气候与全球变化

近50年河北省干旱时空分布特征

  • 闫峰 ,
  • 王艳姣 ,
  • 吴波
展开
  • 1. 中国林业科学研究院荒漠化研究所, 北京 100091;
    2. 中国气象局国家气候中心, 北京 100081
闫峰 (1973-),男,江苏连云港人,博士。主要从事灾害学和环境遥感研究。E-mail :njuyf@163.com

收稿日期: 2009-01-22

  修回日期: 2009-06-25

  网络出版日期: 2010-03-20

基金资助

国家自然科学基金项目(40801173);国家科技支撑计划项目(2007BAC03A10)

Spatial and temporal distributions of drought in Hebei Province over the past 50 years

  • YAN Feng ,
  • WANG Yan-jiao ,
  • WU Bo
Expand
  • 1. Academy of Disaster Reduction &|Emergency Management, Beijing Normal University, Beijing 100875, China;
    2. National Climate Center, China Meteorological Administration, Beijing 100081, China

Received date: 2009-01-22

  Revised date: 2009-06-25

  Online published: 2010-03-20

摘要

干旱是影响我国的主要气象灾害之一,本文采用标准化降水指数SPI作为干旱评价因子对近50年来河北省干旱的时空变化特征进行了研究,得出以下主要结论:(1)春季干旱最为严重,干旱率呈逐渐降低的趋势,夏季干旱率呈逐渐增加、秋季和冬季干旱率略有降低的趋势;(2)春季干旱在20世纪70年代最为严重,夏季、秋季和冬季的年代际干旱分别以2000年以来、20世纪60年代和90年代最为严重;(3)春季干旱发生概率均大于20%,发生概率大于30%的旱情多发地区在各市均有分布;全省大部分地区夏季、秋季和冬季干旱发生概率为20%~30%,夏季干旱多发地区主要集中在河北省北部和西南部,秋季干旱多发地区主要集中在河北省西部和南部,冬季干旱多发地区主要集中在河北省北部。

关键词: 干旱; SPI; 时空分布; 河北省

本文引用格式

闫峰 , 王艳姣 , 吴波 . 近50年河北省干旱时空分布特征[J]. 地理研究, 2010 , 29(3) : 423 -430 . DOI: 10.11821/yj2010030005

Abstract

In the context of global warming and human activities, drought has become one of the most serious meteorological disasters in the world. As a major grain producing province in China, Hebei Province shows great vulnerability to drought. In this paper, standardized precipitation index (SPI) was used as drought indicator and precipitation in meteorological stations of China from 1958 to 2007 was used to calculate the index in spring, summer, autumn and winter. Kriging interpolation was applied to SPI values in each station so that all the values could be spatially and temporally comparable. Based on raster data of seasonal SPI, drought rate and drought probability were calculated to show the spatial and temporal distribution characteristics of drought in Hebei Province over the past 50 years. The results showed that spring drought was the most serious event in a year and the drought rate showed a gradually declining trend. Drought rate in summer presented an upward trend, but in autumn and winter it showed slightly declining trends. The 50-year average drought rates in spring, summer, autumn and winter were 30.0%, 26.0%, 27.6% and 26.0%, respectively. Over the past 50 years in Hebei Province, spring drought in the 1970s was the most severe one. The most serious interdecadal droughts occurred respectively in summer since 2000, autumn in the 1960s and winter in the 1990s. Occurrence probability of spring drought was more than 20% in the whole province and drought-prone areas with the probability more than 30% were almost distributed in each city. In most areas, occurrence probability of summer drought, autumn drought and winter drought was from 20% to 30%. In summer, drought-prone areas were mainly located in the north and southwest of Hebei. Drought-prone areas in autumn were mainly located in the western and southern parts and in winter they were mainly distributed in the northern part. In order to do a good job in drought prevention and mitigation in Hebei Province, government and agricultural managers should pay more attention to the droughts that occur from spring to autumn, especially the spring drought. Moreover, irrigation systems should be further strengthened and improved in the mountain farms mainly located in the west and north of Hebei Province.

参考文献


[1] 黄荣辉,陈际龙,周连童,等.关于中国重大气候灾害与东亚气候系统之间关系的研究.大气科学, 2003, 27(4):770~787.

[2] 闫峰,史培军,武建军,等.基于MODIS-EVI数据的河北省冬小麦生育期特征. 生态学报, 2008, 28(9):4381~4387.

[3] Palmer W C. Meteorological drought. Research Paper No.45, U.S. Weather Bureau, 1965.

[4] Shafer B A, Dezman L E. Development of a Surface Water Supply Index (SWSI) to assess the severity of drought conditions in snowpack runoff areas. Proceedings of the Western Snow Conference, 1982, Colorado State University, Fort Collins, Colorado:164~175.

[5] McKee T B, Doesken N J, Kleist J.The relation of drought frequency and duration to time scales. Proceedings of the Eighth Conference on Applied Climatology. American. Meteorological. Society. Boston, 1993:179~184.

[6] McKee T B,Doesken N J, Kleist J. Drought monitoring with multiple time scales. Proceedings of the Nineth Conference on Applied Climatology. American Meteorological Society. Boston, 1995:233~236.

[7] Guttman N B. Accepting the Standardized Precipitation Index: a calculation algorithm. Journal of the American Water Resources Association, 1999, 35,311~322.

[8] Tsakiris G, Vangelis H.Towards a drought watch system based on spatial SPI.Water Resources Management, 2004,18(1):1~12.

[9] Moreira E E,Coelho C A, Paulo A A. SPI-based drought category prediction using loglinear models.Journal of Hydrology, 2008, 354: 116~130.

[10] Hayes M J,Svodoba M D,Wilhite D A, et al. Monitoring the 1996 drought using the standardized precipitation index. Bulletin of the American Meteorological Society, 1999,80(3):429~438.

[11] Lloyd-Hughes B, Saunders M A. A drought climatology for Europe.International Journal of Climatology, 2002, 22(13):1571~1592.

[12] Mihajlovic D. Monitoring the 2003-2004 meteorological drought over Pannonian part of Croatia. International Journal of Climatology, 2006,26(15):2213~2225.

[13] Livada I, Assimakopoulos V D. Spatial and temporal analysis of drought in Greece using the Standardized Precipitation Index (SPI). Theoretical and Applied Climatology, 2007, 89 (3-4): 143~153.

[14] 袁文平,周广胜.标准化降水指标与Z指数在我国应用的对比分析.植物生态学报,2004, 28(4): 523~529.

[15] 冶明珠,李林,王振宇. SPI指数在青海东部地区干旱监测中的应用及检验.青海气象, 2007,(4): 21~24.

[16] 李伟光,陈汇林,朱乃海,等.标准化降水指标在海南岛干旱监测中的应用分析.中国生态农业学报,2009, 17(1): 178~182.

[17] 赵桂香.干旱化趋势对山西省水资源的影响分析.干旱区研究, 2008, 25(4):492~496.

[18] 王英,曹明奎,陶波,等.全球气候变化背景下中国降水量空间格局的变化特征.地理研究, 2006, 25(6):1031~1040.

[19] Borga M, Vizzaccaro A.On the interpolation of hydrologic variables: formal equivalence of multiquadratic surface fitting and kriging.Journal of Hydrology,1997, 195: 160~171.

[20] Goovaerts P.Geostatistical approaches for incorporating elevation into the spatial interpolation of rainfall. Journal of Hydrology,2000,228,113~129.

[21] 闫峰,王艳姣,武建军,等. 基于Ts-EVI时间序列谱的冬小麦面积提取. 农业工程学报,2009,25(4): 135~140.

文章导航

/