Concept
toa_instantaneous_radiative_forcing
| URI | http://vocab.nerc.ac.uk/collection/P07/current/CFSN0121/2/ | ||
|---|---|---|---|
| Within Vocab | Climate and Forecast Standard Names | ||
| Alternative Labels | |||
| Definition | The abbreviation "toa" means top of atmosphere. 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 | 2019-05-14T17:27:19 | ||
| Identifier | SDN:P07::CFSN0121 | ||
| Note | accepted | ||
| Is Version Of | CFSN0121 | ||
| Previous Version | 1 | ||
| version | 2 | ||
| Same As | MMI | http://mmisw.org/ont/cf/parameter/toa_instantaneous_radiative_forcing | |
| CF | http://vocab.nerc.ac.uk/standard_name/toa_instantaneous_radiative_forcing/ | ||
| Broader | P04:G211 |
EARTH SCIENCE > Atmosphere > Atmospheric Radiation > Radiative Forcing | |
P64:G211 |
EARTH SCIENCE > Atmosphere > Atmospheric Radiation > Radiative Forcing | ||
| Related | P06:UFAA |
Watts per square metre | |
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