Open AccessMulti‐instrumental observation of an exceptionally strong Saharan dust outbreak over Portugal
Author(s) -
Preißler J.,
Wagner F.,
Pereira S. N.,
GuerreroRascado J. L.
Publication year - 2011
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2011jd016527
Subject(s) - lidar , depolarization ratio , raman spectroscopy , angstrom exponent , mineral dust , aerosol , sun photometer , atmospheric sciences , environmental science , asian dust , materials science , physics , meteorology , optics
An exceptionally strong outbreak of Saharan dust was observed in southern Portugal from 4 to 9 April 2011. The event was monitored with a multiwavelength Raman lidar, a CIMEL Sun photometer, the Cloud Aerosol Lidar with Orthogonal Polarization (CALIOP) and two Moderate Resolution Imaging Spectroradiometer (MODIS). Those instruments provided vertically resolved and columnar information about the optical properties of the mineral dust plume. Maximum aerosol optical depths in the free troposphere of 1.8 and 1.9 were observed with Raman lidar at 355 and 532 nm, respectively. The mean extinction‐related Ångström exponents (355, 532 nm) from Raman lidar averaged over the whole period were 0.0 ± 0.2. Backscatter‐related Ångström exponents (355, 532 nm and 532, 1064 nm) were 0.4 on average. Mean lidar ratios calculated from Raman lidar measurements were 45 ± 8 sr at 355 nm and 53 ± 7 sr at 532 nm. The mean linear particle depolarization ratio at 532 nm was 0.28 ± 0.04. Furthermore, intrusion of Saharan dust into the planetary boundary layer could be observed with different ground‐based in‐situ instruments. Maximum particle mass concentration values (PM 10 ) of 162 μ g m −3 were detected at ground. The daily threshold of 50 μ g m −3 for PM 10 was exceeded on three subsequent days during the considered period. The ratio of coarse to fine mode particle number concentration reached maximum values larger than 1, coinciding with the maximum in PM 10 mass concentration. A comparison of ground‐based Raman lidar measurements and CALIOP Level 2 data was done for one CALIPSO overpass. A good agreement was found for backscatter coefficients.