Retrieval of water vapor using ground-based observations from a prototype ATOMMS active centimeter- and millimeter-wavelength occultation instrument
Author
Ward, Dale M.Kursinski, E. Robert
Otarola, Angel C.
Stovern, Michael
McGhee, Josh
Young, Abe
Hainsworth, Jared
Hagen, Jeff
Sisk, William
Reed, Heather
Affiliation
Univ Arizona, Dept Atmospher SciUniv Arizona, Dept Phys
Univ Arizona, Dept Astron
Issue Date
2019-03-27Keywords
Atmospheric Science
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COPERNICUS GESELLSCHAFT MBHCitation
Ward, D. M., Kursinski, E. R., Otarola, A. C., Stovern, M., McGhee, J., Young, A., Hainsworth, J., Hagen, J., Sisk, W., and Reed, H.: Retrieval of water vapor using ground-based observations from a prototype ATOMMS active centimeter- and millimeter-wavelength occultation instrument, Atmos. Meas. Tech., 12, 1955-1977, https://doi.org/10.5194/amt-12-1955-2019, 2019.Rights
© Author(s) 2019. This work is distributed under the Creative Commons Attribution 3.0 License.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
A fundamental goal of satellite weather and climate observations is profiling the atmosphere with in situ-like precision and resolution with absolute accuracy and unbiased, all-weather, global coverage. While GPS radio occultation (RO) has perhaps come closest in terms of profiling the gas state from orbit, it does not provide sufficient information to simultaneously profile water vapor and temperature. We have been developing the Active Temperature, Ozone and Moisture Microwave Spectrometer (ATOMMS) RO system that probes the 22 and 183 GHz water vapor absorption lines to simultaneously profile temperature and water vapor from the lower troposphere to the mesopause. Using an ATOMMS instrument prototype between two mountaintops, we have demonstrated its ability to penetrate through water vapor, clouds and rain up to optical depths of 17 (7 orders of magnitude reduction in signal power) and still isolate the vapor absorption line spectrum to retrieve water vapor with a random uncertainty of less than 1 %. This demonstration represents a key step toward an orbiting ATOMMS system for weather, climate and constraining processes. ATOMMS water vapor retrievals from orbit will not be biased by climatological or first-guess constraints and will be capable of capturing nearly the full range of variability through the atmosphere and around the globe, in both clear and cloudy conditions, and will therefore greatly improve our understanding and analysis of water vapor. This information can be used to improve weather and climate models through constraints on and refinement of processes affecting and affected by water vapor.Note
Open access journalISSN
1867-8548Version
Final published versionSponsors
National Science Foundation Major Research Instrumentation (MRI) Program [0723239]; National Science Foundation, Division of Atmospheric and Geospace Sciences (GEO/AGS) [0946411, 1313563]; PlanetIQ, Golden, COAdditional Links
https://www.atmos-meas-tech.net/12/1955/2019/ae974a485f413a2113503eed53cd6c53
10.5194/amt-12-1955-2019
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Except where otherwise noted, this item's license is described as © Author(s) 2019. This work is distributed under the Creative Commons Attribution 3.0 License.

