近30年青藏高原可可西里盐湖面积动态变化及其影响因素分析

doi:10.13474/j.cnki.11-2246.2023.0096

测绘通报 ›› 2023, Vol. 0 ›› Issue (4): 6-9.doi: 10.13474/j.cnki.11-2246.2023.0096

近30年青藏高原可可西里盐湖面积动态变化及其影响因素分析

郭子瑛¹, 廖中平¹, 刘宝康², 徐正东¹, 刘铭¹

1. 长沙理工大学交通运输工程学院, 湖南长沙 410004;
2. 天水师范学院资源与环境工程学院, 甘肃天水 741000

收稿日期:2022-08-26 发布日期:2023-04-25
作者简介:郭子瑛(1998—),女,硕士,研究方向为摄影测量与遥感。E-mail:18893783468@163.com

Dynamic changes of Yanhu Lake in Hoh Xil area on Qinghai-Tibet Plateau in recent 30 years and analysis of its influencing factors

GUO Ziying¹, LIAO Zhongping¹, LIU Baokang², XU Zhengdong¹, LIU Ming¹

1. School of Traffic & Transportation Engineering, Changsha University of Science & Technology, Changsha 410004, China;
2. College of resources and environmental Engineering, Tianshui Normal University, Tianshui 741000, China

Received:2022-08-26 Published:2023-04-25

摘要/Abstract

摘要： 青藏高原湖泊是全球气候变化的敏感指标,对全球气候变化具有很强的反馈作用。由于卓乃湖的溃堤,地处于青藏高原腹地的可可西里盐湖迅速扩张,这不仅对周边草地植被及流经的冻土造成危害,对青藏铁路和青藏公路的正常运行也产生了干扰。本文利用多源遥感监测手段对可可西里盐湖近30年面积进行监测,从时空变化趋势上提取盐湖面积的动态变化并进行成因分析。结果表明:①2011年9月卓乃湖溃决,导致可可西里盐湖面积1990—2020年增大了178.535 km²;②自2020年可可西里盐湖的引流工程完工,盐湖面积得到有效遏制,并在2021年缩小至191.145 km²;③盐湖湖岸线自1990—2020年主要在东南部和西南部有显著扩张,而最大的变化是盐湖东部由以前伸入湖中央的半岛变为孤岛;④面积与降水、气温呈显著相关关系,与日照时长、冰川融水呈弱相关关系。

关键词: 青藏高原, 可可西里, 盐湖, 水体模型, 湖泊变化, 成因分析

Abstract: The lakes on the Qinghai-Tibet Plateau are sensitive indicators of global climate change and have a strong feedback effect on global climate change. Due to the breakwater of Zhuonai Lake, the Yanhu Lake of Hoh Xil, located in the hinterland of the Qinghai-Tibet Plateau, is expanding rapidly, which not only harms the surrounding grassland vegetation and the permafrost flowing through, but also interferes with the normal operation of the Qinghai-Tibet railway and the Qinghai-Tibet highway. In this paper, multi-source remote sensing monitoring means are used to monitor the Yanhu Lake in Hoh Xil area in recent 30 years, and the dynamic changes of the area of the Yanhu Lake are extracted from the trend of temporal and spatial changes, and the causes are analyzed. The results show that: ① The collapse of Zhuonai Lake in September 2011 increased the Yanhu Lake of Hoh Xil by 178.535 km² from 1990 to 2020.② Since the completion of the diversion project of Yanhu Lake in Hoh Xil area in 2020, the area of the Yanhu Lake has been effectively contained and will be reduced to 191.145 km² in 2021. ③ The shoreline of the Yanhu Lake has expanded significantly in the southeast and southwest from 1990 to 2020, and the biggest change is that the eastern part of the Yanhu Lake has become an island from the peninsula that once stretched into the center of the lake. ④ The area has a significant correlation with precipitation and temperature, and a weak correlation with sunshine duration and glacial melt water.

