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  Forecasting the North African dust outbreak towards Europe in April 2011: a model intercomparison

Huneeus, N., Basart, S., Fiedler, S., Morcrette, J.-J., Benedetti, A., Mulcahy, J., et al. (2016). Forecasting the North African dust outbreak towards Europe in April 2011: a model intercomparison. Atmospheric Chemistry and Physics, 16, 4967-4986. doi:10.5194/acp-16-4967-2016.

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Huneeus, N., Author
Basart, S., Author
Fiedler, Stephanie1, Author           
Morcrette, J.-J., Author
Benedetti, A., Author
Mulcahy, J., Author
Terradellas, E., Author
Perez Garcia-Pando, C., Author
Pejanovic, G., Author
Nickovic, S., Author
Arsenovic, P., Author
Schulz, M., Author
Cuevas, E., Author
Baldasano, J.M., Author
Pey, J., Author
Remy, S., Author
Cvetkovic, B., Author
Affiliations:
1Director’s Research Group AES, The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society, Bundesstraße 53, 20146 Hamburg, DE, ou_913570              

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 Abstract: In the framework of the World Meteorological Organisation's Sand and Dust Storm Warning Advisory and Assessment System, we evaluated the predictions of five state-of-the-art dust forecast models during an intense Saharan dust outbreak affecting Western and Northern Europe in April 2011. We assessed the capacity of the models to predict the evolution of the dust cloud with lead-times of up to 72 h using observations of aerosol optical depth (AOD) from the Aerosol Robotic Network (AERONET) and the Moderate Resolution Imaging Spectroradiometer (MODIS), and dust surface concentrations from a ground-based measurement network. In addition, the predicted vertical dust distribution was evaluated with vertical extinction profiles from the Cloud and Aerosol Lidar with Orthogonal Polarization (CALIOP). To assess the diversity in forecast capability among the models, the analysis was extended to wind field (both surface and profile), synoptic conditions, emissions and deposition fluxes. Models predict the onset and evolution of the AOD for all analysed lead-times. On average, differences among the models are larger than differences among lead-times for each individual model. In spite of large differences in emission and deposition, the models present comparable skill for AOD. In general, models are better in predicting AOD than near-surface dust concentration over the Iberian Peninsula. Models tend to underestimate the long-range transport towards Northern Europe. Our analysis suggests that this is partly due to difficulties in simulating the vertical distribution dust and horizontal wind. Differences in the size distribution and wet scavenging efficiency may also account for model diversity in long-range transport.

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Language(s): eng - English
 Dates: 2015-122015-102016-042016-04-21
 Publication Status: Issued
 Pages: -
 Publishing info: -
 Table of Contents: The work
was partly funded within MACC-II by the European Commission
under the EU Seventh Research Framework Programme,
contract number 283576 and MACC-III by the European Community’s
Horizon 2020 Programme under grant agreement no. 633080.
 Rev. Type: Peer
 Identifiers: DOI: 10.5194/acp-16-4967-2016
 Degree: -

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Project name : MACC-II MAC-III - Horizon 2020 - 633080
Grant ID : 283576
Funding program : Funding Programme 7 (FP7)
Funding organization : European Commission (EC)

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Title: Atmospheric Chemistry and Physics
Source Genre: Journal
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Publ. Info: Katlenburg-Lindau, Germany : European Geosciences Union
Pages: - Volume / Issue: 16 Sequence Number: - Start / End Page: 4967 - 4986 Identifier: ISSN: 1680-7316
CoNE: https://pure.mpg.de/cone/journals/resource/111030403014016