
How much heat the planet radiates to space over a given patch of ocean, here 5N-5S, 160E-160W. Tall clouds are cold on top, so they radiate less: a NEGATIVE anomaly means the cloud tower has moved in.Outgoing longwave radiation (OLR) is the infrared energy that Earth emits back to space. Over the equatorial Pacific, measuring OLR in a specific box (5°N–5°S, 160°E–160°W) reveals where deep convective clouds are active. Tall thunderstorm clouds have very cold tops, so they emit less infrared radiation than the warm ocean surface. Thus, a negative OLR anomaly in this region means that such cloud towers have moved in, indicating strong atmospheric convection and rising air.
Satellite measurements of OLR began in the 1970s with NOAA's polar-orbiting satellites, and the data have been used since then to monitor tropical convection and ENSO. The specific index over the equatorial Pacific became a standard tool in climate diagnostics.
Satellites measure the infrared radiance leaving the top of the atmosphere. In clear skies, the signal comes from the warm ocean surface, producing high OLR values. When thick, tall clouds are present, they block that surface emission and instead radiate from their cold tops, lowering the OLR. By averaging over the specified region and comparing to the long-term average, scientists get an index of convective activity. This is closely tied to the Walker circulation: when OLR is anomalously low (more clouds), it often signals the eastward shift of convection that accompanies El Niño.
OLR anomalies are used to track the Madden–Julian Oscillation and to provide real-time monitoring of convective activity that can trigger or respond to El Niño events.
A single large thunderstorm over the tropical Pacific can cool the local surface by shading it from sunlight, but its cold cloud top also reduces heat loss to space, creating a complex tug-of-war on the energy budget.








