Heterogeneity of Surface Heat Exchange of Slopes and Potential Drivers of the Initiation of Thaw Slump, Qinghai-Tibet Plateau

Xingwen Fan; Wenjiao Li; Xuyang Wu; Miaomiao Yao; Fujun Niu; Zhanju Lin

doi:10.1007/s13753-023-00508-8

Volume 14 Issue 4

Sep. 2023

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Xingwen Fan, Wenjiao Li, Xuyang Wu, Miaomiao Yao, Fujun Niu, Zhanju Lin. Heterogeneity of Surface Heat Exchange of Slopes and Potential Drivers of the Initiation of Thaw Slump, Qinghai-Tibet Plateau[J]. International Journal of Disaster Risk Science, 2023, 14(4): 549-565. doi: 10.1007/s13753-023-00508-8

Citation:

Xingwen Fan, Wenjiao Li, Xuyang Wu, Miaomiao Yao, Fujun Niu, Zhanju Lin. Heterogeneity of Surface Heat Exchange of Slopes and Potential Drivers of the Initiation of Thaw Slump, Qinghai-Tibet Plateau[J]. International Journal of Disaster Risk Science, 2023, 14(4): 549-565. doi: 10.1007/s13753-023-00508-8

Citation:

Xingwen Fan, Wenjiao Li, Xuyang Wu, Miaomiao Yao, Fujun Niu, Zhanju Lin. Heterogeneity of Surface Heat Exchange of Slopes and Potential Drivers of the Initiation of Thaw Slump, Qinghai-Tibet Plateau[J]. International Journal of Disaster Risk Science, 2023, 14(4): 549-565. doi: 10.1007/s13753-023-00508-8

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Heterogeneity of Surface Heat Exchange of Slopes and Potential Drivers of the Initiation of Thaw Slump, Qinghai-Tibet Plateau

doi: 10.1007/s13753-023-00508-8

1. State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, 730000, China;
2. University of Chinese Academy of Sciences, Beijing, 100049, China

Funds:

This work was supported by the Second Tibet Plateau Scientific Expedition and Research Program (STEP) (Grant No. 2019QZKK0905), the Gansu Province Science and Technology Major Special Projects (Grant No. 22ZD6FA004), and the National Natural Science Foundation of China (Grant No. 41971089). We would like to thank the editor, the anonymous reviewers who provided insightful suggestions, and Brendan O’Neill for his constructive comments.

Accepted Date: 2023-05-31
Publish Date: 2023-09-07

Abstract

Abstract

In the mountainous permafrost area, most thaw slumps are distributed in north or northeast-facing shady slope areas. It is commonly known that there is a heterogeneity in permafrost between different slope aspects, but there has been a lack of detailed measured data to quantitatively evaluate their relationships, and in-depth understandings on how the slope aspects are linked to the distribution of thaw slumps. This study examined the heterogenous thermal regime, soil moisture content, and surface radiation at two slope sites with opposing aspects in a warming permafrost region on the Qinghai-Tibet Plateau (QTP). The results indicate that similar air temperatures (T_a) were monitored on the two slopes, but there were significant differences in ground temperature and moisture content in the active layer from 2016 to 2021. The sunny slope exhibited a higher mean annual ground surface temperature (T_s), and over the five years the mean annual temperature at the top of permafrost was 1.3–1.4℃ warmer on the sunny slope than the shady slope. On the contrary, the near-surface soil moisture content was about 10–13% lower on the sunny slope (~22–27%) than the shady slope (~35–38%) during the thawing season (June–September). Radiation data indicate that significantly higher shortwave downward radiation (DR) appeared at the sunny slope site. However, due to the greater surface albedo, the net radiation (R_n) was lower on the sunny slope. Slope aspect also affects the ground ice content due to its influence on ground temperature, freeze-thaw cycles, and soil moisture. Shady slopes have a shallower burial of ice-rich permafrost compared to sunny slopes. The results highlight greatly different near-surface ground thermal conditions at the two slope sites with different aspects in a mountainous permafrost region. This helps identify the slope-related causes of increasing thaw slumps and provides a basis for predicting their future development.
- Mountainous permafrost,
- Slope aspect,
- Soil moisture content,
- Surface heat exchange,
- Thaw slumps

