Abstract
Water and heat dynamics in the active layer at a monitoring site in the Tanggula Mountains, located in the permafrost region of the Qinghai-Xizang (Tibet) Plateau (QXP), were studied using the physical-process-based COUPMODEL model, including the interaction between soil temperature and moisture under freeze-thaw cycles. Meteorological, ground temperature and moisture data from different depths within the active layer were used to calibrate and validate the model. The results indicate that the calibrated model satisfactorily simulates the soil temperatures from the top to the bottom of the soil layers as well as the moisture content of the active layer in permafrost regions. The simulated soil heat flux at depths of 0 to 20 cm was consistent with the monitoring data, and the simulations of the radiation balance components were reasonable. Energy consumed for phase change was estimated from the simulated ice content during the freeze/thaw processes from 2007 to 2008. Using this model, the active layer thickness and the energy consumed for phase change were predicted for future climate warming scenarios. The model predicts an increase of the active layer thickness from the current 330 cm to approximately 350–390 cm as a result of a 1–2°C warming. However, the effect active layer thickness of more precipitation is limited when the precipitation is increased by 20%–50%. The COUPMODEL provides a useful tool for predicting and understanding the fate of permafrost in the QXP under a warming climate.
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Alexeev V A, Nicolsky D J, Romanovsky V E, Lawrence D M. 2007. An evaluation of deep soil configurations in the CLM3 for improved representation of permafrost. Geophys Res Lett, 34: L090502
Allison I, Barry R G, Goodison B E. 2001. Climate and Cryosphere (CLIC) Project Science and Co-ordination Plan (Version 1), WCRP-114, WMO/TD No.1053, 1–96
Brown J, Romanovsky V, Vladimir E. 2008. Report from the International permafrost association: State of permafrost in the first decade of the 21st Century. Permafrost Periglacial Process, 19: 255–260
Buteau S, Fortier R, Delisle G, Allard M. 2004. Numerical simulations of the impacts of climate warming on a permafrost mound. Permafrost Periglacial Process, 15: 41–57
Cheng G D, Wu T H. 2007. Responses of permafrost to climate change and their environmental significance, Qinghai-Tibet Plateau. J Geophys Res, 112: 1–10
Cheng G D, Zhao L. 2000. The problems associated with permafrost in the development of the Qinghai-Xizang Plateau (in Chinese). Quat Sci Rev, 20: 521–531
Cheng G D. 1990. Recent development of geocryological study in China (in Chinese). Acta Geogr Sin, 45: 220–223
Cheng Z G, Liu X D, Fan G Z, Bai A J, Wang B Z. 2011. Spatiotemporal distribution of climate change over the Qinghai-Tibetan Plateau in 21st Century (in Chinese). Arid Zone Res, 28: 669–676
Demchenko P F, Eliseev A V, Arzhanov M M, Mokhov I I. 2006. Impact of global warming rate on permafrost degradation. Izv Atmos Ocean Phy, 42: 32–39
Eckersten H, Blomback K, Katterer T, Nymana P. 2001. Modelling C, N, water and heat dynamics in winter wheat under climate change in southern Sweden. Agric Ecosyst Environ, 86: 221–235
Franchini M, Pacciani M. 1991. Comparative analysis of several conceptual rainfall-runoff models. J Hydrol, 122: 161–219
Gao Z Q, Chae N, Kim J, Hong J, Choi T, Lee H. 2004. Modeling of surface energy partitioning, surface temperature and soil wetness in the Tibetan prairie using the simple biosphere model 2(SiB2). J Geophys Res, 102: D06102
Guglielmin M, Dramis F. 1999. Permafrost as a climatic indicator in northern Victoria Land, Antarctica. Ann Glaciol, 29: 131–135
Hansson K, Simunek J, Mizoguchi M, Lundina L, Van Genuchten M. 2004. Water flow and heat transport in frozen soil: Numerical solution and freeze-thaw applications. Vadose Zone J, 3: 693–704
