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  • 2020-2022  (4)
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  • 1
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    american geophysical union
    In:  EPIC3Journal of geophysocal research oceans, american geophysical union, 125, ISSN: 2169-9291
    Publication Date: 2020-02-14
    Description: Ocean heat transport is often thought to play a secondary role for Arctic surface warm16 ing in part because warm water which ows northward is prevented from reaching the 17 surface by a cold and stable halocline layer. However, recent observations in various re18 gions indicate that occasionally, warm water is found directly below the surface mixed 19 layer. Here we investigate Arctic Ocean surface energy uxes and the cold halocline layer 20 in climate model simulations from the Coupled Model Intercomparison Project Phase 21 5 (CMIP5). An ensemble of 15 models shows decreased sea ice formation and increased 22 ocean energy release during fall, winter, and spring for a high-emission future scenario. 23 Along the main pathways for warm water advection, this increased energy release is not 24 locally balanced by increased Arctic Ocean energy uptake in summer. Because during 25 Arctic winter, the ocean mixed layer is mainly heated from below, we analyze changes 26 of the cold halocline layer in the monthly mean CMIP5 data. Fresh water acts to sta27 bilize the upper ocean as expected based on previous studies. We �nd that in spite of 28 this stabilizing e�ect, periods in which warm water is found directly or almost directly 29 below the mixed layer and which occur mainly in winter and spring become more fre30 quent in high-emission future scenario simulations, especially along the main pathways 31 for warm water advection. This could reduce sea ice formation and surface albedo. 32 Plain Language
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 2
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    In:  EPIC3Journal of Climate, 33(15), pp. 6621-6632
    Publication Date: 2020-07-08
    Description: Air-sea interactions play a critical role in the climate system. This study investigates wind-induced changes in the ocean surface temperature and sea ice cover feeding back onto the atmospheric circulation. This interaction was modeled in the Nordic seas, using a partial coupling method to constrain the ocean with prescribed wind forcing in an otherwise fully coupled Earth system model. This enabled the evaluation of not only the direct oceanic, but also the indirect atmospheric response to idealized forcing scenarios of perturbed winds over the Nordic seas. The results show that an anticyclonic wind anomaly forcing leads to significant surface cooling in the Greenland Sea mostly due to anomalous drift of sea ice. During winter, the cooling reduces the net surface heat flux to the atmosphere and increases sea level pressure. The pressure gradients result in anomalous geostrophic southerly winds, which locally are comparable both in direction and in velocity to the prescribed forcing anomalies, suggesting a positive feedback.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 3
    Publication Date: 2020-03-12
    Description: We revisit the challenges and prospects for ocean circulation models following Griffies et al. (2010). Over the past decade, ocean circulation models evolved through improved understanding, numerics, spatial discretization, grid configurations, parameterizations, data assimilation, environmental monitoring, and process-level observations and modeling. Important large scale applications over the last decade are simulations of the Southern Ocean, the Meridional Overturning Circulation and its variability, and regional sea level change. Submesoscale variability is now routinely resolved in process models and permitted in a few global models, and submesoscale effects are parameterized in most global models. The scales where nonhydrostatic effects become important are beginning to be resolved in regional and process models. Coupling to sea ice, ice shelves, and high-resolution atmospheric models has stimulated new ideas and driven improvements in numerics. Observations have provided insight into turbulence and mixing around the globe and its consequences are assessed through perturbed physics models. Relatedly, parameterizations of the mixing and overturning processes in boundary layers and the ocean interior have improved. New diagnostics being used for evaluating models alongside present and novel observations are briefly referenced. The overall goal is summarizing new developments in ocean modeling, including: how new and existing observations can be used, what modeling challenges remain, and how simulations can be used to support observations
    Description: Published
    Description: Article 65
    Description: 4A. Oceanografia e clima
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 4
    Publication Date: 2021-10-25
    Description: Ocean heat transport is often thought to play a secondary role for Arctic surface warming in part because warm water which flows northward is prevented from reaching the surface by a cold and stable halocline layer. However, recent observations in various regions indicate that occasionally, warm water is found directly below the surface mixed layer. Here we investigate Arctic Ocean surface energy fluxes and the cold halocline layer in climate model simulations from the Coupled Model Intercomparison Project Phase 5. An ensemble of 15 models shows decreased sea ice formation and increased ocean energy release during fall, winter, and spring for a high-emission future scenario. Along the main pathways for warm water advection, this increased energy release is not locally balanced by increased Arctic Ocean energy uptake in summer. Because during Arctic winter, the ocean mixed layer is mainly heated from below, we analyze changes of the cold halocline layer in the monthly mean Coupled Model Intercomparison Project Phase 5 data. Fresh water acts to stabilize the upper ocean as expected based on previous studies. We find that in spite of this stabilizing effect, periods in which warm water is found directly or almost directly below the mixed layer and which occur mainly in winter and spring become more frequent in high-emission future scenario simulations, especially along the main pathways for warm water advection. This could reduce sea ice formation and surface albedo.
    Keywords: 551.46 ; 551.6 ; Arctic ; climate change ; cold halocline ; climate modeling
    Language: English
    Type: map
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