Zobrazeno 1 - 10
of 34
pro vyhledávání: '"M. Schodlok"'
Publikováno v:
The Cryosphere, Vol 17, Pp 2261-2283 (2023)
Land ice discharge from the Antarctic continent into the ocean is restrained by ice shelves, floating extensions of grounded ice that buttress the glacier outflow. The ongoing thinning of these ice shelves – largely due to enhanced melting at their
Externí odkaz:
https://doaj.org/article/7b861fed2b014f81b2ed19f7e8aaddca
Publikováno v:
The Cryosphere, Vol 8, Iss 5, Pp 1699-1710 (2014)
Pine Island Glacier, a major contributor to sea level rise in West Antarctica, has been undergoing significant changes over the last few decades. Here, we employ a three-dimensional, higher-order model to simulate its evolution over the next 50 yr in
Externí odkaz:
https://doaj.org/article/a7275e9021a74df69ab1eba2c05ff68a
Akademický článek
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Publikováno v:
Journal of Geophysical Research: Oceans. 122:6180-6195
Recent studies suggest that the thickness of Winter Water (WW), that is, water with potential temperature below ∼-1°C located below Antarctic Surface Water and above Circumpolar Deep Water (CDW) is critical in determining the ice shelf melt rate,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2bdf1962ecf48885d84b96a1612da18d
https://doi.org/10.1002/2016jc012538
https://doi.org/10.1002/2016jc012538
Publikováno v:
Journal of Geophysical Research: Oceans. 121:1085-1109
PUBLICATIONS Journal of Geophysical Research: Oceans RESEARCH ARTICLE 10.1002/2015JC011117 Key Points: Explicit representation of ice-shelf- ocean interaction in an ocean reanalysis Compare modeled basal melt rates and pattern to estimates derived fr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5f458071bfe198a95a7e1cd3ecd13d52
https://doi.org/10.1002/2015jc011117
https://doi.org/10.1002/2015jc011117
Publikováno v:
Nature Communications
Nature communications, vol 9, iss 1
Nature Communications, Vol 9, Iss 1, Pp 1-9 (2018)
Nature communications, vol 9, iss 1
Nature Communications, Vol 9, Iss 1, Pp 1-9 (2018)
Melting of West Antarctic ice shelves is enhanced by Circumpolar Deep Water (CDW) intruding onto the Amundsen and Bellingshausen Seas (ABS) continental shelves. Despite existing studies of cross-shelf and on-shelf CDW transports, CDW pathways onto th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::53ecf9c480548b9b175895cd60aa1c37
https://pubmed.ncbi.nlm.nih.gov/30143637
https://pubmed.ncbi.nlm.nih.gov/30143637
Akademický článek
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Publikováno v:
Annals of Glaciology. 53:156-162
Two high-resolution (1 km grid) numerical model simulations of the Amundsen Sea, West Antarctica, are used to study the role of the ocean in the mass loss and grounding line retreat of Pine Island Glacier. The first simulation uses BEDMAP bathymetry
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f57eed1f8693282b8f93297ba4e25207
https://doi.org/10.3189/2012aog60a073
https://doi.org/10.3189/2012aog60a073
Autor:
Jill Nicola Schwarz, M. Schodlok
Publikováno v:
Deep Sea Research Part I: Oceanographic Research Papers. 56:1727-1741
Icebergs that calve from the Antarctic ice shelves and drift in the Southern Ocean melt to deliver fresh water, dust and minerogenic particles to the surface ocean along the iceberg's path. Each of these components may have an effect on growth condit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bf1cb73edb91f805d51579deff6d586d
https://doi.org/10.1016/j.dsr.2009.05.003
https://doi.org/10.1016/j.dsr.2009.05.003
Publikováno v:
Deep Sea Research Part II: Topical Studies in Oceanography. 55:1040-1055
The mesozooplankton community, with special emphasis on calanoid copepods, was studied with respect to its species composition, abundance, vertical distribution and developmental structure during the “Ice Station POLarstern” (ISPOL) expedition to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::53589e03bb87ecdab7fe80b1b0792fc6
https://doi.org/10.1016/j.dsr2.2007.12.013
https://doi.org/10.1016/j.dsr2.2007.12.013