TRMM多卫星降水数据在黑河流域的验证与应用

doi:10.7522/j.issn.1000-0240.2013.0037

冰川冻土 ›› 2013, Vol. 35 ›› Issue (2): 310-319.doi: 10.7522/j.issn.1000-0240.2013.0037

TRMM多卫星降水数据在黑河流域的验证与应用

吴雪娇^1,2, 杨梅学¹, 吴洪波^1,2, 吴玉伟^1,2, 王学佳^1,2

1. 中国科学院寒区旱区环境与工程研究所冰冻圈科学国家重点实验室, 甘肃兰州 730000;
2. 中国科学院大学, 北京 100049

收稿日期:2012-08-24 修回日期:2013-01-25 出版日期:2013-04-25 发布日期:2013-05-14
作者简介:吴雪娇(1986-), 女, 黑龙江五大连池人, 2012年在中国科学院寒区旱区环境与工程研究所获硕士学位, 现为在读博士研究生, 主要从事寒区旱区遥感与地理信息系统应用研究. E-mail:wxjiao608@126.com
基金资助:
全球变化研究国家重大科学研究计划项目(2010CB951404); 国家自然科学基金项目(40930526; 41190084; 41201063); 中国科学院"百人计划"项目(29O827B11)资助

Verifying and Applying the TRMM TMPA in Heihe River Basin

WU Xue-jiao^1,2, YANG Mei-xue¹, WU Hong-bo^1,2, WU Yu-wei^1,2, WANG Xue-jia^1,2

1. State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and EngineeringResearch Institute, Chinese Academy of Sciences, Lanzhou Gansu 730000, China;
2. University of Chinese Academy of Sciences, Beijing 100049, China

Received:2012-08-24 Revised:2013-01-25 Online:2013-04-25 Published:2013-05-14

摘要/Abstract

摘要：

利用黑河流域9个气象台站降水数据, 在不同时间尺度和空间分布上分析了2008-2011年TRMM多卫星降水数据(TMPA 3B43)在黑河流域的适用性.结果表明: 用TMPA估测的年降水量在黑河流域平均高估27.3%, 对上游降水量大的山区估测相对好于降水稀少的黑河下游地区; TMPA与气象站降水量的拟合优度夏季(R²=0.851)高于冬季(R²=0.332); TMPA可以较好反映各测站降水量年变化、月变化趋势, 用TMPA估测的黑河流域平均年降水量变化趋势为30 mm·(10 a)^-1. 黑河流域年降水量体现出随海拔高度的递增规律(11.1 mm·(100 m)^-1)、从东向西降水量逐渐减少的分布以及最大降水高度带出现在上游偏东地区(海拔2 800~4 900 m).

关键词: 多卫星降水数据, 黑河, 祁连山, 时空变化

Abstract:

The Tropical Rainfall Measuring Mission (TRMM) Multi-Satellite Precipitation Analysis (TMPA) 3B43 product is evaluated using the gauge precipitations from 9 weather stations in Heihe River basin at different time steps and spatial distribution. It is found that TMPA-3B43 performing result at time step and spatial scale is not so satisfactory. Regional average annual precipitation evaluated by TMPA is overvalued by 27.3%. At the same temporal resolution, in the humid region, such as the upstream of the Heihe River, TMPA performs better than that in the arid regiones, such as downstream of the river. Specially, during summer the overvalued precipitation is obvious in the downstream of the river. The goodness of fit between TMPA precipitation and observed precipitation is better in summer (R²=0.851) than in winter (R²=0.332). TMPA can express annual and month variation trends of precipitation well. Regional average linear trends of annual mean precipitation is estimated to be 30 mm·(10a)^-1 from TMPA. In addition, TMPA estimated data can express the spatial distribution of precipitation in the basin. Annual precipitation increases with height with a rate of 11.1 mm·(100m^-1). Precipitation decreases from east to west and the zone of maximum precipitation lies between 2800 to 4 900 m a.s.l.

