{"id":4757,"date":"2019-12-24T09:32:48","date_gmt":"2019-12-24T12:32:48","guid":{"rendered":"https:\/\/www.nachodelatorre.com.ar\/mosconi\/?p=4757"},"modified":"2020-01-02T12:08:36","modified_gmt":"2020-01-02T15:08:36","slug":"el-continente-antartico-presenta-el-punto-terrestre-mas-profundo","status":"publish","type":"post","link":"https:\/\/www.fie.undef.edu.ar\/ceptm\/?p=4757","title":{"rendered":"El continente ant\u00e1rtico presenta el punto terrestre m\u00e1s profundo"},"content":{"rendered":"

Encuentran en la Ant\u00e1rtida el punto terrestre m\u00e1s profundo del planeta. Se inician as\u00ed otros estudios tales como que suceder\u00e1 en el futuro con los glaciares.<\/p>\n

Description<\/h2>\n

The data are in one single file in NetCDF<\/a> format (795 Mb) and all heights are in meters above mean sea level<\/strong><\/em> (the geoid used is provided in the NetCDF file). All the data use the same 450 m-resolution grid although the \u201ctrue\u201d resolution of the bedrock may vary depending on the method used to map the bed. This dataset uses data from 1993 to 2016 and has a nominal date of 2012 (same as REMA<\/a>).<\/p>\n\n\n\n\n\n
\"\"<\/a><\/td>\nAntarctic mask
\nThe ice\/land masks are from ADD rock outcrop, and the floating ice is derived from InSAR grounding lines (pers. comm.). 0 = ocean, 1 = ice-free land, 2 = grounded ice, 3 = floating ice, 4 = lake Vostok<\/td>\n		\"\"<\/a><\/td>\nSurface elevation
\nThe surface dem is from REMA.<\/td>\n<\/tr>\n
\"\"<\/a><\/td>\nSource
\nMethod used to calculate ice thickness: 0 = none, 1 = REMA\/IBCSO, 2 = Mass conservation, 3 = interpolation, 4 = hydrostatic equilibrium, 5 = streamline diffusion, 6 = gravity, 7=seismic, 10+ = bathymetry data<\/td>\n		\"\"<\/a><\/td>\nIce thickness
\nThe ice thickness is inferred using mass conservation along the peryphery of the ice sheet and ordinary kriging in the interior.<\/td>\n<\/tr>\n
\"\"<\/a><\/td>\nBed topography
\nThe bed elevation is calculated by subtracting the ice thickness from the surface elevation data.<\/td>\n		\"\"<\/a><\/td>\nError map
\nIce thickness and bed topography error.<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n

For the hydrostatic equilibrium calculation, we used a density of ice \u03c1ice<\/sub>=917 kg\/m3<\/sup>, and an ocean water density of \u03c1ocean<\/sub>=1027 kg\/m3<\/sup> (following the densities used in Griggs & Bamber 2011 and Chuter & Bamber 2015).<\/p>\n

As any model output, there are errors in these maps (there is an estimate included in the dataset). Feedback is more than welcome.<\/p>\n

Citation<\/h2>\n

Morlighem, M., Rignot, E., Binder, T. et al.<\/i> Deep glacial troughs and stabilizing ridges unveiled beneath the margins of the Antarctic ice sheet<\/a>. Nat. Geosci.<\/i> (2019) doi:10.1038\/s41561-019-0510-8<\/p>\n

Disclaimer<\/h2>\n

The ice thickness and bed topography are model outputs<\/em> and are not free of error (especially in regions where ice thickness measurements are sparse). This dataset is a work in progress and we encourage users to send us feedback so that we keep improving it.<\/p>\n

Projection<\/h2>\n

The projection is Polar Stereographic South (71\u00baS, 0\u00baE), which corresponds to ESPG 3031<\/a><\/p>\n

Reading with MATLAB<\/h2>\n

MATLAB now has an extensive library<\/a> for NetCDF files.
\nfilename = 'BedMachineAntarctica-2019-09-04.nc';
\nx = ncread(filename,'x');
\ny = ncread(filename,'y');
\nbed = ncread(filename,'bed')'; %Do not forget to transpose (MATLAB is column oriented)
\n%Display bed elevation
\nimagesc(x,y,bed); axis xy equal; caxis([-1000 3000]);<\/code><\/p>\n

Converting heights to WGS84<\/h2>\n

All heights are referenced to mean sea level (using the geoid EIGEN-6C4). To convert the heights to heights referenced to the WGS84 ellipsoid, simply add the geoid height:<\/p>\n

z<\/span>e<\/span>l<\/span>l<\/span>i<\/span>p<\/span>s<\/span>o<\/span>i<\/span>d<\/span><\/span><\/span><\/span>=<\/span>z<\/span>g<\/span>e<\/span>o<\/span>i<\/span>d<\/span><\/span><\/span><\/span>+<\/span>g<\/span>e<\/span>o<\/span>i<\/span>d<\/span><\/span><\/span><\/span><\/p>\n

Surface height and firn depth correction<\/h2>\n

All the quantities provided in BedMachine are in ice equivalent. This affects primarily the upper surface of the ice, to which we have subtracted a firn depth correction to account for the presence of air in the firn layer. The ice thickness is also in ice equivalent. To recover the top of the surface dem from RAME in WGS84:<\/p>\n

z<\/span>R<\/span>E<\/span>M<\/span>A<\/span><\/span><\/span><\/span>=<\/span>s<\/span>u<\/span>r<\/span>f<\/span>a<\/span>c<\/span>e<\/span>+<\/span>f<\/span>i<\/span>r<\/span>n<\/span>+<\/span>g<\/span>e<\/span>o<\/span>i<\/span>d<\/span><\/span><\/span><\/span><\/p>\n

where \u201cfirn\u201d is the firn depth correction, \u201csurface\u201d is the surface height, and \u201cgeoid\u201d is the geoid height. All these quantities are provided in the netCDF file.<\/p>\n

Acknowledgements and References<\/h2>\n

This project is performed at the University of California Irvine under a contract with the National Aeronautics and Space Administration (Sea Level Rise Program #NNX14AN03G and MEaSURES-3) and the National Science Foundation (Thwaites #1739031).<\/p>\n

The ice thickness data are from:<\/p>\n