近60 a伊塞克湖水量平衡变化及影响因素分析

doi:10.13866/j.azr.2022.05.22

干旱区研究 ›› 2022, Vol. 39 ›› Issue (5): 1576-1587.doi: 10.13866/j.azr.2022.05.22 cstr: 32277.14.AZR.20220522

近60 a伊塞克湖水量平衡变化及影响因素分析

王晓飞^1,^2,³(),黄粤^1,²(),刘铁^1,²,李均力^1,²,王正^1,^2,³,昝婵娟^1,^2,³,段永超⁴

1.中国科学院新疆生态与地理研究所荒漠与绿洲生态国家重点实验室,新疆乌鲁木齐 830011
2.新疆维吾尔自治区遥感与地理信息系统应用重点实验室,新疆乌鲁木齐 830011
3.中国科学院大学,北京 100049
4.无锡学院,江苏无锡 214105

收稿日期:2022-01-22 修回日期:2022-08-25 出版日期:2022-09-15 发布日期:2022-10-25
作者简介:王晓飞（1997-）,女,硕士研究生,主要从事空间水文学过程研究. E-mail: wangxiaofei201@mails.ucas.ac.cn
基金资助:
中国科学院A类战略性先导科技专项泛第三极环境变化与绿色丝绸之路建设(XDA20060301);王宽诚教育基金(GJTD-2020-14);中国科学院国际合作项目(131551KYSB20160002);中国科学院国际合作项目(131965KYSB20200029);中国科学院交叉创新团队(JCTD-2019-20);2021年江苏省双创博士项目(JSSCBS20210862);无锡学院人才启动项目(550221020)

Analysis of water balance change and influencing factors in Issyk-Kul Lake in recent 60 years

WANG Xiaofei^1,^2,³(),HUANG Yue^1,²(),LIU Tie^1,²,LI Junli^1,²,WANG Zheng^1,^2,³,ZAN Chanjuan^1,^2,³,DUAN Yongchao⁴

1. State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, Xinjiang, China
2. Key Laboratory of GIS & RS Application Xinjiang Uygur Autonomous Region, Urumqi 830011, Xinjiang, China
3. University of Chinese Academy of Sciences, Beijing 100049, China
4. Wuxi University, Wuxi 214105, Jiangsu, China

Received:2022-01-22 Revised:2022-08-25 Published:2022-09-15 Online:2022-10-25

摘要/Abstract

摘要：

基于卫星遥感数据,提取近60 a伊塞克湖面积、水位变化信息,反演伊塞克湖水量变化时间序列,结合1960—2020年CRU气象数据、1960—2000年乔尔蓬阿塔气象站气温降水观测数据和入湖水量观测数据,建立湖泊水量平衡模型,分析水量平衡各分量的变化特征,并探讨其影响因素。结果表明：（1） 1960年以来伊塞克湖水量变化经历了持续减少-波动增加的过程,1998年为变化的时间拐点;20世纪60—80年代中期,入湖水量主要受灌溉引水影响持续减少,1986年后随灌溉水量减少、降水和冰川融水的增加而转为上升趋势;湖区降水以9.1 mm·(10a)^-1的速率增加,蒸发量随湖区升温和湖体面积增加总体呈显著增加趋势。（2） 20世纪80年代中期以前伊塞克湖大部分年份湖泊水量呈负平衡,地下水持续补给湖泊,1986年起湖泊的水量收支亏损逐渐减小,1998年以来以正平衡为主。（3）入湖径流、降水、蒸发等水量平衡分量的互动关系决定了湖泊水量的变化,而产流区气候变化和灌区灌溉引水通过改变入湖径流间接驱动湖泊水量的变化;1960—1986年,以灌溉引水为主的人类活动是驱动伊塞克湖水量变化的主导因素,贡献率达71.6%,1987年以来,气候变化因子对湖泊水量变化的累计贡献超过80%。

关键词: 伊塞克湖, 水量平衡, 入湖径流, 气候变化

Abstract:

