Zobrazeno 1 - 10
of 54
pro vyhledávání: '"Torge Martin"'
Publikováno v:
Nature Communications, Vol 15, Iss 1, Pp 1-15 (2024)
Abstract Arctic sea ice mediates atmosphere-ocean momentum transfer, which drives upper ocean circulation. How Arctic Ocean surface stress and velocity respond to sea ice decline and changing winds under global warming is unclear. Here we show that s
Externí odkaz:
https://doaj.org/article/db40119550b54d02931f05e1241ee302
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 9, Pp n/a-n/a (2024)
Abstract Freshwater input from Greenland ice sheet melt has been increasing in the past decades from warming temperatures. To identify the impacts from enhanced meltwater input into the subpolar North Atlantic from 1997 to 2021, we use output from tw
Externí odkaz:
https://doaj.org/article/4be515e04b084643a854d4c14fe38a53
Autor:
Jia‐Jia Chen, Neil C. Swart, Rebecca Beadling, Xuhua Cheng, Tore Hattermann, André Jüling, Qian Li, John Marshall, Torge Martin, Morven Muilwijk, Andrew G. Pauling, Ariaan Purich, Inga J. Smith, Max Thomas
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 24, Pp n/a-n/a (2023)
Abstract The additional water from the Antarctic ice sheet and ice shelves due to climate‐induced melt can impact ocean circulation and global climate. However, the major processes driving melt are not adequately represented in Coupled Model Interc
Externí odkaz:
https://doaj.org/article/c45bb3e3bb79423e9cfa1a6052bdde8f
Publikováno v:
Frontiers in Climate, Vol 4 (2022)
Marine Heatwaves (MHWs) are ocean extreme events, characterized by anomalously high temperatures, which can have significant ecological impacts. The Northeast U.S. continental shelf is of great economical importance as it is home to a highly producti
Externí odkaz:
https://doaj.org/article/2a816173fc8a4baa8f89465fe693eb59
Autor:
Thomas W. N. Haine, Torge Martin
Publikováno v:
Scientific Reports, Vol 7, Iss 1, Pp 1-9 (2017)
Abstract The loss of Arctic sea ice is a conspicuous example of climate change. Climate models project ice-free conditions during summer this century under realistic emission scenarios, reflecting the increase in seasonality in ice cover. To quantify
Externí odkaz:
https://doaj.org/article/19191eab6d124efebb3c6af8313cb395
Autor:
Torge Martin, Arne Biastoch
Publikováno v:
eISSN
Increasing Greenland Ice Sheet melting is anticipated to impact water mass transformation in the subpolar North Atlantic and ultimately the meridional overturning circulation. Complex ocean and climate models are widely applied to estimate magnitude
Autor:
Mathias Zeller, Torge Martin
Mesoscale eddies are considered to have a major impact on the horizontal and vertical redistribution of heat, freshwater, carbon and other passive tracers across the Southern Ocean (SO). A way to investigate the role of mesoscale dynamics in a region
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1b9f5267ffa3829983d9814a9a848650
https://doi.org/10.5194/egusphere-egu23-12422
https://doi.org/10.5194/egusphere-egu23-12422
In scenarios with abrupt cessation of CO2 emissions (ZECMIP) the committed warming is expected to be 0±0.3K [1]. It is imperative to understand and narrow this uncertainty range because it is similar in size to the remaining allowable warming until
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8c8ef78bb9ec75778cbc2d1eccddda6a
https://doi.org/10.5194/egusphere-egu23-7493
https://doi.org/10.5194/egusphere-egu23-7493
Accelerated melting of the Greenland Ice Sheet has been identified as a tipping element in the freshwater balance of the subpolar North Atlantic (SPNA), where the East Greenland Current is a primary pathway for transporting Arctic-sourced freshwater
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a7010f25b4d780d79de3e00201d62738
https://doi.org/10.5194/egusphere-egu23-6219
https://doi.org/10.5194/egusphere-egu23-6219
Autor:
Torge Martin, Arne Biastoch
Both Greenland Ice Sheet mass loss and Atlantic Meridional Overturning Circulation weakening are considered tipping elements of the climate system under global warming. Ocean and climate models of varying complexity are widely applied to understand a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8156197fed0353d36fb9b45d973e8f5c
https://doi.org/10.5194/egusphere-egu23-5909
https://doi.org/10.5194/egusphere-egu23-5909