Decreases in atomic hydrogen over the summer pole: Evidence for dehydration from polar mesospheric clouds?
Observations from the Sounding of the Atmosphere with Broadband Emission Radiometry (SABER) instrument on the NASA/Thermospheric Ionosphere Mesosphere Energetics and Dynamics satellite show a surprising decrease in the inferred atomic hydrogen (H) over the polar regions in the lowermost thermosphere during the summer. This contrasts with predictions by global models that H should peak in this region at this time. We suggest the decrease is a consequence of the sequestering of the water vapor by the formation of polar mesospheric clouds (PMCs) that redistributes the H₂O thus reducing the chemical source of H. This decrease is more pronounced in the Northern rather than the Southern summer which is roughly consistent with the known morphology of PMCs. A model calculation which includes a PMC parameterization gives good qualitative agreement with the data suggesting that this process should be considered in global models of the coupling between the middle and upper atmosphere.
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https://n2t.org/ark:/85065/d7d50n5p
eng
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publication
2016-01-01T00:00:00Z
publication
2008-07-08T00:00:00Z
An edited version of this paper was published by AGU. Copyright 2008 American Geophysical Union.
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