Aerosol optical properties as observed from an ultralight aircraft over the Strait of Gibraltar
<p>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 Ray...
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2020-08-01
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| Series: | Atmospheric Measurement Techniques |
| Online Access: | https://amt.copernicus.org/articles/13/4461/2020/amt-13-4461-2020.pdf |
| Summary: | <p>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 <span class="inline-formula">N<sub>2</sub></span>-Raman lidar from the coastal site of San Pedro Alcantara
(<span class="inline-formula">∼</span> 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) <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>∼</mo><mn mathvariant="normal">45</mn><mo>±</mo><mn mathvariant="normal">8</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="42pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="8422c334c77fa4944838b288fe381775"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-13-4461-2020-ie00001.svg" width="42pt" height="10pt" src="amt-13-4461-2020-ie00001.png"/></svg:svg></span></span> sr
higher than those of Saharan aerosols sampled during the same period
(<span class="inline-formula"><34</span> sr) at 355 nm. Furthermore, the particle depolarization ratio
is derived with values of <span class="inline-formula">∼</span> 10 %–15 % for the polluted dust
and <span class="inline-formula">>20</span> % 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.</p> |
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| ISSN: | 1867-1381 1867-8548 |