木孜塔格峰地区冰川反照率时空变化及其影响因素研究

doi:10.12118/j.issn.1000-6060.2024.776

摘要/Abstract

摘要：

冰川反照率是影响冰川融化速度和环境变化的关键因子。采用高空间分辨率的Landsat OLI影像和高时间分辨率的MOD10A1反照率产品，开展了2015—2020年木孜塔格峰地区冰川反照率时空变化特征以及影响因素研究。结果表明：（1） Landsat OLI和MOD10A1反照率两者结果随时间变化的趋势较为一致，具有较高的相关性，决定系数（R²）为0.92。（2）在年际变化上，夏季反照率最低，秋季初期反照率较高。冬春季降雪次数减少，冰川表面积雪密实化，反照率随之减小。（3）在空间变化上，随着海拔升高，冰川表面反照率逐渐升高，呈指数函数关系（消融区和积累区的R²分别为0.23和0.25）。（4）气温和降水是影响冰川反照率的关键因素，气温升高和降雪减少会导致反照率降低。地形对冰川反照率有显著影响，坡度较缓的冰川表面反照率较高，坡度较陡的冰川表面反照率较低。研究结果为理解木孜塔格峰地区冰川变化机制和预测未来气候变化提供了科学依据。

关键词: 冰川反照率, 时空变化, Landsat OLI, MOD10A1, 木孜塔格冰川

Abstract:

Glacier albedo is a key factor influencing the rate of glacier melting and associated environmental changes. In this study, Landsat OLI images with high spatial resolution and MOD10A1 albedo products with high temporal resolution were used to analyze the spatiotemporal variations of glacier albedo and its influencing factors in the Muz Tag Peak area, Xinjiang, China from 2015 to 2020. The results show that: (1) The albedo values derived from Landsat OLI and MOD10A1 are highly consistent, with a strong correlation (R²=0.92). (2) Seasonally, the lowest albedo occurs in summer, while higher values are observed in early autumn. In winter and spring, reduced snowfall and densification of surface snow lead to decreasing albedo. (3) Spatially, glacier surface albedo increases with elevation, following an exponential relationship (R²=0.23 in the ablation area and 0.25 in the accumulation area). (4) Air temperature and precipitation are the primary factors affecting glacier albedo, as higher temperatures and reduced snowfall result in lower albedo. Topography also exerts a significant effect, with gentler slopes exhibiting lower albedo and steeper slopes showing higher albedo. This study provides a scientific basis for understanding glacier change mechanisms in the Muz Tag Peak area and for predicting future climate change.

Key words: glacial albedo, spatio-temporal variation, Landsat OLI, MOD10A1, Muz Tag Glacier

张玉娇, 怀保娟, 王圣杰, 车彦军, 张明军. 木孜塔格峰地区冰川反照率时空变化及其影响因素研究[J]. 干旱区地理, 2025, 48(10): 1760-1770.

ZHANG Yujiao, HUAI Baojuan, WANG Shengjie, CHE Yanjun, ZHANG Mingjun. Spatio-temporal variation of glacial albedo and its influencing factors in the Muz Tag Peak area[J]. Arid Land Geography, 2025, 48(10): 1760-1770.