Harlan R L. 1973. Analysis of coupled heat-fluid transport in partially frozen soil. Water Resour Res, 9: 1314–1323
Henry K, Smith M. 2001. A model-based map of ground temperatures for the permafrost regions of Canada. Permafrost Periglacial Process, 12: 389–398
Hinkel K M, Nelson F E. 2003. Spatial and temporal patterns of active layer thickness at circumpolar active layer monitoring (CALM) sites in northern Alaska, 1995–2000. J Geophys Res, 108: 8168
Hollesen J, Elberling B, Jansson P E. 2011. Future active layer dynamics and carbon dioxide production from thawing permafrost layers in Northeast Greenland. Glob Change Biol, 17: 911–926
Hu G J, Zhao L, Li R, Wu T H, Xiao Y, Jiao K Q, Qiao Y P, Jiao Y L. 2013. The Water-thermal characteristics of frozen soil under freezethaw based on CoupModel (in Chinese). Sci Geogr Sin, 33: 356–362
Hu H P, Ye B S, Zhou Y H, Tian F Q. 2006. A land surface model incorporated with soil freeze/thaw and its application in GAME/Tibet. Sci China Ser D-Earth Sci, 49: 1311–1322
Ikard S J, Gooseff M N, Barrett J E, Takacs-Vesbach C. 2009. Thermal characterization of active layer across a soil moisture gradient in the McMurdo dry valleys, Antarctica. Permafrost Periglacial Process, 20: 389–398
IPCC. 2007. Climate Change Synthesis Report. Cambridge: Cambridge University Press
Jansson P E, Karlberg L. 2004. Theory and practice of coupled heat and mass transfer model for soil-plant-atmosphere system (in Chinese). In: Zhang H J, Cheng J H, Wang W. Translation. Beijing: Science Press
Jansson P E, Moon D. 2001. A coupled model of water, heat and mass transfer using object orientation to improve flexibility and functionality. Environ Modell Softw, 16: 37–46
Jiang Y Y, Zhuang Q L, O’Donnell Q L. 2012. Modeling thermal dynamics of active layer soils and near-surface permafrost using a fully coupled water and heat transport model. J Geophys Res, 117: D11110
Jiang Z H, Zhang X, Wang J. 2008. Projection of climate change in China in the 21st century by IPCC-AR4 Models. Geogr Res, 27: 787–799
Kane D L, Hinzman L D, Zarling J P. 1991. Thermal response of the active layer to climate warming in a permafrost environment. Cold Reg Sci Technol, 19: 111–122
Koven C D, Ringeval B, Friedlingstein P, Ciaisa P, Cadulea P, Khvorostyanovd D, Krinnere G, Tarnocaif C. 2011. Permafrost carbon-climate feedbacks accelerate global warming. Proc Natl Acad Sci USA, 108: 14769–14774
Li R, Zhao L, Ding Y J, Wu T H, Xiao Y, Du E J, Liu G Y, Qiao Y P. 2012. Temporal and spatial variations of the active layer along the Qinghai- Tibet Highway in a permafrost region. Chin Sci Bull, 57: 2867–2871
Liu X D, Chen B D. 2000. Climatic warming in the Tibetan Plateau during recent decades. Int J Climatol, 20: 1729–1742
Lunardini V J. 1996. Climatic warming and the degradation of warm permafrost. Permafrost Periglacial Process, 7: 311–320
Luo D L, Jin H J, Marchenko S, Romanovsky V. 2014. Distribution and changes of active layer thickness (ALT) and soil temperature (TTOP) in the source area of the Yellow River using the GIPL model. Sci China Earth Sci, 57: 1834–1845
Luo S Q, Lü S H, Zhang Y, Hu Z Y, Ma Y M, Li S S, Shang Y L. 2008. Simulation analysis on land surface process of BJ site of central Tibetan Plateau using CoLM (in Chinese). Plateau Meteorol, 27: 259–271
Ma Z G, Wei H L, Fu C B. 1999. Progress in the research on the relationship between soil moisture and climate change (in Chinese). Adv Earth Sci, 14: 299–305
McGechan M B, Graham R, Vinten A J A, Douglasc J T, Hoodad P S. 1997. Parameter selection and testing the soil water model SOIL. J Hydrol, 195: 312–334
Nan Z T, Li S X, Cheng G D. 2005. Prediction of permafrost distribution on the Qinghai-Tibet Plateau in the next 50 and 100 years. Sci China Ser D-Earth Sci, 48: 797–804
Nassar I N, Horton R, Flerchinger G N. 2000. Simultaneous heat and mass transfer in soil columns exposed to freezing/thawing conditions. Soil Sci, 165: 208–216
