexi corridor in recent 50 years
YANG Xiaoling,DING Wenkui,YANG Jinhu,ZHOU Wenxia.Change characteristics and 5 stations contrastive analysis of climatein eastern Hexi corridor in recent 50 years[J].Agricultural Research in the Arid Areas,2011,29(5):259-268.
Authors:YANG Xiaoling  DING Wenkui  YANG Jinhu  ZHOU Wenxia
Institution:Institute of Arid-Meteorology CMA, Key Laboratory of Arid Climate Change and Reducing Disaster, Key Open Laboratory of Arid Climate Change and Disaster Reduction CMA, Lanzhou, Gansu 730020, China; Wuwei Meteorological Bureau, Wuwei, Gansu 733000, China;Dingxi Meteorological Bureau, Dingxi, Gansu 743000, China
Abstract:Using nearly 50a temperature and precipitation data of five stations in Wuwei of eastern Hexi corridor, the characteristics of temporal and spatial change of temperature and precipitation in the area were analyzed, and contrastive analysis was also conducted with statistics method. The results showed: The temperature of north plain area was far higher than that of south mountainous area, and the temperature reduced gradually along with rise of altitude. The precipitation of north plain area was far less than that of south mountainous area, and the precipitation increased gradually along with the rise of altitude. The regional annual mean temperature assumed a trend of escalation, and the temperature had elevated obviously since the 1990s. Viewed from the change of the average temperature, the highest temperature and the lowest temperature, the elevation scopes of various seasons'' temperature were winter > spring > autumn > summer, the winter warming was far greater than other three seasons. The elevation scopes of the average lowest temperature was bigger than that of the average highest tempe rature, which explained that the night warming was bigger than the daytime warming. The high temperature weather mainly appeared from June to September, while t he low temperature weather mainly appeared from November to March of next year. Yearly precipitation of every region (except Gulang) assumed increasing tendency . The increasing scopes of the various seasons'' precipitation were summer > autumn > spring > winter, precipitation''s increase of summer was the biggest to year precipitation''s contribution. Precipitation was mainly light rain. Precipitation days reduced rapidly along with the precipitation magnitude''s enhancement. The strong precipitation only appeared from May to September.
Keywords:eastern Hexi corridor  climate  change characteristic  contrastive analysis
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