图/表 11

图1

表1

表2

图2

图3

图4

图5

图6

图7

图8

图9

参考文献 32

[1]	车彦军, 陈丽花, 谷来磊, 等. 东昆仑木孜塔格峰地区冰湖演变与冰川物质亏损[J]. 冰川冻土, 2023, 45(4): 1254-1265. doi: 10.7522/j.issn.1000-0240.2023.0096
	[Che Yanjun, Chen Lihua, Gu Lailei, et al. Evolution of glacial lakes and glacier mass loss in Ulugh Muztagh area of eastern Kunlun Mountains[J]. Journal of Glaciology and Geocryology, 2023, 45(4): 1254-1265.] doi: 10.7522/j.issn.1000-0240.2023.0096
[2]	Bhattacharya A, Bolch T, Mukherjee K, et al. High Mountain Asian glacier response to climate revealed by multi-temporal satellite observations since the 1960s[J]. Nature Communications, 2021, 12(1): 4133, doi: 10.1038/s41467-021-24180-y.
[3]	Reijmer C H, Knap W H, Oerlemans J, et al. The surface albedo of the Vatnajökull Ice Cap, Iceland: A comparison between satellite-derived and ground-based measurements[J]. Boundary-layer Meteorology, 1999, 92: 123-143.
[4]	岳晓英, 李忠勤, 王飞腾, 等. 天山乌鲁木齐河源1号冰川消融期反照率特征[J]. 冰川冻土, 2021, 43(5): 1412-1423. doi: 10.7522/j.issn.1000-0240.2021.0097
	[Yue Xiaoying, Li Zhongqin, Wang Feiteng, et al. The characteristics of surface albedo on the Urumqi Glacier No.1 during the ablation season in eastern Tien Shan[J]. Journal of Glaciology and Geocryology, 2021, 43(5): 1412-1423.] doi: 10.7522/j.issn.1000-0240.2021.0097
[5]	Oerlemans J, Knap W H. A 1 year record of global radiation and albedo in the ablation zone of Morteratschgletscher, Switzerland[J]. Journal of Glaciology, 1998, 44(147): 231-238.
[6]	廖虹怡, 柳林. 利用Landsat8分析冬克玛底冰川表面反照率时空变化[J]. 测绘地理信息, 2024, 49(3): 19-24.
	[Liao Hongyi, Liu Lin. Temporal and spatial variation of surface albedo of Dongkemadi Glacier based on Landsat8[J]. Journal of Geomatics, 2024, 49(3): 19-24.]
[7]	Yang W, Guo X F, Yao T D, et al. Summertime surface energy budget and ablation modeling in the ablation zone of a maritime Tibetan glacier[J]. Journal of Geophysical Research: Atmospheres, 2011, 116: D14116, doi: 10.1029/2010JD015183.
[8]	Koelemeijer R, Oerlemans J, Tjemkes S. Surface reflectance of Hintereisferner, Austria, from Landsat 5 TM imagery[J]. Annals of Glaciology, 1993, 17: 17-22.
[9]	王杰, 何晓波, 叶柏生, 等. 唐古拉山冬克玛底冰川反照率变化特征研究[J]. 冰川冻土, 2012, 34(1): 21-28.
	[Wang Jie, He Xiaobo, Ye Baisheng, et al. Variations of albedo on the Dongkemadi Glacier, Tanggula Range[J]. Journal of Glaciology and Geocryology, 2012, 34(1): 21-28.]
[10]	王俊瑶, 怀保娟, 王叶堂, 等. 基于MOD10A1的祁连山黑河流域典型冰川反照率时空变化研究[J]. 干旱区研究, 2020, 37(6): 1396-1405.
	[Wang Junyao, Huai Baojuan, Wang Yetang, et al. Spatiotemporal variation of albedo of four representative glaciers in the Heihe River Basin based on multi-source data[J]. Arid Zone Research, 2020, 37(6): 1396-1405.]
[11]	陈满, 陈亚宁, 方功焕, 等. 昆仑山北坡冰川湖变化及其溃决风险评估[J]. 干旱区地理, 2024, 47(10): 1628-1639. doi: 10.12118/j.issn.1000-6060.2024.178
