新疆区域面雨量分布特征及其变化规律
Characteristics of Area Precipitation in Xinjiang Region with Its Variations
-
摘要: 将自然正交分解 (EOF) 和数字高程模型 (DEM) 相结合, 利用新疆区域144个气象站和水文站的1961—2005年降水量资料, 计算得到新疆区域面雨量年、季分布特征和变化规律。分析结果表明:新疆区域年平均面雨量约为2724.6×108t, 年平均降水量为165.5 mm。从空间分布来看, 天山山区面雨量最大, 约占全疆面雨量的40.4%, 该区域年平均降水量为409.1 mm; 北疆地区次之占34.3%, 年降水量为277.3 mm; 南疆地区最少约为25.3%, 年平均降水量仅有66.2 mm。从季节分布来看:夏季面雨量最大, 约占全年面雨量的54.4%;春季次之为23.6%;秋季为16.5 %; 冬季最少, 约为5.5%。新疆区域面雨量年际变化呈现出增多的趋势, 1987年存在突变, 在此之后降水量明显增多。Abstract: Using the data of precipitation including 144 meteorological and hydrological stations in Xinjiang from 1961 to 2005, annual and seasonal distributing features and its variations of area precipitation in Xinjiang are discussed by empirical orthogonal function (EOF), multiple regression analysis, maximum entropy analysis and so on, combining with 1 km×1 km gridding data of digital elevation model (DEM). Results show that mean annual area precipitation in Xinjiang region is 2724.6×108t and mean annual precipitation is 165.5 mm. For space distribution, area precipitation of Tianshan Mountains, Northern Xinjiang and Southern Xinjiang respectively occupy about 40.4%, 34.3% and 25.3% of all regions, and its mean annual precipitation are 409.1 mm, 277.3 mm and 66.2 mm, respectively. Area precipitation in summer is the most one about 54.4% of all year, 23.6% in spring, 16.5% in autumn, and the least 5.5% in winter. In the last 45 years area precipitation in Xinjiang presents clear annual variations and increasing trend, especially since 1987.
-
Key words:
- Xinjiang region;
- area precipitation;
- climate change
-
表 1 特征向量与地理因子的回归方程系数
Table 1 Regress equation coefficients between the characteristic vectors and geography factors
表 2 不同分辨率的面雨量
Table 2 The results of area precipitation in different resolution in Xinjiang region
表 3 新疆面雨量各季节年代际变化 (单位: 108t)
Table 3 Decadal variations of Xinjiang area precipitation (unit:108t)
-
[1] 傅抱璞.山地气候要素空间分布的模拟.气象学报, 1988, (3): 319-326. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB198803007.htm [2] 彭春华, 郑启松.荆江致洪与三峡区间暴雨预报.空军气象学院学报, 1995, 16(2) : 152-159. [3] 王仁乔, 李武阶.日本降水预报的客观订正及三峡区间面雨量的估算.空军气象学院学报, 1996, 17(2): 175-180. [4] 秦承平, 居志刚.清江和长江干支流域面雨量计算方法及其应用, 湖北气象, 1999, (4) : 16-18. http://www.cnki.com.cn/Article/CJFDTOTAL-HBQX199904005.htm [5] 孟遂珍, 彭治班. 流域平均降水量的一种算法∥新一代气象服务体系研究文集 (二). 北京: 气象出版社, 1999: 112-118. [6] 董官臣, 冶林茂.面雨量在气象预报中的应用.气象, 2000, 26(1): 9-13. http://kns.cnki.net/KCMS/detail/detail.aspx?dbcode=CJFQ&dbname=CJFD2000&filename=QXXX200001001&v=MTIwNTBSdEZ5cmdVTHpMTkRYVGRyRzRIdEhNcm85RlpZUjhlWDFMdXhZUzdEaDFUM3FUcldNMUZyQ1VSTDJmWk8= [7] 徐晶, 林建, 姚学祥, 等.七大江河流域面雨量计算方法及应用.气象, 2001, 27 (11): 13-16. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX200111003.htm [8] 周筱兰, 张礼平, 王仁乔.应用最优化订正法制作长江上游面雨量预报.气象, 2003, 29(3): 31-33. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX200303008.htm [9] 毕宝贵, 徐晶, 林建.面雨量计算方法及其在海河流域的应用.气象, 2003, 29(8): 39-42. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX200308009.htm [10] 张学文, 张家宝.新疆气象手册.北京:气象出版社, 2006: 215. [11] 林开平, 孙崇智, 郑凤琴, 等.丘陵地区面雨量计算方法及应用.气象, 2003, 29(10): 8-12. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX200310001.htm [12] 杨扬, 戚建国.数字卫星云图估算面雨量的应用试验.气象, 1995, 21(3): 35-39. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX503.007.htm [13] 杨扬.利用地理信息系统软件计算面雨量.水文, 1997, 6: 24-27. http://www.cnki.com.cn/Article/CJFDTOTAL-SWZZ706.004.htm [14] 林柄干, 张培昌.天气雷达测定区域降水量方法的改进与比较.南京气象学院学报, 1997, 20(3) : 334-346. http://www.cnki.com.cn/Article/CJFDTOTAL-NJQX703.007.htm [15] 熊秋芬, 胡江林, 夏军.神经网络方法在静止卫星多通道资料估算中的作用.气象, 2002, 28(9): 17-21. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX200209004.htm [16] 朱会义, 贾邵凤.降雨信息空间插值的不确定性分析.地理科学进展, 2004, 23(2): 34-42. http://www.cnki.com.cn/Article/CJFDTOTAL-DLKJ200402004.htm [17] 白美兰, 沈建国, 郝润全.地理信息技术在松嫩流域信息查询和面雨量监测中的应用.干旱区资源与环境, 2005, 19(30):51-54. http://www.cnki.com.cn/Article/CJFDTOTAL-GHZH200503009.htm [18] Hewitson B C, Crane R G. Gridded area-averaged daily precipitation via conditional interpolation. J Climate, 2005, 18(1):41-57. doi: 10.1175/JCLI3246.1 [19] Zhang Renhe. Relations of water vapor transports from Indian monsoon with those over East Asia and the summer rainfall in China. Adv Atmos Sci, 2001, 18:1005-1017.