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近50年来甘肃省河东地区春玉米干旱时空特征分析
引用本文:尹海霞,张勃,张建香,张调风,李小亚,靳自宝.近50年来甘肃省河东地区春玉米干旱时空特征分析[J].资源科学,2012,34(12):2347-2355.
作者姓名:尹海霞  张勃  张建香  张调风  李小亚  靳自宝
作者单位:西北师范大学地理与环境科学学院,兰州,730070
基金项目:国家自然科学基金项目(编号:40961038);生态经济学省级重点学科(编号:5001-021);西北师范大学知识与科技创新工程项目(编号:NWNU-KJCXGC-03-66)。
摘    要:根据甘肃省河东地区15个气象站点50年的气象资料,利用FAOPenman-Monteith模型和所提供的作物系数计算出各站点春玉米不同生育阶段的作物需水量,在此基础上计算出作物水分亏缺指数(CWDI),并划分河东地区的干旱等级,分析春玉米干旱发生的时空特征。结果表明:在春玉米生长季内,CWDI呈现先增大后减小的趋势,其中最大值出现在6月中下旬,且每旬的CWDI值均大于10%,即在作物整个生长季,降水都无法满足春玉米需水的要求。不同等级干旱发生的频率:轻旱8%~20%;中旱7%~23%;重旱0~17%;特旱0~47%。生长季内,河东地区春玉米干旱发生程度基本由南向北递增,不同生育阶段干旱的严重程度:抽雄-开花期>拔节期>乳熟前期>出苗-七叶期>乳熟后期-成熟期。近50年来,出苗-七叶期和拔节期的干旱有逐渐缓解的趋势;抽雄-开花期和乳熟前期干旱变化的趋势大致相同:20世纪60年代中后期及70年代初为干旱的严重时期,70年代中后期有所缓解,至今又有加重的趋势;乳熟后期-成熟期,近50年来干旱有加重的趋势。

关 键 词:作物水分亏缺指数  干旱  时空特征  干旱频率  春玉米  甘肃省河东地区

Spatial-Temporal Characteristics of Drought and Spring Maize in Eastern Gansu
YIN Haixi,ZHANG Bo,ZHANG Jianxiang,ZHANG Tiaofeng,LI Xiaoya and JIN Zibao.Spatial-Temporal Characteristics of Drought and Spring Maize in Eastern Gansu[J].Resources Science,2012,34(12):2347-2355.
Authors:YIN Haixi  ZHANG Bo  ZHANG Jianxiang  ZHANG Tiaofeng  LI Xiaoya and JIN Zibao
Institution:Geographic and Environmental Sciences Department of Northwest Normal University, Lanzhou, Gansu 730070, China;Geographic and Environmental Sciences Department of Northwest Normal University, Lanzhou, Gansu 730070, China;Geographic and Environmental Sciences Department of Northwest Normal University, Lanzhou, Gansu 730070, China;Geographic and Environmental Sciences Department of Northwest Normal University, Lanzhou, Gansu 730070, China;Geographic and Environmental Sciences Department of Northwest Normal University, Lanzhou, Gansu 730070, China;Geographic and Environmental Sciences Department of Northwest Normal University, Lanzhou, Gansu 730070, China
Abstract:The total number of droughts is increasing in China due to global climate change. Extraordinary droughts are of a long duration, wide range and severe disaster degree. Eastern Gansu is located in the semi-arid-semi-humid climate zone, and is a rain fed agricultural region. Because the distribution of precipitation is uneven, the water requirements of spring maize are different during various growth stages. Understanding the temporal and spatial distribution and evolution of droughts during spring maize is important to the sustainable development of the economy. Here, according to 50 years of weather data from seven meteorological stations in eastern Gansu, the water requirements of spring maize at different growth stages was calculated using the FAO Penman-monteith model and coefficient. The crop water deficit index (CWDI) was calculated and the drought grade was divided into four communities. The results show that the CWDI became larger initially and then smaller during the growth period for spring maize; the ten days, middle and last ten days of June contained maximum values. The CWDI of every ten days was over 10%, showing that precipitation in the growth period cannot meet the water requirements of spring maize. The frequency of different classes of drought were 8%~20% for light drought, 7%~ 23% for middle drought, 0~17% for heavy drought, and 0~47% for excessive drought. The relative severity of the drought followed the pattern: tasselling stage to flowering stage > jointing stage > pre-milk stage > emergence stage to seven leaf stage > late-milk stage to mature stage. In the last 50 years, the severity of droughts has increased in this area.
Keywords:The crop water deficit index (CWDI)  Drought  Spatial-temporal characteristics  Drought frequency  Spring maize  Eastern Gansu
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