Nelson F E. 2003. (Un) frozen in time. Science, 299: 1673–1675
Nicolsky D J, Romanovsky V E, Alexeev V A, Lawrence D M. 2007. Improved modeling of permafrost dynamics in a GCM land-surface scheme. Geophys Res Lett, 34: L080501
Niu L, Ye B S, Li J, Sheng Y. 2011. Effect of permafrost degradation on hydrological processes in typical basins with various permafrost coverage in Western China. Sci China Earth Sci, 4: 615–624
Oelke C, Zhang T J. 2004. A model study of circum-arctic soil temperature. Permafrost Periglacial Process, 15: 103–121
Pavlov A V. 1994. Current change of climate and permafrost in the Arctic and sub-Arctic of Russia. Permafrost Periglacial Process, 5: 101–110
Poutou E, Krinner G, Genthon C, de Noblet-Ducoudré N. 2004. Role of soil freezing in future boreal climate change. Clim Dynam, 23: 621–639
Riseborough D W, Shiklomanov N I, Etzelmuller B, Gruber S, Marchenko S. 2008. Recent advances in permafrost modeling. Permafrost Periglacial Process, 19: 137–156
Riseborough D W. 2002. The mean annual temperature at the top of permafrost, the TTOP model, and the effect of unfrozen water. Permafrost Periglacial Process, 13: 137–143
Scherler M, Hauck C, Hoelzle M, Stähli M, Völksch I. 2010. Meltwater Infiltration into the Frozen Active Layer at an Alpine Permafrost Site. Permafrost Periglacial Process, 21: 325–334
Shoop S A, Bigl S R. 1997. Moisture migration during freeze and thaw of unsaturated soils: Modeling and large scale experiments. Cold Reg Sci Technol, 25: 33–45
Smith L C, Sheng Y, MacDonald G M, Hinzman L D. 2005. Disappearing arctic lakes. Science, 308: 1429
Smith M W, Riseborough D W. 2002. Climate and the limits of permafrost: A zonal analysis. Permafrost Periglacial Process, 13: 1–15
Sridhar V, Elliott R L, Chen F, Brotzge J A. 2002. Validation of the NOAH-OSU land surface model using surface flux measurements in Oklahoma. J Geophys Res, 107(D20): ACL 3-1-ACL 3–18
Stendel M, Christensen J H. 2002. Impact of global warming on permafrost conditions in a coupled GCM. Geophys Res Lett, 29: 1632
Sturm M, Douglas T, Racine C, Liston G E. 2005. Changing snow and shrub conditions affect albedo with global implications. J Geophys Res, 110: G01004
Sun L C, Zhao L, Li R, Yao J M, Liu Y, Qiao Y P, Jiao K Q. 2014. Effects of precipitation on the permafrost ground surface energy fluxes. J Longdong Univ, 25: 41–46
Tang M C, Shen Z B, Chen Y Y. 1979. On climatic characteristics of the Xizang Plateau monsoon (in Chinese). Acta Geogr Sin, 34: 33–42
Tian H, Wei C, Wei H, Zhou J Z. 2014. Freezing and thawing characteristics of frozen soils: Bound water content and hysteresis phenomenon. Cold Reg Sci Technol, 103: 74–81
Vinnikov K Y, Robock A, Speranskaya N A. 1996. Scales of temporal and spatial variability of mid-latitude soil moisture. J Geophys Res, 101: 7163–7174
Wang C H, Shi R. 2007. Simulation of the land surface processes in the Western Tibetan Plateau in summer (in Chinese). J Glaciol Geocryol, 29: 73–81
Wang Y B, Gao Z Y, Wen J, Liu G H, Geng D, Li X B. 2014. Effect of a thermokarst lake on soil physical properties and infiltration processes in the permafrost region of the Qinghai-Tibet Plateau, China. Sci China Earth Sci, 57: 2357–2365
Wang Q C, Li L, Li D L, Qin N S, Wang Z Y, Zhu X D, Shi X H. 2005. Response of permafrost over Qinghai Plateau to climate warming (in Chinese). Plateau Meteorol, 24: 708–713
Wei Z, Jin H J, Zhang J M, Yu S P, Han X J, Ji Y J, He R X, Chang X L. 2011. Prediction of permafrost changes in Northeastern China under a changing climate. Sci China Earth Sci, 6: 924–935
Wu Q, Zhang T J. 2008. Recent permafrost warming on the Qinghai- Tibetan Plateau. J Geophys Res, 113: 1–22
Wu Q B, Cheng G D, Ma W, Niu F, Sun Z Z. 2006. Technical approaches on permafrost thermal stability for Qinghai-Tibet Railway. Geomech Geoeng, 1: 119–127
Wu Q B, Liu Y Z. 2004. Ground temperature monitoring and its recent change in Qinghai-Tibet Plateau. Cold reg Sci Technol, 38: 85–92