	[Chen Man, Chen Yaning, Fang Gonghuan, et al. Changes in glacial lakes on the northern slope of Kunlun Mountains and assessment of their outburst risks[J]. Arid Land Geography, 2024, 47(10): 1628-1639.] doi: 10.12118/j.issn.1000-6060.2024.178
[12]	郭万钦, 刘时银, 许君利, 等. 木孜塔格西北坡鱼鳞川冰川跃动遥感监测[J]. 冰川冻土, 2012, 34(4): 765-774.
	[Guo Wanqin, Liu Shiyin, Xu Junli, et al. Monitoring recent surging of the Yulinchuan Glacier on north slopes of Muztag Range by remote sensing[J]. Journal of Glaciology and Geocryology, 2012, 34(4): 765-774.]
[13]	毛瑞娟, 吴红波, 贺建桥, 等. 昆仑山木孜塔格冰川反照率变化特征及其与粉尘的关系[J]. 冰川冻土, 2013, 35(5): 1133-1142. doi: 10.7522/j.issn.1000-0240.2013.0128
	[Mao Ruijuan, Wu Hongbo, He Jianqiao, et al. Spatiotemporal variation of albedo of Muztagh Glacier in the Kunlun Mountains and its relation to dust[J]. Journal of Glaciology and Geocryology, 2013, 35(5): 1133-1142.] doi: 10.7522/j.issn.1000-0240.2013.0128
[14]	Wang A, Smith J A, Wang G, et al. Late Quaternary river terrace sequences in the eastern Kunlun Range, northern Tibet: A combined record of climatic change and surface uplift[J]. Journal of Asian Earth Sciences, 2009, 34(4): 532-543.
[15]	吴佳康, 陈丽花, 车彦军, 等. 东昆仑木孜塔格峰地区水汽来源分析[J]. 干旱区研究, 2024, 41(2): 211-219. doi: 10.13866/j.azr.2024.02.04
	[Wu Jiakang, Chen Lihua, Che Yanjun, et al. Analysis of moisture feeding in the Ulugh Muztagh area of the East Kunlun Mountains[J]. Arid Zone Research, 2024, 41(2): 211-219.] doi: 10.13866/j.azr.2024.02.04
[16]	Wang S, Li H, Zhang M, et al. Assessing gridded precipitation and air temperature products in the Ayakkum Lake, Central Asia[J]. Sustainability, 2022, 14(17): 10654, doi: 10.3390/su141710654.
[17]	毛瑞娟, 蒋熹, 郭忠明, 等. 基于TM/ETM+影像反演祁连山七一冰川反照率精度比较研究[J]. 冰川冻土, 2013, 35(2): 301-309. doi: 10.7522/j.issn.1000-0240.2013.0036
	[Mao Ruijuan, Jiang Xi, Guo Zhongming, et al. Study of the inversion precision of albedo on the Qiyi Glacier in the Qilian Mountain based on TM/ETM+ image[J]. Journal of Glaciology and Geocryology, 2013, 35(2): 301-309.] doi: 10.7522/j.issn.1000-0240.2013.0036
[18]	余凤臣, 王璞玉, 刘琳, 等. 萨吾尔山木斯岛冰川反照率时空变化特征研究[J]. 冰川冻土, 2022, 44(6): 1717-1729. doi: 10.7522/j.issn.1000-0240.2022.0150
	[Yu Fengchen, Wang Puyu, Liu Lin, et al. Study on the spatial and temporal variations of the surface albedo on Muz Taw Glacier, Sawir Mountains[J]. Journal of Glaciology and Geocryology, 2022, 44(6): 1717-1729.] doi: 10.7522/j.issn.1000-0240.2022.0150
[19]	秦春, 王建. CIVCO地形校正模型的改进及其应用[J]. 遥感技术与应用, 2008(1): 82-88.
	[Qin Chun, Wang Jian. Improved CIVCO topographic correction model and application[J]. Remote Sensing Technology and Application, 2008(1): 82-88.]
[20]	阿布都瓦斯提·吾拉木, 秦其明. 基于辐射模拟反演ETM+数据宽波段反照率[J]. 北京大学学报(自然科学版), 2007(4): 474-483.
	[Ghulam Abduwasti, Qin Qiming. Calculation of ETM+ broadband albedos by radiative simulations[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 2007(4): 474-483.]
