祁连山老虎沟12号冰川表面能量和物质平衡模拟

doi:10.7522/j.issn.1000-0240.2014.0005

冰川冻土 ›› 2014, Vol. 36 ›› Issue (1): 38-47.doi: 10.7522/j.issn.1000-0240.2014.0005

祁连山老虎沟12号冰川表面能量和物质平衡模拟

陈记祖^1,2, 秦翔^1,2, 吴锦奎², 杜文涛², 孙维君², 刘宇硕², 黄哲¹, 杨俊华²

1. 兰州大学资源环境学院, 甘肃兰州 730000;
2. 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/祁连山冰川与生态环境综合观测研究站, 甘肃兰州 730000

收稿日期:2013-08-26 修回日期:2013-12-05 出版日期:2014-02-25 发布日期:2014-03-18
通讯作者: 秦翔，E-mail：qinxiang@lzb.ac.cn E-mail:qinxiang@lzb.ac.cn
作者简介:陈记祖（1990-），男，甘肃天水人，2011年毕业于兰州大学，现为硕士研究生，主要从事冰川气象和冰川水文的研究工作. E-mail：chenjz2011@lzu.edu.cn
基金资助:
国家重大科学研究计划项目（2013CBA01801）；国家自然科学基金项目（41201067；41371091；41271085；41271085）；冰冻圈科学国家重点实验室自主课题（SKLCS-ZZ-2012-01-05）资助

Simulating the energy and mass balances on the Laohugou Glacier No. 12 in the Qilian Mountains

CHEN Jizu^1,2, QIN Xiang^1,2, WU Jinkui², DU Wentao², SUN Weijun², LIU Yushuo², HUANG Zhe¹, YANG Junhua²

1. College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China;
2. State Key Laboratory of Cryospheric Sciences / Qilian Shan Station of Glaciology and Ecologic Environment, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China

Received:2013-08-26 Revised:2013-12-05 Online:2014-02-25 Published:2014-03-18

摘要/Abstract

摘要：

采用HOCK的分布式能量物质平衡模型对老虎沟12号冰川消融期的物质平衡进行了模拟，时间步长为1 h，空间分辨率为30 m. 模型结果利用物质平衡观测数据和气象站观测数据验证，模型模拟时期为2012年6月1日-9月30日. 模型模拟结果表明，地形因子对太阳辐射影响相当显著；散射辐射在总辐射中的比例较大为39%，模拟期冰川表面物质平衡为-506 mm w.e.. 在模拟期整个冰川平均上净辐射占能量收入的84%，感热通量占有16%；消融耗热则是能量的主要支出占有62%，潜热通量占有能量支出的38%.

关键词: 老虎沟12号冰川, 分布式能量-物质平衡模型, 地形因子, 散射辐射

Abstract:

By using a 1-h temporal resolution and 30-m spatial resolution grid-based distributive surface mass-energy model, the energy distribution and mass balance on the Laohugou No.12 Glacier were simulated. The period of simulation was from June 1st to September 30 th, 2012. The simulated results were validated by solar and net radiation data from meteorological stations and measured mass-balance data, respectively. The simulated results show that terrain factors have a considerably effect on solar radiation. Diffuse radiation accounts for 38% of global radiation. The mass balance averaged over the simulated period is 893 mm w.e. During the simulative period and over the glacier, the net radiation is the principal energy source (84%), followed by the sensible het flux (16%); whereas the main energy expenditure is the heat flux for snow/ice ablation (62%), followed by the latent heat flux (38%).

Key words: Laohugou Glacier No. 12, distributive mass-energy balance model, terrain factor, diffuse radiation

中图分类号:

P343.6

陈记祖, 秦翔, 吴锦奎, 杜文涛, 孙维君, 刘宇硕, 黄哲, 杨俊华. 祁连山老虎沟12号冰川表面能量和物质平衡模拟[J]. 冰川冻土, 2014, 36(1): 38-47.

CHEN Jizu, QIN Xiang, WU Jinkui, DU Wentao, SUN Weijun, LIU Yushuo, HUANG Zhe, YANG Junhua. Simulating the energy and mass balances on the Laohugou Glacier No. 12 in the Qilian Mountains[J]. JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY, 2014, 36(1): 38-47.

