Spatial and temporal characteristics of Outgoing Longwave Radiation (OLR): an update

A study of the Outgoing longwave radiation (OLR) values (Unit, W/m) observed by various satellites during 1979-2002 revealed that the OLR values varied considerably from one geographical region to another ( ~ 100-300 units). The climatology was latitude dependent. At middle and high latitudes, the range (minimum to maximum) was ~ 40-60 units, with maximum in local summer and minimum in local winter, but at lower latitudes, the range reduced considerably and was uncertain near equator. Near equator, the long-term changes (as seen in 12-month moving averages) were: OLR decreases during ENSO events in the eastern Pacific up to the dateline, and OLR increases during ENSO events in the Australasian region. Outside the equatorial region, the OLR changes were small during ENSO events and negligible in other years. In some longitudes at middle and high latitudes, the OLR changes occurred several months after the El Niño events, coinciding with La Niña (cold water events, opposite of warm water El Niño events).

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Main Author: Kane,Rajaram Purushottam
Format: Digital revista
Language:English
Published: Sociedade Brasileira de Geofísica 2008
Online Access:http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0102-261X2008000200009
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spelling oai:scielo:S0102-261X20080002000092008-09-22Spatial and temporal characteristics of Outgoing Longwave Radiation (OLR): an updateKane,Rajaram Purushottam spectra OLR (Outgoing Longwave Radiation) A study of the Outgoing longwave radiation (OLR) values (Unit, W/m) observed by various satellites during 1979-2002 revealed that the OLR values varied considerably from one geographical region to another ( ~ 100-300 units). The climatology was latitude dependent. At middle and high latitudes, the range (minimum to maximum) was ~ 40-60 units, with maximum in local summer and minimum in local winter, but at lower latitudes, the range reduced considerably and was uncertain near equator. Near equator, the long-term changes (as seen in 12-month moving averages) were: OLR decreases during ENSO events in the eastern Pacific up to the dateline, and OLR increases during ENSO events in the Australasian region. Outside the equatorial region, the OLR changes were small during ENSO events and negligible in other years. In some longitudes at middle and high latitudes, the OLR changes occurred several months after the El Niño events, coinciding with La Niña (cold water events, opposite of warm water El Niño events).info:eu-repo/semantics/openAccessSociedade Brasileira de GeofísicaRevista Brasileira de Geofísica v.26 n.2 20082008-06-01info:eu-repo/semantics/articletext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0102-261X2008000200009en10.1590/S0102-261X2008000200009
institution SCIELO
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country Brasil
countrycode BR
component Revista
access En linea
databasecode rev-scielo-br
tag revista
region America del Sur
libraryname SciELO
language English
format Digital
author Kane,Rajaram Purushottam
spellingShingle Kane,Rajaram Purushottam
Spatial and temporal characteristics of Outgoing Longwave Radiation (OLR): an update
author_facet Kane,Rajaram Purushottam
author_sort Kane,Rajaram Purushottam
title Spatial and temporal characteristics of Outgoing Longwave Radiation (OLR): an update
title_short Spatial and temporal characteristics of Outgoing Longwave Radiation (OLR): an update
title_full Spatial and temporal characteristics of Outgoing Longwave Radiation (OLR): an update
title_fullStr Spatial and temporal characteristics of Outgoing Longwave Radiation (OLR): an update
title_full_unstemmed Spatial and temporal characteristics of Outgoing Longwave Radiation (OLR): an update
title_sort spatial and temporal characteristics of outgoing longwave radiation (olr): an update
description A study of the Outgoing longwave radiation (OLR) values (Unit, W/m) observed by various satellites during 1979-2002 revealed that the OLR values varied considerably from one geographical region to another ( ~ 100-300 units). The climatology was latitude dependent. At middle and high latitudes, the range (minimum to maximum) was ~ 40-60 units, with maximum in local summer and minimum in local winter, but at lower latitudes, the range reduced considerably and was uncertain near equator. Near equator, the long-term changes (as seen in 12-month moving averages) were: OLR decreases during ENSO events in the eastern Pacific up to the dateline, and OLR increases during ENSO events in the Australasian region. Outside the equatorial region, the OLR changes were small during ENSO events and negligible in other years. In some longitudes at middle and high latitudes, the OLR changes occurred several months after the El Niño events, coinciding with La Niña (cold water events, opposite of warm water El Niño events).
publisher Sociedade Brasileira de Geofísica
publishDate 2008
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0102-261X2008000200009
work_keys_str_mv AT kanerajarampurushottam spatialandtemporalcharacteristicsofoutgoinglongwaveradiationolranupdate
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