Zobrazeno 1 - 9
of 9
pro vyhledávání: '"I. A. Krickov"'
Autor:
O. S. Pokrovsky, R. M. Manasypov, S. V. Loiko, I. A. Krickov, S. G. Kopysov, L. G. Kolesnichenko, S. N. Vorobyev, S. N. Kirpotin
Publikováno v:
Biogeosciences, Vol 13, Iss 6, Pp 1877-1900 (2016)
Towards a better understanding of trace element (TE) transport in permafrost-affected Earth surface environments, we sampled ∼ 60 large and small rivers (2 watershed area) of the Western Siberian Lowland (WSL) during spring flood and summer and win
Externí odkaz:
https://doaj.org/article/97477c5b4bf44ced92924cc8991ee0ad
Autor:
O. S. Pokrovsky, R. M. Manasypov, S. Loiko, L. S. Shirokova, I. A. Krickov, B. G. Pokrovsky, L. G. Kolesnichenko, S. G. Kopysov, V. A. Zemtzov, S. P. Kulizhsky, S. N. Vorobyev, S. N. Kirpotin
Publikováno v:
Biogeosciences, Vol 12, Iss 21, Pp 6301-6320 (2015)
Analysis of organic and inorganic carbon (DOC and DIC, respectively), pH, Na, K, Ca, Mg, Cl, SO4 and Si in ~ 100 large and small rivers (< 10 to ≤ 150 000 km2) of western Siberia sampled in winter, spring, and summer over a more than 1500 km latitu
Externí odkaz:
https://doaj.org/article/6eb6a264e0d2443499d36149bcbba356
Autor:
A. G. Lim, I. V. Krickov, S. N. Vorobyev, M. A. Korets, S. Kopysov, L. S. Shirokova, J. Karlsson, O. S. Pokrovsky
Publikováno v:
Biogeosciences, Vol 19, Pp 5859-5877 (2022)
Despite recent progress in the understanding of the carbon (C) cycle of Siberian permafrost-affected rivers, spatial and seasonal dynamics of C export and emission from medium-sized rivers (50 000–300 000 km2 watershed area) remain poorly known. He
Externí odkaz:
https://doaj.org/article/ace87c72fbfc4a4e920163c271bed397
Autor:
V. P. Shevchenko, O. S. Pokrovsky, S. N. Vorobyev, I. V. Krickov, R. M. Manasypov, N. V. Politova, S. G. Kopysov, O. M. Dara, Y. Auda, L. S. Shirokova, L. G. Kolesnichenko, V. A. Zemtsov, S. N. Kirpotin
Publikováno v:
Hydrology and Earth System Sciences, Vol 21, Pp 5725-5746 (2017)
In order to better understand the chemical composition of snow and its impact on surface water hydrochemistry in the poorly studied Western Siberia Lowland (WSL), the surface layer of snow was sampled in February 2014 across a 1700 km latitudinal
Externí odkaz:
https://doaj.org/article/b69c90e4962d4efc990e5573e3fa770b
Autor:
R. M. Manasypov, A. G. Lim, I. V. Krickov, L. S. Shirokova, V. P. Shevchenko, R. A. Aliev, J. Karlsson, O. S. Pokrovsky
Publikováno v:
Biogeochemistry. 2022. Vol. 159, № 1. P. 69-86
Thermokarst (thaw) lakes of the Western Siberian Lowland (WSL), the World´s largest permafrost peatland, contain important but poorly constrained stocks of organic carbon (OC) and nitrogen. These lakes are highly vulnerable to climate warming and pe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a893626d730565b3035ed9b3135f156b
https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:000996391
https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:000996391
Autor:
O. S. Pokrovsky, R. M. Manasypov, S. Loiko, I. A. Krickov, S. G. Kopysov, L. G. Kolesnichenko, S. N. Vorobyev, S. N. Kirpotin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::14956a926beeb6658930dee8e1759f7e
https://doi.org/10.5194/bgd-12-17857-2015-supplement
https://doi.org/10.5194/bgd-12-17857-2015-supplement
Autor:
S. Serikova, O. S. Pokrovsky, H. Laudon, I. V. Krickov, A. G. Lim, R. M. Manasypov, J. Karlsson
Publikováno v:
Nature Communications, Vol 10, Iss 1, Pp 1-7 (2019)
The Western Siberia Lowland (WSL) is the world’s largest frozen peatland complex, however carbon emissions (CO2+CH4) from lakes in this region remain unknown. Here, the authors sample 76 lakes and show high carbon emissions from lakes across all pe
Externí odkaz:
https://doaj.org/article/d958c3d188f746d4a3c7e18cee8613aa
Autor:
I. V. Krickov, A. G. Lim, R. M. Manasypov, S. V. Loiko, L. S. Shirokova, S. N. Kirpotin, J. Karlsson, O. S. Pokrovsky
Publikováno v:
Biogeosciences, Vol 15, Pp 6867-6884 (2018)
In contrast to numerous studies on the dynamics of dissolved ( 0.45 µm) matter (RSM) in these regions. In order to test the effect of climate, permafrost and physio-geographical landscape parameters (bogs, forest and lake coverage of the waters
Externí odkaz:
https://doaj.org/article/6c01890ec862409fa80419b9c7d86bf4
Autor:
T. V. Raudina, S. V. Loiko, A. G. Lim, I. V. Krickov, L. S. Shirokova, G. I. Istigechev, D. M. Kuzmina, S. P. Kulizhsky, S. N. Vorobyev, O. S. Pokrovsky
Publikováno v:
Biogeosciences, Vol 14, Pp 3561-3584 (2017)
Mobilization of dissolved organic carbon (DOC) and related trace elements (TEs) from the frozen peat to surface waters in the permafrost zone is expected to enhance under ongoing permafrost thaw and active layer thickness (ALT) deepening in high-l
Externí odkaz:
https://doaj.org/article/02384a456cfb4aa7b638eccc30f2efee