参考文献

[1] 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.
[2] Ren Jiawen, Jing Zhefan, Pu Jianchen, et al. Glacier variations and climate change in the central Himalaya over the past few decades[J]. Annals of Glaciology, 2006, 43(1): 218-222.
[3] He Jianqiao, Song Gaoju, Jiang Xi, et al. Relation between glacial meltwater runoff and mountainous runoff in 2006 in four typical river basins of Heihe River water system[J]. Journal of Desert Research, 2008, 28(6): 1186-1189. [贺建桥, 宋高举, 蒋熹, 等. 2006年黑河水系典型流域冰川融水径流与出山径流的关系[J]. 中国沙漠, 2008, 28(6): 1186-1189.]
[4] Gao Xin, Zhang Shiqiang, Ye Baisheng, et al. Glacier runoff change in the upper stream of Yarkant River and its impact on river runoff during 1961-2006[J]. Journal of Glaciology and Geocryology, 2010, 32(3): 445-453. [高鑫, 张世强, 叶柏生, 等. 1961-2006年叶尔羌河上游流域冰川融水变化及其对径流的影响[J]. 冰川冻土, 2010, 32(3): 445-453.]
[5] Gao Xin, Zhang Shiqiang, Ye Baisheng, et al. Recent changes of glacier runoff in the Hexi inland river basin[J]. Advances in Water Science, 2011, 22(3): 344-350. [高鑫, 张世强, 叶柏生, 等. 河西内陆河流域冰川融水近期变化[J]. 水科学进展, 2011, 22(3): 344-350.]
[6] Cui Hang, Wang Jie. The methods for estimating the equilibrium line altitudes of a glacier[J]. Journal of Glaciology and Geocryology, 2013, 35(2): 345-354. [崔航, 王杰. 冰川物质平衡线的估计方法[J]. 冰川冻土, 2013, 35(2): 345-354.]
[7] 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. [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.]
[8] Zhou Jian, Zhang Wei, Pomeroy J W, et al. Simulating the cold regions hydrological processes in Northwest China with modular modeling method[J]. Journal of Glaciology and Geocryology, 2013, 35(2): 389-400. [周剑, 张伟, Pomeroy J W, 等. 基于模块化建模方法的寒区水文过程模拟在中国西北寒区的应用[J]. 冰川冻土, 2013, 35(2): 389-400.]
[9] Bie Qiang, Qiang Wenli, Wang Chao, et al. Monitoring glacier variation in the upper reaches of the Heihe River based on remote sensing in 1960-2010[J]. Journal of Glaciology and Geocryology, 2013, 35(3): 574-582. [别强, 强文丽, 王超, 等. 1960-2010年黑河流域冰川变化的遥感监测[J]. 冰川冻土, 2013, 35(3): 574-582.]
[10] Braithwaite R J, Zhang Yu. Sensitivity of mass balance of five Swiss glaciers to temperature changes assessed by tuning a degree-day model[J]. Journal of Glaciology, 2000, 46(152): 7-14.
[11] Hock R. Temperature index melt modelling in mountain areas[J]. Journal of Hydrology, 2003, 282(1): 104-115.
[12] Arnold N, Willis I C, Sharp M J, et al. A distributed surface energy balance model for a small valley glacier: I. Development and testing for Haut Glacier d'Arolla, Valais, Switzerland[J]. Journal of Glaciology, 1996, 42(140): 77-89.
[13] Klok E J, Oerlemans J. Model study of the spatial distribution of the energy and mass balance of Morteratschgletscher, Switzerland[J]. Journal of Glaciology, 2002, 48(163): 505-518.
[14] Arnold N S, Rees W G, Hodson A J, et al. Topographic controls on the surface energy balance of a high Arctic valley glacier[J]. Journal of Geophysical Research: Earth Surface, 2006, 111(F2), doi:10.1029/2005JF000426.
[15] Hock R, Holmgren B. A distributed surface energy-balance model for complex topography and its application to Storglaciären, Sweden[J]. Journal of Glaciology, 2005, 51(172): 25-36.
