一种基于MODIS积雪产品的雪线高度提取方法

doi:10.7522/j.issn.1000-0240.2017.0030

冰川冻土 ›› 2017, Vol. 39 ›› Issue (2): 259-272.doi: 10.7522/j.issn.1000-0240.2017.0030

一种基于MODIS积雪产品的雪线高度提取方法

鲍伟佳^1,2, 刘时银^1,3, 吴坤鹏^1,2, 王荣军^1,2, 蒋宗立⁴

1. 中国科学院西北生态环境资源研究院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;
3. 云南大学国际河流与生态安全研究院, 云南昆明 650091;
4. 湖南科技大学煤炭资源清洁利用与矿山环境保护湖南省重点实验室, 湖南湘潭 411201

收稿日期:2016-12-16 修回日期:2017-02-16 出版日期:2017-04-25 发布日期:2017-07-08
通讯作者: 刘时银,E-mail:liusy@lzb.ac.cn E-mail:liusy@lzb.ac.cn
作者简介:鲍伟佳(1986-),男,安徽南陵人,2007年毕业于长春师范学院,现为中国科学院西北生态环境资源研究院在读博士研究生,从事冰川物质平衡遥感监测和模型模拟研究.E-mail:baowj@lzb.ac.cn
基金资助:
科技部基础性工作专项（2013FY111400）；中科院重点部署项目（KZZD-EW-12-1）；国家自然科学基金重点项目（41130641）；国家自然科学基金项目（41471067）资助

A method for extracting snow line altitude based on MODIS snow product

BAO Weijia^1,2, LIU Shiyin^1,3, WU Kunpeng^1,2, WANG Rongjun^1,2, JIANG Zongli⁴

1. State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China;
2. University of Chinese Academy of Sciences, Beijing 100049, China;
3. Institute of International Rivers and Eco-Security, Yunnan University, Kunming 650091, China;
4. Hunan Province Key Laboratory of Coal Resources Clean-Utilization and Mine Environment Protection, Hunan University of Science and Technology, Xiangtan 41120, Hunan, China

Received:2016-12-16 Revised:2017-02-16 Online:2017-04-25 Published:2017-07-08

摘要/Abstract

摘要： 冰川雪线高度的遥感提取对冰川物质平衡研究具有重要意义。提出一种基于晴空环境下积雪覆盖频率的雪线高度提取方法。使用MOD10A1积雪产品中的像元积雪面积比例数据，提取了2000/2001-2014/2015年间高亚洲地区冰川消融期末雪线高度。使用实测的冰川年物质平衡资料和气象格网数据对提取的雪线高度变化的可信度进行分析。研究表明：近15 a高亚洲雪线高度变化及趋势具有明显的东西差异，雪线高度变化幅度自青藏高原内部地区向四周呈增加趋势，西部大于东部。提取的冰川雪线高度变化与观测的年物质平衡序列具有很高的相关性，对物质平衡波动的平均解释率可高达75%；与气象要素（气温、降水）的年际变化的相关性也较高，约61.58%的格网冰川雪线高度变化可以由夏季气温和季节降水解释。而高亚洲各分区冰川雪线高度的波动规律也与大气环流背景分布一致。因此提取的雪线高度变化具有冰川学意义，可以进一步应用于冰川物质平衡估算及模拟研究中。

关键词: 高亚洲冰川, 雪线高度, MODIS积雪产品

Abstract: The snow line altitude extraction is very important for studying glacier mass balance. A method was presented to calculate the snow line altitude in mountain areas based on MOD10A1 snow product by using the snow cover frequency in the clear-sky days in hydrological years. The fractional snow cover data were used to class the snow line or above snow line pixels. In this paper, snow line altitudes of glaciers in High Mountain Asia at the end of ablation periods between 2000/2001 to 2014/2015 were extracted. The result shows that the extracted snow line attitude time series are very high correlated with the observed annual glacier mass balance series. 75% of mass balance change could be explained by snow line altitude variation. About 61.58% snow line altitude change has significant relationship with summer air temperature or seasonal precipitation in the 30 km grid scale. Finally, the sub-regional snow line altitude time series seems to illuminate that the snow line altitude in the whole High Mountain Asia has changed in recent 15 years. The snow line altitude change has associated with the distribution of atmospheric circulations in high Mountain Asia. The snow line altitude extraction method proposed here could be applied to research glaciers in the other mountains.

Key words: glaciers in High Mountain Asia, snow line altitude, MODIS snow cover product

中图分类号:

TP79

鲍伟佳, 刘时银, 吴坤鹏, 王荣军, 蒋宗立. 一种基于MODIS积雪产品的雪线高度提取方法[J]. 冰川冻土, 2017, 39(2): 259-272.

BAO Weijia, LIU Shiyin, WU Kunpeng, WANG Rongjun, JIANG Zongli. A method for extracting snow line altitude based on MODIS snow product[J]. JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY, 2017, 39(2): 259-272.

