Skip to main content
Log in

Prediction of permafrost changes in Northeastern China under a changing climate

  • Research Paper
  • Published:
Science China Earth Sciences Aims and scope Submit manuscript

Abstract

Northeastern China has the second largest expanse of permafrost in China, primarily known as Xing’an-Baikal permafrost. Located on the southeastern edges of the Eurasian cryolithozone, the permafrost is thermally unstable and ecologically sensitive to external changes. The combined impacts of climatic, environmental, and anthropogenic changes cause 3-dimensional degradation of the permafrost. To predict these changes on the southern limit and ground temperature of permafrost in Northeastern China, an equivalent latitude model (ELM) for the mean annual ground surface temperature (MAGSTs) was proposed, and further improved to take into account of the influences of vegetation and snow-cover based on observational data and using the SHAW model. Using the finite element method and assuming a climate warming rate of 0.048°C a−1, the ELM was combined with the unsteady-state heat conduction model to simulate permafrost temperatures at present, and to predict those after 50 and 100 a. The results indicate that at present, sporadic permafrost occurs in the zones with MAGSTs of 1.5°C or colder, and there would still be a significant presence of permafrost in the zones with the present MAGSTs of 0.5°C or colder after 50 a, and in those of −0.5°C or colder after 100 a. Furthermore, the total areal extent of permafrost would decrease from 2.57×105 km2 at present to 1.84×105 km2 after 50 a and to 1.29×105 km2 after 100 a, i.e., a reduction of 28.4% and 49.8% in the permafrost area, respectively. Also the permafrost would degrade more substantially in the east than in the west. Regional warming and thinning of permafrost would also occur. The area of stable permafrost (mean annual ground temperature, or MAGT⩽−1.0°C) would decrease from present 1.07×105 to 8.8×104 km2 after 50 a, and further decrease to 5.6×104 km2 after 100 a. As a result, the unstable permafrost and seasonally frozen ground would expand, and the southern limit of permafrost would shift significantly northwards. The changes in the permafrost environment may adversely affect on ecological environments and engineering infrastructures in cold regions. Avoidance of unnecessary anthropogenic changes in permafrost conditions is a practical approach to protect the permafrost environment.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  1. Jin H J, Yu S P, Lü L Z, et al. Degradation of permafrost in the Da and Xiao Hinggan Mountains, Northeast China, and preliminary assessment of its trend (in Chinese). J Glaciol Geocryol, 2006, 28: 467–476

    Google Scholar 

  2. Cui Z J, Yang J Q, Zhang W, et al. Discovery of a large area of ice-wedge networks in Ordos: Implications for the southern boundary of permafrost in the north of China as well as for the environment in the latest 20 ka BP. Chin Sci Bull, 2004, 49: 1177–1184

    Article  Google Scholar 

  3. Cui Z J, Xie Y Y. On the southern boundary of permafrost and periglacial environment during the late period of Late Pleistocene in north and northeast China (in Chinese). Act Geol Sin, 1984, 2: 165–176

    Google Scholar 

  4. Guo D X, Li Z F. Preliminary approach to the history and age of permafrost in northeast China (in Chinese). J Glaciol Geocryol, 1981, 3: 1–16

    Google Scholar 

  5. Dong G R, Gao S Y, Li B S, et al. The palaeo-periglacial phenomena and their signification in climate stratigraphy in Ordos Plateau from Late Pleistocene (in Chinese). Geogr Res, 1985, 4: 1–11

    Google Scholar 

  6. Zhou Y W, Guo D X, Qiu G Q, et al. Geocryology in China (in Chinese). Beijing: Science Press, 2000. 170–194

    Google Scholar 

  7. Jones P D, Wigley T M, Wright P B. Global temperature variations between 1861 and 1984. Nature, 1986, 322: 430–434

    Article  Google Scholar 

  8. Anisimov O A, Nelson F E. Permafrost distribution in the Northern Hemisphere under scenarios of climatic change. Glob Planet Chan, 1996, 14: 59–72

    Article  Google Scholar 

  9. Jin H J, Li S X, Wang S L, et al. Impacts of climatic change on permafrost and cold regions environments in China (in Chinese). Acta Geogr Sin, 2000, 55: 161–173

    Google Scholar 

  10. Jin H J, Yu Q H, Lü L Z, et al. Degradation of permafrost in the Xing’anling Mountains, Northeastern China. Permafrost Periglac Process, 2007, 18: 245–258