Key words: Multi-satellite Precipitation Analysis (TMPA), Heihe River basin, Qilian Mountains, temporal and spatial variation

中图分类号:

P426.6

吴雪娇, 杨梅学, 吴洪波, 吴玉伟, 王学佳. TRMM多卫星降水数据在黑河流域的验证与应用[J]. 冰川冻土, 2013, 35(2): 310-319.

WU Xue-jiao, YANG Mei-xue, WU Hong-bo, WU Yu-wei, WANG Xue-jia. Verifying and Applying the TRMM TMPA in Heihe River Basin[J]. JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY, 2013, 35(2): 310-319.

参考文献

[1] Su F, Hong Y, Lettenmaier D P. Evaluation of TRMM Multisatellite Precipitation Analysis (TMPA) and its utility in hydrologic prediction in the La Plata Basin[J]. Journal of Hydrometeorology, 2008, 9(4): 622-640.

[2] Wang Ninglian, He Jianqiao, Jiang Xi, et al.Study on the zone of maximum precipitation in the north slopes of the Central Qilian Mountains[J]. Journal of Glaciology and Geocryology, 2009, 31(3): 395-403. [王宁练, 贺建桥, 蒋熹, 等. 祁连山中段北坡最大降水高度带观测与研究[J]. 冰川冻土, 2009, 31(3): 395-403.]

[3] Xu Juanjuan, Wang Keli, Jiang Hao, et al.A numerical simulation of the effects of westerly and monsoon on precipitation in the Heihe River basin[J]. Journal of Glaciology and Geocryology, 2010, 32(3): 489-496. [徐娟娟, 王可丽, 江灏, 等. 西风与季风扰动对黑河流域降水影响的数值模拟[J]. 冰川冻土, 2010, 32(3): 489-496.]

[4] Zhang Kai, Wang Runyuan, Han Haitao, et al. Hydrological and water resources effects under climate change in Heihe River basin[J]. Resources Science, 2007, 29(1): 77-83. [张凯, 王润元, 韩海涛, 等. 黑河流域气候变化的水文水资源效应[J]. 资源科学, 2007, 29(1): 77-83.]

[5] Wang Ninglian, Zhang Shibiao, He Jianqiao, et al.Tracing the major source area of the mountainous runoff generation of the Heihe River in northwest China using stable isotope technique[J]. Chinese Science Bulletin, 2009, 54(16): 2751-2757. [王宁练, 张世彪, 贺建桥, 等. 祁连山中段黑河上游山区地表径流水资源主要形成区域的同位素示踪研究[J]. 科学通报, 2009, 54(15): 2148-2152.]

[6] Xiao Shengchun, Xiao Honglang, Lan Yongchao, et al.Water issues and integrated water resource management in Heihe River Basin in recent 50 years[J]. Journal of Desert Research, 2011, 31(2): 529-535. [肖生春, 肖洪浪, 蓝永超, 等. 近50 a来黑河流域水资源问题与流域集成管理[J]. 中国沙漠, 2011, 31(2): 529-535.]

[7] Zhang Huawei, Lu Anxin, Wang Lihong, et al. Glacier change in the Shulenan Mountain monitored by remote sensing[J]. Journal of Glaciology and Geocryology, 2011, 33(1): 8-13. [张华伟, 鲁安新, 王丽红, 等. 祁连山疏勒南山地区冰川变化的遥感研究[J]. 冰川冻土, 2011, 33(1): 8-13.]

[8] Chen Qian, Chen Tianyu, Zhang Yixuan. Analyses of energy field characteristics and precipitation in Qilian Mountains[J]. Journal of Glaciology and Geocryology, 2011, 33(5): 1046-1054. [陈乾, 陈添宇, 张逸轩. 祁连山区能量场特征与降水分布的关系分析[J]. 冰川冻土, 2011, 33(5): 1046-1054.]

[9] Liu Junfeng, Chen Rensheng, Han Chuntan, et al. Evaluating TRMM multi-satellite precipitation analysis using gauge precipitation and MODIS snow-cover products[J]. Advances in Water Science, 2010, 21(3): 343-348. [刘俊峰, 陈仁升, 韩春坛, 等. 多卫星遥感降水数据精度评价[J]. 水科学进展, 2010, 21(3): 343-348.]

