Journal cover Journal topic
Geoscientific Model Development An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

IF value: 5.240
IF5.240
IF 5-year value: 5.768
IF 5-year
5.768
CiteScore value: 8.9
CiteScore
8.9
SNIP value: 1.713
SNIP1.713
IPP value: 5.53
IPP5.53
SJR value: 3.18
SJR3.18
Scimago H <br class='widget-line-break'>index value: 71
Scimago H
index
71
h5-index value: 51
h5-index51
Volume 10, issue 12
Geosci. Model Dev., 10, 4605–4618, 2017
https://doi.org/10.5194/gmd-10-4605-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: The Lagrangian particle dispersion model FLEXPART

Geosci. Model Dev., 10, 4605–4618, 2017
https://doi.org/10.5194/gmd-10-4605-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Development and technical paper 18 Dec 2017

Development and technical paper | 18 Dec 2017

Source–receptor matrix calculation for deposited mass with the Lagrangian particle dispersion model FLEXPART v10.2 in backward mode

Sabine Eckhardt et al.

Viewed

Total article views: 1,851 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,136 655 60 1,851 251 94 93
  • HTML: 1,136
  • PDF: 655
  • XML: 60
  • Total: 1,851
  • Supplement: 251
  • BibTeX: 94
  • EndNote: 93
Views and downloads (calculated since 30 Jun 2017)
Cumulative views and downloads (calculated since 30 Jun 2017)

Viewed (geographical distribution)

Total article views: 1,728 (including HTML, PDF, and XML) Thereof 1,718 with geography defined and 10 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

No saved metrics found.

Saved (preprint)

No saved metrics found.

Discussed (final revised paper)

No discussed metrics found.

Discussed (preprint)

No discussed metrics found.
Latest update: 22 Sep 2020
Publications Copernicus
Download
Short summary
We extend the backward modelling technique in the existing model FLEXPART to substances deposited at the Earth’s surface by wet scavenging and dry deposition. This means that for existing measurements of a substance in snow, ice cores or rain samples the source regions can be determined. This will help the interpretation of the measurement as well as gaining information of emission strength at the source of the deposited substance.
We extend the backward modelling technique in the existing model FLEXPART to substances...
Citation