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References(69)

References

[1]	Beltrami, H., and L. Kellman. 2003. An examination of short- and long-term air-ground temperature coupling. Global and Planetary Change 38(3-4):291-303.
[2]	Brown, R.J.E. 1973. Influence of climatic and terrain factors on ground temperatures at three locations in the permafrost region of Canada. In Proceedings of the 2nd International Conference on Permafrost, 13-28 July 1973, Yakutsk, USSR, 27-34.
[3]	Camill, P. 2000. How much do local factors matter for predicting transient ecosystem dynamics? Suggestions from permafrost formation in boreal peatlands. Global Change Biology 6(2):169-182.
[4]	Camill, P., and G.S. Clark. 1998. Climate change disequilibrium of boreal permafrost peatlands caused by local processes. The American Naturalist 15(3):207-222.
[5]	Chen, S., J. Chen, G. Lin, W. Zhang, H. Miao, L. Wei, J. Huang, and X. Han. 2009. Energy balance and partition in Inner Mongolia steppe ecosystems with different land use types. Agricultural and Forest Meteorology 149(11):1800-1809.
[6]	Cheng, G. 1983. Vertical and horizontal zonation of high altitude permafrost. In Proceedings of the 4th International Conference on Permafrost, 18-22 July 1983, Fairbanks, USA, 136-141.
[7]	Cheng, G. 2003. Influences of local factors on the distribution of permafrost and its enlightenment to the design of Qinghai-Tibet Railway. Science in China (Series D) 33(6):602-607 (in Chinese).
[8]	Cheng, G. 2004. Influences of local factors on permafrost occurrence and their implications for Qinghai-Xizang Railway design. Science in China (Series D) 47(8):704-709.
[9]	Cheng, G., and F. Dramis. 1992. Distribution of mountain permafrost and climate. Permafrost and Periglacial Processes 3:83-91.
[10]	Chou, Y., Y. Sheng, Z. Wen, and W. Ma. 2008. Calculation of temperature difference between sunny slope and shady slope along railways in permafrost regions on Qinghai-Tibet Plateau. Cold Regions Science and Technology 53:346-354.
[11]	Eaton, A.K., W.R. Rouse, P.M. Lafleur, P. Marsh, and P.D. Blanken. 2001. Surface energy balance of the western and central Canadian subarctic:Variations in the energy balance among five major terrain types. Journal of Climate 14:3692-3703.
[12]	Everett, D.H. 1961. The thermodynamics of frost damage to porous solids. Transactions of the Faraday Society 57:1541-1551.
[13]	Fan, X., Z. Lin, Z. Gao, X. Meng, F. Niu, J. Luo, G. Yin, F. Zhou, and A. Lan. 2021. Investigation into cryostructures and ground ice content in ice-rich permafrost area of the Qinghai-Tibet Plateau with CT scanning. Journal of Mountain Science 18(5):1208-1221.
[14]	Fan, X., Z. Lin, F. Niu, A. Lan, M. Yao, and W. Li. 2022. Near-surface heat transfer at two gentle slope sites with differing aspects, Qinghai-Tibet Plateau. Frontier in Environment Science 10:Article 1037331.
[15]	Ferrians, O.J. Jr, and G.D. Hobson. 1973. Mapping and predicting permafrost in North America:A review, 1963-1973. In Proceedings of the 2nd International Conference on Permafrost, 13-28 July 1973, Yakutsk, USSR, 479-498.
[16]	French, H.M. 2018. The periglacial environment, 4th edn. West Sussex, UK:Wiley.
[17]	Gorbunov, A.P. 1978. Permafrost in the mountains of Central Asia. In Proceedings of the 3rd International Conference on Permafrost, 10-13 July 1978, Edmonton, Canada, 372-377.
[18]	Gorbunov, A.P. 1988. The alpine permafrost zone of the USSR. In Proceedings of the 5th International Conference on Permafrost, 2-5 August 1988, Trondheim, Norway, 154-158.