    Article  Google Scholar 

  11. Wei Z, Jin H J, Zhang J M, et al. Modeling forecasting on permafrost changes in Northeastern China. In: Proceeding of 9th Int Conf on Permafrost, Fairbanks, Alaska, USA, 29 June to 3 July 2008. Fairbanks, Alaska, USA: University of Alaska Fairbanks, 2008. 1939–1944

    Google Scholar 

  12. Ding Y J. Recent degradation of permafrost in China and the response to climatic warming. In: Proceedings of 7th Int Conf on Permafrost, Yellowknife, NWT, Canada, 23–36 June 1998. University of Laval, 1998. 225–230

  13. Ren Q J. Some new data about permafrost in Northeastern China (in Chinese). Hydro Eng Geol, 1957, (5): 10–14

    Google Scholar 

  14. Xin K D, Ren Q J. Permafrost distribution in northeastern China (in Chinese). Geol Knowledge, 1956, (10): 2–3

  15. Guo D X, Wang S L, Lu G W, et al. Division of permafrost regions in the Da and Xiao Xing’anling Mountains of Northeastern China (in Chinese). J Glaciol Geocryol, 1981, 3: 1–9

    Google Scholar 

  16. The Study Committee of Permafrost in the Northeast China. Distributive characteristics of permafrost in Northeast China. In: Proceedings of 2nd Chinese Conf on Geocryol (in Chinese). Lanzhou: Gansu People’s Press, 1983. 36–42

    Google Scholar 

  17. Lu G W, Wen B L, Guo D X. Geographical southern limit of permafrost in Northeastern China (in Chinese). J Glaciol Geocryol, 1993, 15: 214–218

    Google Scholar 

  18. Zhang B L, Wang C H, Cong C C. Preliminary study on renewable mechanism of placer gold in permafrost area in the northeastern Da and Xiao Xing’anling Mountains. In: Proceedings of 5th Chin Conf on Glaciol Geocryol (Vol 2) (in Chinese). Beijing: Science Press, 1996. 243–246

    Google Scholar 

  19. Zhao K Y, Zhang W F, Zhou Y W, et al. Impact of forest fire on environment in the Da Xing’anling Mountains and its mitigation (in Chinese). Beijing: Science Press, 1994. 1–150

    Google Scholar 

  20. Wei Z. Forecast on the changes of permafrost in Northeastern China and of the permafrost conditions for engineering geology along Mo’he-Daqing Crude Oil Pipeline route (in Chinese). Doctoral Dissertation. Lanzhou: Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, 2008. 30–32

    Google Scholar 

  21. Wang T, Wang N L, Li S X, et al. Map of Glaciers, Frozen Ground and Deserts in China (1:4000000). Beijing: SinoMaps Press, 2005

    Google Scholar 

  22. Cheng G D. Influences of local factors on permafrost occurrence and their implications for Qinghai-Xizang Railway design. Sci China Ser D-Earth Sci, 2004, 47: 704–709

    Google Scholar 

  23. Wang G X, Yao J Z, Guo Z G, et al. Changes in permafrost ecosystem under the influences of human engineering activities and its enlightenment to railway construction. Chin Sci Bull, 2004, 49: 1741–1750

    Google Scholar 

  24. Brown R G E, Péwé T L. Distribution of permafrost in north America and its relationship to the environment: A review, 1963–1973. In: Permafrost: The North Amer Contrib to the 2nd Int Conf. Washington DC: Nat Acad Sci, 1973. 71–100

    Google Scholar 

  25. He R X, Jin H J, Lü L Z, et al. Recent changes of permafrost and cold regions environment in the northern Northeastern China (in Chinese). J Glaciol Geocryol, 2009, 31: 525–531

    Google Scholar 

  26. Chang X L, Jin H J, He R X, et al. Advances in permafrost and cold regions environments studies in the Da Xing’anling (Da Hinggan) Mountains, Northeastern China (in Chinese). J Glaciol Geocryol, 2008, 30: 176–181

    Google Scholar 

  27. Nekrasov I A, Klimovskii I V. Permafrost along the Baikal-Amur Main (Railway). Yakutsk: Science Press (Siberia Branch), 1978

    Google Scholar 

  28. Keller F. Automated mapping of mountain permafrost using the program PERMAKART within the geographic information system ARC/INFO. Permafrost Periglac Process, 1992, 3: 139–142

    Article  Google Scholar 

  29. Li X, Cheng G D, Wu Q B, et al. Modeling Chinese cryospheric change by using GIS technology. Cold Reg Sci Technol, 2003, 36: 1–9

    Article  Google Scholar 

  30. Li X, Cheng G D. A GIS-aided response model of high-altitude permafrost to global change. Sci China Ser-D Earth Sci, 1999, 42: 72–79

