Spatial and temporal variability in aerosol properties over the Mediterranean basin based on 6-year (2000-2006) MODIS data
dc.contributor.author | Papadimas, C. D. | en |
dc.contributor.author | Hatzianastassiou, N. | en |
dc.contributor.author | Mihalopoulos, N. | en |
dc.contributor.author | Querol, X. | en |
dc.contributor.author | Vardavas, I. | en |
dc.date.accessioned | 2015-11-24T18:35:10Z | |
dc.date.available | 2015-11-24T18:35:10Z | |
dc.identifier.issn | 0148-0227 | - |
dc.identifier.uri | https://olympias.lib.uoi.gr/jspui/handle/123456789/17056 | |
dc.rights | Default Licence | - |
dc.subject | north-atlantic oscillation | en |
dc.subject | resolution imaging spectroradiometer | en |
dc.subject | optical depth | en |
dc.subject | tropospheric aerosols | en |
dc.subject | climate | en |
dc.subject | aeronet | en |
dc.subject | sea | en |
dc.subject | thickness | en |
dc.subject | transport | en |
dc.subject | cloud | en |
dc.title | Spatial and temporal variability in aerosol properties over the Mediterranean basin based on 6-year (2000-2006) MODIS data | en |
heal.abstract | The temporal variability of aerosol optical properties is investigated over the broader Mediterranean basin, with emphasis on aerosol optical depth ( AOD) that is an effective measure of aerosol load. The study is performed using Collection 005 Level-3 mean daily spectral aerosol data from the Moderate Resolution Imaging Spectroradiometer ( MODIS) instrument on board the Terra and Aqua satellites, which cover the 6-year period from 2000 to 2006. The results of our analysis reveal a significant interannual variability of AOD in the study region. Specifically, the regional mean visible AOD over land and ocean has decreased over the period 2000-2006 by 20% in relative percentage terms ( or by 0.04 in absolute terms). This tendency is statistically significant according to the Man-Kendall test. However, the decreasing tendency of AOD is not uniform over the whole basin. It appears mainly in the western parts of Iberian, Italian, and Balkan peninsulas ( and coastal areas), as well as in the southern Anatolian peninsula. The analysis for summer ( June to September) and winter ( November to March) seasons revealed different tendencies in both AOD and precipitation. The summer-period AOD has decreased by 0.04 ( or by 14%) probably due to decreased emission rates of anthropogenic pollution. In contrast, the winter AOD has increased by 0.03 ( or 19%) mainly related to decreased precipitation ( associated with an increasing tendency in the NAO index). The decreasing tendency in MODIS AOD is in good agreement with corresponding AOD tendencies based on data from Aerobot Robotic Network ( AERONET) stations in the study region and ground based PM10 measurements at selected stations. | en |
heal.access | campus | - |
heal.fullTextAvailability | TRUE | - |
heal.identifier.primary | Doi 10.1029/2007jd009189 | - |
heal.identifier.secondary | <Go to ISI>://000256561000002 | - |
heal.identifier.secondary | http://www.agu.org/journals/jd/jd0811/2007JD009189/2007JD009189.pdf | - |
heal.journalName | Journal of Geophysical Research-Atmospheres | en |
heal.journalType | peer reviewed | - |
heal.language | en | - |
heal.publicationDate | 2008 | - |
heal.recordProvider | Πανεπιστήμιο Ιωαννίνων. Σχολή Επιστημών και Τεχνολογιών. Τμήμα Βιολογικών Εφαρμογών και Τεχνολογιών | el |
heal.type | journalArticle | - |
heal.type.el | Άρθρο Περιοδικού | el |
heal.type.en | Journal article | en |
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