Based on the satellite data, the water level and area information of Lake Issyk-Kul was extracted, and the water volume was reconstruct; combined with CRU meteorological data from 1960-2020, the temperature and precipitation observation data from 1960-2000 at the Cholpon-Ata meteorological station and the water volume observation data into the lake, the lake water balance model was established to analyze the changing characteristics of each element of the water balance and to explore its influencing factors. The results indicated that: (1) Since 1960, the water volume of Issyk-Kul Lake has undergone a process of continuous decrease and fluctuating increase, with 1998 being the inflection point of the change; from the 1960s to the mid-1980s, the water volume into the lake decreased continuously mainly due to the influence of irrigation diversions, and then turned to an increasing trend after 1986 with the decrease of irrigation water and the increase of precipitation and glacial meltwater; precipitation in the lake area increased at a rate of 9.1 mm·(10a)^-1, and the evapotranspiration tends to increase significantly with increasing temperature and lake area. (2) Before the mid-1980s, Issyk-Kul had a negative water balance in most years, and groundwater continued to recharge the lake; since 1986, the water balance deficit of the lake gradually decreased, and since 1998, the positive balance has been dominated. (3) The interaction of water balance components such as runoff, precipitation and evaporation determines the changes in lake water volume, while climate change in the flow-producing areas and irrigation diversions in irrigation areas indirectly drive the changes in lake water volume by changing runoff; from 1960 to 1986, human activities, mainly irrigation diversions, were the dominant factor driving the changes in Issyk-Kul water volume, with a contribution of 71.6%, and since 1987 the cumulative contribution of climate change factors to changes in lake water volume exceeds 80%.

Key words: Issyk-Kul Lake, water balance, runoff, climate change

王晓飞,黄粤,刘铁,李均力,王正,昝婵娟,段永超. 近60 a伊塞克湖水量平衡变化及影响因素分析[J]. 干旱区研究, 2022, 39(5): 1576-1587.

WANG Xiaofei,HUANG Yue,LIU Tie,LI Junli,WANG Zheng,ZAN Chanjuan,DUAN Yongchao. Analysis of water balance change and influencing factors in Issyk-Kul Lake in recent 60 years[J]. Arid Zone Research, 2022, 39(5): 1576-1587.

