Title :

Aerosol measurements with a shipborne sun-sky-lunar photometer and collocated multiwavelength raman polarization lidar over the atlantic ocean

Author(s) :

Yin, Zhenping [Auteur]
Ansmann, Albert [Auteur]
Leibniz-Institut für Troposphärenforschung [TROPOS]
Baars, Holger [Auteur]
Leibniz Institute for Tropospheric Research [TROPOS]
Seifert, Patric [Auteur]
Leibniz Institute for Tropospheric Research [TROPOS]
Engelmann, Ronny [Auteur]
Leibniz Institute for Tropospheric Research [TROPOS]
Radenz, Martin [Auteur]
Jimenez, Cristofer [Auteur]
Herzog, Alina [Auteur]
Ohneiser, Kevin [Auteur]
Hanbuch, Karsten [Auteur]
Blarel, Luc [Auteur]
Laboratoire d’Optique Atmosphérique - UMR 8518 [LOA]
Goloub, Philippe [Auteur]
Laboratoire d'Optique Atmosphérique (LOA) - UMR 8518
Dubois, Gael [Auteur]
Laboratoire d'Optique Atmosphérique (LOA) - UMR 8518
Victori, Stephane [Auteur]
Maupin, Fabrice [Auteur]

Journal title :

Atmospheric Measurement Techniques

Abbreviated title :

Atmos. Meas. Tech.

Volume number :

12

Publication date :

2019-10-28

ISSN :

1867-1381

HAL domain(s) :

Physique [physics]

English abstract : [en]

A shipborne Sun–sky–lunar photometer of type CE318-T was tested during two trans-Atlantic cruises aboard the German research vessel Polarstern from 54∘ N to 54∘ S in May/June and December 2018. The continuous observations ...
Show more >A shipborne Sun–sky–lunar photometer of type CE318-T was tested during two trans-Atlantic cruises aboard the German research vessel Polarstern from 54∘ N to 54∘ S in May/June and December 2018. The continuous observations of the motion-stabilized shipborne CE318-T enabled the first-time observation of a full diurnal cycle of aerosol optical depth (AOD) and column-mean Ångström coefficient of a mixed dust–smoke episode. The latitudinal distribution of the AOD from the shipborne CE318-T, Raman lidar and MICROTOPS II shows the same trend with highest values in the dust belt from 0 to 20∘ N and overall low values in the Southern Hemisphere. The linear-regression coefficients of determination between MICROTOPS II and the CE318-T were 0.988, 0.987, 0.994 and 0.994 for AODs at 380, 440, 500 and 870 nm and 0.896 for the Ångström exponent at 440–870 nm. The root-mean-squared differences of AOD at 380, 440, 500 and 870 nm were 0.015, 0.013, 0.010 and 0.009, respectively.Show less >

Language :

Anglais

Peer reviewed article :

Oui

Audience :

Internationale

Popular science :

Non

Administrative institution(s) :

CNRS
Université de Lille

Collections :

• Laboratoire d'Optique Atmosphérique (LOA) - UMR 8518

Submission date :

2024-01-30T11:45:47Z
2024-02-26T14:12:45Z