fraction_of_time_with_sea_ice_area_fraction_above_threshold

complete
Created: July 27, 2016
Proposer: Dirk Notz
Proposed Date: 2016-07-19
CMIP6 - SIMIP. 1.1
Change Date: July 27, 2016, 3:22 p.m.
Term: proportion_of_model_time_steps_with_sea_ice_fraction_above_threshold
Unit: 1
Unit ref:
AMIP:
GRIB:
Change Date: July 27, 2016, 3:23 p.m.
Term: proportion_of_model_time_steps_with_sea_ice_fraction_above_threshold
Unit: 1
Unit ref: UUUU
AMIP:
GRIB:
Fraction of time steps which had sea ice during the averaging period of typically one month. It allows one to differentiate half a month of 100% sea-ice cover from a full month of 50 % sea-ice concentration.
Change Date: Aug. 5, 2016, 1:15 a.m.
Term: fraction_of_time_with_sea_ice_area_fraction_above_threshold
Unit: 1
Unit ref: UUUU
AMIP:
GRIB:
Fraction of time steps which had sea ice during the averaging period of typically one month. It allows one to differentiate half a month of 100% sea-ice cover from a full month of 50 % sea-ice concentration.
Change Date: June 14, 2018, 3:27 p.m.
Term: fraction_of_time_with_sea_ice_area_fraction_above_threshold
Unit: 1
Unit ref: UUUU
AMIP:
GRIB:
"X_area_fraction" means the fraction of horizontal area occupied by X. Sea ice area fraction is area of the sea surface occupied by sea ice. The area threshold value must be specified by supplying a coordinate variable or scalar coordinate variable with the standard name of sea_ice_area_fraction. "Sea_ice" means all ice floating on the sea with the exception of floating ice shelves, which are regarded as land ice in models.
Change Date: June 21, 2018, 3:14 a.m.
Term: fraction_of_time_with_sea_ice_area_fraction_above_threshold
Unit: 1
Unit ref: UUUU
AMIP:
GRIB:
"X_area_fraction" means the fraction of horizontal area occupied by X. Sea ice area fraction is area of the sea surface occupied by sea ice. The area threshold value must be specified by supplying a coordinate variable or scalar coordinate variable with the standard name of sea_ice_area_fraction. "Sea ice" means all ice floating in the sea which has formed from freezing sea water, rather than by other processes such as calving of land ice to form icebergs.