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参考文献 40

[1]	成晨, 傅文学, 胡召玲, 等. 基于遥感技术的近30年中亚地区主要湖泊变化[J]. 国土资源遥感, 2015, 27(1): 146-152.
	[Cheng Chen, Fu Wenxue, Hu Zhaoling, et al. Changes of major lakes in Central Asia over the past 30 years revealed by remote sensing technology[J]. Remote Sensing for Land and Resources, 2015, 27(1): 146-152. ]
[2]	姚俊强, 刘志辉, 杨青, 等. 近130年来中亚干旱区典型流域气温变化及其影响因子[J]. 地理学报, 2014, 69(3): 291-302. doi: 10.11821/dlxb201403001
	[Yao Junqiang, Liu Zhihui, Yang Qing, et al. Temperature variability and its possible causes in the typical basins of the arid Central Asia in recent 130 years[J]. Acta Geographica Sinica, 2014, 69(3): 291-302. ] doi: 10.11821/dlxb201403001
[3]	李均力, 包安明, 胡汝骥, 等. 亚洲中部干旱区湖泊的地域分异性研究[J]. 干旱区研究, 2013, 30(6): 941-950.
	[Li Junli, Bao Anming, Hu Ruji, et al. Regional difference of lakes in the arid regions in Central Asia[J]. Arid Zone Research, 2013, 30(6): 941-950. ]
[4]	邵新媛. 伊塞克湖近期变化及其原因[J]. 干旱区地理, 1992, 15(2): 81-88.
	[Shao Xinyuan. The recent change of water level of Yiseke lake and its cause[J]. Arid Land Geography, 1992, 15(2): 81-88. ]
[5]	米热古力·艾尼瓦尔, 海米提·依米提, 麦麦提吐尔逊·艾则孜, 等. 基于小波分析的伊塞克湖水位变化特征[J]. 水土保持研究, 2014, 21(1): 168-172.
	[Mihrigul Anwar, Hamid Yimit, Mamattursun Eziz, et al. Water level variations of Issyk-Kul lake based on wavelet analysis[J]. Research of Soil and Water Conservation, 2014, 21(1): 168-172. ]
[6]	Romanovsky V V. WaterLevel Variations and Water Balance of Lake Issyk-Kul. Lake Issyk-Kul: Its Natural Environment[M]. Kluwer Academic Publishers: Dordrecht, The Netherlands, 2002, 13: 45-58.
[7]	米热古力·艾尼瓦尔. 博斯腾湖和伊塞克湖水位变化对气候变化的响应对比研究[D]. 乌鲁木齐: 新疆大学, 2014.
	[Mihrigul Anwar. Comparative Study on Water Level Change and Its Climate Change Response of Baghrash Lake and Issyk-Kul[D]. Urumqi: Xinjiang University, 2014. ]
[8]	李均力, 陈曦, 包安明. 2003—2009年中亚地区湖泊水位变化的时空特征[J]. 地理学报, 2011, 66(9): 1219-1229. doi: 10.11821/xb201109007
	[Li Junli, Chen Xi, Bao Anming. Spatial-temporal characteristics of lake level changes in Central Asia during 2003-2009[J]. Acta Geographica Sinica, 2011, 66(9): 1219-1229. ] doi: 10.11821/xb201109007
[9]	阿依努尔·买买提, 玉米提·哈力克, 阿依加马力·克然木. 天山典型湖泊水位变化影响因素对比分析——以博斯腾湖与伊塞克湖为例[J]. 干旱区资源与环境, 2017, 31(8): 143-147.
	[Aynur Mamat, Umit Halik, Ayjamal Keram. Remote sensing based analysis on environment changes of typical lakes in Tian shan mountains: A case study of Bosten Lake and Issyk-Kul Lake[J]. Journal of Arid Land Resources and Environment, 2017, 31(8): 143-147. ]
[10]	王国亚, 沈永平, 王宁练, 等. 气候变化和人类活动对伊塞克湖水位变化的影响及其演化趋势[J]. 冰川冻土, 2010, 32(6): 1097-1105.
	[Wang Guoya, Shen Yongping, Wang Ninglian, et al. The effects of climate change and human activities on the lake level of Issyk-Kul during the past 100 years[J]. Journal of Glaciology and Geocryology, 2010, 32(6): 1097-1105. ]
[11]	闫政新, 郭万钦. 1991—2014年中亚伊塞克湖湖泊面积变化遥感监测[J]. 测绘与空间地理信息, 2018, 41(2): 142-146.
	[Yan Zhengxin, Guo Wanqin. Remote sensing monitoring of the lake area of Issyk-Kul lake in Central Asia from 1991-2014[J]. Geomatics and Spatial Information Technology, 2018, 41(2): 142-146. ]
[12]	白洁, 陈曦, 李均力, 等. 1975—2007年中亚干旱区内陆湖泊面积变化遥感分析[J]. 湖泊科学, 2011, 23(1): 80-88. doi: 10.18307/2011.0113
	[Bai Jie, Chen Xi, Li Junli, et al. Changes of inland lake area in arid Central Asia during 1975-2007: A remote-sensing analysis[J]. Journal of Lake Sciences, 2011, 23(1): 80-88. ] doi: 10.18307/2011.0113
[13]	朱德祥. 伊塞克湖水资源问题[J]. 干旱区地理, 1988, 11(3): 84-86.