[10] Feidas H. Validation of satellite rainfall products over Greece[J]. Theoretical and Applied Climatology, 2010, 99(1-2): 193-216.

[11] Nair S, Srinivasan G, Nemani R. Evaluation of multi-satellite TRMM derived rainfall estimates over a western state of India[J]. Journal of the Meteorological Society of Japan, Ser. II, 2009, 87(6): 927-939.

[12] Romilly T, Gebremichael M. Evaluation of satellite rainfall estimates over Ethiopian river basins[J]. Hydrology and Earth System Sciences, 2011, 15(5): 1505-1514.

[13] Huffman G J, Adler R F, Bolvin D T, et al. The TRMM multi-satellite precipitation analysis (TMPA)[C]//Gebremichael M, Hossain F. Satellite Rainfall Applications for Surface Hydrology. Springer Netherlands, 2010: 3-22.

[14] Zeng H, Li L, Li J. The evaluation of TRMM Multisatellite Precipitation Analysis (TMPA) in drought monitoring in the Lancang River Basin[J]. Journal of Geographical Sciences, 2012, 22(2): 273-282.

[15] Kummerow C, Simpson J, Thiele O,et al. The status of the Tropical Rainfall Measuring Mission (TRMM) after two years in orbit[J]. Journal of Applied Meteorology, 2000, 39(12): 1965-1982.

[16] Fu R, Hu L, Gu G J, et al. A comparison study of summer-time synoptic-scale waves in South China and the Yangtze River basin using the TRMM Multi-Satellite Precipitation Analysis daily product[J]. Science in China Series D: Earth Sciences, 2008, 51(1): 114-122. [付容, 胡亮, 谷国军, 等. 利用TRMM降水资料对华南和长江流域夏季天气尺度波的对比分析. 中国科学(D辑): 地球科学, 2007, 37(9): 1252-1259.]

[17] Du Jun, Ma Yucai. Climatic trend of rainfall over Tibetan Plateau from 1971 to 2000[J]. Acta Geographic Sinica, 2004, 59(3):375-382. [杜军, 马玉才. 西藏高原降水变化趋势的气候分析[J]. 地理学报, 2004, 59(3): 375-382.]

[18] Huffman G J, Bolvin D T, Nelkin E J, et al. The TRMM Multisatellite Precipitation Analysis (TMPA): Quasi-global, multiyear, combined-sensor precipitation estimates at fine scales[J]. Journal of Hydrometeorology, 2007, 8(1): 38-55.

[19] Ebert E E. Satellite vs. model rainfall-Which one to use?[C]//Proceedings of the 5th International Scientific Conference on the Global Energy and Water Cycle.Costa Mesa, California, USA: Global Energy and Water Cycle Experiment & World Climate Research Programme & United States National Oceanic and Atmospheric Administration & Office of Global Programs, June 20-24, 2005.

[20] Huffman G J, Adler R F, Arkin P, et al. The Global Precipitation Climatology Project (GPCP) combined precipitation dataset[J]. Bulletin of the American Meteorological Society, 1997, 78(1): 5-20.

[21] Katsanos D, Lagouvardos K, Kotroni V, et al. Statistical evaluation of MPA-RT high-resolution precipitation estimates from satellite platforms over the central and eastern Mediterranean[J]. Geophysical Research Letters, 2004, 31(6), doi: 10.1029/2003GL019142.

[22] Tang Maocang. The distribution of precipitation in Mountain Qilian (Nanshan)[J]. Acta Geographic Sinica, 1985, 40(4): 323-332. [汤懋苍. 祁连山区降水的地理分布特征[J]. 地理学报, 1985, 40(4): 323-332.]

[23] Ding Yongjian, Ye Baisheng, Zhou Wenjuan. Temporal and spatial precipitation distribution in the Heihe Catchment, northwest China, during the past 40 a[J]. Journal of Glaciology and Geocryology, 1999, 21(1): 42-48. [丁永建, 叶柏生, 周文娟. 黑河流域过去40 a来降水时空分布特征[J]. 冰川冻土, 1999, 21(1): 42-48.]

