[1]凯丽比努尔·克热木,海米提·依米提,麦麦提吐尔逊·艾则孜.喀什地区1957-2013年潜在蒸散量变化及其影响因子[J].水土保持研究,2017,24(05):247-251,258.
　Kalbinur·Kerim,Hamit·Yimit,Mamattursun·Eziz.Dynamic Change of Potential Evapotranspiration and Its Influence Factors in Kashi Area During 1957-2013[J].Research of Soil and Water Conservation,2017,24(05):247-251,258.
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喀什地区1957-2013年潜在蒸散量变化及其影响因子

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 24 期数: 2017年05期 页码: 247-251,258 栏目: 出版日期: 2017-10-28
Title:
Dynamic Change of Potential Evapotranspiration and Its Influence Factors in Kashi Area During 1957-2013
作者:
凯丽比努尔·克热木1, 海米提·依米提2,3, 麦麦提吐尔逊·艾则孜2,3
1. 新疆大学 资源与环境科学学院, 乌鲁术齐 830046;
2. 新疆师范大学 干旱区湖泊环境与资源重点实验室, 乌鲁术齐 830054
Author(s):
Kalbinur·Kerim1, Hamit·Yimit2,3, Mamattursun·Eziz2,3
1. School of Resources and Environmental Science, Xinjiang University, Urumqi 830046, China;
2. Key Laboratory of Lake Environment and Resources in Arid Area, Xinjiang Normal University, Urumqi 830054, China
关键词:
潜在蒸散量; Penman-Monteith模型; 影响因子; 喀什地区
Keywords:
potential evapotranspiration; Penman-Monteith model; impact factor; Kashi area
分类号:
S161.4
摘要:
基于喀什地区4个气象站点1957—2013年的最高气温、最低气温、月平均气温、相对湿度、风速、日照时数以及降水量数据，采用Penman-Monteith模型、一元回归分析、累积距平和Mann-Kendall非线性突变检验法，分析其年潜在蒸散量的时间序列变化及其影响因子。结果表明：近57 a来，喀什和巴楚的潜在蒸散量呈减少趋势，倾向率分别为-7.53 mm/10 a，-7.47 mm/10 a；塔什库尔干与莎车的潜在蒸散量呈现增加趋势，倾向率分别为8.27 mm/10 a，6.25 mm/10 a；在四季变化中，夏季最多，春、秋季次之，冬季最少；喀什地区潜在蒸散量突变点存在明显差异：喀什年潜在蒸散量突变点为1981年，巴楚的为1962年，塔什库尔干的为1974年和1983年，莎车年潜在蒸散量突变点为1961年、1965年、1968年和1978年；喀什地区年蒸散量最主要受风速和日照时数的影响。
Abstract:
Based on maximum temperature, minimum temperature, monthly mean temperature, relative humidity, wind speed, sunshine duration and rainfall data collected from four meteorological stations during 1957—2013 in Kashi area, we used Penman-Monteith model, regression analysis, accumulative anomaly and Mann-Kendall nonlinear mutation test method to analyze annual potential evapotranspiration dynamic change and its influence factor of time series. The results show that: (1) in the past 57 years, the potential evapotranspiration in Kashi and Bachu showed the decreasing trend and its tendency rates were -7.53 mm/decade, -7.47 mm/decade, potential evapotranspiration of Tashikuergan and Shache increased with the tendency rates of 8.27 mm/decade and 6.25 mm/decade; (2) during the four seasons, the dynamic change tendency rate was higher in summer than spring and autumn, and lowest occurred in winter; (3) there was a significant difference among the potential evapotranspiration mutation points in Kashi area; the annual potential evapotranspiration mutation point of Kashi occurred in 1981, 1962 for Bachu, 1974 and 1983 for Tashikuergan, annual potential evapotranspiration mutation points of Shache occurred in 1961, 1965, 1968 and 1978; (4) the wind speed and sunshine hours have the effect on the annual evapotranspiration in Kashi area.

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备注/Memo

收稿日期:2016-10-24;改回日期:2016-11-28。
基金项目:国家自然科学基金重点项目—新疆联合基金“新疆博斯腾湖环境演变及对气候变化的响应”（U1138302）
作者简介:凯丽比努尔·克热木(1992-),女(维吾尔族),新疆阿图什人,硕士研究生,研究方向:干旱区资源与环境。E-mail:1040014059@qq.com

更新日期/Last Update: 1900-01-01