Zobrazeno 1 - 10
of 18
pro vyhledávání: '"ANKIT PRAMANIK"'
Autor:
Sunil N. Oulkar, Meloth Thamban, Parmanand Sharma, Bhanu Pratap, Ajit T. Singh, Lavkush Kumar Patel, Ankit Pramanik, M. Ravichandran
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Various regional climatic factors influence glacier mass balance and thus control the water budget of the Himalayan rivers. However, the scarcity of observational data hinders a detailed understanding of the processes governing glacier mass balances
Externí odkaz:
https://doaj.org/article/2bdd50ab5bcc4e51b6d6d96b4f007692
Publikováno v:
Polar Research, Vol 38, Iss 0, Pp 1-13 (2019)
We evaluate how precipitation forcing data used in glacier mass balance models characterize snow accumulation events on synoptic timescales for two glaciers in north-western Svalbard (Kongsvegen and Holtedahlfonna). Using sonic ranger (snow depth) an
Externí odkaz:
https://doaj.org/article/cee88bb4b14d47e7878a569dd2691264
Publikováno v:
Journal of Glaciology, Vol 64, Pp 943-956 (2018)
The Kongsfjord basin in northwest Svalbard is the site of a number of interdisciplinary studies concerned with the effect of fresh water from seasonal snow and glacier melt on the physical and biological environment. We use an energy-balance model co
Externí odkaz:
https://doaj.org/article/661eef4d0753407e89c791c46d39d498
Autor:
Laura Halbach, Mikko Vihtakari, Pedro Duarte, Alistair Everett, Mats A. Granskog, Haakon Hop, Hanna M. Kauko, Svein Kristiansen, Per I. Myhre, Alexey K. Pavlov, Ankit Pramanik, Agnieszka Tatarek, Tomas Torsvik, Józef M. Wiktor, Anette Wold, Angela Wulff, Harald Steen, Philipp Assmy
Publikováno v:
Frontiers in Marine Science, Vol 6 (2019)
Meltwater discharge from tidewater glaciers impacts the adjacent marine environment. Due to the global warming, tidewater glaciers are retreating and will eventually terminate on land. Yet, the mechanisms through which meltwater runoff and subglacial
Externí odkaz:
https://doaj.org/article/fcd7b32fefde4aa181150440e524367e
The Greenland ice-sheet surface melt has increased substantially in intensity and spatial extent over the recent decades. The rapid migration of melt towards upstream areas of Greenland ice sheet is expected to incur major changes in hydrological beh
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::694bcbc63aa86b5d5c40385a47f6b5e4
https://doi.org/10.5194/egusphere-egu23-10571
https://doi.org/10.5194/egusphere-egu23-10571
Autor:
Philip Pika, Sandra Arndt, Veronica Tsibulskaya, Ankit Pramanik, Jade Hatton, Jakub Zarsky, Lia Costa Pinto Wentzel, Jakub Trubac, Anna Stehrer-Polášková, Petra Vinšová, Jon R. Hawkings, Marek Stibal
Recent studies have shown the release of methane (CH4) through the melting Greenland Ice Sheet, and have thus identified it to have an additional potential positive climate feedback. This CH4 is thought to originate from biologically active methanoge
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e1424de914c2e1eede7f45c43285ffda
https://doi.org/10.5194/egusphere-egu23-15748
https://doi.org/10.5194/egusphere-egu23-15748
Publikováno v:
Progress in Oceanography. 206:102844
The Greenland ice sheet surface melt has increased substantially in intensity and spatial extent over the recent decades. The rapid migration of melt towards upstream areas of Greenland ice sheet is expected to incur major changes in hydrological beh
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b0e58d18f592363195c12796d2b3c370
https://doi.org/10.5194/egusphere-egu21-15070
https://doi.org/10.5194/egusphere-egu21-15070