参考文献

[1] Yang Xingguo, Qin Dahe, Qin Xiang. Progress in the study of interaction between ice/snow and atmosphere[J]. Journal of Glaciology and Geocryology, 2012, 34(2): 392-402. [杨兴国, 秦大河, 秦翔. 冰川/积雪-大气相互作用研究进展［J]. 冰川冻土, 2012, 34(2): 392-402.］
[2] Shi Yafeng, Liu Shiyin. Estimation on the response of glaciers in China to the global warming in the 21st century[J]. Chinese Science Bulletin, 2000, 45(7): 668-672. [施雅风, 刘时银. 中国冰川对21世纪全球变暖响应的预估［J]. 科学通报, 2000, 45(4): 434-438.］
[3] Paterson W S B. The physics of glaciers [M]. 3rd ed. Oxford Pergamon, 1994: 26-32.
[4] Braithwaite R J. Can the mass balance of a glacier be estimated from its equilibrium line altitude[J]. Journal of Glaciology, 1984, 30(106): 364-368.
[5] Rabatel A, Bermejo A, Loarte E, et al. Can the snowline be used as an indicator of the equilibrium line and mass balance for glaciers in the outer tropics?[J]. Journal of Glaciology, 2012, 58(212): 1027-1036.
[6] Rabatel A, Letreguilly A, Dedieu J P, et al. Changes in glacier equilibrium-line altitude in the western Alps from 1984 to 2010: evaluation by remote sensing and modeling of the morpho-topographic and climate controls[J]. Cryosphere, 2013, 7(5): 1455-1471.
[7] Huang Lei, Li Zhen, Tian Bangsen, et al. Classification and snow line detection for glacial areas using the polarimetric SAR image[J]. Remote Sensing of Environment, 2011, 115(7): 1721-1732.
[8] Huang Lei, Li Zhen. Comparison of different methods in glacier snow line detection using the polarimetric SAR image[C]//Geoscience and Remote Sensing Symposium (IGARSS), 2012 IEEE International. Ieee, 2012: 4426-4429.
[9] Rabatel A, Dedieu J P, Thibert E, et al. 25 years (1981-2005) of equilibrium-line altitude and mass-balance reconstruction on Glacier Blanc, French Alps, using remote-sensing methods and meteorological data[J]. Journal of Glaciology, 2008, 54(185): 307-314.
[10] Guo Zhongming, Wang Ninglian, Kehrwald N M, et al. Temporal and spatial changes in Western Himalayan firn line altitudes from 1998 to 2009[J]. Global and Planetary Change, 2014, 118: 97-105.
[11] Hall D K, Riggs G A. Accuracy assessment of the MODIS snow products[J]. Hydrological Processes, 2007, 21(12): 1534-1547.
[12] Paudel K P, Andersen P. Monitoring snow cover variability in an agropastoral area in the Trans Himalayan region of Nepal using MODIS data with improved cloud removal methodology[J]. Remote Sensing of Environment, 2011, 115(5): 1234-1246.
[13] Dietz A J, Kuenzer C, Conrad C. Snow-cover variability in central Asia between 2000 and 2011 derived from improved MODIS daily snow-cover products[J]. International Journal of Remote Sensing, 2013, 34(11): 3879-3902.
[14] Tekeli A E, Akyurek Z, Sorman A A, et al. Using MODIS snow cover maps in modeling snowmelt runoff process in the eastern part of Turkey[J]. Remote Sensing of Environment, 2005, 97(2): 216-230.
[15] Immerzeel W W, Droogers P, De Jong S M, et al. Large-scale monitoring of snow cover and runoff simulation in Himalayan river basins using remote sensing[J]. Remote Sensing of Environment, 2009, 113(1): 40-49.
[16] Konz M, Finger D, Buergi C, et al. Calibration of a distributed hydrological model for simulations of remote glacierized Himalayan catchments using MODIS snow cover data[J]. Global Change: Facing Risks and Threats to Water Resources, 2010, 340: 465-473.
[17] Gafurov A, Bárdossy A. Cloud removal methodology from MODIS snow cover product[J]. Hydrology and Earth System Sciences, 2009, 13(7): 1361.
[18] Wang Xianmei, Xie Hongjie. New methods for studying the spatiotemporal variation of snow cover based on combination products of MODIS Terra and Aqua[J]. Journal of Hydrology, 2009, 371(1): 192-200.
