Zobrazeno 1 - 10
of 41
pro vyhledávání: '"I. Rogóż"'
Publikováno v:
Energy Reports, Vol 10, Iss , Pp 3263-3271 (2023)
Anaerobic digestion is the most popular technic for obtaining biomethane from substrates like cow manure and other organic materials, however, chlortetracycline (CTC) and sulfadiazine (SDZ) which are commonly used in animal husbandry and present in c
Externí odkaz:
https://doaj.org/article/fe585d70047d4cfdb8af7788d5482b05
Autor:
A. Castillo-Llarena, F. Retamal-Ramírez, J. Bernales, M. Jacques-Coper, M. Prange, I. Rogozhina
Publikováno v:
Climate of the Past, Vol 20, Pp 1559-1577 (2024)
During the Last Glacial Maximum (LGM, ∼ 23 000 to 19 000 years ago), the Patagonian Ice Sheet (PIS) covered the central chain of the Andes between ∼ 38 to 55° S. Existing paleoclimate evidence – mostly derived from glacial landforms – sugges
Externí odkaz:
https://doaj.org/article/db9c6524c2574e2291b6243340f70d50
Akademický článek
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Autor:
M. Mas e Braga, R. Selwyn Jones, J. C. H. Newall, I. Rogozhina, J. L. Andersen, N. A. Lifton, A. P. Stroeven
Publikováno v:
The Cryosphere, Vol 15, Pp 4929-4947 (2021)
Numerical models predict that discharge from the polar ice sheets will become the largest contributor to sea-level rise over the coming centuries. However, the predicted amount of ice discharge and associated thinning depends on how well ice sheet mo
Externí odkaz:
https://doaj.org/article/35305fba958b4715bac17cbddc999069
Publikováno v:
The Cryosphere, Vol 15, Pp 459-478 (2021)
Studying the response of the Antarctic ice sheets during periods when climate conditions were similar to the present can provide important insights into current observed changes and help identify natural drivers of ice sheet retreat. In this context,
Externí odkaz:
https://doaj.org/article/86ae94df71844e53976292394aef2c7d
Publikováno v:
Climate of the Past, Vol 16, Pp 371-386 (2020)
Climate change in Siberia is currently receiving a lot of attention because large permafrost-covered areas could provide a strong positive feedback to global warming through the release of carbon that has been sequestered there on glacial–interglac
Externí odkaz:
https://doaj.org/article/e7b254ec178843c9a2ac7a53d50b43f2
Publikováno v:
Solid Earth, Vol 9, Pp 649-668 (2018)
The orientation and tectonic regime of the observed crustal/lithospheric stress field contribute to our knowledge of different deformation processes occurring within the Earth's crust and lithosphere. In this study, we analyze the influence of the
Externí odkaz:
https://doaj.org/article/91b6ece205c74568a87e0614d9033cd8
Publikováno v:
The Cryosphere, Vol 11, Iss 1, Pp 247-265 (2017)
The shallow ice approximation (SIA) is commonly used in ice-sheet models to simplify the force balance equations within the ice. However, the SIA cannot adequately reproduce the dynamics of the fast flowing ice streams usually found at the margins of
Externí odkaz:
https://doaj.org/article/bab29ded91304a8da282d02b6ca4bb31
Publikováno v:
The Cryosphere, Vol 10, Iss 2, Pp 639-664 (2016)
After more than a century of geological research, the Cordilleran ice sheet of North America remains among the least understood in terms of its former extent, volume, and dynamics. Because of the mountainous topography on which the ice sheet formed,
Externí odkaz:
https://doaj.org/article/c7d46b6d46dd4934a35d45098fecb1a3
Autor:
B. de Boer, A. M. Dolan, J. Bernales, E. Gasson, H. Goelzer, N. R. Golledge, J. Sutter, P. Huybrechts, G. Lohmann, I. Rogozhina, A. Abe-Ouchi, F. Saito, R. S. W. van de Wal
Publikováno v:
The Cryosphere, Vol 9, Iss 3, Pp 881-903 (2015)
In the context of future climate change, understanding the nature and behaviour of ice sheets during warm intervals in Earth history is of fundamental importance. The late Pliocene warm period (also known as the PRISM interval: 3.264 to 3.025 million
Externí odkaz:
https://doaj.org/article/995420ed22dd469f85e631bc5958b44a