OPeNDAP Dataset Query Form

OPeNDAP Dataset Access Form

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Global Attributes:	history: version 1, 13-Sep-2013; by script build-gia-ts-1.py contact: mark.carson@uni-hamburg.de references: Carson et al. 2016, Slangen et. al 2014 notes: from the Peltier ICE-5G (VM2) ice history and viscosity model

Variables:	time: Array of 64 bit Reals [time = 0..94] time: long_name: time units: days since 0001-01-01 00:00:00 bounds: time_bnds calendar: 365_day axis: T
	time_bnds: Array of 64 bit Reals [time = 0..94][bnds = 0..1] time: bnds:
	lat: Array of 64 bit Reals [lat = 0..179] lat: standard_name: latitude long_name: latitude coordinate units: degrees_north axis: Y
	lon: Array of 64 bit Reals [lon = 0..359] lon: standard_name: longitude long_name: longitude coordinate units: degrees_east axis: X
	gia: Grid lat: lon: _FillValue: 1.0E20 long_name: GIA sea level change relative to dry land, 2081-2100 mean minus 1986-2005 mean units: m missing_value: 1.0E20 comment: Estimate of the contribution to sea level rise from GIA. This is from the Peltier ICE-5G (VM2) ice history and viscosity model. In this variable, the GIA field was multiplied by -1 to yield the sense of relative sea level change to dry land, and is thus the opposite of the motion of the earth's crust. coordinates: lat lon
	gia_ts: Grid time: lat: lon: _FillValue: 1.0E20 long_name: Glacial Isostatic Adjustment annual time series, reversed; sea level change relative to dry land units: m missing_value: 1.0E20 comment: Estimate of the contribution to sea level rise from GIA. This is from the Peltier ICE-5G (VM2) ice history and viscosity model. In this variable, the GIA field was multiplied by -1 to yield the sense of relative sea level change to dry land, and is thus the opposite of the motion of the earth's crust. coordinates: lat lon
	gia_sd: Grid time: lat: lon: _FillValue: 1.0E20 long_name: GIA uncertainty annual time series, ; sea level change relative to dry land units: m missing_value: 1.0E20 comment: Estimate of GIA uncertainty. The estimate is from the absolute difference between the Peltier ICE-5G (VM2) ice history and viscosity model and the Lambeck ice history and ANU viscoity model. This absolute difference is treated as the 'standard error' for the uncertainty estimates in the papers listed under the 'references' global attribute. coordinates: lat lon

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DDS:

Dataset {
    Float64 time[time = 95];
    Float64 time_bnds[time = 95][bnds = 2];
    Float64 lat[lat = 180];
    Float64 lon[lon = 360];
    Grid {
     ARRAY:
        Float32 gia[lat = 180][lon = 360];
     MAPS:
        Float64 lat[lat = 180];
        Float64 lon[lon = 360];
    } gia;
    Grid {
     ARRAY:
        Float32 gia_ts[time = 95][lat = 180][lon = 360];
     MAPS:
        Float64 time[time = 95];
        Float64 lat[lat = 180];
        Float64 lon[lon = 360];
    } gia_ts;
    Grid {
     ARRAY:
        Float32 gia_sd[time = 95][lat = 180][lon = 360];
     MAPS:
        Float64 time[time = 95];
        Float64 lat[lat = 180];
        Float64 lon[lon = 360];
    } gia_sd;
} ftpthredds/coastal_sea_level_changes/gia.nc;

OPeNDAP Dataset Access Form

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