Dataset Open Access

FLEPXART backward dispersion simulations

Henne, Stephan


MARC21 XML Export

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    <subfield code="a">&lt;p&gt;The dataset contains results of the Lagrangian Particle Dispersion Model FLEXPART as used in Schoenenberger et al. (2017).&lt;/p&gt;

&lt;p&gt;FLEXPART was run in backward, receptor-oriented mode for 4 sites: Jungfraujoch, Monte Cimone, Mace Head, Finokalia.&lt;br&gt;
FLEXPART was driven by ECMWF IFS windfields with a global resolution of 1&amp;deg; x 1&amp;deg; and 0.2&amp;deg; x 0.2&amp;deg; for the Alpine area. 50,000 particles are released every 3 hours and followed backward in time for 10 days.&lt;/p&gt;

&lt;p&gt;&lt;strong&gt;Data format&lt;/strong&gt;&lt;/p&gt;

&lt;p&gt;Each sub-folder for each site contains individual footprint files for the main and nested output domain of FLEXPART. Individual files are provided for every 3 hour interval and follow a custom binary format.&lt;br&gt;
Binary representation of total surface footprint.&lt;br&gt;
The binary files are written with R on linux and contain no stop bytes. For reading them with FORTRAN you will need to use form=&amp;#39;unformatted&amp;#39; and access=&amp;#39;direct&amp;#39;.&lt;br&gt;
The files have the following structure:&lt;br&gt;
Longitude range of grid (2 element 4 byte real)&lt;br&gt;
Latitude range of grid (2 element 4 byte real)&lt;br&gt;
Number of grid in longitude direction, nx (1 element 4 byte integer)&lt;br&gt;
Number of grid in latitude direction, ny (1 element 4 byte integer)&lt;br&gt;
Year, Month, Day, Hour, Minute of latest realease (5 element 4 byte integer)&lt;br&gt;
Level top of surface layer in metres (1 element 4 byte real)&lt;br&gt;
Residence times (nx x ny element 4 byte real; elements are written along longitudes first, from the largest to the smallest latitude)&lt;/p&gt;

&lt;p&gt;&amp;nbsp;&lt;/p&gt;

&lt;p&gt;Schoenenberger, F., S. Henne, M. Hill, M. K. Vollmer, G. Kouvarakis, N. Mihalopoulos, S. O&amp;#39;Doherty, M. Maione, L. Emmenegger, T. Peter, and S. Reimann&amp;nbsp; (2017), Abundance and Sources of Atmospheric Halocarbons in the Eastern Mediterranean, Atmos. Chem. Phys. Discuss., 2017, 1-46, doi: 10.5194/acp-2017-451.&lt;/p&gt;</subfield>
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