Concept
Toa instantaneous longwave forcing
| URI | http://vocab.nerc.ac.uk/standard_name/toa_instantaneous_longwave_forcing/ | ||
|---|---|---|---|
| Within Vocab | Climate and Forecast Standard Names | ||
| Definition | The abbreviation "toa" means top of atmosphere. The term "longwave" means longwave radiation. Instantaneous forcing is the radiative flux change caused instantaneously by an imposed change in radiative forcing agent (greenhouse gases, aerosol, solar radiation, etc.). A positive radiative forcing or radiative effect is equivalent to a downward radiative flux and contributes to a warming of the earth system. | ||
| Date | None | ||
| Note | accepted | ||
| modified | 2019-05-14 17:27:19.0 | ||
| Broad Match | P04:G206 |
EARTH SCIENCE > Atmosphere > Atmospheric Radiation > Longwave Radiation | |
P64:G206 |
EARTH SCIENCE > Atmosphere > Atmospheric Radiation > Longwave Radiation | ||
P02:LWRD |
Long-wave radiation | ||
| Exact Match | http://mmisw.org/ont/cf/parameter/toa_instantaneous_longwave_forcing | ||
| http://vocab.nerc.ac.uk/standard_name/toa_instantaneous_longwave_forcing/ | |||
P07:CFSN0120 |
toa_instantaneous_longwave_forcing | ||
| Related | P06:UFAA |
Watts per square metre | |
Alternate Formats
Other formats for this page:
RDF/XML Turtle JSON-LDAlternate Profiles
Other views of this page:
Alternate Profiles ?Different Media Types (HTML, text, RDF, JSON etc.) and different information model views, profiles, are available for this resource.
NVS html view ? Default NVS html view.
