Zobrazeno 1 - 10
of 67
pro vyhledávání: '"C, Heuzé"'
Publikováno v:
Ocean Science, Vol 20, Pp 917-930 (2024)
The Fram Strait is the only deep gateway between the Arctic and the rest of the World Ocean, and it is thus a key region to understand how the deep Arctic will evolve. However, studies and data regarding the deep ocean are scarce, making it difficult
Externí odkaz:
https://doaj.org/article/d8aab5033d974ab29bd62a49d38bbaf3
Publikováno v:
Ocean Science, Vol 20, Pp 201-215 (2024)
From generating metrics representative of a wide region to saving costs by reducing the density of an observational network, the reasons to split the ocean into distinct regions are many. Traditionally, this has been done somewhat arbitrarily using t
Externí odkaz:
https://doaj.org/article/66c121ad910142159005f983eca6038c
Autor:
C. Heuzé, O. Huhn, M. Walter, N. Sukhikh, S. Karam, W. Körtke, M. Vredenborg, K. Bulsiewicz, J. Sültenfuß, Y.-C. Fang, C. Mertens, B. Rabe, S. Tippenhauer, J. Allerholt, H. He, D. Kuhlmey, I. Kuznetsov, M. Mallet
Publikováno v:
Earth System Science Data, Vol 15, Pp 5517-5534 (2023)
Trace gases have demonstrated their strength for oceanographic studies, with applications ranging from the tracking of glacial meltwater plumes to estimates of the abyssal overturning duration. Yet measurements of such passive tracers in the ice-cove
Externí odkaz:
https://doaj.org/article/8a3954c6a01b4b37bbc4706ecabda9b3
Publikováno v:
The Cryosphere, Vol 15, Pp 4281-4313 (2021)
Polynyas facilitate air–sea fluxes, impacting climate-relevant properties such as sea ice formation and deep water production. Despite their importance, polynyas have been poorly represented in past generations of climate models. Here we present a
Externí odkaz:
https://doaj.org/article/e13dc47752ca4730be1d8af433ca3c7d
Autor:
A. Solomon, C. Heuzé, B. Rabe, S. Bacon, L. Bertino, P. Heimbach, J. Inoue, D. Iovino, R. Mottram, X. Zhang, Y. Aksenov, R. McAdam, A. Nguyen, R. P. Raj, H. Tang
Publikováno v:
Ocean Science, Vol 17, Pp 1081-1102 (2021)
The Arctic climate system is rapidly transitioning into a new regime with a reduction in the extent of sea ice, enhanced mixing in the ocean and atmosphere, and thus enhanced coupling within the ocean–ice–atmosphere system; these physical changes
Externí odkaz:
https://doaj.org/article/54499b002fe54a6bb6a4c995fd5a718b
Publikováno v:
The Cryosphere, Vol 15, Pp 3401-3421 (2021)
Knowing when sea ice will open is crucial, notably for scientific deployments. This was particularly obvious when the Weddell Polynya, a large opening in the winter Southern Ocean sea ice, unexpectedly re-appeared in 2016. As no precursor had been de
Externí odkaz:
https://doaj.org/article/f94cf9b6bb3a456598f42300490221f1
Autor:
C. Heuzé
Publikováno v:
Ocean Science, Vol 17, Pp 59-90 (2021)
Deep and bottom water formation are crucial components of the global ocean circulation, yet they were poorly represented in the previous generation of climate models. We here quantify biases in Antarctic Bottom Water (AABW) and North Atlantic Deep Wa
Externí odkaz:
https://doaj.org/article/d5a7f1117de94d0bae7bf1a08c5b64fc
Autor:
C. Heuzé
Publikováno v:
Ocean Science, Vol 13, Pp 609-622 (2017)
Deep water formation in climate models is indicative of their ability to simulate future ocean circulation, carbon and heat uptake, and sea level rise. Present-day temperature, salinity, sea ice concentration and ocean transport in the North Atlan
Externí odkaz:
https://doaj.org/article/7025aad866bb4a9ebaf6fa1ec63d920a
Autor:
M. A. Stiller-Reeve, C. Heuzé, W. T. Ball, R. H. White, G. Messori, K. van der Wiel, I. Medhaug, A. H. Eckes, A. O'Callaghan, M. J. Newland, S. R. Williams, M. Kasoar, H. E. Wittmeier, V. Kumer
Publikováno v:
Hydrology and Earth System Sciences, Vol 20, Iss 7, Pp 2965-2973 (2016)
Science, in our case the climate and geosciences, is increasingly interdisciplinary. Scientists must therefore communicate across disciplinary boundaries. For this communication to be successful, scientists must write clearly and concisely, yet the h
Externí odkaz:
https://doaj.org/article/96ca548437dc4687954f08ad3b62a6a0
Publikováno v:
Geoscientific Model Development, Vol 8, Iss 10, Pp 3119-3130 (2015)
Most CMIP5 (Coupled Model Intercomparison Project Phase 5) models unrealistically form Antarctic Bottom Water by open ocean deep convection in the Weddell and Ross seas. To identify the mechanisms triggering Southern Ocean deep convection in models,
Externí odkaz:
https://doaj.org/article/8efbc2c333c1453fb7bebef9f1a0dcca