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A VARIATION OF STABLE ISOTOPE COMPOSITION OF SNOW WITH ALTITUDE ON THE ELBRUS MOUNTAIN, CENTRAL CAUCASUS

https://doi.org/10.24057/2071-9388-2018-22

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Abstract

This study aims to analyze the stable isotope composition of the snow cover of the Elbrus Mountain – the highest mountain in Europe. Snow sampled in the middle accumulation period in January 2017, February 2016, January 2001 and during snowmelt in July 1998 and August 2009. Snow sampled at the south slope of Mt. Elbrus at different elevations, and the total altitude range is approximately 1700 m. A significant altitude effect in fresh snow precipitation was determined in February 2001 with gradient –1.3‰ δ18O/100 m (–11.1‰ δ2 H /100 m) at 3100-3900 m a.s.l. and inverse altitude effect in February 2016 with gradient +1.04‰ δ18O /100 m (+8.7‰ δ2 H /100 m) at 3064-3836 m a.s.l. There is no obvious altitude effect of the δ2 H and δ18O values in snow at the Elbrus slope in 2017, except for the height range 2256-3716 m a.s.l., where altitudinal effect of δ18O values was roughly -0.32‰/100m. The δ18O values in the winter snowpack in some cases decrease with increasing altitude, but sometimes are not indicating a temperaturealtitude effect. Post-depositional processes cause isotopic changes, which can result from drifting, evaporation, sublimation, and ablation. The study of altitude effect in snow is important for understanding the processes of snow-ice and snow-meltwater transformation and the snow/ice potential to provide paleo-environmental data.

About the Authors

Yurij Vasil’chuk
Lomonosov Moscow State University, Faculty of Geography
Russian Federation
Moscow


Julia Chizhova
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry (IGEM RAS)
Russian Federation
Moscow


Natalia Frolova
Lomonosov Moscow State University, Faculty of Geography
Russian Federation
Moscow


Nadine Budantseva
Lomonosov Moscow State University, Faculty of Geography
Russian Federation
Moscow


Maria Kireeva
Lomonosov Moscow State University, Faculty of Geography
Russian Federation
Moscow


Alexander Oleynikov
Lomonosov Moscow State University, Faculty of Geography
Russian Federation
Moscow


Igor Tokarev
Centre for Geo-Environmental Research and Modelling (GEOMODEL) at St. Petersburg University
Russian Federation
St. Petersburg


Ekaterina Rets
Lomonosov Moscow State University, Faculty of Geography
Russian Federation
Moscow


Alla Vasil’chuk
Lomonosov Moscow State University, Faculty of Geography
Russian Federation
Moscow


References

1. Ambach W., Eisner H. and Pessl K. (1972). Isotopic oxygen composition of firn, old snow and precipitation in alpine regions. Z. Gletscherk. Glazialgeol., 8, pp. 125–135.

2. Ciais P. and Jouzel J. (1994). Deuterium and oxygen-18 in precipitation: Isotopic model, including mixed cloud processes. J. Geoph. Res., 99(D8), pp. 16793-16803.

3. Dansgaard W. (1964). Stable isotopes in precipitation. Tellus, 16, pp. 436–468.

4. Dietermann N. and Weiler M. (2013). Spatial distribution of stable water isotopes in alpine snow cover. Hydrol. Earth Syst. Sci., 17, pp. 26057–2668.

5. Draxler R.R. and Rolph G.D. (2011). HYSPLIT (Hybrid Single-Particle Lagrangian Integrated Trajectory) Model access via NOAA ARL READY Website (http://ready.arl.noaa.gov/HYSPLIT. php). NOAA Air Resources Laboratory, Silver Spring, MD.

6. Gat J.R. and Carmi I. (1970). Evolution of the isotopic composition of atmospheric waters in the Mediterranean Sea Area. Journal of Geophysical Research, 75, pp. 3039–3048.

7. Grasby S.E. and Lepitzki D.A.W. (2002). Physical and chemical properties of the Sulphur Mountain thermal springs, Banff National Park, and implications for endangered snails. Canadian Journal of Earth Sciences, 39, pp. 1349–1361.

8. He Y., Pang H., Theakstone W.H., Zhang D., Lu A., Song B., Yuan L. and Ning B. (2006). Spatial and temporal variation of oxygen isotopes in snowpacks and glacial runoff in different types of glacial area in western China. Annals of Glaciology, 43, pp. 269–274.

9. Holdworth G., Fogarasi S. and Krouse H.R. (1991). Variation of the stable isotopes of water with altitude in the Saint Elias Mountains of Canada. J. Geophysical Res., 96(4), pp. 7483– 7494.

