surface_sea_water_alkalinity_natural_analogue_expressed_as_mole_equivalent
rejected
Created: 12 Oct 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: 12 Oct 2016, 1:39 p.m.
surface_sea_water_alkalinity_expressed_as_mole_equivalent_due_to_natural_component mol m-3 [MLM3]
Change Date: 12 Oct 2016, 1:40 p.m.
surface_sea_water_alkalinity_expressed_as_mole_equivalent_due_to_natural_component mol m-3 [MLM3] 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: 27 Mar 2017, 1:23 a.m.
surface_sea_water_alkalinity_natural_analogue_expressed_as_mole_equivalent mol m-3 [MLM3] 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: 27 Mar 2017, 1:24 a.m.
surface_sea_water_alkalinity_natural_analogue_expressed_as_mole_equivalent mol m-3 [MLM3] 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.