Key words: Qinghai-Tibet Plateau, Hoh Xil, Yanhu Lake, water model, lake change, cause analysis

中图分类号:

P237

郭子瑛, 廖中平, 刘宝康, 徐正东, 刘铭. 近30年青藏高原可可西里盐湖面积动态变化及其影响因素分析[J]. 测绘通报, 2023, 0(4): 6-9.

GUO Ziying, LIAO Zhongping, LIU Baokang, XU Zhengdong, LIU Ming. Dynamic changes of Yanhu Lake in Hoh Xil area on Qinghai-Tibet Plateau in recent 30 years and analysis of its influencing factors[J]. Bulletin of Surveying and Mapping, 2023, 0(4): 6-9.

参考文献

[1] 姚晓军,孙美平,宫鹏,等. 可可西里盐湖湖水外溢可能性初探[J]. 地理学报,2016,71(9):1520-1527.
[2] 车向红,冯敏,姜浩,等. 2000-2013年青藏高原湖泊面积MODIS遥感监测分析[J]. 地球信息科学学报,2015,17(1):99-107.
[3] 张国庆. 青藏高原湖泊变化遥感监测及其对气候变化的响应研究进展[J]. 地理科学进展,2018,37(2):214-223.
[4] ZHANG Zengxin,CHANG Juan,XU Chongyu,et al. The response of lake area and vegetation cover variations to climate change over the Qinghai-Tibetan Plateau during the past 30years[J]. The Science of the Total Environment,2018,635:S0048-S9697(18)31278-6.
[5] 董斯扬,薛娴,尤全刚,等. 近40年青藏高原湖泊面积变化遥感分析[J]. 湖泊科学,2014,26(4):535-544.
[6] 姚晓军,刘时银,李龙,等. 近40年可可西里地区湖泊时空变化特征[J]. 地理学报,2013,68(7):886-896.
[7] 陈强,冶富寿,陈育红,等. 青藏高原可可西里盐湖水量平衡初步分析[J]. 人民长江,2020,51(5):94-98.
[8] 杜玉娥,刘宝康,贺卫国,等. 1976-2017年青藏高原可可西里盐湖面积动态变化及成因分析[J]. 冰川冻土,2018,40(1):47-54.
[9] 刘宝康,李林,杜玉娥,等. 青藏高原可可西里卓乃湖溃堤成因及其影响分析[J]. 冰川冻土,2016,38(2):305-311.
[10] 谢昌卫,张钰鑫,刘文惠,等. 可可西里卓乃湖溃决后湖区环境变化及盐湖可能的溃决方式[J]. 冰川冻土,2020,42(4):1344-1352.
[11] 贺鹏文,童立强文,涂杰楠文,等. 与时间赛跑:可可西里盐湖漫溢险情化解始末[J]. 自然资源科普与文化,2021(3):20-27.
[12] 陈强,温得平,文雄飞,等. 青海可可西里盐湖水文监测方案初步构想[J]. 人民黄河,2019,41(11):7-10.
[13] 刘文惠,谢昌卫,王武,等. 青藏高原可可西里盐湖水位上涨趋势及溃决风险分析[J]. 冰川冻土,2019,41(6):1467-1474.
[14] 李琳,谭德宝,文雄飞,等.气候变化对可可西里盐湖流域湖泊水量变化的影响分析[J/OL].长江科学院院报.[2022-09-30].http://kns.cnki.net/kcms/detail/42.1171.TV.20220223.1435.002.html.
[15] 罗永臻,董春. 基于遥感影像和DEM数据的高原湖泊溢流模拟[J]. 遥感信息,2022,37(3):28-33.
[16] MCFEETERS S K. The use of the normalized difference water index (NDWI) in the delineation of open water features[J]. International Journal of Remote Sensing,1996,17(7):1425-1432.
[17] 王仁军,刘宝康,杜玉娥,等. 基于GF-6的可可西里典型湖泊水体面积提取方法研究[J]. 测绘通报,2022(5):32-37.
[18] 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.

近30年青藏高原可可西里盐湖面积动态变化及其影响因素分析

Dynamic changes of Yanhu Lake in Hoh Xil area on Qinghai-Tibet Plateau in recent 30 years and analysis of its influencing factors

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