	[Zhu Dexiang. Water resources of Issyk-Kul Lake[J]. Arid Land Geography, 1988, 11(3): 84-86. ]
[14]	秦伯强. 近百年来亚洲中部内陆湖泊演变及其原因分析[J]. 湖泊科学, 1999, 11(1): 11-19. doi: 10.18307/1999.0102
	[Qin Boqiang. A preliminary investigation of lake evolution in 20-century in inland mainland Asia with relation to the global warming[J]. Journal of Lake Sciences, 1999, 11(1): 11-19. ] doi: 10.18307/1999.0102
[15]	秦伯强. 气候变化对内陆湖泊影响分析[J]. 地理科学, 1993, 13(3): 212-219, 295.
	[Qin Boqiang. Analysis of the influence of climate change on inland lakes[J]. Scientia Geographica Sinica, 1993, 13(3): 212-219, 295. ]
[16]	伊丽努尔·阿力甫江, 吉力力·阿不都外力, 丁之勇, 等. 伊塞克湖典型小流域径流变化差异性及其影响因素分析[J]. 水土保持学报, 2020, 34(6): 198-210.
	[Yilinuer Alifujiang, Jilili Abudouwaili, Ding Zhiyong, et al. Analysis of the difference of runoff variation and its influencing factors in typical small watershed of Issyk-Kul Basin[J]. Journal of Soil and Water Conservation, 2020, 34(6): 198-210. ]
[17]	尹仔锋, 尚华明, 魏文寿, 等. 基于树轮宽度的伊塞克湖入湖径流量重建与分析[J]. 沙漠与绿洲气象, 2014, 8(4): 8-14.
	[Yin Zaifeng, Shang Huaming, Wei Wenshou, et al. Runoff reconstruction and analysis of Issyk-Kul Lake based on tree-ring width[J]. Desert and Oasis Meteorology, 2014, 8(4): 8-14. ]
[18]	王国亚, 沈永平, 秦大河. 1860—2005年伊塞克湖水位波动与区域气候水文变化的关系[J]. 冰川冻土, 2006, 28(6): 854-860.
	[Wang Guoya, Shen Yongping, Qin Dahe. Issyk-Kul Lake level fluctuation during 1860-2005 and its relation with regional climatic and hydrological changes[J]. Journal of Glaciology and Geocryology, 2006, 28(6): 854-860. ]
[19]	沈永平. 1883—2001年(部分年份)吉尔吉斯斯坦逐月平均降水量数据. 国家冰川冻土沙漠科学数据中心(www.ncdc.ac.cn), 2019.
	[Shen Yongping. Monthly average precipitation data of Kyrgyzstan from 1883 to 2001 (partial years). National Cryosphere Desert Data Center(www.ncdc.ac.cn), 2019. ]
[20]	沈永平. 1879—2003年(部分年份)中亚地区吉尔吉斯斯坦逐月平均气温数据. 国家冰川冻土沙漠科学数据中心(www.ncdc.ac.cn), 2019.
	[Shen Yongping. Monthly average temperature data of Kyrgyzstan in Central Asia from 1879 to 2003 (partial years). National Cryosphere Desert Data Center (www.ncdc.ac.cn), 2019. ]
[21]	Uwamahoro Solange, Liu T, Nzabarinda Vincent, et al. Modifications to snow-melting and flooding processes in the hydrological model: A case study in Issyk-Kul, Kyrgyzstan[J]. Atmosphere, 2021, 12(12): 1580. https://doi.org/10.3390/atmos12121580. doi: 10.3390/atmos12121580
[22]	Pierre. (2020). 中亚五国土地利用类型数据集(2000, 2005, 2010, 2015). 国家青藏高原科学数据中心, 2020.
	[Pierre. (2020). Data set of land use types of five Central Asian countries (2000, 2005, 2010, 2015). National Tibetan Plateau Data Center, 2020. ]
[23]	方晖. 中亚五国1:100万水系数据(2010年). 国家冰川冻土沙漠科学数据中心(www.ncdc.ac.cn), 2019.
	[Fang Hui. 1:1 million water system data of five Central Asian countries (2010). National Cryosphere Desert Data Center (www.ncdc.ac.cn), 2019. ]
[24]	骆剑承, 盛永伟, 沈占锋, 等. 分步迭代的多光谱遥感水体信息高精度自动提取[J]. 遥感学报, 2009, 13(4): 604-615.
	[Luo Jiancheng, Sheng Yongwei, Shen Zhanfeng, et al. Step by step iterative multi-spectral remote sensing water information extraction with high precision[J]. Journal of Remote Sensing, 2009, 13(4): 604-615. ]
[25]	闫政新. 基于遥感影像的伊塞克湖泊变化研究[D]. 沈阳: 辽宁工程技术大学, 2016.
	[Yan Zhengxin. Based on Remote Sensing Image to Study on the Issyk-Kul Lake’s Change[D]. Shenyang: Liaoning Technical University, 2016. ]
[26]	FAO. Crop Evapotranspiration Guidelines for Computing Crop Water Requirements[J]. Food and Agriculture Organization of the United Nations Rome, 1998.
