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Response of River Runoff in the Cryolithic Zone of Eastern Siberia (Lena River Basin) to Future Climate Warming

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Environmental Change in Siberia

Part of the book series: Advances in Global Change Research ((AGLO,volume 40))

Abstract

During the last several decades significant climate warming has been observed in the permafrost regions of Eastern Siberia. Observed environmental changes include increasing air temperature and to a lesser degree precipitation. Changes in regional climate are accompanied by changes in river runoff. Seasonal and long-term changes of river runoff in different parts of the Lena river basin are characterized by distinct differences that can be explained by regional distinctions of climatic conditions, types and properties of permafrost, character of relief, hydrogeological conditions, etc. These factors determine the non-uniform response of river runoff amount and seasonal distribution to contemporary climate changes within the Lena river basin. Over the past 15–20 years river runoff has increased in different parts of the Lena river basin, but the scale of this increase over its territory is quite variable. Hydrological responses to climate warming have been evaluated for the plain part of the Lena river basin based on a macroscale hydrological model featuring simplified descriptions of processes developed at the Institute of Geography of the Russian Academy of Sciences. Two atmosphere-ocean global circulation models used by the IPCC (ECHAM4/OPY3 and GFDL-R30) were used to model scenarios of future global climate. According to the results from hydrological modelling the expected anthropogenic climate warming in the twenty-first century can bring more significant river runoff changes in the Lena river basin compared to the twentieth century.

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References

  • Anisimov OA, Shiklomanov NI, Nelson FE (1997) Effects of global warming on permafrost and active-layer thickness: results from transient general circulation models. Global Planet Change 15(2):61–77

    Article  Google Scholar 

  • Anon (1989) Manual on hydrological forecasts. Issue 1: Long-term forecasts of water regime of rivers, lakes and water reserves. Gidrometeoizdat, Leningrad, 358 pp (in Russian)

    Google Scholar 

  • Belchikov VA, Koren VI (1979) Model of snow melting and rain runoff forming for forest watersheds. Proceedings of Hydrometeocenter of the USSR, Issue 218, pp 3–21 (in Russian)

    Google Scholar 

  • Broccoli AJ, Manabe S (1992) The effects of orography on midlatitude Northern Hemisphere dry climates. J Climate 5(11):1181–1201

    Article  Google Scholar 

  • Chapman WL, Walsh JE (1993) Recent variations in sea ice and air temperature in high latitudes. Bull Am Meteorol Soc 74:33–47

    Article  Google Scholar 

  • Cramer WP, Leemans R (1999) Global 30-year mean monthly climatology, 1930–1960. V.2.1 (Cramer and Leemans). Available online [http://www.daac.ornl.gov/] from the ORNL Distributed Active Archive Center, Oak Ridge National Laboratory, Oak Ridge, Tennessee, USA

  • Demchenko PF, Velichko AA, Eliseev AV, Mokhov II, Nechaev VP (2002) Dependence of permafrost conditions on global warming: comparison of models, scenarios, and paleoclimatic reconstructions. Izvestiya, Atmos Ocean Phys 38(2):143–151. Translated from Izvestiya AN. Fizika Atmosfery i Okeana 38(2):165–174, 2002. English Translation Copyright © 2002 by AIK

    Google Scholar 

  • Georgiadi AG, Milyukova IP (2002) Possible scales of hydrological changes in the Volga river basin during anthropogenic climate warming. Meteorol Hydrol 2:72–79 (in Russian)

    Google Scholar 

  • Georgiadi AG, Milyukova IP (2006) Possible river runoff changes in the largest river basins of Russian Plain in XXI. Water management complex of Russia. No. 1, pp 62–77 (in Russian)

    Google Scholar 

  • Georgiadi AG, Milyukova IP, Kashutina EA (2008) Recent and projected river runoff changes in permafrost regions of eastern siberia (Lena River Basin). Ninth International Conference on Permafrost. Kane DL and Hinkel KM (eds). Institute of Northern Engineering, University of Alaska Fairbanks 511–515

    Google Scholar 

  • Georgievsky VYu, Ezhov AV, Shalygin AL, Shiklomanov IA, Shiklomanov AI (1999) Evaluation of possible climate change impact on hydrological regime and water resources of the former USSR rivers. “Meteorology and Hydrology”, 1996, 11, pp 89–99. ISSN 0130-2906 (in Russian)

