基于GRACE重力卫星数据的黄河源区实际蒸发量估算

doi:10.7522/j.issn.1000-0240.2013.0016

冰川冻土 ›› 2013, Vol. 35 ›› Issue (1): 138-147.doi: 10.7522/j.issn.1000-0240.2013.0016

基于GRACE重力卫星数据的黄河源区实际蒸发量估算

许民^1,2, 叶柏生^1,2, 赵求东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. 中国科学院寒区旱区环境与工程研究所, 甘肃兰州 730000

收稿日期:2012-08-13 修回日期:2012-11-26 出版日期:2013-02-25 发布日期:2013-07-22
作者简介:许民(1984-),男,新疆沙湾人,2010年在兰州大学资源环境学院获硕士学位,现为中国科学院寒区旱区环境与工程研究所在读博士研究生,主要从事寒旱区水文和陆面过程方面的研究.E-mail:xumin@126.com
基金资助:
全球变化研究国家重大科学研究计划项目(2010CB951401); 国家自然科学基金项目 (41130638; 41201025; 41030527); 中国科学院寒区旱区环境与工程研究所青年人才基金项目(51Y251A61)资助

Estimation of the Real Evaporation in the Source Regions of the Yellow River Using GRACE Satellite Data

XU Min^1,2, YE Bai-sheng^1,2, ZHAO Qiu-dong²

1. State Key Laboratory of Cryophereic Science, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou Gansu 730000, China;
2. Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou Gansu 730000, China

Received:2012-08-13 Revised:2012-11-26 Online:2013-02-25 Published:2013-07-22

摘要/Abstract

摘要：

利用GRACE卫星数据反演得到黄河源区唐乃亥流域2003-2008年流域水储量变化, 结合同时间段黄河源区降雨及径流资料, 根据水量平衡方程, 估算流域逐月实际蒸发量. 结果表明: 估算的结果与20 cm蒸发皿观测值和SiB2模型模拟的结果具有较好的一致性和相关性. 黄河源区2003-2008年年平均实际蒸发量约为506.4 mm, 其中, 春季(3-5月)为130.9 mm, 约占全年的25.8%; 夏季(6-8月)为275.2 mm, 约占全年的54.3%; 秋季(9-11月) 为74.3 mm, 约占全年的14.7%; 冬季(12月至翌年2月)为26.2 mm, 约占全年的5.2%. 2003-2008年源区降水基本保持不变, 蒸发呈减少趋势, 径流略有增加, 径流峰值期提前, 黄河源区水储量增加速率为0.51 mm·month^-1, 相当于82.6×10⁴ m³·a^-1, 总增加水量约496.6×10⁴ m³. 降水平均增加速率为0.019 mm·month^-1, 水储量增加速率为0.51 mm·month^-1, 而蒸发的下降速率为0.52 mm·month^-1, 径流的增加速率为0.034 mm·month^-1. 因此, 在降水量变化不大的情况下, 蒸发的下降和冻土消融导致水储量的增加明显, 这也是引起地表径流增加的原因.

关键词: 黄河源区, GRACE, 水储量变化, 水量平衡方程, 实际蒸发量

Abstract:

The water storage change data from 2003 to 2008 in the source regions of the Yellow River is retrieved from GRACE satellite data. Furthermore, the monthly real evaporation in the source regions is estimated according to water balance equation by using runoff and precipitation data. It is found that they are consistent better and correlative with not only the observation with evaporation pan (20 cm), but also with the simulated result of SiB2 model. The annual average evaporation in Tangnag basin is nearly 506.4 mm, of which 130.9 mm in spring (Mar., Apr. and May), 275.2 mm in summer (June, July and Aug.), 74.3 mm in autumn (Sep., Oct. and Nov.) and 26.1mm in winter (Dec., Jan. and Feb.). From 2003 to 2008, precipitation had increased slightly and real evaporation had decreased obviously; precipitation had increased with a rate of 0.019 mm·month^-1, water storage had changed with a rate of 0.51 mm/month, while evaporation had decreased with a rate of 0.52 mm/month. During the study period, the water storage in the source regions of the Yellow River had increased about 496.6×10⁴ m³, equivalent to 82.6×10⁴ m³·a^-1. Precipitation had changed not so much. However, decline of evaporation and degradation of permafrost had led storage capacity increasing significantly and then surface runoff increasing.

Key words: source regions of the Yellow River, GRACE, water storage change, water balance equation, real evaporation

中图分类号:

P333.2

许民, 叶柏生, 赵求东. 基于GRACE重力卫星数据的黄河源区实际蒸发量估算[J]. 冰川冻土, 2013, 35(1): 138-147.

XU Min, YE Bai-sheng, ZHAO Qiu-dong. Estimation of the Real Evaporation in the Source Regions of the Yellow River Using GRACE Satellite Data[J]. JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY, 2013, 35(1): 138-147.

