Spatio-temporal variability of dust aerosols over the Sistan region in Iran based on satellite observations

dc.contributor.authorRashki, Alireza
dc.contributor.authorKaskaoutis, Dimitris G.
dc.contributor.authorEriksson, Patrick George
dc.contributor.authorRautenbach, Cornelis Johannes de Wet
dc.contributor.authorFlamant, C.
dc.contributor.authorAbdi Vishkaee, F.
dc.contributor.emailalireza.rashki@up.ac.zaen_ZA
dc.date.accessioned2015-11-13T07:15:32Z
dc.date.available2015-11-13T07:15:32Z
dc.date.issued2014-03
dc.description.abstractSatellite remote sensing provides important observational constraints for monitoring dust life cycle and improving the understanding of its effects on local to global scales. The present work analyses the dust-aerosol patterns over the arid environment of the Sistan region-in southeastern Iran, by means of multiple satellite platforms aiming to reveal the spatiotemporal distribution and trends. The dataset includes records of Aerosol Index (AI) from Total Ozone Mapping Spectrometer (TOMS) (1978–2001) and 6-year AI records from the Ozone Monitoring Instrument (OMI) aboard Aura. Moreover, the aerosol optical depth (AOD) is analyzed through 11-year records from Multi-angle Imaging Spectro-Radiometer (MISR) aboard Terra (2000-2010) and from Moderate Resolution Imaging Spectroradiometer (MODIS) onboard Terra (2000-2007) and Aqua (2002-2011). The main focus is to determine similarities and differences in dust variability over southwest Asia, in general, and the Sistan region, in particular. The results show a marked seasonal cycle with high aerosol loading during summer and lower in winter, while MISR, MODIS and TOMS/OMI observations agree in both terms of monthly and seasonally mean spatial and temporal patterns. The higher aerosol concentrations during summer are interpreted as a result of the combined effect of the seasonal drying of the Hamoun lakes and the strong northerly Levar winds favoring dust erosion from the alluvial deposits in Sistan . After prolonged drought period, the dust-aerosol load over the area has increased in the beginning of the 2000s and decreased after 2004, thereby leading to an overall declining trend during the last decade. Such a trend is absent during the winter period when dust emission over the region is minimal.en_ZA
dc.description.librarianhb2015en_ZA
dc.description.urihttp://link.springer.com/journal/11069en_ZA
dc.identifier.citationRashki, A, Kaskaoutis, DG, Eriksson, PG, Rautenbach, CJdeW, Flamant, C & Abdi Vishkaee, F 2014, 'Spatio-temporal variability of dust aerosols over the Sistan region in Iran based on satellite observations', Natural Hazards, vol. 71, no. 1, pp. 563-585.en_ZA
dc.identifier.issn0921-030X (print)
dc.identifier.other573-0840 (online)
dc.identifier.other10.1007/s11069-013-0927-0
dc.identifier.urihttp://hdl.handle.net/2263/50451
dc.language.isoenen_ZA
dc.publisherSpringeren_ZA
dc.rights© Springer Science+Business Media Dordrecht 2013. The original publication is available at : http://link.springer.comjournal/11069.en_ZA
dc.subjectAerosol variabilityen_ZA
dc.subjectRemote sensingen_ZA
dc.subjectDusten_ZA
dc.subjectSistanen_ZA
dc.subjectHamoun lakesen_ZA
dc.subjectTotal ozone mapping spectrometer (TOMS)en_ZA
dc.subjectAerosol optical depth (AOD)en_ZA
dc.subjectModerate resolution imaging spectroradiometer (MODIS)en_ZA
dc.subjectOzone monitoring instrument (OMI)en_ZA
dc.titleSpatio-temporal variability of dust aerosols over the Sistan region in Iran based on satellite observationsen_ZA
dc.typePostprint Articleen_ZA

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