10. Holobâcă J-H. (2016). Recent retreat of the Elbrus glacier system. Journal of Glaciology, 62(231), pp. 94–102.

11. Friedman I. and Smith G. (1970). Deuterium content of snow cores from Sierra Nevada area. Science, 169, pp. 467–470.

12. Jouzel J. and Merlivat L. (1984). Deuterium and oxygen-18 in precipitation: modeling of the isotopic effects during snow formation. Journal Geophysical Res., 89(7), pp. 11749–11757.

13. Judy C., Meiman J.R. and Friedman I. (1970). Deuterium variations in an annual snowpack. Water Resour. Res., 6, pp. 125–129.

14. Kang S., Kreutz K.J., Mayewski P.A., Qin D. and Yao T. (2002). Stable-isotopic composition of precipitation over the northern slope of the central Himalaya. Journal of Glaciology, 48(163), pp. 519–526.

15. Kozachek A., Mikhalenko V., Masson-Delmotte V., Ekaykin A., Ginot P., Kutuzov S., Legrand M., Lipenkov V. and Preunkert S. (2017). Large-scale drivers of Caucasus climate variability in meteorological records and Mt Elbrus ice cores. Climate of the Past, 13, pp. 473–489.

16. Königer P., Hubbart J.A., Link T. and Marshall J.D. (2008). Isotopic variation of snow cover and streamflow in response to changes in canopy structure in a snow-dominated mountain catchment. Hydrol. Process., 22, pp. 557–566.

17. Kutuzov S., Shahgedanova M., Mikhalenko V., Ginot P., Lavrentiev I. and Kemp S. (2013). High-resolution provenance of desert dust deposited on Mt. Elbrus, Caucasus in 2009– 2012 using snow pit and firn core records. The Cryosphere, 7, pp. 1481–1498.

18. Merlivat L. and Jouzel J. (1979). Global climatic interpretation of the deuterium oxygen 18 relationship for precipitation. J. Geophys. Res., 84, pp. 5029–5033.

19. Mikhalenko V., Sokratov S., Kutuzov S., Ginot P., Legrand M., Preunkert S., Lavrentiev I., Kozachek A., Ekaykin A., Faïn X., Lim S., Schotterer U., Lipenkov V. and Toropov P. (2015). Investigation of a deep ice core from the Elbrus western plateau, the Caucasus, Russia. The Cryosphere, 9, pp. 2253–2270.

20. Moore G.W.K., Field R. and Benson C.S. (2016). Impact of Source Region on the δ18O Signal in Snow: A case study from Mount Wrangell, Alaska. Journal of Hydrometeorology, 17, pp. 139–151.

21. Moran T.A., Marshall S.J., Evans E.C. and Sinclair K.E. (2007). Altitudinal gradients of stable isotopes in lee-slope precipitation in the Canadian Rocky Mountains. Arct. Antarct. Alpine Res., 39(3), pp. 455–467.

22. Moser H. and Stichler W. (1970). Deuterium measurements on snow samples from the Alps. In Isotope Hydrology (Proceedings of a Symposium on Use of Isotopes in Hydrology), IAEA, Vienna, 43–57.

23. Moser H. and Stichler W. (1974). Deuterium and oxygen-18 contents as an index of the properties of snow covers. In Snow Mechanics (Proceedings of the Grindelwald Symposium, Switzerland, April 1974), IAHS Publ., 114: 122–135.

24. Niewodnizański J., Grabczak J., Barański L. and Rzepka J. (1981). The altitude effect on the isotopic composition of snow in high mountains. Journal of Glaciology, 27(95), pp. 99–111.

25. Pang Z., Kong Y., Froehlich K., Huang T., Yuan L., Li Z. and Wang F. (2011). Processes affecting isotopes in precipitation of an arid region. Tellus, 63(3), pp. 352–359.

26. Poage M.A. and Chamberlain C.P. (2001). Empirical relationships between elevation and the stable isotope composition of precipitation and surface waters: considerations for studies of paleoelevation change. American Journal of Science, 31, pp. 1–15.

27. Raben P. and Theakstone W.H. (1994). Isotopic and ionic changes in a snow cover at different altitudes: observations at Austre Okstindbreen in 1991. Ann. Glaciol., 19, pp. 85–91.

28. Risi C., Bony S., Vimeux F., Chong M. and Descroix L. (2010). Evolution of the stable water isotopic composition of the rain sampled along Sahelian squall lines. Q. J. R. Meteorol. Soc., 136(s1), pp. 227–242.