参考文献

[1] Milly P C D, Shmakin A B.Global modeling of land water and energy balances. Part Ⅰ: The Land Dynamics (LaD) model[J]. J. Hydrometeorology, 2002, 3: 283-299.

[2] Döll P, Kaspar F, Lehner B.A global hydrological model for driving water availability indicators: model tuning and validation[J]. J. Hydrol., 2003, 270: 105-134.

[3] Wang Yanjun, Jiang Tong, Xu Chongyu, et al. Trends of evapotranspiration in the Yangtze River Basin in 1961-2000[J]. Advances in climate change research, 2005, 1(3): 99-105. [王艳君, 姜彤, 许崇育, 等. 长江流域1961-2000年蒸发量变化趋势研究[J].气候变化研究进展, 2005, 1(3): 99-105.]

[4] Zhang Yinsheng, Yao Tandong, Pu Jianchen, et al. The feature of hydrological processes in the Dongkemadi River Basin, Tanggula Pass, Tibetan Plateau[J]. Journal of Glaciology and Geocryology, 1997, 19(3): 214-222. [张寅生, 姚檀栋, 蒲健辰, 等. 青藏高原唐古拉冬克玛底流域水文过程特征分析[J]. 冰川冻土, 1997, 19(3): 214-222.]

[5] Wang Yanjun, Jiang Tong, Liu Bo. Trends of estimated and simulated actual evaporation in the Yangtze River Basin[J]. Acta Geographic Sinica, 2010, 65(9): 1079-1088. [王艳君, 姜彤, 刘波.长江流域实际蒸发量的变化趋势[J]. 地理学报, 2010, 65(9): 1079-1088.]

[6] Wang Yanjun, Jiang Tong, Xu Chongyu. Spatial-temporal change of 20 cm pan evaporation over the Yangtze River basin[J]. Advances in Water Science, 2006, 17(6): 830-833. [王艳君, 姜彤, 许崇育.长江流域20 cm蒸发皿蒸发量的时空变化[J]. 水科学进展, 2006, 17(6): 830-833.]

[7] Wu Xianing, Hu Tiesong, Wang Xiugui, et al. Review of estimating and measuring regional evaporation[J]. Transactions of the CSAE, 2006, 22(10): 257-262. [武夏宁, 胡铁松, 王修贵. 区域蒸散发估算测定方法综述[J]. 农业工程学报, 2006, 22(10): 257-262.]

[8] Ohmura A, Wild M. Is the hydrological cycle accelerating? [J]. Science, 2002, 298: 1345-1346.

[9] Rodell M, Houser P R, Jambor U, et al.The global land data assimilation system [J]. Bull Am Meteorol Soc, 2004, 85(3): 381-394.

[10] Zhong M, Duan J B, Xu H Z, et al. Trend of China land water storage redistribution at medi-and large-spatial scales in recent five years by satellite gravity observations[J]. Chinese Sci Bull, 2009, 54(5): 816-821. [钟敏, 段建宾, 许厚泽, 等. 利用卫星重力观测研究近5年中国陆地水量中长空间尺度的变化趋势[J]. 科学通报, 2009, 54(9): 1290-1294.]

[11] Wahr J, Swenson S.Time variability of the Earth gravity field: hydrological and oceanic effects and their possible detection using GRACE[J]. J Geophys Res, 1998, 103(12): 30205-30229.

[12] Wahr J, Swenson S, Zlotnicki V, et al. Time-variable gravity from GRACE: First results [J]. Geophy Res Lett, 2004, 31, doi: 10.1029/2004GL019779.

[13] Tapley B D, Bettadpur S, Ries J C, et al. GRACE measurements of mass variability in the Earth system[J]. Science, 2004, 305: 503-505.

[14] Cazenave R A, Brunau O. Global time variations of hydrological signals from GRACE satellite gravimetry[J]. Geophys J Int, 2004, 158: 813-826.

[15] Velicogna I, Wahr J. Measurements of time-variable gravity show mass loss in Antarctica[J]. Science, 2006, 311: 1745-1756.

[16] Hu Xiaogong, Chen Jianli, Zhou Yonghong, et al. GRACE space gravity measurements to monitor the use of the Yangtze River seasonal changes in water storage [J]. Science in China (Ser. D), 2006, 36(3): 225-232. [胡小工, 陈剑利, 周永宏, 等. 利用GRACE空间重力测量监测长江流域水储量的季节性变化[J]. 中国科学(D辑), 2006, 36(3): 225-232.]

[17] Yang Yuande, E Dongchen, Chao Dingbo, et al.Seasonal and inter-annual change in land water storage from GRACE[J]. Chinese J Geophys, 2009, 52(12): 2987-2992. [杨元德, 鄂栋臣, 晁定波, 等.GRACE估算陆地水储量季节和年际变化[J]. 地球物理学报, 2009, 52(12): 2987-2992.]

