Cloud Forcing
Term · Environment · MLC-T-ENV-005321
The difference between the radiation budget components for average cloud conditions and cloud-free conditions. Roughly speaking, clouds increase the albedo from 15 to 30%, which results in a reduction of absorbed solar radiation of about 50 W/m^2. This cooling is offset somewhat by the greenhouse effect of clouds which reduces the OLR by about 30 W/m^2, so the net cloud forcing of the radiation budget is a loss of about 20 W/m^2. Were the clouds to be removed with all else remaining the same, the Earth would gain this last amount in net radiation and begin to warm up.
| Identifier | MLC-T-ENV-005321 |
|---|---|
| Field | Environment |
| References | NASA Earth Observatory Glossary |
Record as JSON
{
"id": "MLC-T-ENV-005321",
"term": "Cloud Forcing",
"field": "Environment",
"definition": "The difference between the radiation budget components for average cloud conditions and cloud-free conditions. Roughly speaking, clouds increase the albedo from 15 to 30%, which results in a reduction of absorbed solar radiation of about 50 W/m^2. This cooling is offset somewhat by the greenhouse effect of clouds which reduces the OLR by about 30 W/m^2, so the net cloud forcing of the radiation budget is a loss of about 20 W/m^2. Were the clouds to be removed with all else remaining the same, the Earth would gain this last amount in net radiation and begin to warm up.",
"references": [
"NASA Earth Observatory Glossary"
],
"url": "https://mlchart.com/terminology/environment/cloud-forcing/"
}
Record 5,321 of 30,736 in Environment terminology (MLC-0121). Request the full dataset.