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dc.contributor.authorHaywood, J.M.
dc.contributor.authorAllan, R.P.
dc.contributor.authorCulverwell, I.
dc.contributor.authorSlingo, T.
dc.contributor.authorMilton, S.
dc.contributor.authorEdwards, J.
dc.contributor.authorClerbaux, N.
dc.coverage.temporal21st century
dc.descriptionMeasurements of the top-of-the-atmosphere outgoing longwave radiation (OLR) for July 2003 from Meteosat-7 are used to assess the performance of the numerical weather prediction version of the Met Office Unified Model. A significant difference is found over desert regions of northern Africa where the model emits too much OLR by up to 35 Wm−2 in the monthly mean. By cloud-screening the data we find an error of up to 50 Wm−2 associated with cloud-free areas, which suggests an error in the model surface temperature, surface emissivity, or atmospheric transmission. By building up a physical model of the radiative properties of mineral dust based on in situ, and surface-based and satellite remote sensing observations we show that the most plausible explanation for the discrepancy in OLR is due to the neglect of mineral dust in the model. The calculations suggest that mineral dust can exert a longwave radiative forcing by as much as 50 Wm−2 in the monthly mean for 1200 UTC in cloud-free regions, which accounts for the discrepancy between the model and the Meteosat-7 observations. This suggests that inclusion of the radiative effects of mineral dust will lead to a significant improvement in the radiation balance of numerical weather prediction models with subsequent improvements in performance.
dc.relation.ispartofseriesJournal of geophysical research, Vol. 110
dc.titleCan desert dust explain the outgoing longwave radiation anomaly over the Sahara during July 2003?
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceGeneral Public
dc.subject.freemineral dust
dc.subject.freeradiative effect
dc.subject.freeradiation budget
dc.source.issueJournal of geophysical research, Vol. 110
dc.source.pagepp. 1-14
Orfeo.peerreviewedNot pertinent

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