English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

We present a case study of tropospheric aerosol transport in the eastern Mediterranean, based on airbornemeasurements obtained south of Greece on 7 June 1997. Airborne observations (backscattering lidar at0.532 mm with polarization measurements, in situ particlecounters/sizers, and standard meteorological measurements) are complemented by monitoring with Meteosat visible and infrared images and a ground-basedsun-photometer, air-mass back-trajectory computations, and meteorological analyses. As already observed fromground-based lidars in the Mediterranean region, the vertical structure of the lower troposphere appears complex,with a superposition of several turbid layers from the surface up to the clean free troposphere which is foundhere above 2 to 4 km in altitude. The aircraft observations also reveal an important horizontal variability. Weidentify the presence of depolarising dust from northern Africa in the most elevated turbid layer, which isrelatively humid and has clouds embedded. The lowermost troposphere likely contains pollution water-solubleaerosols from eastern continental Greece, and an intermediate layer is found with a probable mixture of the twotypes of particles. The column optical depth at 0.55 mm estimated from Meteosat is in the range0.15-0.35. It is used to constrain the aerosol backscattering-to-extinction ratio needed for the backscattering lidar data inversion.The column value of 0.017 sr -1 is found applicable to the various aerosol layers and allows us to derive theaerosol extinction vertical profile. The aerosol extinction coefficient ranges from0.03 km-1 in the lower clean free troposphere to more than 0.25km-1 in the marine boundary layer. Values are <0.1 km-1 in the elevated dustlayer but its thickness makes it dominate the aerosol optical depth at some places

atmospheric chemistry and physics

Airborne study of a multi-layer aerosol structure in the eastern Mediterranean observed with the airborne polarized lidar ALEX during a STAAARTE campaign (7 June 1997)