[19]	Guo, D., and J. Sun. 2015. Permafrost thaw and associated settlement hazard onset timing over the Qinghai-Tibet Engineering Corridor. International Journal of Disaster Risk Science 6(3):347-358.
[20]	Harris, S.A. 1981. Climatic relationships of permafrost zones in areas of low winter snow-cover. Arctic 34(1):64-70.
[21]	Harris, S.A. 1986. Permafrost distribution, zonation and stability along the eastern ranges of the cordillera of North America. Arctic 39(1):29-38.
[22]	Heggem, E.S.F., B. Etzelmuller, S. Anarmaa, N. Sharkhuu, C.E. Goulden, and B. Nandinsetseg. 2006. Spatial distribution of ground surface temperatures and active layer depths in the Hovsgol area, northern Mongolia. Permafrost and Periglacial Processes 17:357-369.
[23]	Hu, Z., Z. Qian, G. Cheng, and J. Wang. 2002. Influence of solar radiation on embankment surface thermal regime of the Qinghai-Xizang Railway. Journal of Glaciology and Geocryology 24(2):121-128 (in Chinese).
[24]	Ishikawa, M., N. Sharkhuu, Y. Zhang, T. Kadota, and T. Ohata. 2010. Ground thermal and moisture conditions at the southern boundary of discontinuous permafrost. Mongolia. Permafrost and Periglacial Processes 16(2):209-216.
[25]	King, L. 1986. Zonation and ecology of high mountain permafrost in Scandinavia. Geografiska Annaler:Series A, Physical Geography 68(3):131-139.
[26]	Kokelj, S.V., and C.R. Burn. 2010. Near-surface ground ice in sediments of the Mackenzie delta, Northwest Territories. Canada. Permafrost and Periglacial Processes 16(3):291-303.
[27]	Kokelj, S.V., J. Tunnicliffe, D. Lacelle, T.C. Lantz, K.S. Chin, and R. Fraser. 2015. Increased precipitation drives mega slump development and destabilization of ice-rich permafrost terrain, northwestern Canada. Global and Planetary Change 129:56-58.
[28]	Lachenbruch, A.H., T.T. Cladouhos, and R.W. Saltus. 1988. Permafrost temperature and the changing climate. In Proceedings of the 5th International Conference on Permafrost, 2-5 August 1988, Trondheim, Norway, 9-17.
[29]	Lai, Y., S. Zhang, L. Zhang, and J. Xiao. 2004. Adjusting temperature distribution under the south and north slopes of embankment in permafrost regions by the ripped-rock revetment. Cold Regions Science and Technology 39:67-79.
[30]	Lewkowicz, A.G., and R.G. Way. 2019. Extremes of summer climate trigger thousands of thermokarst landslides in a high Arctic environment. Nature Communications 10(1):1-11.
[31]	Li, B., G. Gu, and S. Li. 1996. Natural environment in the Hoh Xil hill region of Qinghai. Beijing:Science Press.
[32]	Li, S., P. Yang, and F. Zhao. 2018. A study of the thermal physical properties of frozen soil in gravel layers. Hydrogeology & Engineering Geology 45(6):122-126 (in Chinese).
[33]	Lin, Z., Z. Gao, X. Fan, F. Niu, J. Luo, G. Yin, and M. Liu. 2020. Factors controlling near surface ground-ice characteristics in a region of warm permafrost, Beiluhe Basin, Qinghai-Tibet Plateau. Geoderma 376:4540.
[34]	Lin, Z., Z. Gao, F. Niu, J. Luo, G. Yin, M. Liu, and X. Fan. 2019. High spatial density ground thermal measurements in a warming permafrost region, Beiluhe Basin, Qinghai-Tibet Plateau. Geomorphology 340:1-14.
[35]	Lin, Z., F. Niu, H. Liu, and J. Lu. 2011. Hydrothermal processes of alpine tundra lakes, Beiluhe Basin, Qinghai-Tibet Plateau. Cold Regions Science and Technology 65:446-455.
[36]	Lin, Z., F. Niu, J. Luo, M. Liu, and G. Yin. 2015. Permafrost thermal regime at north and south aspects, Kunlun Mountain, Qinghai-Tibet Plateau. In Proceedings of the 7th Canadian Permafrost Conference (GeoQuebec 2015), 20-23 September 2015, Quebec City, Canada.
