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dc.contributor.authorDewitte, S.
dc.contributor.authorCrommelynck,D.
dc.contributor.authorMekaoui, S.
dc.contributor.authorJoukoff, A.
dc.coverage.temporal21st century
dc.date2004
dc.date.accessioned2016-03-07T16:16:49Z
dc.date.accessioned2021-12-09T09:53:31Z
dc.date.available2016-03-07T16:16:49Z
dc.date.available2021-12-09T09:53:31Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/8679
dc.descriptionA possible long-term trend of the total solar irradiance could be a natural cause for climate variations on Earth. Measurement of the total solar irradiance with space radiometers started in 1978. We present a new total solar irradiance composite, with an uncertainty of ± 0.35 W m−2. From the minimum in 1995 to the maximum in 2002 the total solar irradiance increased by 1.6 W m−2. In between the minima of 1987 and 1995 the total solar irradiance increased by 0.15 W m−2.
dc.languageeng
dc.publisherIRM
dc.publisherKMI
dc.publisherRMI
dc.relation.ispartofseriesSol Phys, Vol 224
dc.title"Measurement and uncertainty of the long term total solar irradiance trend"
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceGeneral Public
dc.audienceScientific
dc.subject.freesolar irradiance
dc.subject.freeClimate variations
dc.subject.free1987
dc.subject.free1995
dc.subject.free2002
dc.source.issueSol Phys, Vol 224
dc.source.pagepp. 209-216
Orfeo.peerreviewedNot pertinent


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