Abstract

Abstract. An unprecedented scientific flight was conducted over the Strait of Gibraltar to study the optical properties of the atmospheric aerosols from the sea surface to the lower free troposphere within the framework of the southern Spain experiment for spaceborne mission validation (SUSIE). A Rayleigh–Mie lidar was installed on an ultralight aircraft (ULA) for vertical (nadir) and horizontal line-of-sight measurements. This experiment took place on 13 August 2011 in parallel with continuous observations with a N2-Raman lidar from the coastal site of San Pedro Alcantara (∼ 50 km north-east of Gibraltar). Significant differences were observed between the optical properties of the aerosol layers sampled over the Strait of Gibraltar and San Pedro Alcantara. These differences are related to the surface–atmosphere interface in the planetary boundary layer and the origins and transport processes in the lower free troposphere. A significant contribution of terrigenous aerosols originating from the Iberian Peninsula is highlighted over the two areas. These polluted dusts are identified with lidar ratios (LRs) ∼45±8 sr higher than those of Saharan aerosols sampled during the same period (<34 sr) at 355 nm. Furthermore, the particle depolarization ratio is derived with values of ∼ 10 %–15 % for the polluted dust and >20 % for the Saharan dusts. The difference in LRs is the opposite of what is usually assumed for these two types of aerosols and highlights the need to update the classification of aerosols in terms of LR to be used in the inversion of vertical profiles from future spaceborne missions embedding a lidar operating at 355 nm.

Highlights

  • Very little data exist on the aerosol characterization above the Strait of Gibraltar and its surrounding area where the Atlantic Ocean and the Mediterranean Sea meet

  • This can be explained by the passage of lows, which, together with the Azores high, favours the transport of desert aerosols through the Strait of Gibraltar towards the Iberian Peninsula and along an inverse path towards north-west Africa

  • The profiles were obtained from airborne lidar observations over Gibraltar and ground-based N2-Raman lidar measurements near Gibraltar at San Pedro Alcantara located ∼ 50 km east of Gibraltar

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Summary

Introduction

Very little data exist on the aerosol characterization above the Strait of Gibraltar and its surrounding area where the Atlantic Ocean and the Mediterranean Sea meet. In order to characterize the vertical distribution of aerosols over a long period, from mid-June to the end of August 2011, a ground-based remote sensing station was installed in southern Spain in the municipality of San Pedro Alcantara (36◦29 11 N, 4◦59 33 W) near Marbella in Andalusia This installation was one of the components of the Fennec programme which was conducted from June to July 2011 (Ryder et al, 2013) and was extended by the southern Spain experiment for spaceborne mission validation (SUSIE) to support an airborne experiment planned in August 2011 over the Strait of Gibraltar.

Payload
Flight plan
Ground-based tools
Data processing for lidar measurements
Airborne lidar
N2-Raman lidar
Cross-calibration
Vertical profiles of aerosol optical properties
Aerosol optical properties from the airborne lidar
Link with the ground-based lidar
Origin of aerosols observed over Gibraltar
Meteorological situation
Spaceborne observations
Air mass origins
Findings
Conclusion
Full Text
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