Multi-spectral remote sensing based land surface temperature retrieval and isolated permafrost zone segmentation

Wang Chunjiao; Shan Monan; Hu Zhaoguang; Shan Wei

Volume 44 Issue 4

May 2015

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Article Navigation > Infrared and Laser Engineering > 2015 > 44(4): 1390-1396

Wang Chunjiao, Shan Monan, Hu Zhaoguang, Shan Wei. Multi-spectral remote sensing based land surface temperature retrieval and isolated permafrost zone segmentation[J]. Infrared and Laser Engineering, 2015, 44(4): 1390-1396.

Citation:

Wang Chunjiao, Shan Monan, Hu Zhaoguang, Shan Wei. Multi-spectral remote sensing based land surface temperature retrieval and isolated permafrost zone segmentation[J]. Infrared and Laser Engineering, 2015, 44(4): 1390-1396.

Multi-spectral remote sensing based land surface temperature retrieval and isolated permafrost zone segmentation

1.
Institute of Cold Regions Science and Engineering,Northeast Forestry University,Harbin 150040,China;
2.
Forestry Department of Beijing Forestry University,Beijing 100083,China

Received Date: 2014-08-05
Rev Recd Date: 2014-09-10
Publish Date: 2015-04-25

Abstract

Affected by global climate change, the permafrost in northeast high latitude permafrost area of our country was degraded significantly, and the water phase change seriously affected the mechanical indexes of soil during the thawing process of frozen soil. Due to the permafrost melting of high latitude permafrost regions in China in recent years, a plurality of freeway roadbed has landslide, and uneven subsidence and other geological disasters had repeated in the northern part of Heilongjiang Province. In order to study the island permafrost distribution, choosing the K153-K183 Road area from Bei'an to Heihe expressway as the study area, the 3 Landsat 7 ETM+ image data converging the study area was choosen respectively on March, May, September in 2009. The surface temperature map of the corresponding date was obtained and the relationship between ground temperature and NDVI, DEM was analyzed through the retrieval of the infrared surface temperature in the study area using the radiation transfer equation method. Then the map layer of the inversion results was classified using natural breakpoint classification. The distribution map of the low temperature area of the corresponding moment was obtained through the analysis and the artificial interpretation of the surface temperature change of the study area. Frozen soil distribution map was obtained in the study area in 2009 on the intersection operation of the low temperature zone. It had a good consistency comparing with the expressway permafrost investigation results from Bei'an to Heihe.
- permafrost,
- permafrost distribution,
- infrared LST,
- lesser Khingan mountains,
- multispectral RS

