MLchartDataset catalogue

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.

Table 1. Record
IdentifierMLC-T-ENV-005321
FieldEnvironment
ReferencesNASA 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.