[19] Tang Zhiguang, Wang Jian, Li Hongyi, et al. Accuracy validation and cloud obscuration removal of MODIS fractional snow cover products over Tibetan[J]. Remote Sensing Technology and Application, 2013, 28(3): 423-430. [唐志光, 王建, 李弘毅, 等. 青藏高原MODIS积雪面积比例产品的精度验证与去云研究［J]. 遥感技术与应用, 2013, 28(3): 423-430.］
[20] Xie Zichu, Zhou Zaigen, Li Qiaoyuan, et al. Progress and prospects of mass balance characteristic and responding to global change of glacier system in High Asia[J]. Advances in Earth Science, 2009, 24(10): 1065-1072. [谢自楚, 周宰根, 李巧媛, 等. 高亚洲冰川系统物质平衡特征及其对全球变化响应研究进展与展望［J]. 地球科学进展, 2009, 24(10): 1065-1072.］
[21] Arendt A, Bliss A, Bolch T, et al. Randolph glacier inventory: a dataset of global glacier outlines: version 5.0[DB/OL]. Boulder Colorado, USA, 2015[2015-07-20]. http://www.glims.org/RGI/index.html.
[22] Xie Zichu. High Asia glacier mass balance reaserch[J]. Bulletin of Chinese Academy of Sciences, 1994, 3: 5-248. [谢自楚. 高亚洲冰川物质平衡研究［J]. 中国科学院院刊, 1994, 3: 5-248.］
[23] Yao Tandong, Thompson L, Yang Wei, et al. Different glacier status with atmospheric circulations in Tibetan Plateau and surroundings[J]. Nature Climate Change, 2012, 2(9): 663-667.
[24] Xie Zichu,Ding Liangfu. Glacier mass balance in High-Asia and its response to climatic change[J]. Journal of Glaciology and Geocryology, 1996, 18(S1): 4-11. [谢自楚, 丁良福. 高亚洲冰川物质平衡及其对气候变化的响应研究［J]. 冰川冻土, 1996, 18(S1): 4-11.］
[25] Sakai A, Nuimura T, Fujita K, et al. Climate regime of Asian glaciers revealed by GAMDAM glacier inventory[J]. Cryosphere, 2015, 9(3): 865-880.
[26] Liu Shiyin, Ding Yongjian, Ye Baisheng, et al. Regional characteristics of glacier mass balance variations in High Asia[J]. Journal of Glaciology and Geocryology, 2000, 22(2): 97-105. [刘时银, 丁永建, 叶佰生, et al. 高亚洲地区冰川物质平衡变化特征研究［J]. 冰川冻土, 2000, 22(2): 97-105.］
[27] Yao Tandong, Liu Shiyin, Pu Jianchen, et al. Recent glacial retreat in High Asia in China and its impact on water resource in Northwest China[J]. Science in China: Series D Earth Sciences, 2004, 47(12): 1065-1075.. [姚檀栋, 刘时银, 蒲健辰, 等. 高亚洲冰川的近期退缩及其对西北水资源的影响［J]. 中国科学: D辑地球科学, 2004, 34(6): 535-543.］
[28] Bolch T, Kulkarni A, Kaab A, et al. The State and Fate of Himalayan Glaciers[J]. Science, 2012, 336(6079): 310-314.
[29] Gardner A S, Moholdt G, Cogley J G, et al. A reconciled estimate of glacier contributions to sea level rise: 2003 to 2009[J]. science, 2013, 340(6134): 852-857.
[30] Gardelle J, Berthier E, Arnaud Y, et al. Region-wide glacier mass balances over the Pamir-Karakoram-Himalaya during 1999-2011[J]. Cryosphere, 2013, 7(4): 1263-1286.
[31] WGMS. Fluctuations of glaciers database[EB/OL]. Zurich, Switzerland: World Glacier Monitoring Service (WGMS), 2016[2015-08-31]. http://dx.doi.org/10.5904/wgms-fog-2016-08.
[32] Hall D K, Riggs G A, Salomonson V V. Development of methods for mapping global snow cover using moderate resolution imaging spectroradiometer data[J]. Remote sensing of Environment, 1995, 54(2): 127-140.
[33] Hall D K, Riggs G A, Salomonson V V, et al. MODIS snow-cover products[J]. Remote Sensing of Environment, 2002, 83(1/2): 181-194.
[34] Ault T W, Czajkowski K P, Benko T, et al. Validation of the MODIS snow product and cloud mask using student and NWS cooperative station observations in the Lower Great Lakes Region[J]. Remote Sensing of Environment, 2006, 105(4): 341-353.
[35] Wang Xianwei, Xie Hongjie, Liang Tiangang, et al. Comparison and validation of MODIS standard and new combination of Terra and Aqua snow cover products in northern Xinjiang, China[J]. Hydrological Processes, 2009, 23(3): 419-429.
[36] Salomonson V V, Appel I. Estimating fractional snow cover from MODIS using the normalized difference snow index[J]. Remote Sensing of Environment, 2004, 89(3): 351-360.
