The Relationship between Dissolved Solids Yield and the Presence of Snow cover in the Periglacial Basin of the Obruchev Glacier (Polar Urals) during the Ablation Season

Łukasz Stachnik; Łukasz Uzarowicz

doi:10.2478/v10117-011-0009-x

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The Relationship between Dissolved Solids Yield and the Presence of Snow cover in the Periglacial Basin of the Obruchev Glacier (Polar Urals) during the Ablation Season

Quaestiones Geographicae

Volume 30 (2011): Issue 1 (March 2011)

By: Łukasz Stachnik and Łukasz Uzarowicz

Open Access

|Mar 2011

Beylich A., Sandberg O., Molau U. & Wache S., 2006. Intensity and spatio-temporal variability of fluvial sediment transfers in an Arctic-oceanic periglacial environment in northernmost Swedish Lapland (Latnjavagge catchment).80(1-2): 114-130, DOI:10.1016/j.geomorph.2005.09.014.
Open DOI Search in Google Scholar
Beylich A. Kolstrup E. Thyrsted T. & Gintz D., 2004. Water chemistry and its diversity in relation to local factors in the Latnjavagge drainage basin, arctic-oceanic Swedish Lapland.58 (1-4): 125-143, DOI:10.1016/S0169-555X(03)00228-9.
Open DOI Search in Google Scholar
Bolewski A., 1982.Wydawnictwa Geologiczne, Warszawa.
Search in Google Scholar
Brown G., 2002. Glacial meltwater hydrochemistry.17(7): 855-883, DOI:10.1016/S0883-2927(01)00123-8.
Open DOI Search in Google Scholar
Caine N., 1992. Spatial patterns of geochemical denudation rate in a Colorado Alpine Environment. In: J. C. Dixon, A. D. Abrahams (eds.),, John Wiley and sons, Chichester: 63-88.
Open DOI Search in Google Scholar
Caine, N., 1979. Rock weathering rates at the soil surface in an alpine environment.6(2): 131-144, DOI:10.1016/0341-8162(79)90003-1.
Open DOI Search in Google Scholar
Collins N., 1979. Hydrochemistry of meltwaters draining from an alpine glacier (Gornergletsher, Switzerland)., 11(3): 307-324.
Open DOI Search in Google Scholar
Darmody R. G., Thorn C. E., Harder R. L., Schlyter J. P. & Dixon J. C., 2000. Weathering implications of water chemistry in an arctic-alpine environment, northern Sweden., 34(1-2): 89-100, DOI:10.1016/S0169-555X(00)00002-7.
Open DOI Search in Google Scholar
Dixon J. C., Thorn C. E. & Darmody R. G., 1984. Chemical weathering processes on the Vantage Peak Nunatak, Juneau Icefield, southern Alaska., 5: 111-131.
Open DOI Search in Google Scholar
Hodson A., Tranter M. & Vante G., 2000. Contemporary rates of chemical denudation and COsequestration in glacier basins: an Arctic perspective., 25: 1447-1471, DOI: 10.1002/1096.9837(200012)25:13<1447::AID-ESP156>3.0.CO; 2-9.
Search in Google Scholar
Hounslow A. W., 1995.Lewis Publisher, Los Angeles.
Search in Google Scholar
Kononov Y., Ananicheva, M. & Willis, I., 2005. High-resolution reconstruction of Polar Ural glaciers mass balance for the last millennium., 42: 163-170, DOI: 10.3189/172756405781812709.
Open DOI Search in Google Scholar
Krawczyk W. & Pettersson L.-E. 2007. Chemical denudation rates and carbon dioxide drawdown in an ice-free polar karst catchment: Londonelva, Svalbard.18(4): 337-350, DOI: 10.1002/ppp.599.
Open DOI Search in Google Scholar
Lessovaia S. N. & Polekhovsky Yu., 2009. Mineralogical composition of shallow soils on basic and ultrabasic rocks of East Fennoscandia and of the Ural Mountains, Russia., 57(4): 476-485, DOI: 10.1346/CCMN.2009.0570408.
Open DOI Search in Google Scholar
Mangerud J., Gosse J., Matiouchkov A. & Dolvik T., 2008. Glaciers in the Polar Urals, Russia, were not much larger during the Last Global Glacial Maximum than today., 27 (9-10): 1047-1057, DOI: 10.1016/j.quascirev.2008.01.015.
Open DOI Search in Google Scholar
Rapp A., 1960. Recent development of mountain slopes in Karkevagge and surroundings, northern Scandinavia., 42: 71-200.
Open DOI Search in Google Scholar
Stupnicka E., 1978.Wydawnictwa Geologiczne, Warszawa.
Search in Google Scholar
Tranter M., Brown G. H., Hodson A. J. & Gurnell A. M. 1996: Hydrochemistry as an indicator of subglacial drainage system structure: A comparison of alpine and sub-polar environments.10(4): 541-556, DOI: 10.1002/(SICI)1099-1085(199604)10:4<541::AID-HYP391>3.0.CO; 2-9.
Search in Google Scholar
Troitsky L. S., 1961. Some features of modern glaciation of Polar Urals. (Nekotoriye osobennosti sovremennogo oledeneniya Poliarnogo Urala).6: 70-85.
Search in Google Scholar
Tushinskiy G. K., 1963.State Publishing House of Geographical Literature, Moscow.
Search in Google Scholar
Wadham J. L., Hodson A. J., Tranter M. & Dowdeswell J. A., 1998. The hydrochemistry of meltwaters draining a polythermal-based, high arctic glacier, south Svalbard: I. The ablation season.12(12): 1825-1849, DOI: 10.1002/(SICI)1099-1085(19981015)12:12<1825::AID-HYP669>3.0.CO; 2-R.
Search in Google Scholar
Wadham J. L., Tranter M. & Dowdeswell J. A., 2000. Hydrochemistry of meltwaters draining a polythermal-based, high-arctic glacier, south Svalbard: II. winter and early spring.14(10): 1767-1786, DOI: 10.1002/1099-1085(200007)14:10<1767::AID-HYP103>3.0.CO; 2-Q.
Search in Google Scholar
Wałach P., 2008. The daily air temperature course in the bottom of selected glacier cirques in the Polar Ural., 18: 171-180.
Open DOI Search in Google Scholar
Wałach P. & Stachnik Ł., 2011. Wpływ warunków meteorologicznych na kształtowanie się odpływu i chemizmu wód w zlewni lodowca Obrucheva (Ural Polarny). Przegląd Geograficzny. (in review)
Search in Google Scholar
Voloshina A. P., 1987. Some totals of the mass balance studies of Polar Ural glaciers.61: 44-51.
Search in Google Scholar
Zakharova E. A., Pokrovsky O. S., Dupré B., Gaillardet J. & Efimova L. E., 2007. Chemical weathering of silicate rocks in Karelia region and Kola peninsula, NW Russia: Assessing the effect of rock composition, wetlands and vegetation.242: 255-277, DOI: 10.1016/j.chemgeo.2007.03.018.
Open DOI Search in Google Scholar