29. Rototaeva O.V., Nosenko G.A., Tarasova L.N. and Khmelevskoy I.F. (2006). General characteristics of glacierization of the north slope of the Gteater Caucasus). In: V.M. Kotlyakov, ed. Glaciation in North and Central Eurasia at Present Time. Moscow: Nauka Publ. House, pp. 141–144. (in Russian).

30. Rozanski K. and Araguas-Araguas L. (1995). Spatial and temporal variability of stable isotope composition over the South American continent. Bull. Inst. Fr. Etud. Andin., 24, pp. 379–390.

31. Schotterer U., Fröhlich K., Stichler W. and Trimbom P. (1993). Temporal variations of oxygen-18 and deuterium excess in alpine regions of Switzerland. In: Isotope Techniques in the Study of Past and Current Environmental Changes in the Hydrosphere and the Atmosphere (Proc. Symp. Int. Atomic Energy Agency, Vienna), pp. 53–64.

32. Schotterer U., Gäggeler H.W., Fröhlich K., Sandjordj S. and Stichler W. (1997). Isotope records from Mongolian and alpine ice cores as climate indicator. Climatic Change, 36, pp. 519– 530.

33. Shahgedanova M., Kutuzov S., White K.H., and Nosenko G. (2013). Using the significant dust deposition event on the glaciers of Mt. Elbrus, Caucasus Mountains, Russia on 5 May 2009 to develop a method for dating and “provenancing” of desert dust events recorded in snow pack. Atmos. Chem. Phys., 13, pp. 1797–1808.

34. Siegenthaler U. and Oeschger H. (1980). Correlation of O-18 in precipitation with temperature and altitude. Nature, 285, pp. 314–317.

35. Sokratov S.A. and Golubev V.N. (2009). Snow isotopic content change by sublimation. Journal of Glaciology, 55, pp. 823–828.

36. Stichler W., Schotterer U., Fröhlich K., Ginot P., Kull C., Gäggeler H. and Pouyaud B. (2001). Influence of sublimation on stable isotope records recovered from high-altitude glaciers in the tropical Andes. J. Geophys. Res., 19, pp. 22613–22620.

37. Tielidze L.G. and Wheate R.D. (2017). The Greater Caucasus Glacier Inventory (Russia/ Georgia/Azerbaijan). The Cryosphere Discuss., doi:10.5194/tc-2017-48. 27 p.

38. Vasil’chuk Y.K. and Chizhova J.N. (2010). Altitude gradient of δ18O and δD in precipitation and snow cover in high mountain. Earth Cryosphere, 14(1), pp. 13–21 (in Russian).

39. Vasil’chuk Y.K., Chizhova J.N., Budantseva N.A. and Mukhina J.S. (2010). Rapid reduction of the glacier Big Azau, Elbrus on stable climatic conditions and risks appearing in this case. Georisk, 2, pp. 16–29 (in Russian).

40. Vasil’chuk Y.K., Chizhova J.N. and Budantseva N.A. (2006). Isotope composition of Bolchoy Azau glacier tongue, Elbrus. Earth Cryosphere, 1(10), pp. 56–68 (in Russian).

41. Vasil’chuk Yu.K., Chizhova Ju.N., Papesh V. and Papesch W.(2005). Trend of isotope composition of a separate winter snowfall in northeastern Europe. Earth Cryosphere, 9(3), pp. 81-87. (in Russian).

42. Volodicheva N.A. (2002). The Caucasus. In: M. Shahgedanova, ed. The Physical Geography of Northern Eurasia, Oxford: Oxford University Press, pp. 350–376.

43. Yamanaka T. and Yamada Y. (2017). Regional Assessment of Recharge Elevation of Tap Water Sources Using the Isoscape Approach. Mountain Research and Development, 37(2), pp. 198–205.

44. Zolotarev Y.A. and Kharkovets Y.G. (2010). Evolution of the Elbrus glaciation since the mid XIX century under changing climate. Key findings of the glacio-cartographical monitoring. Geogr. Environ. Sustainability, 2, pp. 13–32.


For citation:


Vasil’chuk Y., Chizhova J., Frolova N., Budantseva N., Kireeva M., Oleynikov A., Tokarev I., Rets E., Vasil’chuk A. A VARIATION OF STABLE ISOTOPE COMPOSITION OF SNOW WITH ALTITUDE ON THE ELBRUS MOUNTAIN, CENTRAL CAUCASUS. GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY. 0;. https://doi.org/10.24057/2071-9388-2018-22

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ISSN 2071-9388 (Print)
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