[18] Ye Baisheng, Yang Daqing, Ding Yongjian, et al. A bias-corrected precipitation climatology for China[J]. Acta Geographic Sinica, 2007, 62(1): 3-13. [叶柏生, 杨大庆, 丁永建, 等. 中国降水观测误差分析及其修正[J].地理学报, 2007, 62(1): 3-13.]

[19] Ding Yongjian, Yang Daqing, Ye Baisheng, et al. Effects of bias correction on precipitation trend over China[J]. Journal of Geophysical Research, 2007, 112(D13), doi: 10.1029/2006JD007938.

[20] Xu Min, Wang Yan, Zhou Zhaoye, et al. Discussion of methods on spatial interpolation for monthly temperature data in Yangtze River basin[J]. Resources and Environment in the Yangtze Basin, 2012, 21(3): 327-334. [许民, 王雁, 周兆叶, 等. 长江流域逐月气温空间插值方法探讨[J]. 长江流域资源与环境, 2012, 21(3): 327-334.]

[21] Zhai Ning, Wang Zemin, E Dongchen. Investigation on Antarctic mass balance with GRACE [J]. Chinese Journal of Polar Research, 2009, 21(1): 43-47. [翟宁, 王泽民, 鄂栋臣. 基于GRACE反演南极物质平衡的研究[J]. 极地研究, 2009, 21(1): 43-47.]

[22] Rodell M, Houser P R, Jambor U, et al. The global land data assimilation system [J]. Bulletin of the American Meteorological Society, 2004, 85(3): 381-394.

[23] Yang Kun, Ye Baisheng, Zhou Degang, et al. Response of hydrological cycle to recent climate changes in the Tibetan Plateau[J].Climatic Change, 2011, 109(3-4): 517-534.

[24] Kinfu Habte Haile. Estimation of Terrestrial Water Storage in the Upper Reach of Yellow River [D]. Master Thesis, Enschede, Nederland: The Faculty of Geo-Information Science and Earth Observation University of Twent, 2011.

[25] Niu L, Ye B S, Li J, et al. Effect of permafrost degradation on hydrological processes in typical basins with varying permafrost coverage in Western China[J]. Sci China Earth Sci, 2011, 54(4): 615-624.

[26] Qiu Xinfa, Liu Changming, Zeng Yan. Changes of pan evaporation in the recent 40 years over the Yellow River Basin [J]. Journal of Natural Resource, 2003, 18: 437-442. [邱新法, 刘昌明, 曾燕.黄河流域近40年蒸发皿蒸发量的气候变化特征[J]. 自然资源学报, 2003, 18: 437-442.]

[27] Bouchet R J. Evapotranspiration reelet potentielle, Signification climatique[C]//Association Science Hydrology Process. Berkeley California Symposia Publication, 1963, 62: 134-142.

[28] Shi Chengxi(Shih Chenghsi), Niu Keyuon, Chen Tianzhu, et al. The study of pan coefficients of evaporation pans of water [J]. Sci Geo Sin, 1986, 6(4): 305-313. [施成熙, 牛克源, 陈天珠, 等. 水面蒸发器折算系数研究[J]. 地理科学1986, 6(4): 305-313.]

[29] Yang Zhengniang, Woo M K, Liu Xinren, et al. Alpine permafrost zone water balance and runoff characteristics[J].Science in China (Ser. D), 1996, 26(6): 567-573. [杨针娘, 胡鸣高, 刘新仁, 等. 高山冻土区水量平衡及地表径流特征[J].中国科学(D辑), 1996, 26(6): 567-573.]

[30] Zhao Lin, Wu Qingbai, Marchenko S S, et al. Thermal state of permafrost and active layer in Central Asia during the International Polar Year[J]. Permafrost and Periglacial Processes, 2010, 21: 198-207.

[31] Peng Wen, Gao Yanhong.A simulation of the energy and water cycles in seasonal freezing-thawing process on the Tibetan Plateau [J]. Journal of Glaciology and Geocryology, 2011, 33(2): 364-373. [彭雯, 高艳红. 青藏高原冻融过程中能量和水分循环的模拟研究[J]. 冰川冻土, 2011, 33(2): 364-373.]

[32] Gao Hongkai, He Xiaobo, Ye Baisheng, et al. The simulation of HBV hydrology model in the Dongkemadi River Basin, headwear of the Yangtze River[J]. Journal of Glaciology and Geocryology, 2011, 33(1): 171-181. [高红凯, 何晓波, 叶柏生, 等. 1955-2008年冬克玛底河流域冰川径流模拟研究[J]. 冰川冻土, 2011, 33(1): 171-181.]

基于GRACE重力卫星数据的黄河源区实际蒸发量估算

Estimation of the Real Evaporation in the Source Regions of the Yellow River Using GRACE Satellite Data

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