Concept
volume_absorption_coefficient_of_radiative_flux_in_sea_water_due_to_dissolved_organic_matter
URI | http://vocab.nerc.ac.uk/collection/P07/current/CFSN0063/1/ | ||
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Within Vocab | Climate and Forecast Standard Names | ||
Alternative Labels | |||
Definition | 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. Radiative flux is the sum of shortwave and longwave radiative fluxes. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. The volume scattering/absorption/attenuation coefficient is the fractional change of radiative flux per unit path length due to the stated process. Coefficients with canonical units of m2 s-1 i.e. multiplied by density have standard names with specific_ instead of volume_. The scattering/absorption/attenuation coefficient is assumed to be an integral over all wavelengths, unless a coordinate of radiation_wavelength is included to specify the wavelength. | ||
Date | 2006-09-26T18:12:43 | ||
Identifier | SDN:P07::CFSN0063 | ||
Note | accepted | ||
Is Version Of | CFSN0063 | ||
version | 1 | ||
Same As | MMI | http://mmisw.org/ont/cf/parameter/volume_absorption_coefficient_of_radiative_flux_in_sea_water_due_to_dissolved_organic_matter | |
CF | http://vocab.nerc.ac.uk/standard_name/volume_absorption_coefficient_of_radiative_flux_in_sea_water_due_to_dissolved_organic_matter/ | ||
Broader | P04:G940 |
EARTH SCIENCE > Oceans > Ocean Optics > Absorption | |
P64:G940 |
EARTH SCIENCE > Oceans > Ocean Optics > Absorption | ||
P02:PPAB |
Light absorption in the water column | ||
Related | P06:UPRM |
per metre |
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