1962—2010年甘肃省黄土高原区干旱时空动态格局

生态学杂志 ›› 2012, Vol. 31 ›› Issue (08): 2066-2074.

1962—2010年甘肃省黄土高原区干旱时空动态格局

张调风¹,张勃^1**,张苗²,刘秀丽^1,3,孙力炜¹,安美玲¹

(¹西北师范大学地理与环境科学学院，兰州 730070； ²甘肃农业大学林学院，兰州 73007； ³忻州师范学院地理系，山西忻州 034000)

出版日期:2012-08-10 发布日期:2012-08-10

Spatiotemporal pattern of drought in Loess Plateau of Gansu Province, Northwest China in 1961-2010.

ZHANG Tiao-feng¹, ZHANG Bo^1**， ZHANG Miao², LIU Xiu-li^1,3，SUN Li-wei¹, AN Mei-ling¹

(¹School of Geography and Environment Science, Northwest Normal University, Lanzhou 730070, China; ²College of Forestry, Gansu Agricultural University, Lanzhou 730070, China; ³ Department of Geography, Xinzhou Teachers University, Xinzhou 034000, Shanxi, China)

Online:2012-08-10 Published:2012-08-10

摘要/Abstract

摘要： 借助ArcGIS 9.3和SPSS软件平台，根据甘肃省黄土高原区33个气象站1962—2010年气象资料，利用综合气象干旱指数(CI)从干旱率、干旱强度和干旱频率三方面对甘肃省黄土高原区近50年的干旱时空变化特征进行了分析。结果表明：春、秋季干旱率呈现显著增加趋势，夏、冬季干旱率呈略微增加趋势；夏季干旱频率最大，春季、秋季次之，冬季最少；春、秋季干旱以2000年来最为严重，夏季干旱以2000年以来、20世纪70年代和90年代均较严重，冬季干旱以20世纪80年代最为严重；甘肃省黄土高原区逐年干旱持续日数和干旱强度存在明显的年际波动，线性变化趋势明显；从空间分布来看，春、夏和秋季干旱多发区主要集中在甘肃省黄土高原区西北部，而106°E以西“临洮通渭天水”一线和庆阳东南部是干旱多发区变幅最大的地方，冬季干旱多发区主要集中在甘肃省黄土高原区南部。

Abstract: Drought, one of the most severe hazards resulting in significant economic losses in agriculture and industry, is a natural phenomenon caused by the imbalance between the input of and the demand for water. As a major grain production zone in Gansu Province, the Loess Plateau of the Province shows great vulnerability in drought. In this paper, the characteristics of interannual and seasonal droughts in the Loess Plateau of Gansu Province were analyzed in terms of drought rate, drought intensity, and drought frequency, and by using the compound index of meteorological drought (CI) and the data of daily precipitation, air temperature, wind speed, relative humidity, and sunshine duration from 33 weather stations during the period from 1962 to 2010. Kriging interpolation was also applied to calculate the CI value for each station, so that all the CI values could be spatially and temporally comparable. In the Plateau of the Province, drought rate showed a significant increasing trend in spring and autumn but a slight increasing trend in summer and winter, and drought frequency was the most in summer, followed by in spring and autumn, and in winter. The 50-year average drought rate in spring, summer, autumn, and winter was 53.26%, 65.18%, 42.2%, and 44.16%, respectively. Over the past 50 years, the most serious inter-decadal drought in the Plateau of the Province occurred in spring and autumn since 2000, and in winter in the 1980s. In the 1970s and 1980s and since 2000, summer drought was more serious. There was a notable interannual fluctuation in the average annual lasting days and annual occurrence severity of meteorological droughts in the whole region, and their linear change tendency was obvious. Spatially, in spring, summer, and autumn, the droughtprone area was mainly located in the northwest of the region. Meanwhile, in the districts of “LintaoTongweiTianshui” and southeast of Qingyang, the change range was the largest. The droughtprone area in winter was mainly located in south of the region. In order to well prevent and mitigate the drought in the Loess Plateau of Gansu Province, government and agricultural managers should pay more attention to the droughts that occur from spring to autumn, especially in summer.

张调风1,张勃1**,张苗2,刘秀丽1,3,孙力炜1,安美玲1. 1962—2010年甘肃省黄土高原区干旱时空动态格局[J]. 生态学杂志, 2012, 31(08): 2066-2074.

ZHANG Tiao-feng1, ZHANG Bo1**， ZHANG Miao2, LIU Xiu-li1,3，SUN Li-wei1, AN Mei-ling1. Spatiotemporal pattern of drought in Loess Plateau of Gansu Province, Northwest China in 1961-2010.[J]. cje, 2012, 31(08): 2066-2074.