[37] Salomonson V V, Appel I. Development of the Aqua MODIS NDSI fractional snow cover algorithm and validation results[J]. IEEE Transactions on Geoscience and Remote Sensing, 2006, 44(7): 1747-1756.
[38] Rittger K, Painter T H, Dozier J. Assessment of methods for mapping snow cover from MODIS[J]. Advances in Water Resources, 2013, 51: 367-380.
[39] Nuimura T, Sakai A, Taniguchi K, et al. The GAMDAM glacier inventory: a quality-controlled inventory of Asian glaciers[J]. The Cryosphere, 2015, 9(3): 849-864.
[40] Guo Wanqin, Liu Shiyin, Yao Xiaojun, et al. The second glacier inventory dataset of China (Version 1.0)[J]. Lanzhou: Cold and Arid Regions Science Data Center at Lanzhou, China, 2014. DOI: 10.3972/glacier.001.2013.db.
[41] Liu Shiyin, Yao Xiaojun, Guo Wangqin, et al. The contemporary glaciers in China based on the Second Chinese Glacier Inventory[J]. Progress in Geography, 2015, 70(1): 3-16. [刘时银, 姚晓军, 郭万钦, 等. 基于第二次冰川编目的中国冰川现状［J]. 地理学报, 2015, 70(1): 3-16.］
[42] Sun G, Ranson K, Kharuk V, et al. Validation of surface height from shuttle radar topography mission using shuttle laser altimeter[J]. Remote Sensing of Environment, 2003, 88(4): 401-411.
[43] Moelg T, Maussion F, Scherer D. Mid-latitude westerlies as a driver of glacier variability in monsoonal High Asia[J]. Nature Climate Change, 2014, 4(1): 68-73.
[44] Maussion F, Scherer D, Moelg T, et al. Precipitation seasonality and variability over the Tibetan Plateau as resolved by the High Asia reanalysis[J]. Journal of Climate, 2014, 27(5): 1910-1927.
[45] Mölg T, Maussion F, Scherer D. Mid-latitude westerlies as a driver of glacier variability in monsoonal High Asia[J]. Nature Climate Change, 2013, 4(1): 68-73.
[46] Molg T, Maussion F, Yang W, et al. The footprint of Asian monsoon dynamics in the mass and energy balance of a Tibetan glacier[J]. Cryosphere, 2012, 6(6): 1445-1461.
[47] Tang Zhiguang, Wang Jian, Ling Ji, et al. Monitoring of snowline altitude over the Tibetan Plateau based on MODIS data[J]. Remote Sensing Technology and Application, 2015, 30(4): 767-744. [唐志光, 王建, 梁继, 等. 基于MODIS的青藏高原雪线高度遥感监测［J]. 遥感技术与应用, 2015, 30(4): 767-774.］
[48] Liu Chaohai, Shi Yafeng, Wang Zongtai, et al. Glacier resources and their distributive characteristics in China: a review on Chinese Glacier Inventory[J]. Journal of Glaciology and Geocryology, 2000, 22(2): 106-112. [刘潮海, 施雅风, 王宗太, 等. 中国冰川资源及其分布特征: 中国冰川目录编制完成［J]. 冰川冻土, 2000, 22(2): 106-112.］
[49] Li Zhongqin, Shen Yongping, Wang Feiteng, et al. Response of glacier melting to climate change: take Vrümqi Glacier No.1 as an example[J]. Journal of Glaciology and Geocryology, 2007, 29(3): 5-14. [李忠勤, 沈永平, 王飞腾, 等. 冰川消融对气候变化的响应: 以乌鲁木齐河源1号冰川为例［J]. 冰川冻土, 2007, 29(3): 5-14.］
[50] Liu Shiyin, Ding Yongjian, Wang Ninglian, et al. Mass balance sensitivity to climate change of Glacier No.1 at the Ürümqi River head, Tianshan Mts.[J]. Journal of Glaciology and Geocryology, 1998, 20(1): 9-13. [刘时银, 丁永建, 王宁练, 等. 天山乌鲁木齐河源1号冰川物质平衡对气候变化的敏感性研究［J]. 冰川冻土, 1998, 20(1): 9-13.］
[51] Wagnon P, Vincent C, Arnaud Y, et al. Seasonal and annual mass balances of Mera and Pokalde glaciers (Nepal Himalaya) since 2007[J]. Cryosphere, 2013, 7(6): 1769-1786.
[52] Dobhal D P, Mehta M, Srivastava D. Influence of debris cover on terminus retreat and mass changes of Chorabari Glacier, Garhwal region, central Himalaya, India[J]. Journal of Glaciology, 2013, 59(217): 961-971.
[53] Hewitt K. The Karakoram anomaly? Glacier expansion and the‘elevation effect,’ Karakoram Himalaya[J]. Mountain Research and Development, 2005, 25(4): 332-340.

一种基于MODIS积雪产品的雪线高度提取方法

A method for extracting snow line altitude based on MODIS snow product

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