surface_sea_water_alkalinity_natural_analogue_expressed_as_mole_equivalent

rejected
Created: Oct. 12, 2016
Proposer: Paul Durack
Proposed Date: 2016-09-28
CMIP6 - OMIP Added to rejected list following agreement to use generic name sea_water_alkalinity_natural_analogue_expressed_as_mole_equivalent (now accepted).
Change Date: Oct. 12, 2016, 12:39 p.m.
Term: surface_sea_water_alkalinity_expressed_as_mole_equivalent_due_to_natural_component
Unit: mol m-3
Unit ref: MLM3
AMIP:
GRIB:
Change Date: Oct. 12, 2016, 12:40 p.m.
Term: surface_sea_water_alkalinity_expressed_as_mole_equivalent_due_to_natural_component
Unit: mol m-3
Unit ref: MLM3
AMIP:
GRIB:
The surface called "surface" means the lower boundary of the atmosphere. sea_water_alkalinity_expressed_as_mole_equivalent is the total alkalinity equivalent concentration (including carbonate, nitrogen, silicate, and borate components). 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.
Change Date: March 27, 2017, 12:23 a.m.
Term: surface_sea_water_alkalinity_natural_analogue_expressed_as_mole_equivalent
Unit: mol m-3
Unit ref: MLM3
AMIP:
GRIB:
The surface called "surface" means the lower boundary of the atmosphere. sea_water_alkalinity_expressed_as_mole_equivalent is the total alkalinity equivalent concentration (including carbonate, nitrogen, silicate, and borate components). 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.
Change Date: March 27, 2017, 12:24 a.m.
Term: surface_sea_water_alkalinity_natural_analogue_expressed_as_mole_equivalent
Unit: mol m-3
Unit ref: MLM3
AMIP:
GRIB:
The surface called "surface" means the lower boundary of the atmosphere. sea_water_alkalinity_expressed_as_mole_equivalent is the total alkalinity equivalent concentration (including carbonate, nitrogen, silicate, and borate components). In ocean biogeochemistry models, a "natural analogue" is used to simulate the effect on a modelled variable of imposing preindustrial atmospheric carbon dioxide concentrations, even when the model as a whole may be subjected to varying forcings.