sea_ice_y_force_per_unit_area_due_to_coriolis_effect

complete
Created: Aug. 4, 2016
Proposer: Dirk Notz
Proposed Date: 2016-07-19
CMIP6 - SiMIP. 1.25.
Change Date: Aug. 4, 2016, 5:48 p.m.
Term: sea_ice_spcecific_y_force_due_to_coriolis_term
Unit: N m-2
Unit ref: UNSM
AMIP:
GRIB:
Y-component of force on sea ice caused by coriolis force.
Change Date: May 21, 2018, 12:41 p.m.
Term: sea_ice_specific_y_force_due_to_coriolis_term
Unit: N m-2
Unit ref: UNSM
AMIP:
GRIB:
Y-component of force on sea ice caused by coriolis force.
Change Date: June 14, 2018, 2:07 p.m.
Term: sea_ice_y_force_per_unit_area_due_to_coriolis_effect
Unit: N m-2
Unit ref: UNSM
AMIP:
GRIB:
Change Date: June 14, 2018, 2:08 p.m.
Term: sea_ice_y_force_per_unit_area_due_to_coriolis_effect
Unit: N m-2
Unit ref: UNSM
AMIP:
GRIB:
"y" indicates a vector component along the grid y-axis, positive with increasing y. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. In meteorology and oceanography, the Coriolis effect per unit mass arises solely from the earth's rotation and acts as a deflecting force, normal to the velocity, to the right of the motion in the Northern Hemisphere and to the left in the Southern Hemisphere. Reference: American Meteorological Society Glossary http://glossary.ametsoc.org/wiki/Coriolis_force. "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, 3:03 a.m.
Term: sea_ice_y_force_per_unit_area_due_to_coriolis_effect
Unit: N m-2
Unit ref: UNSM
AMIP:
GRIB:
"y" indicates a vector component along the grid y-axis, positive with increasing y. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. In meteorology and oceanography, the Coriolis effect per unit mass arises solely from the earth's rotation and acts as a deflecting force, normal to the velocity, to the right of the motion in the Northern Hemisphere and to the left in the Southern Hemisphere. Reference: American Meteorological Society Glossary http://glossary.ametsoc.org/wiki/Coriolis_force. "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.