Wu Q B, Shen Y P, Shi B. 2003. Relationship between frozen soil together with its water-heat process and ecological environment in the Tibetan Plateau (in Chinese). J Glaciol Geocryol, 25: 250–255
Wu S H, Jansson P E, Zhang X Y. 2011. Modeling temperature, moisture and surface heat balance in bare soil under seasonal frost conditions in China. Eur J Soil Sci, 62: 780–796
Wu S H, Jansson P E, Kolari P. 2012. The role of air and soil temperature in the seasonality of photosynthesis and transpiration in a boreal scots pine ecosystem. Agr Forest Meteorol, 156: 85–103
Wu S H, Jansson P E, Kolari P. 2011. Modeling seasonal course of carbon fluxes and evapotranspiration in response to low temperature and moisture in a boreal Scots pine ecosystem. Ecol, 222: 3103–3119
Wu J C, Sheng Y, Wu Q B, Wen Z. 2010. Processes and modes of permafrost degradation on the Qinghai-Tibet Plateau. Sci China Earth Sci, 1: 150–158
Xiao Y, Zhao L, Dai Y J, Li R, Pang Q Q, Yao J M. 2013. Representing permafrost properties in CoLM for the Qinghai-Xizang (Tibetan) Plateau. Cold Reg Sci Technol, 87: 68–77
Xiao Y, Zhao L, Li R, Yao J M. 2011. Seasonal variation characteristics of surface energy budget components in permafrost regions of Northern Tibetan Plateau (in Chinese). J Glaciol Geocryol, 33: 1033–1037
Xiao Y. 2013. A Study on Water-Heat Processes and Simulation along the Qinghai-Tibet Highway in Permafrost Regions (in Chinese. Doctoral Dissertation. Chinese Academy of Sciences
Yang J P, Ding Y J, Chen R S. 2004. Permafrost change and its effect on eco-environment in the source regions of the Yangtze and Yellow Rivers (in Chinese). J Mt Sci, 22: 278–285
Yang Y, Chen R S, Ji X B, Qing W W, Liu J F, Han C T. 2010. Heat and water transfer processes on alpine meadow frozen grounds of Heihe mountainous in Northwest China (in Chinese). Adv Water Sci, 21: 30–34
Yao J M, Zhao L, Ding Y J, Gu L L, Jiao K Q, Qiao Y P, Wang Y X. 2008. The surface energy budget and evapotranspiration in the Tanggula region on the Tibetan Plateau. Cold Reg Sci Technol, 52: 326–340
Zhang S L, Lövdahl L, Grip H, Jansson P E, Tong Y. 2007. Modelling the effects of mulching and fallow cropping on water balance in the Chinese Loess Plateau. Soil Till Res, 100: 311–319
Zhang T J. 2005. Influence of the seasonal snow cover on the ground thermal regime: An overview. Rev Geophys, 43: RG4002
Zhang Y W, Lü S H, Li D L, Huang J. 2003. Numerical simulation of freezing soil process on Qinghai-Xizang Plateau in early winter (in Chinese). Plateau Meteorol, 22: 471–477
Zhao L, Li R, Ding Y J. 2008. Simulation on the soil water-thermal characteristics of the active layer in tanggula range (in Chinese). J Glaciol Permafrost Eng, 30: 930–937
Zhao L, Ping C L, Yang D Q, Cheng G D, Ding Y J, Liu S Y. 2004. Changes of climate and seasonally frozen ground over the past 30 years in Qinghai-Xizang (Tibetan) Plateau, China. Global Planet Change, 43: 19–31
Zhao L, Wu Q B, Marchenko S S, Sharkhuu N. 2010. Thermal state of permafrost and active layer in Central Asia during the International Polar Year, Permafrost Periglacial Process, 21: 198–207
Zhao L. 2004. The freezing-thawing processes of active layer and changes of seasonally frozen ground on the Tibetan plateau (in Chinese). Doctoral Dissertation. Chinese Academy of Sciences
Zhou J, Kinzelbach W, Cheng G D, Zhang W, He X B, Ye B S. 2013. Monitoring and modelling the influence of snow pack and organic soil on a permafrost active layer, Qinghai-Tibetan Plateau of China. Cold Reg Sci Technol, 90-91: 38–52
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Hu, G., Zhao, L., Wu, X. et al. Modeling permafrost properties in the Qinghai-Xizang (Tibet) Plateau. Sci. China Earth Sci. 58, 2309–2326 (2015). https://doi.org/10.1007/s11430-015-5197-0
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DOI: https://doi.org/10.1007/s11430-015-5197-0