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Outgoing Longwave Radiation (OLR): AVHRR

OLR (Outgoing Longwave Radiation) is a measure of the amount of energy emitted to space by earth's surface, oceans and atmosphere. As such, it is a critical component of the earth's radiation budget. In a different context, OLR values are often used as a proxy for convection in tropical and subtropical regions since cloud top temperatures (colder is higher) are an indicator of cloud height. OLR observations are made via the Advanced Very High Resolution Radiometer (AVHRR) instrument aboard the NOAA polar orbiting spacecraft. The raw ascending and descending swath data have been spatially and temporarally interpolated onto grids to facilitate use.

OLR estimates are a key component for the standard Madden-Julian Oscillation (MJO) CLIVAR diagnostics which are used to study the MJO and for climate model evaluation.

Key Strengths:

  • Long time series of up-to-date OLR values
  • High quality data access site

Key Limitations:

  • 2.5x2.5 resolution may be too coarse for certain studies

Years of Record

1974/06 to 2013/12
temporal metadataID:

Formats

Timestep

Climatology | Sub-daily | Daily | Monthly

Data Time Period Extended?

yes, data set is extended

Domain

Global

Spatial Resolution

2.5x2.5

Vertical Levels

Single level (not surface)

Input Data

NOAA Polar Orbiting Satelite series (AVHRR)

Earth system components and main variables

Atmosphere, Outgoing Longwave Radiation

Data Access: Please Cite data sources, following the data providers' instructions.

  1. NOAA Interpolated Outgoing Longwave Radiation (OLR)
  2. ftp ftp.cpc.ncep.noaa.gov ; cd precip/noaa* ; look for OLR directories
  3. NOAA Daily (non-interpolated) Outgoing Longwave Radiation (OLR)

Key Figures

Click the thumbnails to view larger sizes

Thumbnails

Captions
Daily interpolated OLR anomalies for 31 Dec. 2013. Anomalies are relative to the 1981-2010 daily climatology. (Source ESRL/PSD)
Daily non-interpolated OLR anomalies for 3 Sept 2014. Anomalies are relative to the 1981-2010 daily climatology. (Source ESRL/PSD)
Raw and smoothed daily OLR for 26-years (1980-2005) of daily data. OLR anomalies are used in many standardized MJO CLIVAR diagnostics (Climate Data Guide; D. Shea)
20-100 day band passed OLR anomalies for 1996-1997. (Climate Data Guide; D. Shea)
Spatial patterns for 31 Dec 1996: (top) OLR anomaly for each grid point; (bottom) 20-100 day band-pass filtered for the data. (Climate Data Guide; D. Shea)
OLR and zonal wind anomaly cross-spectra: coherence-squared and phase relationships in wavenumber-frequency space. (Climate Data Guide; D. Shea)
OLR average wavenumber-frequency spectra for all the summer seasons 1980-2005. (Climate Data Guide; D. Shea)
Life cycle of 20-100 day band passed filtered anomaly OLR, U850, V850 for the years 1995-1999. (Climate Data Guide; D. Shea)

Cite this page

National Center for Atmospheric Research Staff (Eds). Last modified 05 Sep 2014. "The Climate Data Guide: Outgoing Longwave Radiation (OLR): AVHRR ." Retrieved from https://climatedataguide.ucar.edu/climate-data/outgoing-longwave-radiation-olr-avhrr.

Acknowledgement of any material taken from this page is appreciated. On behalf of experts who have contributed data, advice, and/or figures, please cite their work as well.

Outgoing Longwave Radiation (OLR): AVHRR

OLR (Outgoing Longwave Radiation) is a measure of the amount of energy emitted to space by earth's surface, oceans and atmosphere. As such, it is a critical component of the earth's radiation budget. In a different context, OLR values are often used as a proxy for convection in tropical and subtropical regions since cloud top temperatures (colder is higher) are an indicator of cloud height. OLR observations are made via the Advanced Very High Resolution Radiometer (AVHRR) instrument aboard the NOAA polar orbiting spacecraft. The raw ascending and descending swath data have been spatially and temporarally interpolated onto grids to facilitate use. OLR estimates are a key component for the standard Madden-Julian Oscillation (MJO) CLIVAR diagnostics which are used to study the MJO and for climate model evaluation.

1974-06/2013-12