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3 results for “Antarctic Bottom Water”
Full Inverse Velocity Fields for "Transport of Antarctic Bottom Water entering the Brazil Basin in a Planetary Geostrophic Inverse Model"
<p>Velocity fields on all approximate neutral surfaces from the inverse model presented in "Transport of Antarctic Bottom Water entering the Brazil Basin in a Planetary Geostrophic Inverse Model". The pressure of the approximate neutral surface is contoured in the background. The number in the title represents the pressure of the approximate neutral surface at the reference station in the Hunter Channel.</p>
Data in support of "Antarctic Bottom Water sensitivity to spatio-temporal variations in Antarctic meltwater fluxes"
<p> <em>This data contains the unprocessed output from the five equilibrium simulations used in the paper "Antarctic Bottom Water sensitivity to spatio-temporal variations in Antarctic meltwater fluxes". Simulations were run using the ocean and sea-ice components of CESM1, and the atmosphere was data-driven, and based on ERA5 reanalysis from 1958 until 1980. All data is in netcdf, and includes the description of flag values, and units. The five simulations differ in the freshwater flux scheme as described below:</em></p> <p><br> <em>Simulation UNIF - files: ga1.f09_g16.308<br> Forced with freshwater fluxes from the Antarctic Ice Sheet (AIS), uniformly distributed around the Antarctic coast. Total freshwater flux from AIS: 2075 Gt/yr<br> <br> Simulation BM - files: ga1.f09_g16.208<br> Forced with asymmetric zonal freshwater fluxes from the AIS.<br> Total freshwater flux from AIS: 2075 Gt/yr<br> <br> Simulation VARI - files: ga1.f09_g16.108<br> Forced with asymmetric zonal and meridional freshwater fluxes from the AIS. Total freshwater flux from AIS: 2075 Gt/yr<br> <br> Simulation CV - files: ga1.f09_g16.408<br> Forced with asymmetric meridional freshwater fluxes from the AIS, to mimic iceberg melting. Total freshwater flux from AIS: 934 Gt/yr<br> <br> Simulation VARI120% - files: ga1.f09_g16.x18<br> Same as VARI, but the total freshwater fluxes were increased by 20%. Total freshwater flux from AIS: 2490 Gt/yr</em><br> </p> <p> </p> <p>[30S 90S] , [180W 180E]</p> <p> </p> <p><strong>Variables:</strong> Ocean Temperature [Celius], Salinity [PSU], Sea ice Fraction [fraction], Salt flux from sea ice [kg/m2/s], and ocean overturning [SV]</p> <p><em>For more information, check:<a href="https://doi.org/10.1002/essoar.10512610.1">https://doi.org/10.1002/essoar.10512610.1</a></em></p>
Boundary upwelling of Antarctic Bottom Water by topographic turbulence
<p>Software and data associated with the following publication:</p> <p>Baker, L. E., Mashayek, A., & Naveira Garabato, A. C. (2023). Boundary upwelling of Antarctic Bottom Water by topographic turbulence. AGU Advances, 4, e2022AV000858. https://doi. org/10.1029/2022AV000858</p>
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