tidal_sea_surface_height_above_mean_sea_level

complete
Created: April 27, 2018
Proposer: Andrew Saulter
Proposed Date: 2018-04-04
Change Date: April 27, 2018, 3:21 p.m.
Term: sea_surface_height_above_mean_sea_level_due_to_tide
Unit: m
Unit ref: ULAA
AMIP:
GRIB:
"Sea surface height" is a time-varying quantity. "Height_above_X" means the vertical distance above the named surface X. "Mean sea level" means the time mean of sea surface elevation at a given location over an arbitrary period sufficient to eliminate the tidal signals. 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. Tides are a significant contributor to the observed sea surface height; here "tide" denotes a generic variable describing the time varying tidal signal, for example as generated based on a summation of harmonically analysed components, or resulting from the application of such components as boundary conditions to a numerical tidal model.
Change Date: July 26, 2018, 8:42 a.m.
Term: tidal_sea_surface_height_above_mean_sea_level
Unit: m
Unit ref: ULAA
AMIP:
GRIB:
"Sea surface height" is a time-varying quantity. "Height_above_X" means the vertical distance above the named surface X. "Mean sea level" means the time mean of sea surface elevation at a given location over an arbitrary period sufficient to eliminate the tidal signals.
Change Date: July 26, 2018, 8:42 a.m.
Term: tidal_sea_surface_height_above_mean_sea_level
Unit: m
Unit ref: ULAA
AMIP:
GRIB:
"Sea surface height" is a time-varying quantity. "Height_above_X" means the vertical distance above the named surface X. "Mean sea level" means the time mean of sea surface elevation at a given location over an arbitrary period sufficient to eliminate the tidal signals. The tidal component of sea surface height describes the predicted variability of the sea surface due to astronomic forcing (chiefly lunar and solar cycles) and shallow water resonance of tidal components; for example as generated based on harmonic analysis, or resulting from the application of harmonic tidal series as boundary conditions to a numerical tidal model.