    Google Scholar 

  31. Zhang T, Osterkamp T E, Stamnes K. Effects of climate on the active layer and permafrost on the north slope of Alaska, U.S.A. Permafrost Periglac Process, 1997, 8: 45–67

    Article  Google Scholar 

  32. Dai J B, Li A Y. Influence of snow cover to the ground temperature in the permafrost region in the northern part of the Great Xin’an Mountain (in Chinese). J Glaciol Geocryol, 1981, 3: 10–18

    Google Scholar 

  33. Esch D C. Thermal Analysis, Construction, and Monitoring Methods for Frozen Ground. Virginia: American Society of Civil Engineering, 2004. 239–254

    Google Scholar 

  34. Li Y W, Tong C J, Zhang L H. Computation of the permafrost thickness in Yituli’he observations field. In: Proceedings of 5th Chinese Conference on Glaciology and Geocryology (Vol. 2), 1996, August 18–22 (in Chinese). Lanzhou: Gansu Culture Press. 1143–1148

  35. Xu X Z, Wang J C, Zhang L X. Physics of Frozen Soils (in Chinese). Beijing: Science Press, 2001. 151–155

    Google Scholar 

  36. Zhang Y, Wu Q B, Liu J P. Distribution characteristics of the permafrost in the section from Hei’he to Bei’an in the Xiao Hinggan Mountains (in Chinese). J Glaciol Geocryol, 2001, 23: 312–317

    Google Scholar 

  37. Jin H J, Zhao L, Wang S L, et al. Thermal regimes and degradation modes of permafrost along the Qinghai-Tibet Highway. Sci China-Ser D-Earth Sci, 2006, 49: 1170–1183

    Article  Google Scholar 

  38. Rover M, Heinemeyer O, Kaiser E A. Microbial induced nitrous oxide emissions from an arable soil during winter. Soil Biol Biochem, 1998, 30: 1859–1865

    Article  Google Scholar 

  39. Yu J B, Liu J S, Sun Z G, et al. Fluxes and controlling factors of N2O and CH4 emissions from freshwater marshes in Northeast China. Sci China- Earth Sci, 2010, 53: 700–709

    Article  Google Scholar 

  40. An S Q, Li H B, Guan B H, et al. China’s natural wetlands: Past problems, current status, and future challenges. Ambio, 2007, 36: 335–342

    Article  Google Scholar 

  41. Wang Q B, Du M G. Current situation and prospect of wetland restoration in Northeast China. Forest Prospect Design, 2006, 140: 25–27

    Google Scholar 

  42. Li W H, Zhou X F, Liu X T. Strategic study on the protection of forests and wetlands and forestry development strategies in Northeastern China (Forestry Part). In: Shen G F, Shi Y L, eds. Study on Several Strategic Problems about Allocation of Water and Soil Resources, Ecology, Environmental Protection and the Sustainable Development in the Northeastern China (in Chinese). Beijing: Science Press, 2007. 1–418

    Google Scholar 

  43. Sun G Y. Discussion on the symbiotic mechanisms of swamp with permafrost—Taking Da and Xiao Hinggan Mountains as examples. J Glaciol Geocryol, 2000, 22: 309–316

    Google Scholar 

  44. Zhang S Q, Na X D, Kong B, et al. Identifying wetland change in China’s Sanjiang Plain using remote sensing. Wetlands, 2009, 29: 302–313

    Article  Google Scholar 

  45. Wang Z Q, Liu B Y, Wang X Y, et al. Erosion effect on the productivity of black soil in Northeast China. Sci China Ser D-Earth Sci, 2009, 52: 1005–1021

    Article  Google Scholar 

  46. Liang A Z, Zhang X P, Yang X M, et al. Estimation of total erosion in cultivated Black soils in Northeast China from vertical profiles of soil organic carbon. Eur J Soil Sci, 2009, 60: 223–229

    Article  Google Scholar 

  47. Xu W D. Preliminary study of correlations between distribution of main forest trees and thermal climate in northeast China (in Chinese). J Northeast Forest Inst, 1982, (4): 1–10

  48. Liang B, Zhang G S, Liu D R. Experimental study on thawing subsidence characters of permafrost under frost heaving and thawing circulation (in Chinese). Chin J Geot Eng, 2006, 28: 1213–1217

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to HuiJun Jin.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Wei, Z., Jin, H., Zhang, J. et al. Prediction of permafrost changes in Northeastern China under a changing climate. Sci. China Earth Sci. 54, 924–935 (2011). https://doi.org/10.1007/s11430-010-4109-6

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s11430-010-4109-6

Keywords

Navigation