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  The vertical distribution of aerosol over Europe - synthesis of one year of EARLINET aerosol lidar measurements and aerosol transport modeling with LMDzT-INCA

Guibert, S., Matthias, V., Schulz, M., Boesenberg, J., Eixmann, R., Mattis, I., et al. (2005). The vertical distribution of aerosol over Europe - synthesis of one year of EARLINET aerosol lidar measurements and aerosol transport modeling with LMDzT-INCA. Atmospheric Environment, 39(16), 2933-2943.

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AtmosEnv_39-2933.pdf (Publisher version), 2MB
 
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 Creators:
Guibert, S., Author
Matthias, Volker1, Author           
Schulz, M., Author
Boesenberg, Jens2, Author           
Eixmann, R., Author
Mattis, I., Author
Pappalardo, G., Author
Perroneg, M. R., Author
Spinelli, N., Author
Vaughan, G., Author
Affiliations:
1Climate Processes, MPI for Meteorology, Max Planck Society, ou_913551              
2The Land in the Earth System, MPI for Meteorology, Max Planck Society, ou_913551              

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Free keywords: aerosol extinction; vertical profiles; aerosol composition; Saharan dust; GCM
 Abstract: Aerosol extinction vertical profiles measured with Raman lidar in the framework of EARLINET in 2000 are compared to profiles modeled by a general circulation model, LMDzT-INCA, at seven stations in Europe. Comparisons based on individual profiles show moderate correlation between model and data. Averaging aerosol extinction values on larger temporal or spatial scales improves the comparison. Furthermore, we show that the model succeeds to reproduce the mean annual aerosol distribution over Europe. Comparisons of the aerosol vertical distribution in two distinct regions of Europe are presented. For the northern stations, the observed yearly average aerosol extinction coefficient vertical profile and the modeled one show an average bias of 22%. For the southern stations the mean bias is slightlyhigher (29%). Both model and lidar show different extinction profiles in different parts of Europe, with higher values in upper heights in the South. According to modeled profiles of each aerosol component, this is caused bythe presence of dust at altitudes between 2 and 6 km. In addition vertical mixing in the South seems to be more effective for the other aerosol components

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Language(s): eng - English
 Dates: 2005-05
 Publication Status: Issued
 Pages: -
 Publishing info: -
 Table of Contents: -
 Rev. Type: Peer
 Identifiers: eDoc: 256484
ISI: 000230184500010
 Degree: -

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Title: Atmospheric Environment
  Alternative Title : Atmos. Environ.
Source Genre: Journal
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Pages: - Volume / Issue: 39 (16) Sequence Number: - Start / End Page: 2933 - 2943 Identifier: ISSN: 1352-2310