Articles | Volume 16, issue 18
https://doi.org/10.5194/acp-16-11671-2016
https://doi.org/10.5194/acp-16-11671-2016
Research article
 | 
21 Sep 2016
Research article |  | 21 Sep 2016

The Zugspitze radiative closure experiment for quantifying water vapor absorption over the terrestrial and solar infrared – Part 3: Quantification of the mid- and near-infrared water vapor continuum in the 2500 to 7800 cm−1 spectral range under atmospheric conditions

Andreas Reichert and Ralf Sussmann

Viewed

Total article views: 2,820 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,604 1,129 87 2,820 300 83 80
  • HTML: 1,604
  • PDF: 1,129
  • XML: 87
  • Total: 2,820
  • Supplement: 300
  • BibTeX: 83
  • EndNote: 80
Views and downloads (calculated since 25 Apr 2016)
Cumulative views and downloads (calculated since 25 Apr 2016)

Cited

Latest update: 23 Nov 2024
Short summary
Quantitative knowledge of water vapor infrared absorption is crucial for remote sensing and climate simulations. The water vapor continuum is a major contribution to atmospheric absorption in the near infrared (NIR), but recent laboratory studies show inconsistent results and cannot be transferred to atmospheric conditions. Therefore, we performed atmospheric measurements of the NIR continuum (2500–7800 cm−1) and found significant differences relative to the MT_CKD model and laboratory studies.
Altmetrics
Final-revised paper
Preprint