[16] Macdougall A H, Flowers G E. Spatial and temporal transferability of a distributed energy-balance glacier melt model[J]. Journal of Climate, 2010, 24: 1480-1498.
[17] Jiang Xi, Wang Ninglian, He Jianqiao, et al. A distributed surface energy and mass balance model and its application to a mountain glacier in China[J]. Chinese Science Bulletin, 2010, 55(20): 2079-2087. [蒋熹, 王宁练, 贺建桥, 等. 山地冰川表面分布式能量-物质平衡模型及其应用[J]. 科学通报, 2010, 55(18): 1757-1765.]
[18] Reuter H I, Nelson A, Strobl P, et al. A first assessment of Aster GDEM tiles for absolute accuracy, relative accuracy and terrain parameters[C]//Proceedings of 2009 IEEE International Geoscience & Remote Sensing Symposium: Vol. V, Cape Town, South Africa, July 12-17, 2009, doi:10.1109/IGARSS.2009.5417688.
[19] Kang Xingcheng, Ding Liangfu. The correlation between the glacial mass balance, snowline location and weather climate conditions in the Tian Shan and Qilian Shan[J]. Journal of Glaciology and Geocryology, 1981, 3(1): 53-58. [康兴成, 丁良福. 天山和祁连山的冰川物质平衡、雪线位置与天气气候的关系[J]. 冰川冻土, 1981, 3(1): 53-58.]
[20] Sun Weijun, Qin Xiang, Ren Jiawen, et al. Surface energy balance in the accumulation zone of the Laohugou Glacier No. 12 in the Qilian Mountains during ablation period[J]. Journal of Glaciology and Geocryology, 2011, 33(1): 38-46. [孙维君, 秦翔, 任贾文, 等. 祁连山老虎沟12号冰川积累区消融期能量平衡特征[J]. 冰川冻土, 2011, 33(1): 38-46.]
[21] Fröhlich C. Changes of total solar irradiance[J]. Geophysical Monograph Series, 1993, 75: 123-129.
[22] Cess R D, Zhang M H, Minnis P, et al. Absorption of solar radiation by clouds: Observations versus models[J]. Science, 1995, 267(5197): 496-499.
[23] Zhao Bolin, Zhang Xiaoli, Zhu Yuanjing. The cloud and radiative balance in China[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 1992, 28(3): 371-383. [赵柏林, 张晓黎, 朱元竟. 中国地区云与辐射对气候的影响[J]. 北京大学学报(自然科学版), 1992, 28(3): 371-383.]
[24] Cutler P M, Munro D S. Visible and near-infrared reflectivity during the ablation period on Peyto Glacier, Alberta, Canada[J]. Journal of Glaciology, 1996, 42(141): 333-340.
[25] Brock B W, Willis I C, Sharp M J. Measurement and parameterization of albedo variations at Haut Glacier d'Arolla, Switzerland[J]. Journal of Glaciology, 2000, 46(155): 675-688.
[26] Jonsell U, Hock R, Holmgren B. Spatial and temporal variations in albedo on Storglaciären, Sweden[J]. Journal of Glaciology, 2003, 49: 59-68.
[27] Warren S G, Wiscombe W J. A model for the spectral albedo of snow. II: Snow containing atmospheric aerosols[J]. Journal of the Atmospheric Sciences, 1980, 37(12): 2734-2745.
[28] Choudhury B J, Chang A T C. On the angular variation of solar reflectance of snow[J]. Journal of Geophysical Research: Oceans, 1981, 86(C1): 465-472.
[29] Marshall S E, Warren S G. Parameterization of snow albedo for climate models[C]//Goodison B E, Barry R G, Dozier J. Large Scale Effects of Seasonal Snow Cover: IAHS Publication No. 166. Wallingford, UK: IAHS, 1987: 43-50.
[30] Marks D, Dozier J. Climate and energy exchange at the snow surface in the alpine region of the Sierra Nevada: 2. Snow cover energy balance[J]. Water Resources Research, 1992, 28(11): 3043-3054.