References

[1]
[2]	Jin Huijun, Yu Shaopeng, Lv Lanzhi, et al. Preliminary evaluation of permafrost degradation and its trend in Greater Khingan Range[J]. Journal of Glaciology and Geocryology, 2006, 28(4): 467-474. (in Chinese) 金会军, 于少鹏, 吕兰芝, 等. 大兴安岭多年冻土退化及其趋势初步评估[J]. 冰川冻土, 2006, 28(4): 467-474.
[3]
[4]	San Wei, Guo Ying, Wang Fawu, et al. Environmental science and engineering：landslides in cold regions in the context of climate change[D]. Switzerland: Springer International Publishing, 2013.
[5]	Xin Kuide, Ren Qijia. Permafrost distribution in Northeast China[J]. Geological Knowledge, 1956, 1(10): 15-18. (in Chinese) 辛奎德, 任其甲. 中国东北地区多年冻土的分布[J]. 地质知识, 1956, 1(10): 15- 18.
[6]
[7]	Zhou Youwu, Wang Yinxue. Permafrost temperature, distribution and global warming in China[J]. Journal of Glaciology and Geocryology, 1996, 18(special issue): 139-147. (in Chinese) 周幼吾, 王银学. 我国东北部冻土温度和分布与气候变暖[J]. 冰川冻土, 1996, 18 (special issue): 139-147.
[8]
[9]
[10]	Wei Zhi, Jin Huijun. Prediction of permafrost change in northeast area under conditions of climate changing[J]. China Science, 2011, 41(1): 74-84. (in Chinese) 魏智, 金会军. 气候变化条件下东北地区多年冻土变化预测[J]. 中国科学, 2011, 41(1): 74-84.
[11]
[12]	Zhou Qing, Zhao Fengsheng, Gao Wenhua. NCEP/NCAR hourly analysis and measured surface temperature and ground temperature contrast analysis in China[J]. Meteorology, 2008, 34(2): 83-91. (in Chinese) 周青, 赵凤生, 高文华. NCEP/NCAR逐时分析与中国实测地表温度和地面气温对比分析[J]. 气象, 2008, 34(2): 83-91.
[13]
[14]	McClymont, Alastair F, Hayashi Masaki, et al. Geophysical imaging and thermal modeling of subsurface morphology and thaw evolution of discontinuous permafrost[J]. Journal of Geophysical Research-earth Surface, 2013, 118(3): 1826-1837.
[15]	Otto J C, Keuschnig M, Gotz J, et al. Detection of mountain permafrost by combining high resolution surface and subsurface information an example from the glatzbach catchment, austrian alps.[J]. Geografiska Annaler Series A-Physical Geography, 2012, 94A(1): 43-57.
[16]
[17]
[18]	De Pascale, Gregory P, Pollard, et al. Geophysical mapping of ground ice using a combination of capacitive coupled resistivity and ground-penetrating radar, northwest Territories, Canada[J]. Journal of Geophysical Research-Earth Surface, 2008, 113(F2): 1-15.
[19]
[20]	Wu T H, Li S X, Cheng G D, et al. Using ground-penetrating radar to detect permafrost degradation in the northern limit of permafrost on the Tibetan Plateau[J]. Cold Regions Science and Technology, 2005, 41(3): 211 -219.
[21]
[22]	Shi Rui. Simulation of land surface process characteristics in cold region[D]. Lanzhou: Lanzhou University, 2007. (in Chinese) 师锐. 寒区陆面过程特征的模拟研究[D]. 兰州: 兰州大学, 2007.
[23]
[24]	Qin Zhihao, Li Wenjuan, Xu Bin, et al. Land surface emissivity estimate of Landsat TM6 band range[J]. Land Resources Remote Sensing, 2004(3): 28-41. (in Chinese) 覃志豪, 李文娟, 徐斌, 等. 陆地卫星TM6波段范围内地表比辐射率的估计[J]. 国土资源遥感, 2004(3): 28-41.
[25]
[26]	Li Miaomiao, Wu Bingfang. Vegetation coverage estimate of Miyun Reservoir upstream by remote sensing[J]. Recourses Science, 2004, 26(4): 153-159. (in Chinese) 李苗苗, 吴炳方. 密云水库上游植被覆盖度的遥感估计[J]. 资源科学, 2004, 26 (4): 153-159.

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通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

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Multi-spectral remote sensing based land surface temperature retrieval and isolated permafrost zone segmentation

1. Institute of Cold Regions Science and Engineering,Northeast Forestry University,Harbin 150040,China;

2. Forestry Department of Beijing Forestry University,Beijing 100083,China

Received Date: 2014-08-05

Rev Recd Date: 2014-09-10

Publish Date: 2015-04-25

Key words:

Abstract: Affected by global climate change, the permafrost in northeast high latitude permafrost area of our country was degraded significantly, and the water phase change seriously affected the mechanical indexes of soil during the thawing process of frozen soil. Due to the permafrost melting of high latitude permafrost regions in China in recent years, a plurality of freeway roadbed has landslide, and uneven subsidence and other geological disasters had repeated in the northern part of Heilongjiang Province. In order to study the island permafrost distribution, choosing the K153-K183 Road area from Bei'an to Heihe expressway as the study area, the 3 Landsat 7 ETM+ image data converging the study area was choosen respectively on March, May, September in 2009. The surface temperature map of the corresponding date was obtained and the relationship between ground temperature and NDVI, DEM was analyzed through the retrieval of the infrared surface temperature in the study area using the radiation transfer equation method. Then the map layer of the inversion results was classified using natural breakpoint classification. The distribution map of the low temperature area of the corresponding moment was obtained through the analysis and the artificial interpretation of the surface temperature change of the study area. Frozen soil distribution map was obtained in the study area in 2009 on the intersection operation of the low temperature zone. It had a good consistency comparing with the expressway permafrost investigation results from Bei'an to Heihe.

