Journal article icon

Journal article

Transient HCl in the atmosphere of Mars

Abstract:
A major quest in Mars' exploration has been the hunt for atmospheric gases, potentially unveiling ongoing activity of geophysical or biological origin. Here, we report the first detection of a halogen gas, HCl, which could, in theory, originate from contemporary volcanic degassing or chlorine released from gas-solid reactions. Our detections made at ~3.2 to 3.8 μm with the Atmospheric Chemistry Suite and confirmed with Nadir and Occultation for Mars Discovery instruments onboard the ExoMars Trace Gas Orbiter, reveal widely distributed HCl in the 1- to 4-ppbv range, 20 times greater than previously reported upper limits. HCl increased during the 2018 global dust storm and declined soon after its end, pointing to the exchange between the dust and the atmosphere. Understanding the origin and variability of HCl shall constitute a major advance in our appraisal of martian geo- and photochemistry.
Publication status:
Published
Peer review status:
Peer reviewed

Actions


Access Document


Publisher copy:
10.1126/sciadv.abe4386

Authors


More by this author
Role:
Author
ORCID:
0000-0003-1115-0656
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Physics
Sub department:
Atmos Ocean & Planet Physics
Role:
Author
ORCID:
0000-0002-2173-9889
More by this author
Role:
Author
ORCID:
0000-0003-4041-4972
More by this author
Role:
Author
ORCID:
0000-0001-5294-5426
More by this author
Role:
Author
ORCID:
0000-0002-4187-1457


Publisher:
American Association for the Advancement of Science
Journal:
Science Advances More from this journal
Volume:
7
Issue:
7
Article number:
eabe4386
Publication date:
2021-02-10
Acceptance date:
2020-12-28
DOI:
EISSN:
2375-2548
Pmid:
33568485


Language:
English
Keywords:
Pubs id:
1161511
Local pid:
pubs:1161511
Deposit date:
2021-04-19

Terms of use



Views and Downloads






If you are the owner of this record, you can report an update to it here: Report update to this record

TO TOP