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Mariana Adam

Researcher at Met Office

Publications -  44
Citations -  604

Mariana Adam is an academic researcher from Met Office. The author has contributed to research in topics: Lidar & Water vapor. The author has an hindex of 12, co-authored 40 publications receiving 537 citations. Previous affiliations of Mariana Adam include Aberystwyth University & Howard University.

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Four-dimensional distribution of the 2010 Eyjafjallajökull volcanic cloud over Europe observed by EARLINET

Gelsomina Pappalardo, +62 more
TL;DR: In this article, the authors show the four-dimensional (4-D) distribution of the Eyjafjallajokull volcanic cloud in the troposphere over Europe as observed by EARLINET during the entire volcanic event (15 April-26 May 2010).
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EARLINET instrument intercomparison campaigns: overview on strategy and results

Ulla Wandinger, +62 more
TL;DR: In this paper, the European Aerosol Research Lidar Network (EARLINET) quality-assurance efforts at instrument level have been discussed at signal and product level.
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Airborne and Ground-Based Measurements Using a High-Performance Raman Lidar

TL;DR: The same RASL hardware as described in part I was installed in a ground-based mobile trailer and used in a water vapor lidar intercomparison campaign, hosted at Table Mountain, CA, under the auspices of the Network for the Detection of Atmospheric Composition Change (NDACC) as mentioned in this paper.
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Aerosol hygroscopicity at a regional background site (Ispra) in Northern Italy

TL;DR: In this paper, the Mie theory was used to calculate the mean monthly diurnal values of the aerosol hygroscopic growth factor at 90% relative humidity GF(90) based on measurements performed at the atmospheric research station in Ispra (Italy) with a Hygroscopicity Tandem Differential Mobility Analyzer over eight months in 2008 and 2009.
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Comparison of Tropospheric Emission Spectrometer nadir water vapor retrievals with in situ measurements

TL;DR: In this paper, a comparison of Tropospheric Emission Spectrometer (TES) water vapor retrievals with in situ measurements is presented, showing that TES reported water vapor comparison statistics are not weighted by the water vapor layer amounts, and that the estimated systematic errors from the forward model, TES measurements, in situ observations, retrieved temperature profiles, and clouds are likely not large enough to account for radiance differences between TES observations and forward model calculations using in situ profiles as input.