Zobrazeno 1 - 10
of 53
pro vyhledávání: '"R M, Manasypov"'
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:
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:
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:
R. M. Manasypov, S. N. Vorobyev, S. V. Loiko, I. V. Kritzkov, L. S. Shirokova, V. P. Shevchenko, S. N. Kirpotin, S. P. Kulizhsky, L. G. Kolesnichenko, V. A. Zemtzov, V. V. Sinkinov, O. S. Pokrovsky
Publikováno v:
Biogeosciences, Vol 12, Iss 10, Pp 3009-3028 (2015)
Despite relatively good knowledge of the biogeochemistry of Siberian thermokarst lakes during summer base flow, their seasonal dynamics remains almost unexplored. This work describes the chemical composition of ~130 thermokarst lakes ranging in size
Externí odkaz:
https://doaj.org/article/1f367ac5b0dc4295bc9b5267a4e6855c
Publikováno v:
The Cryosphere, Vol 8, Iss 4, Pp 1177-1193 (2014)
This work describes the hydrochemical composition of thermokarst lake and pond ecosystems, which are observed in various sizes with different degrees of permafrost influence and are located in the northern part of western Siberia within the continuou
Externí odkaz:
https://doaj.org/article/6096d1a5fb434e7e83d7eb14e07063a1
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:
Y M Polishchuk, A N Bogdanov, I N Muratov, V Y Polishchuk, A Lim, R M Manasypov, L S Shirokova, O S Pokrovsky
Publikováno v:
Environmental Research Letters, Vol 13, Iss 4, p 045002 (2018)
Despite the potential importance of small (
Externí odkaz:
https://doaj.org/article/1ec4ddeacddf426f8aeb833279e50400
Autor:
Ivan V. Krickov, Oleg S. Pokrovsky, Jérôme Viers, Artem G. Lim, R. M. Manasypov, Liudmila S. Shirokova
Publikováno v:
Geochimica et Cosmochimica Acta
Geochimica et Cosmochimica Acta, Elsevier, 2019, 265, pp.221-241. ⟨10.1016/j.gca.2019.08.041⟩
Geochimica et Cosmochimica Acta, 2019, 265, pp.221-241. ⟨10.1016/j.gca.2019.08.041⟩
Geochimica et Cosmochimica Acta, Elsevier, 2019, 265, pp.221-241. ⟨10.1016/j.gca.2019.08.041⟩
Geochimica et Cosmochimica Acta, 2019, 265, pp.221-241. ⟨10.1016/j.gca.2019.08.041⟩
In contrast to fairly good knowledge of dissolved ( 0.45 µm) fluxes of carbon, nutrients and metals from the land to the ocean, colloidal (1 kDa−0.45 µm) forms of solutes are rarely quantified. This is especially true for Siberian rivers draining