[27]	Huang Y, Ma Y, Liu T, et al. Climate change impacts on extreme flows under IPCC RCP scenarios in the mountainous Kaidu watershed, Tarim River Basin[J]. Sustainability, 2020, 12(5): 2090. doi: 10.3390/su12052090
[28]	Hargreaves G H, Samani Z A. Reference crop evapotranspiration from temperature[J]. Applied Engineering in Agriculture, 1985, 1(2): 96-99. doi: 10.13031/2013.26773
[29]	Szczypta C, Calvet J-C, Albergel C, et al. Verification of the new ECMWF ERA-Interim reanalysis over France[J]. Hydrology and Earth System Sciences, 2011, 15(2): 647-666. doi: 10.5194/hess-15-647-2011
[30]	喻雪晴, 穆振侠. 降水资料匮乏地区不同再分析数据降尺度效果的评价[J]. 水电能源科学, 2020, 38(9): 5-8, 23.
	[Yu Xueqing, Mu Zhenxia. Evaluation of downscaling effect of different reanalysis data in regions with insufficient precientation data[J]. Water Resources and Power, 2020, 38(9): 5-8, 23. ]
[31]	罗敏. 干旱区气候变化对新疆典型流域水资源的影响研究[D]. 北京: 中国科学院大学, 2019.
	[Luo Min. Study on the Climate Change in Arid Regions and Its Impact on Water Resources in Typical River Basing of Xinjiang[D]. Beijing: University of Chinese Academy of Sciences, 2019. ]
[32]	中华人民共和国水利部. 水文情报预报规范: SL 250-2000[S]. 北京: 中国水利水电出版社, 2000.
	[Ministry of Water Resources of the People’s Republic of China. Standard for Hydrological Information and Hydrological Forecasting: SL 250-2000[S]. Beijing: China Water & Power Press, 2000. ]
[33]	昝婵娟, 黄粤, 李均力, 等. 1990—2019年咸海水量平衡及其影响因素分析[J]. 湖泊科学, 2021, 33(4): 1265-1275. doi: 10.18307/2021.0426
	[Zan Chanjuan, Huang Yue, Li Junli, et al. Analysis of water balance in Aral Sea and the influencing factors from 1990 to 2019[J]. Journal of Lake Sciences, 2021, 33(4): 1265-1275. ] doi: 10.18307/2021.0426
[34]	РОМАНОВСКИЙВ В, 秦伯强. 关于伊塞克湖水位下降的原因[J]. 湖泊科学, 1992, 4(3): 38-43.
	[РОМАНОВСКИЙВ В, Qin Boqiang. On decline of Issyk-Kul Lake level[J]. Journal of Lake Sciences, 1992, 4(3): 38-43. ]
[35]	Yilinuer Alifujiang, Jilili Abuduwaili, Ma Long, et al. System dynamics modeling of water level variations of Lake Issyk-Kul, Kyrgyzstan[J]. Water, 2017, 9(12): 989. doi: 10.3390/w9120989
[36]	沈永平, 刘时银, 丁永建, 等. 天山南坡台兰河流域冰川物质平衡变化及其对径流的影响[J]. 冰川冻土, 2003, 25(2): 124-129.
	[Shen Yongping, Liu Shiyin, Ding Yongjian, et al. Glacier mass balance change in Tailanhe River watersheds on the south slope of the Tianshan Mountains and its impact on water resources[J]. Journal of Glaciology and Geocryology, 2003, 25(2): 124-129. ]
[37]	沈伟峰, 缪启龙, 魏铁鑫, 等. 中亚地区近130多a温度变化特征[J]. 干旱气象, 2013, 31(1): 32-36, 42.
	[Shen Weifeng, Miao Qilong, Wei Tiexin, et al. Analysis of temperature variation in recent 130 years in Central Asia[J]. Journal of Arid Meteorology, 2013, 31(1): 32-36, 42. ]
[38]	康世昌, 郭万钦, 钟歆玥, 等. 全球山地冰冻圈变化、影响与适应[J]. 气候变化研究进展, 2020, 16(2): 143-152.
	[Kang Shichang, Guo Wanqin, Zhong Xinyue, et al. Changes in the mountain cryosphere and their impacts and adaptation measures[J]. Climate Change Research, 2020, 16(2): 143-152. ]
[39]	施雅风. 山地冰川与湖泊萎缩所指示的亚洲中部气候干暖化趋势与未来展望[J]. 地理学报, 1990, 45(1): 1-13. doi: 10.11821/xb199001001
	[Shi Yafeng. Glacier recession and lake shrinkage indicating the climatic warming and drying trend in Central Asia[J]. Acta Geographica Sinica, 1990, 45(1): 1-13. ] doi: 10.11821/xb199001001
[40]	Kapitsa V, Shahgedanova M, Severskiy I, et al. Assessment of changes in mass balance of the Tuyuksu group of Glaciers, northern Tien Shan, between 1958 and 2016 using ground-based observations and pléiades satellite imagery[J]. Frontiers in Earth Science, 2020, 8: 259. doi: 10.3389/feart.2020.00259

