Spatial-temporal variations in near-surface soil freeze-thaw cycles in the source region of the Yellow River during the period 2002-2011 based on the Advanced Microwave Scanning Radiometer for the Earth Observing System (AMSR-E) data
WANG Rui1, ZHU Qingke1, *, MA Hao2, AI Ning3
1 School of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China; 2 Northwest Institute of Forest Inventory and Planning and Design, State Forestry Administration, Xi'an 710048, China; 3 College of Life Science, Yan'an University, Yan'an 716000, China
Spatial-temporal variations in near-surface soil freeze-thaw cycles in the source region of the Yellow River during the period 2002-2011 based on the Advanced Microwave Scanning Radiometer for the Earth Observing System (AMSR-E) data
WANG Rui1, ZHU Qingke1, *, MA Hao2, AI Ning3
1 School of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China; 2 Northwest Institute of Forest Inventory and Planning and Design, State Forestry Administration, Xi'an 710048, China; 3 College of Life Science, Yan'an University, Yan'an 716000, China
摘要 Detecting near-surface soil freeze-thaw cycles in high-altitude cold regions is important for understanding the Earth's surface system, but such studies are rare. In this study, we detected the spatial-temporal variations in near-surface soil freeze-thaw cycles in the source region of the Yellow River (SRYR) during the period 2002-2011 based on data from the Advanced Microwave Scanning Radiometer for the Earth Observing System (AMSR-E). Moreover, the trends of onset dates and durations of the soil freeze-thaw cycles under different stages were also analyzed. Results showed that the thresholds of daytime and nighttime brightness temperatures of the freeze-thaw algorithm for the SRYR were 257.59 and 261.28 K, respectively. At the spatial scale, the daily frozen surface (DFS) area and the daily surface freeze-thaw cycle surface (DFTS) area decreased by 0.08% and 0.25%, respectively, and the daily thawed surface (DTS) area increased by 0.36%. At the temporal scale, the dates of the onset of thawing and complete thawing advanced by 3.10 (±1.4) and 2.46 (±1.4) days, respectively; and the dates of the onset of freezing and complete freezing were delayed by 0.9 (±1.4) and 1.6 (±1.1) days, respectively. The duration of thawing increased by 0.72 (±0.21) day/a and the duration of freezing decreased by 0.52 (±0.26) day/a. In conclusion, increases in the annual minimum temperature and winter air temperature are the main factors for the advanced thawing and delayed freezing and for the increase in the duration of thawing and the decrease in the duration of freezing in the SRYR.
Abstract：
Detecting near-surface soil freeze-thaw cycles in high-altitude cold regions is important for understanding the Earth's surface system, but such studies are rare. In this study, we detected the spatial-temporal variations in near-surface soil freeze-thaw cycles in the source region of the Yellow River (SRYR) during the period 2002-2011 based on data from the Advanced Microwave Scanning Radiometer for the Earth Observing System (AMSR-E). Moreover, the trends of onset dates and durations of the soil freeze-thaw cycles under different stages were also analyzed. Results showed that the thresholds of daytime and nighttime brightness temperatures of the freeze-thaw algorithm for the SRYR were 257.59 and 261.28 K, respectively. At the spatial scale, the daily frozen surface (DFS) area and the daily surface freeze-thaw cycle surface (DFTS) area decreased by 0.08% and 0.25%, respectively, and the daily thawed surface (DTS) area increased by 0.36%. At the temporal scale, the dates of the onset of thawing and complete thawing advanced by 3.10 (±1.4) and 2.46 (±1.4) days, respectively; and the dates of the onset of freezing and complete freezing were delayed by 0.9 (±1.4) and 1.6 (±1.1) days, respectively. The duration of thawing increased by 0.72 (±0.21) day/a and the duration of freezing decreased by 0.52 (±0.26) day/a. In conclusion, increases in the annual minimum temperature and winter air temperature are the main factors for the advanced thawing and delayed freezing and for the increase in the duration of thawing and the decrease in the duration of freezing in the SRYR.
基金资助:This study was supported by the National Science and Technology Support Plan of China (2015BAD07B02). We sincerely thank the anonymous reviewers and editors for their valuable comments.
通讯作者: ZHU Qingke (E-mail: zhuqingke@sohu.com)
引用本文:
WANG Rui,ZHU Qingke,MA Hao等. Spatial-temporal variations in near-surface soil freeze-thaw cycles in the source region of the Yellow River during the period 2002-2011 based on the Advanced Microwave Scanning Radiometer for the Earth Observing System (AMSR-E) data[J]. Journal of Arid Land, 2017, 9(6): 850-864.
WANG Rui,ZHU Qingke,MA Hao et al. Spatial-temporal variations in near-surface soil freeze-thaw cycles in the source region of the Yellow River during the period 2002-2011 based on the Advanced Microwave Scanning Radiometer for the Earth Observing System (AMSR-E) data[J]. Journal of Arid Land, 2017, 9(6): 850-864.
2017, Vol. 9 