[24] Li Yanying, Zhang Qiang, Xu Xia, et al.Relationship between precipitation and terrain over the Qilian Mountains and their ambient areas[J]. Journal of Glaciology and Geocryology, 2010, 32(1): 52-61. [李岩瑛, 张强, 许霞, 等. 祁连山及周边地区降水与地形的关系[J]. 冰川冻土, 2010, 32(1): 52-61.]

[25] Zhang Qiang, Zhang Jie, Sun Guowu, et al. Research on atmospheric water-vapor distribution over Qilianshan Mountains[J]. Acta Meteorologica Sinica, 2007, 65(4): 633-643. [张强, 张杰, 孙国武, 等. 祁连山山区空中水汽分布特征研究[J]. 气象学报, 2007, 65(4): 633-643.]

TRMM多卫星降水数据在黑河流域的验证与应用

Verifying and Applying the TRMM TMPA in Heihe River Basin

PDF (PC)

赞

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

Metrics

本文评价

推荐阅读 0

[1]	路倩, 李宝富, 王志慧, 孙佳瑶, 仝天. 1979-2014年东北地区雪深时空变化与大气环流的关系[J]. 冰川冻土, 2018, 40(5): 907-915.
[2]	任媛, 刘普幸. 基于EVI和MNDWI指数的石羊河流域水体、植被时空变化特征[J]. 冰川冻土, 2018, 40(4): 853-861.
[3]	高雅芳, 王雷, 杜海波, 吴正方, 杨岳, 郭湘宇, 李思其. 长白山苔原带土壤温度与肥力随海拔的变化特征[J]. 冰川冻土, 2018, 40(4): 702-714.
[4]	梁鹏斌, 李忠勤, 张慧, 王飞腾, 牟建新, 何海迪. 1984-2016年全球参照冰川物质平衡时空变化特征[J]. 冰川冻土, 2018, 40(3): 415-425.
[5]	马素辉, 牟翠翠, 郭红, 张现凯, 栗泽苑, 张廷军. 祁连山黑河上游多年冻土区不同植被类型土壤有机碳密度分布特征[J]. 冰川冻土, 2018, 40(3): 426-433.
[6]	韩涛, 王大为, 李丽丽. FY-3A/MERSI积雪制图中NDSI指标建立及积雪判识模型研究——以祁连山区为例[J]. 冰川冻土, 2018, 40(3): 511-527.
[7]	苏芳, 尚海洋, 丁杨. 水足迹视角下低水消费模式研究——以黑河流域张掖市居民消费为例[J]. 冰川冻土, 2018, 40(3): 625-633.
[8]	高思如, 曾文钊, 吴青柏, 蒋观利, 张中琼. 1990-2014年西藏季节冻土最大冻结深度的时空变化[J]. 冰川冻土, 2018, 40(2): 223-230.
[9]	陈惠雄, 徐菲菲, 王晓鹏. 水资源管理制度超模博弈分析——以钱塘江与黑河为例[J]. 冰川冻土, 2017, 39(5): 1089-1097.
[10]	王玥彤, 李栋梁. 中国西南地区冻雨灾害特征分析与评估[J]. 冰川冻土, 2017, 39(5): 967-978.
[11]	蒋友严, 杜文涛, 黄进, 赵慧珍, 王成福. 2000-2015年祁连山植被变化分析[J]. 冰川冻土, 2017, 39(5): 1130-1136.
[12]	唐霞, 张志强. 基于文献记录的黑河流域历史时期旱涝特征分析[J]. 冰川冻土, 2017, 39(3): 490-497.
[13]	马晓华, 赵景波, 温震军. 鄂尔多斯高原西南部清代霜雪灾害研究[J]. 冰川冻土, 2017, 39(3): 498-504.
[14]	冯亚伟, 孙自永, 补建伟, 蔡鹤生. 祁连山黑河源区八一冰川-黄藏寺段河水水文地球化学特征[J]. 冰川冻土, 2017, 39(3): 680-687.
[15]	王涛, 高峰, 王宝, 王鹏龙, 王勤花, 宋华龙, 尹常亮. 祁连山生态保护与修复的现状问题与建议[J]. 冰川冻土, 2017, 39(2): 229-234.