	校正前		校正后
	R²	ARE/%	R²	ARE/%
气温	0.78	104.86	0.78	3.71
降水	0.63	30.91	0.74	12.51

影响因子	贡献率/%
影响因子	1960—1986年	1987—2017年
山区降水	15.17	22.11
山区气温	2.31	3.08
灌溉引水	71.64	13.85
湖区降水	10.34	15.72
湖区蒸发	0.55	45.25

近60 a伊塞克湖水量平衡变化及影响因素分析

Analysis of water balance change and influencing factors in Issyk-Kul Lake in recent 60 years

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[4]	唐可欣, 郭建斌, 何亮, 陈林, 万龙. 中国旱区GPP时空演变特征及影响因素研究[J]. 干旱区研究, 2024, 41(6): 964-973.
[5]	张嘉琪, 刘招, 韩忠青, 王丽霞, 张晋霞, 岳甲寅, 管子隆. 气候变化下泾河流域蓝绿水变化趋势及预测[J]. 干旱区研究, 2024, 41(12): 2045-2055.
[6]	张倩, 曹广超, 张乐乐, 赵美亮. 祁连山南坡植被绿度时空变化及其对气候变化和人类活动的响应[J]. 干旱区研究, 2024, 41(12): 2143-2153.
[7]	胡广录, 樊亚仑, 陶虎, 李昊辰, 杨鹏华. 石羊河下游蔡旗站径流变化趋势及影响因素[J]. 干旱区研究, 2024, 41(11): 1842-1852.
[8]	杨斐, 张文韬, 张飞民, 王澄海. 1961—2022年祁连山气候特征及其变化[J]. 干旱区研究, 2024, 41(10): 1627-1638.
[9]	张音, 孙从建, 刘庚, 钞锦龙, 耿甜伟. 近20 a塔里木河流域山区NDSI对气候变化的响应[J]. 干旱区研究, 2024, 41(10): 1639-1648.
[10]	程倩, 齐月, 刘明春, 张鹏, 丁文魁, 李兴宇, 任丽雯, 杨华. 气候变化及人类活动背景下石羊河流域生态与水资源变化特征[J]. 干旱区研究, 2024, 41(10): 1672-1684.
[11]	樊玉科, 任菊, 王润龙, 周栋栋, 潘自凯, 张晓玮, 周晓雷. 气候变化背景下白皮松在中国潜在适宜分布预测[J]. 干旱区研究, 2024, 41(10): 1719-1730.
[12]	齐容镰, 李庆波, 任佳, 邹苗, 杨昊鹏, 魏耀峰, 唐琼. “三北”工程地区植被覆盖变化特征及其驱动力分析——以宁夏为例[J]. 干旱区研究, 2024, 41(10): 1740-1752.
[13]	赵雨琪, 魏天兴. 1990—2020年黄土高原典型县域植被覆盖变化及影响因素[J]. 干旱区研究, 2024, 41(1): 147-156.
[14]	胡广录,陶虎,焦娇,白元儒,陈海志,麻进. 黑河中游正义峡径流变化趋势及归因分析[J]. 干旱区研究, 2023, 40(9): 1414-1424.
[15]	周小东, 常顺利, 王冠正, 张毓涛, 喻树龙, 张同文. 天山北坡中段雪岭云杉径向生长对气候变化的响应[J]. 干旱区研究, 2023, 40(8): 1215-1228.