[21]	Kruse F A. Comparison of Atrem, Acorn, and FLAASH atmospheric corrections using low-altitude AVIRIS data of Boulder[C]// Summaries of the 13^th JPL Airborne Geoscience Workshop. Pasadena, CA, USA: Jet Propulsion Laboratory, National Aeronautics and Space Administration (JPL, NASA), 2004: 1-10.
[22]	ASCF Center. FLASH user's guide[EB/OL]. [2005]. http://flash.rochester.edu.
[23]	Kaufman Y J, Wald A E, Remer L A, et al. The MODIS 2. 1-/spl mu/m channel-correlation with visible reflectance for use in remote sensing of aerosol[J]. IEEE Transactions on Geoscience and Remote Sensing, 1997, 35(5): 1286-1298.
[24]	Knap W H, Reijmer C H, Oerlemans J. Narrowband to broadband conversion of Landsat TM glacier albedos[J]. International Journal of Remote Sensing, 1999, 20(10): 2091-2110.
[25]	Liang S. Narrowband to broadband conversions of land surface albedo I: Algorithms[J]. Remote Sensing of Environment, 2001, 76(2): 213-238.
[26]	Naegeli K, Damm A, Huss M, et al. Cross-comparison of albedo products for glacier surfaces derived from airborne and satellite (Sentinel-2 and Landsat 8) optical data[J]. Remote Sensing, 2017, 9(2): 110, doi: 10.3390/rs9020110.
[27]	Traversa G, Fugazza D, Senese A, et al. Landsat 8 OLI broadband albedo validation in Antarctica and Greenland[J]. Remote Sensing, 2021, 13(4): 799, doi: 10.3390/rs13040799.
[28]	Greuell W, de Wildt M R. Anisotropic reflection by melting glacier ice: Measurements and parametrizations in Landsat TM bands 2 and 4[J]. Remote Sensing of Environment, 1999, 70(3): 265-277.
[29]	Boggild C E, Warren S G, Brandt R E, et al. Effects of dust and black carbon on albedo of the greenland ablation zone[C]// AGU Fall Meeting Abstracts. Washington, DC: American Geophysical Union, 2006: U22A-05.
[30]	Braithwaite R J, Raper S C B. Estimating equilibrium-line altitude (ELA) from glacier inventory data[J]. Annals of Glaciology, 2009, 50(53): 127-132.
[31]	胡安洵, 郝卫峰, 马超, 等. 大高加索山脉冰川反照率时空分布及与物质平衡的关系[J]. 地球物理学报, 2024, 67(4): 1314-1329.
	[Hu Anxun, Hao Weifeng, Ma Chao, et al. The spatio-temporal distribution of the albedos and its relationship with glacier mass balance in the glaciers of the Greater Caucasus Mountains[J]. Chinese Journal of Geophysics, 2024, 67(4): 1314-1329.]
[32]	Ren S, Jia L, Menenti M, et al. Changes in glacier albedo and the driving factors in the Western Nyainqentanglha Mountains from 2001 to 2020[J]. Journal of Glaciology, 2023, 69(277): 1500-1514.

影像中心点	传感器类型	飞行日期	高程/m	分辨率/m	大气模式	气溶胶模式
87.55875278°E 36.03851667°N	OLI	2015/4/14 04：45：20	4959	30	Sub-Arctic Summer	Rural
能见度/km	气溶胶高度/km	CO₂混合比	Modtran分辨率/cm^-1	散射模型	DISORT流数
40	1.25	390	15	scale DISCORT	8

像元值	含义
0~100	积雪反照率
101	不确定的地物类型
111	夜间
125	无积雪覆盖的陆地
137	内流湖
139	开阔水体
150	云层覆盖
251	自身阴影
252	陆地界限不匹配
253	BRDF故障
254	没有匹配的数据
250	缺失的数据