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Reference (26)

[1]
[2]	Jin Huijun, Yu Shaopeng, Lv Lanzhi, et al. Preliminary evaluation of permafrost degradation and its trend in Greater Khingan Range[J]. Journal of Glaciology and Geocryology, 2006, 28(4): 467-474. (in Chinese) 金会军, 于少鹏, 吕兰芝, 等. 大兴安岭多年冻土退化及其趋势初步评估[J]. 冰川冻土, 2006, 28(4): 467-474.
[3]
[4]	San Wei, Guo Ying, Wang Fawu, et al. Environmental science and engineering：landslides in cold regions in the context of climate change[D]. Switzerland: Springer International Publishing, 2013.
[5]	Xin Kuide, Ren Qijia. Permafrost distribution in Northeast China[J]. Geological Knowledge, 1956, 1(10): 15-18. (in Chinese) 辛奎德, 任其甲. 中国东北地区多年冻土的分布[J]. 地质知识, 1956, 1(10): 15- 18.
[6]
[7]	Zhou Youwu, Wang Yinxue. Permafrost temperature, distribution and global warming in China[J]. Journal of Glaciology and Geocryology, 1996, 18(special issue): 139-147. (in Chinese) 周幼吾, 王银学. 我国东北部冻土温度和分布与气候变暖[J]. 冰川冻土, 1996, 18 (special issue): 139-147.
[8]
[9]
[10]	Wei Zhi, Jin Huijun. Prediction of permafrost change in northeast area under conditions of climate changing[J]. China Science, 2011, 41(1): 74-84. (in Chinese) 魏智, 金会军. 气候变化条件下东北地区多年冻土变化预测[J]. 中国科学, 2011, 41(1): 74-84.
[11]
[12]	Zhou Qing, Zhao Fengsheng, Gao Wenhua. NCEP/NCAR hourly analysis and measured surface temperature and ground temperature contrast analysis in China[J]. Meteorology, 2008, 34(2): 83-91. (in Chinese) 周青, 赵凤生, 高文华. NCEP/NCAR逐时分析与中国实测地表温度和地面气温对比分析[J]. 气象, 2008, 34(2): 83-91.
[13]
[14]	McClymont, Alastair F, Hayashi Masaki, et al. Geophysical imaging and thermal modeling of subsurface morphology and thaw evolution of discontinuous permafrost[J]. Journal of Geophysical Research-earth Surface, 2013, 118(3): 1826-1837.
[15]	Otto J C, Keuschnig M, Gotz J, et al. Detection of mountain permafrost by combining high resolution surface and subsurface information an example from the glatzbach catchment, austrian alps.[J]. Geografiska Annaler Series A-Physical Geography, 2012, 94A(1): 43-57.
[16]
[17]
[18]	De Pascale, Gregory P, Pollard, et al. Geophysical mapping of ground ice using a combination of capacitive coupled resistivity and ground-penetrating radar, northwest Territories, Canada[J]. Journal of Geophysical Research-Earth Surface, 2008, 113(F2): 1-15.
[19]
[20]	Wu T H, Li S X, Cheng G D, et al. Using ground-penetrating radar to detect permafrost degradation in the northern limit of permafrost on the Tibetan Plateau[J]. Cold Regions Science and Technology, 2005, 41(3): 211 -219.
[21]
[22]	Shi Rui. Simulation of land surface process characteristics in cold region[D]. Lanzhou: Lanzhou University, 2007. (in Chinese) 师锐. 寒区陆面过程特征的模拟研究[D]. 兰州: 兰州大学, 2007.
[23]
[24]	Qin Zhihao, Li Wenjuan, Xu Bin, et al. Land surface emissivity estimate of Landsat TM6 band range[J]. Land Resources Remote Sensing, 2004(3): 28-41. (in Chinese) 覃志豪, 李文娟, 徐斌, 等. 陆地卫星TM6波段范围内地表比辐射率的估计[J]. 国土资源遥感, 2004(3): 28-41.
[25]
[26]	Li Miaomiao, Wu Bingfang. Vegetation coverage estimate of Miyun Reservoir upstream by remote sensing[J]. Recourses Science, 2004, 26(4): 153-159. (in Chinese) 李苗苗, 吴炳方. 密云水库上游植被覆盖度的遥感估计[J]. 资源科学, 2004, 26 (4): 153-159.

Multi-spectral remote sensing based land surface temperature retrieval and isolated permafrost zone segmentation

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