Factors Influencing the Spatiotemporal Changes of Permafrost in Northeast China from 1982 to 2020

被引:4
作者
Yang, Dongyu [1 ,2 ]
Zhan, Daqing [1 ,2 ]
Li, Miao [1 ,2 ]
Zang, Shuying [1 ,2 ]
机构
[1] Harbin Normal Univ, Coll Geog Sci, Harbin 150025, Peoples R China
[2] Heilongjiang Prov Key Lab Geog Environm Monitoring, Harbin 150025, Peoples R China
基金
中国国家自然科学基金;
关键词
permafrost; northeast permafrost area; surface frost number model; influencing factors; change trend; SURFACE FROST NUMBER; ACTIVE-LAYER; SNOW COVER; TEMPERATURE; CLIMATE; VEGETATION; RESPONSES; DEGRADATION; AGREEMENT;
D O I
10.3390/land12020350
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Permafrost in northeast China, which is at the southern edge of the high-latitude permafrost belt in Eurasia, is extremely sensitive to climate warming. However, the distribution of permafrost in the region in recent years has been poorly studied, and there is a lack of understanding of the relative importance of environmental factors affecting the region. Based on observed ground surface temperature (GST) data, this study quantifies changes in the permafrost area in northeast China from 1982 to 2020 using a surface frost number model, and the influencing factors are identified based on dominance analysis and spatial correlation analysis. The results suggest that the permafrost in northeast China during the observation period underwent degradation with a degradation rate of 0.33 x 10(4) km(2)/a. In addition, the permafrost degradation also exhibited altitudinal and latitudinal zonality. Permafrost degradation under typical grassland, deciduous forest, and savannah cover was more significant than that under evergreen forest, mixed forest, and shrubbery cover. As revealed by the dominance analysis results, the annual average snow cover, annual average snow depth and annual average normalized difference vegetation index (NDVI) had the largest contributions to the variance of the permafrost area in northeast China, accounting for 88.3% of the total variance contribution of the six influencing factors. The spatial correlation results reveal that areas with a significantly increased NDVI and significantly reduced snow depth and snow cover were coincident with areas with significantly degraded permafrost. Hence, the snow cover, snow depth, and NDVI were found to have the greatest influence on the permafrost distribution in northeast China. The results of this study evidently increase the understanding of the changing permafrost in northeast China, providing important knowledge about permafrost for researchers and the related community.
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页数:22
相关论文
共 70 条
[1]  
[高红豆 Gao Hongdou], 2022, [干旱区资源与环境, Journal of Arid Land Resources and Environment], V36, P99
[2]   Global observed changes in daily climate extremes of temperature and precipitation [J].
Alexander, LV ;
Zhang, X ;
Peterson, TC ;
Caesar, J ;
Gleason, B ;
Tank, AMGK ;
Haylock, M ;
Collins, D ;
Trewin, B ;
Rahimzadeh, F ;
Tagipour, A ;
Kumar, KR ;
Revadekar, J ;
Griffiths, G ;
Vincent, L ;
Stephenson, DB ;
Burn, J ;
Aguilar, E ;
Brunet, M ;
Taylor, M ;
New, M ;
Zhai, P ;
Rusticucci, M ;
Vazquez-Aguirre, JL .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2006, 111 (D5)
[3]   Controls on Soil Organic Matter Degradation and Subsequent Greenhouse Gas Emissions Across a Permafrost Thaw Gradient in Northern Sweden [J].
AminiTabrizi, Roya ;
Wilson, Rachel M. ;
Fudyma, Jane D. ;
Hodgkins, Suzanne B. ;
Heyman, Heino M. ;
Rich, Virginia, I ;
Saleska, Scott R. ;
Chanton, Jeffrey P. ;
Tfaily, Malak M. .
FRONTIERS IN EARTH SCIENCE, 2020, 8
[4]  
[Anonymous], 1988, MAP SNOW ICE FROZEN
[5]  
[Anonymous], 1993, Journal of Glaciology and Geocryology
[6]  
[Anonymous], 1981, Journal of Glaciology and Geocryology
[7]  
Ban J., 2019, HEILONGJIANG METEORO, V36, P14, DOI [10.3969/j.issn.1002-252X.2019.01.004, DOI 10.3969/J.ISSN.1002-252X.2019.01.004]
[8]  
Benesty Jacob, 2009, The SAGE Encyclopedia of Educational Research, Measurement, and Evaluation, P1, DOI DOI 10.4135/9781506326139
[9]   Thermal and hydrologic dynamics of the active layer at a continuous permafrost site (Taymyr Peninsula, Siberia) [J].
Boike, J ;
Roth, K ;
Overduin, PP .
WATER RESOURCES RESEARCH, 1998, 34 (03) :355-363
[10]   Long-term perspectives on lagged ecosystem responses to climate change: Permafrost in boreal peatlands and the Grassland/Woodland boundary [J].
Camill, P ;
Clark, JS .
ECOSYSTEMS, 2000, 3 (06) :534-544