[37]	Lin, Z., F. Niu, Z. Xu, J. Xu, and P. Wang. 2010. Thermal regime of a thermokarst lake and its influence on permafrost, Beiluhe Basin, Qinghai-Tibet Plateau. Permafrost and Periglacial Processes 21:315-324.
[38]	Lunardini, V.J. 1978. Theory of n-factors and correlation of data. In Proceedings of the 3rd International Conference on Permafrost, 10-13 July 1978, Edmonton, Canada, 40-46.
[39]	Luo, D., H. Jin, Q. Wu, F. Victor, R. He, Q. Ma, S. Gao, X. Jin, and L. Lv. 2018. Thermal regime of warm-dry permafrost in relation to ground surface temperature in the source areas of the Yangtze and Yellow Rivers on the Qinghai-Tibet Plateau, SW China. Science of the Total Environment 618:1033-1045.
[40]	Luo, J., Z. Lin, G. Yin, F. Niu, M. Liu, Z. Gao, and X. Fan. 2019. The ground thermal regime and permafrost warming at two upland, sloping, and undisturbed sites, Kunlun Mountain, Qinghai-Tibet Plateau. Cold Regions Science and Technology 167:Article 102862.
[41]	Luo, D., L. Liu, H. Jin, X. Wang, and F. Chen. 2020. Characteristics of ground surface temperature at Chalaping in the source area of the Yellow River, northeastern Tibetan Plateau. Agricultural and Forest Meteorology 281:819.
[42]	Luo, J., F. Niu, Z. Lin, M. Liu, G. Yin, and Z. Gao. 2022. Inventory and frequency of retrogressive thaw slumps in permafrost region of the Qinghai-Tibet Plateau. Geophysical Research Letters 49:Article e2022GL099829.
[43]	Ma, Y., Y. Wang, R. Wu, Z. Hu, K. Yang, M. Li, W. Ma, and L. Zhong et al. 2009. Recent advances on the study of atmosphere-land interaction observations on the Tibetan Plateau. Hydrology and Earth System Sciences 13:1103-1111.
[44]	Mackay, J.R., and C.R. Burn. 2011. The first 20 years (1978-1979 to 1998-1999) of active-layer development, Illisarvik experimental drained lake site, western arctic coast. Canada. Canadian Journal of Earth Sciences 39(11):1657-1674.
[45]	Matsuoka, N. 1990. The rate of bedrock weathering by frost action:Field measurements and a predictive model. Earth Surface Processes and Landforms 15:73-90.
[46]	Matsuoka, N. 1994. Diurnal freeze-thaw depth in rockwalls:Field measurements and theoretical considerations. Earth Surface Processes and Landforms 19:423-435.
[47]	Morse, P.D., C.R. Burn, and S.V. Kokelj. 2009. Near-surface ground-ice distribution, Kendall Island Bird Sanctuary, Western Arctic Coast, Canada. Permafrost and Periglacial Processes 20:155-171.
[48]	Munkhjargal, M., G. Yadamsuren, J. Yamkhin, and L. Menze. 2020. Ground surface temperature variability and permafrost distribution over mountainous terrain in northern Mongolia. Arctic Antarctic and Alpine Research 52(1):13-26.
[49]	Nelson, F.E., and S.I. Outcalt. 1983. A frost index number for spatial prediction of ground-frost zones. In Proceedings of the 4th International Conference on Permafrost, 18-22 July 1983, Fairbanks, USA, 907-911. Washington, DC:National Academy Press.
[50]	Nelson, F.E., and S.I. Outcalt. 1987. A computational method for prediction and regionalization of permafrost. Arctic Antarctic and Alpine Research 19(3):279-288.
[51]	Niu, F., M. Liu, G. Cheng, Z. Lin, J. Luo, and G. Yin. 2015. Long-term thermal regimes of the Qinghai-Tibet Railway embankments in plateau permafrost regions. Science China-Earth Sciences 58(9):1669-1676.
[52]	O'Neill, B. 2011. The development of near-surface ground ice at Illisarvik, Richards Island, Northwest Territories. Ottawa, Ontario:Carleton University.