[31] Munro D S, Young G J. An operational net shortwave radiation model for glacier basins[J]. Water Resources Research, 1982, 18(2): 220-230.
[32] Hock R, Noetzli C. Areal melt and discharge modeling of Storglaciären, Sweden[J]. Annals of Glaciology, 1997, 24: 211-216.
[33] Escher-Vetter H. Energy balance calculations for the ablation period 1982 at Vernagtferner, Oetztal Alps[J]. Annals of Glaciology, 1985, 6: 158-160.
[34] Blöschl G, Kirnbauer R, Gutknecht D. Distributed snowmelt simulations in an Alpine catchment: 1. Model Evaluation on the basis of snow cover patterns[J]. Water Resources Research, 1991, 27(12): 3171-3179.
[35] Jiang Xi, Wang Ninglian, He Jianqiao, et al. A study of parameterization of albedo on the Qiyi Glacier in Qilian Mountains, China[J]. Journal of Glaciology and Geocryology, 2011, 33(1): 30-37. [蒋熹, 王宁练, 贺建桥, 等. 祁连山七一冰川反照率的参数化研究[J]. 冰川冻土, 2011, 33(1): 30-37.]
[36] Plüss C, Ohmura A. Longwave radiation on snow-covered mountainous surfaces[J]. Journal of Applied Meteorology, 1997, 36(6): 818-824.
[37] Forrer J, Rotach M W. On the turbulence structure in the stable boundary layer over the Greenland ice sheet[J]. Boundary-Layer Meteorology, 1997, 85(1): 111-136.
[38] Beljaars A, Holtslag A. Flux parameterization over land surface for atmospheric models[J]. Journal of Applied Meteorology, 1991, 30(3): 327-341.
[39] Sun Weijun. Modelling of Surface Energy-Mass Balance on the Laohugou Glacier No. 12 in the Qilian Mountains, China[D]. PhD Thesis, Lanzhou: Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, 2012. [孙维君. 祁连山老虎沟12号冰川能量-物质平衡模拟研究[D]. 博士论文, 兰州: 中国科学院寒区旱区环境与工程研究所, 2012.]
[40] Munro D S. Comparison of melt energy computations and ablatometer measurements on melting ice and snow[J]. Arctic and Alpine Research, 1990, 22(2): 153-162.
[41] Chen Liang, Duan Keqin, Wang Ninglian, et al. Characteristics of the surface energy balance of the Qiyi Glacier in Qilian Mountains in melting season[J]. Journal of Glaciology and Geocryology, 2007, 29(6): 882-888. [陈亮, 段克勤, 王宁练, 等. 祁连山七一冰川消融期间能量平衡特征[J]. 冰川冻土, 2007, 29(6): 882-888.]
[42] Zhang Jian, He Xiaobo, Ye Baisheng, et al. Recent variation of mass balance of the Xiao Dongkemadi Glacier in the Tanggula Range and its influencing factors[J]. Journal of Glaciology and Geocryology, 2013, 35(2): 263-271. [张健, 何晓波, 叶柏生, 等. 近期小冬克玛底冰川物质平衡变化及其影响因素分析[J]. 冰川冻土, 2013, 35(2): 263-271.]
[43] Zhang Guofei, Li Zhongqin, Wang Wenbin, et al. Change processes and characteristics of mass balance of the Vrümqi Glacier No. 1 at the headwaters of the Vrümqi River, Tianshan Mountains, during 1959-2009[J]. Journal of Glaciology and Geocryology, 2012, 34(6): 1301-1309. [张国飞, 李忠勤, 王文斌, 等. 天山乌鲁木齐河源1号冰川1959-2009年物质平衡变化过程及特征研究[J]. 冰川冻土, 2012, 34(6): 1301-1309.]
[44] Gao Hongkai, He Xiaobo, Ye Baisheng, et al. The simulation of HBV hydrology model in the Dongkemadi River basin, headwater 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.]

祁连山老虎沟12号冰川表面能量和物质平衡模拟

Simulating the energy and mass balances on the Laohugou Glacier No. 12 in the Qilian Mountains

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