Monitoring Changes to Arctic Vegetation and Glaciers at Ny-Alesund, Svalbard, Based on Time Series Remote Sensing

被引:1
|
作者
Ren, Guangbo [1 ]
Wang, Jianbu [1 ]
Lu, Yunfei [2 ]
Wu, Peiqiang [1 ]
Lu, Xiaoqing [2 ]
Chen, Chen [1 ]
Ma, Yi [1 ]
机构
[1] Minist Nat Resources, Lab Marine Phys & Remote Sensing, Inst Oceanog 1, Qingdao 266061, Peoples R China
[2] Minist Nat Resources, Natl Satellite Ocean Applicat Serv, Beijing 100081, Peoples R China
基金
中国国家自然科学基金;
关键词
arctic coastal zone; arctic vegetation remote sensing; arctic glacier remote sensing; change monitoring; CLIMATE-CHANGE; COVER; AREA; NDVI; ELEVATION; FORELAND; BALANCE; GROWTH; CLOUD; ICE;
D O I
10.3390/rs13193845
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Climate change has profoundly affected global ecological security. The most vulnerable region on Earth is the high-latitude Arctic. Identifying the changes in vegetation coverage and glaciers in high-latitude Arctic coastal regions is important for understanding the process and impact of global climate change. Ny-Alesund, the northern-most human settlement, is typical of these coastal regions and was used as a study site. Vegetation and glacier changes over the past 35 years were studied using time series remote sensing data from Landsat 5/7/8 acquired in 1985, 1989, 2000, 2011, 2015 and 2019. Site survey data in 2019, a digital elevation model from 2009 and meteorological data observed from 1985 to 2019 were also used. The vegetation in the Ny-Alesund coastal zone showed a trend of declining and then increasing, with a breaking point in 2000. However, the area of vegetation with coverage greater than 30% increased over the whole study period, and the wetland moss area also increased, which may be caused by the accelerated melting of glaciers. Human activities were responsible for the decline in vegetation cover around Ny-Alesund owing to the construction of the town and airport. Even in areas with vegetation coverage of only 13%, there were at least five species of high-latitude plants. The melting rate of five major glaciers in the study area accelerated, and approximately 82% of the reduction in glacier area occurred after 2000. The elevation of the lowest boundary of the five glaciers increased by 50-70 m. The increase in precipitation and the average annual temperature after 2000 explains the changes in both vegetation coverage and glaciers in the study period.
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页数:23
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