Journal cover Journal topic
Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

IF value: 5.153
IF5.153
IF 5-year value: 5.460
IF 5-year
5.460
CiteScore value: 7.8
CiteScore
7.8
SNIP value: 1.623
SNIP1.623
IPP value: 4.91
IPP4.91
SJR value: 2.092
SJR2.092
Scimago H <br class='widget-line-break'>index value: 123
Scimago H
index
123
h5-index value: 65
h5-index65
Volume 21, issue 1
Hydrol. Earth Syst. Sci., 21, 533–548, 2017
https://doi.org/10.5194/hess-21-533-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 21, 533–548, 2017
https://doi.org/10.5194/hess-21-533-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 27 Jan 2017

Research article | 27 Jan 2017

Response of water vapour D-excess to land–atmosphere interactions in a semi-arid environment

Stephen D. Parkes et al.

Viewed

Total article views: 1,623 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
996 562 65 1,623 168 53 77
  • HTML: 996
  • PDF: 562
  • XML: 65
  • Total: 1,623
  • Supplement: 168
  • BibTeX: 53
  • EndNote: 77
Views and downloads (calculated since 30 Jun 2016)
Cumulative views and downloads (calculated since 30 Jun 2016)

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: 24 Oct 2020
Publications Copernicus
Download
Short summary
Determining atmospheric moisture sources is required for understanding the water cycle. The role of land surface fluxes is a particular source of uncertainty for moisture budgets. Water vapour isotopes have the potential to improve constraints on moisture sources. In this work relationships between water vapour isotopes and land–atmosphere exchange are studied. Results show that land surface evaporative fluxes play a minor role in the daytime water and isotope budgets in semi-arid environments.
Determining atmospheric moisture sources is required for understanding the water cycle. The role...
Citation