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  • 551.46  (1)
  • ANT-Land_2012; Atka_Bay_Transect_7; Atka Bay; AWI_SeaIce; ICESUR; Ice survey; Identification; LATITUDE; LONGITUDE; NEUMAYER III; Platelet-layer conductivity; Platelet-layer thickness; Root mean square error; Sea ice conductivity; Sea Ice Physics @ AWI; Sea ice thickness; Validation flag/comment  (1)
  • Argo_float_Weddell_Gyre; Argo floats; Argo profiles; Argo trajectories; Geostrophic; HAFOS; Horizontal circulation; Hybrid Antarctic Float Observation System; ocean circulation; SO-CHIC; Southern Ocean Carbon and Heat Impact on Climate; Stream Function; TRR181; TRR181 Energy transfers in Atmosphere and Ocean; Weddell Gyre; Weddell Sea
Document type
Keywords
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Language
Years
  • 1
    Publication Date: 2023-11-24
    Keywords: ANT-Land_2012; Atka_Bay_Transect_7; Atka Bay; AWI_SeaIce; ICESUR; Ice survey; Identification; LATITUDE; LONGITUDE; NEUMAYER III; Platelet-layer conductivity; Platelet-layer thickness; Root mean square error; Sea ice conductivity; Sea Ice Physics @ AWI; Sea ice thickness; Validation flag/comment
    Type: Dataset
    Format: text/tab-separated-values, 20209 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-06-12
    Description: All available Argo float data from 2002 to 2016 in the Weddell Sea region were used to fit a stream function of the horizontal circulation of the Weddell Gyre. Argo float trajectories where sequences of positions are available (i.e., under ice profiles have an interpolated position and are therefore excluded) were used to estimate absolute velocity at the parking depth, which is then objectively mapped and fitted with a stream function using a cost function. Within the cost function, boundary conditions are defined such that the flow at the boundary is parallel to the boundary itself. The cost function provides the best fit stream function representative of the entire gyre circulation. The resulting stream function represents horizontal circulation at the parking depth of the Argo floats (usually 800 m; those with a different parking depth were corrected accordingly). Objectively mapped density data from the Argo float profiles were then incorporated to provide geostrophic stream functions for 41 levels between 50 and 2000 dbar. These were then vertically integrated to ultimately provide a geostrophic stream function of the upper 50-2000 dbar of the Weddell Gyre, representative of its mean horizontal circulation. Units are in Sverdrups (Sv), where 1 Sv = 1x10^6 m^3/s, and is the standard unit for quantifying volume transports. Full details of the method for the original stream function data, and the subsequent improvements for the published dataset are available in the supplemental links.
    Keywords: Argo_float_Weddell_Gyre; Argo floats; Argo profiles; Argo trajectories; Geostrophic; HAFOS; Horizontal circulation; Hybrid Antarctic Float Observation System; ocean circulation; SO-CHIC; Southern Ocean Carbon and Heat Impact on Climate; Stream Function; TRR181; TRR181 Energy transfers in Atmosphere and Ocean; Weddell Gyre; Weddell Sea
    Type: Dataset
    Format: application/x-hdf, 92.2 kBytes
    Location Call Number Limitation Availability
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  • 3
    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
    Location Call Number Limitation Availability
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