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dc.contributor.authorOsborne, S.R.
dc.contributor.authorBaran, A.J.
dc.contributor.authorJohnson, B.T.
dc.contributor.authorHaywood, J.M.
dc.contributor.authorHesse, Evelyn
dc.contributor.authorNewman, S.
dc.date.accessioned2011-09-06T14:01:02Z
dc.date.available2011-09-06T14:01:02Z
dc.date.issued2011
dc.identifier.citationOsborne , S R , Baran , A J , Johnson , B T , Haywood , J M , Hesse , E & Newman , S 2011 , ' Short-wave and long-wave radiative properties of Saharan dust aerosol ' , Quarterly Journal of the Royal Meteorological Society , vol. 137 , no. 658 , pp. 1149-1167 . https://doi.org/10.1002/qj.771
dc.identifier.issn0035-9009
dc.identifier.otherORCID: /0000-0002-2721-7600/work/62749827
dc.identifier.urihttp://hdl.handle.net/2299/6375
dc.descriptionThe definitive version can be found at: http://onlinelibrary.wiley.com/ Copyright Royal Meteorological Society
dc.description.abstractThe radiative properties of mineral dust aerosol during the GERB Intercomparison of Long-wave and Short-wave (GERBILS) are presented. GERBILS consisted of aircraft flights over land areas between Mauritania and Niger during June 2007. During one case of large aerosol optical depth (AOD=1.0 at 0.55μm), a short-wave spectrometer measured sky radiances versus scattering angle that are compared to modelled data. The modelling used phase functions of spheres, spheroids and irregular-shaped particles using T-matrix and ray-tracing methods. Irregular particles provided the most satisfactory solution. In another case of full short-wave and long-wave radiative closure, measurements and modelled clear sky conditions allowed calculation of the direct radiative effect (DRE) at high and low level. The modelled AOD (0.92) required to simulate the measured spectral irradiances agrees with the aircraft AOD (0.79) within measurement uncertainty. The simulated irradiances are less sensitive to particle shape than radiances. However, it is shown through modelling of the surface and top-of-atmosphere (TOA) DRE over all daylight hours that significant differences exist at TOA due to variation in the asymmetry parameter. The TOA short-wave diurnally averaged DRE was modelled as between 0 and -20 W m-2 depending on particle shape. A long-wave interferometer measured downwelling and upwelling radiances to derive surface emissivity across the window region. Measured nadir brightness temperatures from high level show signature of dust. A drop in brightness temperature of 14K was determined using modelled pristine-sky spectra. The modelled outgoing long-wave DRE due to dust from this case was +14 W m-2 averaged over 24 h, or +17 W m-2 per unit AOD. Modelling studies illustrate the sensitivity to aerosol refractive index and size distribution for both short-wave and long-wave DREs. Considering the full spectrum, a refractive index dataset from the literature has been selected that best represents the Saharan dust encountered during GERBILS. the Met Office.en
dc.format.extent1057883
dc.language.isoeng
dc.relation.ispartofQuarterly Journal of the Royal Meteorological Society
dc.subjectaircraft measurements
dc.subjectbrightness temperature
dc.subjectdirect radiative effect
dc.subjectnon-spherical particles
dc.subjectphase function
dc.subjectsky radiance
dc.titleShort-wave and long-wave radiative properties of Saharan dust aerosolen
dc.contributor.institutionCentre for Atmospheric and Climate Physics Research
dc.contributor.institutionLight Scattering and Radiative Processes
dc.contributor.institutionSchool of Physics, Engineering & Computer Science
dc.contributor.institutionDepartment of Physics, Astronomy and Mathematics
dc.description.statusPeer reviewed
dc.date.embargoedUntil2014-03-07
rioxxterms.versionofrecord10.1002/qj.771
rioxxterms.typeJournal Article/Review
herts.preservation.rarelyaccessedtrue


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