[53]	Otterman, J. 1974. Baring high-albedo soils by overgrazing:A hypothesized desertification mechanism. Science 186(4163):532-533.
[54]	Pang, Q., L. Zhao, and S. Li. 2011. Influences of local factors on ground temperatures in permafrost regions along the Qinghai-Tibet Highway. Journal of Glaciology and Geocryology 33(2):350-356 (in Chinese).
[55]	Pastick, N.J., M.T. Jorgenson, B.K. Wylie, J.R. Rose, M. Rigge, and M.A. Walvoord. 2014. Spatial variability and landscape controls of near-surface permafrost within the Alaskan Yukon River basin. Journal of Geophysical Research Biogeosciences 119(6):1244-1265.
[56]	Price, L.W. 1971. Vegetation, microtopography, and depth of active layer on different exposures in subarctic alpine tundra. Ecology 52(4):638-647.
[57]	Prick, A. 2003. Frost weathering and rock fall in an arctic environment, Longyearbyen, Svalbard. In Proceedings of the 8th International Conference on Permafrost, 21-25 July 2003, Zürich, Switzerland, 907-912.
[58]	Riseborough, D., N. Shiklomanov, B. Etzelmu, S. Gruber, and S. Marchenko. 2008. Recent advances in permafrost modelling. Permafrost and Periglacial Processes 19:137-156.
[59]	Wang, Q., H. Jin, T. Zhang, Q. Wu, B. Cao, X. Peng, K. Wang, and L. Li. 2016. Active layer seasonal freeze-thaw processes and influencing factors in the alpine permafrost regions in the upper reaches of the Heihe River in Qilian Mountains. Chinese Science Bulletin 61(24):2742-2756 (in Chinese).
[60]	Wang, K., P. Wang, J. Liu, M. Sparrow, S. Haginoya, and X. Zhou. 2005. Variation of surface albedo and soil thermal parameters with soil moisture content at a semi-desert site on the western Tibetan Plateau. Boundary-Layer Meteorology 116:117-129.
[61]	Ward Jones, M.K.W., W.H. Pollard, and B.M. Jones. 2019. Rapid initialization of retrogressive thaw slumps in the Canadian high Arctic and their response to climate and terrain factors. Environmental Research Letters 14(5):Article 055006.
[62]	Williams, P.G., and M.W. Smith. 1989. The frozen earth. Cambridge:Cambridge University Press.
[63]	Xu, X., and L. Chen. 2006. Advances of the study on Tibetan Plateau experiment of atmospheric sciences. Journal of Applied Meteorology and Climatology 17(6):756-772 (in Chinese).
[64]	Yin, G., F. Niu, Z. Lin, J. Luo, and M. Liu. 2017. Effects of local factors and climate on permafrost conditions and distribution in Beiluhe Basin, Qinghai-Tibet Plateau, China. Science of the Total Environment 581-582:472-485.
[65]	You, Q., X. Xue, F. Peng, S. Dong, and Y. Gao. 2017. Surface water and heat exchange comparison between alpine meadow and bare land in a permafrost region of the Tibetan Plateau. Agricultural and Forest Meteorology 232:48-65.
[66]	Zhang, D., L. Fengquan, and B. Jianmin. 2000. Eco-environmental effects of the Qinghai-Tibet Plateau uplift during the Quaternary in China. Environmental Geology 39(12):1352-1358.
[67]	Zhang, M., W. Pei, S. Li, J. Lu, and L. Jin. 2017. Experimental and numerical analyses of the thermo-mechanical stability of an embankment with shady and sunny slopes in a permafrost region. Applied Thermal Engineering 127:1478-1487.
[68]	Zhou, Y., D. Guo, G. Qiu, G. Cheng, and S. Li. 2000. Geocryology in China. Beijing:Science Press.
[69]	Zhou, F., M. Yao, X. Fan, G. Yin, X. Meng, and Z. Lin. 2022. Evidences of warming from long-term records of climate and permafrost in the hinterland of the Qinghai-Tibet Plateau. Frontiers in Environmental Science 10:Article 836085.