Exploring air-sea gas transfer by active thermography

Active thermography has been used for almost 30 years to explore air-sea gas transfer both in laboratory and field experiments. In the early 2000s, some doubt arose whether it was possible to extrapolate heat transfer velocities to gas transfer velocities. Because of the large difference in the mole...

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Main Authors: Kunz, Jakob, Krall, Kerstin, Jähne, Bernd
Format: Conference Object
Language:unknown
Published: Zenodo 2015
Subjects:
Online Access:https://doi.org/10.5281/zenodo.17670
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record_format openpolar
spelling ftzenodo:oai:zenodo.org:17670 2024-09-15T18:23:55+00:00 Exploring air-sea gas transfer by active thermography Kunz, Jakob Krall, Kerstin Jähne, Bernd 2015-05-18 https://doi.org/10.5281/zenodo.17670 unknown Zenodo https://zenodo.org/communities/asi https://doi.org/ https://doi.org/10.5281/zenodo.17670 oai:zenodo.org:17670 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode GTWS 2015, 7th International Symposium on Gas Transfer at Water Surfaces, Seattle WA, USA, 18-21 May 2015 air-sea gas transfer heat transfer thermography SOPRAN info:eu-repo/semantics/conferencePoster 2015 ftzenodo https://doi.org/10.5281/zenodo.17670 2024-07-26T21:13:40Z Active thermography has been used for almost 30 years to explore air-sea gas transfer both in laboratory and field experiments. In the early 2000s, some doubt arose whether it was possible to extrapolate heat transfer velocities to gas transfer velocities. Because of the large difference in the molecular diffusivity, different mechanisms may govern the transfer of heat and mass. However, in a recent experimental study at the large annular wind-wave tank in Heidelberg, the Aeolotron, Nagel et al. [2014] could show that heat transfer velocities can be scaled to gas transfer velocities with an accuracy of better than 10%, provided the Schmidt number exponent is known. These measurements were performed using the original active thermographic technique proposed by Jähne et al. [1989], by heating a rather large area at the water surface of up to one square meter. This is required to ensure that water parcels stay longer in the heated patch than the response time of heat transfer across the boundary layer. The setup used by Nagel et al. [2014] still had one disadvantage. The heated patch showed some inhomogeneity in cross-wind direction, caused by the method to expand the beam of the CO2 laser. By using a holographic beam expander, a much more homogeneous irradiation could be achieved. With this improvement it was possible to acquire significantly more accurate heat transfer measurements. In November 2014 this technique was used in air-sea gas exchange measurements using natural seawater from the North Atlantic with various degrees of contamination by natural surface films at the Heidelberg Aeolotron, within the BMBF project SOPRAN (Surface Ocean Processes in the Anthropocene). First results from this experiment will be shown. Conference Object North Atlantic Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
topic air-sea gas transfer
heat transfer
thermography
SOPRAN
spellingShingle air-sea gas transfer
heat transfer
thermography
SOPRAN
Kunz, Jakob
Krall, Kerstin
Jähne, Bernd
Exploring air-sea gas transfer by active thermography
topic_facet air-sea gas transfer
heat transfer
thermography
SOPRAN
description Active thermography has been used for almost 30 years to explore air-sea gas transfer both in laboratory and field experiments. In the early 2000s, some doubt arose whether it was possible to extrapolate heat transfer velocities to gas transfer velocities. Because of the large difference in the molecular diffusivity, different mechanisms may govern the transfer of heat and mass. However, in a recent experimental study at the large annular wind-wave tank in Heidelberg, the Aeolotron, Nagel et al. [2014] could show that heat transfer velocities can be scaled to gas transfer velocities with an accuracy of better than 10%, provided the Schmidt number exponent is known. These measurements were performed using the original active thermographic technique proposed by Jähne et al. [1989], by heating a rather large area at the water surface of up to one square meter. This is required to ensure that water parcels stay longer in the heated patch than the response time of heat transfer across the boundary layer. The setup used by Nagel et al. [2014] still had one disadvantage. The heated patch showed some inhomogeneity in cross-wind direction, caused by the method to expand the beam of the CO2 laser. By using a holographic beam expander, a much more homogeneous irradiation could be achieved. With this improvement it was possible to acquire significantly more accurate heat transfer measurements. In November 2014 this technique was used in air-sea gas exchange measurements using natural seawater from the North Atlantic with various degrees of contamination by natural surface films at the Heidelberg Aeolotron, within the BMBF project SOPRAN (Surface Ocean Processes in the Anthropocene). First results from this experiment will be shown.
format Conference Object
author Kunz, Jakob
Krall, Kerstin
Jähne, Bernd
author_facet Kunz, Jakob
Krall, Kerstin
Jähne, Bernd
author_sort Kunz, Jakob
title Exploring air-sea gas transfer by active thermography
title_short Exploring air-sea gas transfer by active thermography
title_full Exploring air-sea gas transfer by active thermography
title_fullStr Exploring air-sea gas transfer by active thermography
title_full_unstemmed Exploring air-sea gas transfer by active thermography
title_sort exploring air-sea gas transfer by active thermography
publisher Zenodo
publishDate 2015
url https://doi.org/10.5281/zenodo.17670
genre North Atlantic
genre_facet North Atlantic
op_source GTWS 2015, 7th International Symposium on Gas Transfer at Water Surfaces, Seattle WA, USA, 18-21 May 2015
op_relation https://zenodo.org/communities/asi
https://doi.org/
https://doi.org/10.5281/zenodo.17670
oai:zenodo.org:17670
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.17670
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