    Google Scholar 

  • IPCC (2001a) Climate change 2001: the scientific basis. In: Houghton JT, Ding Y, Griggs DJ, Noguer M, van der Linden PJ, Dai X, Maskell K, Johnson CA (eds) Contribution of working Group I to the third assessment report of the intergovernmental panel on climate change. Cambridge University Press, Cambridge, UK and New York, NY, USA, 881 pp

    Google Scholar 

  • IPCC II (2001b) Climate change 2001, impacts, adaptation, and vulnerability. In: McCarthy JJ, Canziani OF, Leary NA, Dokken DJ, White KS (eds). Cambridge University Press, 1032 p

    Google Scholar 

  • Malevsky-Malevich SP, Molkentin EK, Nadyozhina ED, Shklyarevich OB (2001) Numerical simulation of permafrost parameters distribution in Russia. Cold Reg Sci Technol 32:1–11

    Article  Google Scholar 

  • Pavlov AV (1979) Thermophysics of landscapes. Nauka, Novosibirsk, 285 pp (in Russian)

    Google Scholar 

  • Razuvaev VN, Apasova EG, Bulygina ON, Martuganov RA (1996) Assessment of natural variability of extreme temperatures over the former Soviet Union territory during the second half of 20th century. Trans RIHMI-WDC 162:3–13 (in Russian)

    Google Scholar 

  • Roeckner E, Arpe K, Bengtsson L, Christoph M, Claussen M, Dümenil L, Esch M, Giorgetta M, Schlese U, Schulzweida U (1996) The atmospheric general circulation model ECHAM-4: model description and simulation of present-day climate. Max-Planck Institute for Meteorology. Report No. 218, Hamburg, Germany, 90 pp

    Google Scholar 

  • Rosenbrock H, Story S (1968) Computational methods for chemist engineer. Translated from English. Moscow, Mir, 440 pp

    Google Scholar 

  • Savelieva NI, Semiletov IP, Vasilevskaya LN, Pugach SP (2000) A climate shift in seasonal values of meteorological and hydrological parameters for Northeastern Asia. Prog Oceanogr 47(2–4):279–297

    Article  Google Scholar 

  • Serreze MC, Walsh JE, Chapin FS III, Osterkamp TE, Dyurgerov M, Romanovsky VE, Oechel WC, Morison J, Zhang T, Barry RG (2000) Observational evidence of recent change in the northern high-latitude environment. Climatic Change 46:159–207

    Article  Google Scholar 

  • Simonov Yu A, Khristoforov AV (2005) Analysis of long-term variability of stream flow of rivers of Arctic Ocean basin. Water Resour 32(6):645–652, in Russian

    Google Scholar 

  • Varlamov SP, Skachkov Yu B, Skryabin PN (2002) Ground temperature regime of Central Yakutia permafrost landscapes. SB RAS, Yakutsk, 218 pp (in Russian)

    Google Scholar 

  • Wang XL, Cho H-R (1997) Spatial-temporal structures of trend and oscillatory variabilities of precipitation over Northern Eurasia. J Clim 10:2285–2298

    Article  Google Scholar 

  • Wetherald RT, Manabe S (1988) Cloud feedback processes in a general circulation model. J Atmos Sci 45:1397–1415

    Article  Google Scholar 

  • Willmott CJ, Rowe CM, Mintz Y (1985) Climatology of the terrestrial seasonal water cycle. J Climatol 5:589–606

    Article  Google Scholar 

  • Yang D, Kane DL, Hinzman LD, Zhang X, Zhang T, Ye H (2002) Siberian Lena River hydrologic regime and recent change. J Geophys Res 107(d 23, 4694):14-4–14-10

    Google Scholar 

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Acknowledgments

The authors are grateful to Dr. R. Leemans, who contributed global database on the modern climate, prepared in the International Institute of Applied System Analysis, Laxenburg, Austria.

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Correspondence to A. G. Georgiadi .

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Georgiadi, A.G., Milyukova, I.P., Kashutina, E.A. (2010). Response of River Runoff in the Cryolithic Zone of Eastern Siberia (Lena River Basin) to Future Climate Warming. In: Balzter, H. (eds) Environmental Change in Siberia. Advances in Global Change Research, vol 40. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-8641-9_10

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