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Aerosol Direct Radiative Impact Experiment (ADRIEX) overview
Author(s) -
Highwood E. J.,
Haywood J. M.,
Coe H.,
Cook J.,
Osborne S.,
Williams P.,
Crosier J.,
Bower K.,
Formenti P.,
McQuaid J.,
Brooks B.,
Thomas G.,
Grainger R.,
Barnaba F.,
Gobbi G. P.,
de Leeuw G.,
Hopkins J.
Publication year - 2007
Publication title -
quarterly journal of the royal meteorological society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.744
H-Index - 143
eISSN - 1477-870X
pISSN - 0035-9009
DOI - 10.1002/qj.89
Subject(s) - aerosol , aeronet , environmental science , radiative transfer , radiative forcing , atmospheric sciences , black sea , optical depth , lidar , meteorology , satellite , climatology , remote sensing , geography , geology , oceanography , physics , quantum mechanics , astronomy
Abstract The Aerosol Direct Radiative Experiment (ADRIEX) took place over the Adriatic and Black Seas during August and September 2004 with the aim of characterizing anthropogenic aerosol in these regions in terms of its physical and optical properties and establishing its impact on radiative balance. Eight successful flights of the UK BAE‐146 Facility for Atmospheric Airborne Measurements were completed together with surface‐based lidar and AERONET measurements, in conjunction with satellite overpasses. This paper outlines the motivation for the campaign, the methodology and instruments used, describes the synoptic situation and provides an overview of the key results. ADRIEX successfully measured a range of aerosol conditions across the northern Adriatic, Po Valley and Black Sea. Generally two layers of aerosol were found in the vertical: in the flights over the Black Sea and the Po Valley these showed differences in chemical and microphysical properties, whilst over the Adriatic the layers were often more similar. Nitrate aerosol was found to be important in the Po Valley region. The use of new instruments to measure the aerosol chemistry and mixing state and to use this information in determining optical properties is demonstrated. These results are described in much more detail in the subsequent papers of this special issue. Copyright © 2007 Royal Meteorological Society