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Atmospheric Measurement Techniques An interactive open-access journal of the European Geosciences Union
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Volume 10, issue 3
Atmos. Meas. Tech., 10, 1093-1110, 2017
https://doi.org/10.5194/amt-10-1093-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Meas. Tech., 10, 1093-1110, 2017
https://doi.org/10.5194/amt-10-1093-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 16 Mar 2017

Research article | 16 Mar 2017

Tropospheric dry layers in the tropical western Pacific: comparisons of GPS radio occultation with multiple data sets

Therese Rieckh et al.
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Anthes, R. A.: Exploring Earth's atmosphere with radio occultation: contributions to weather, climate and space weather, Atmos. Meas. Tech., 4, 1077–1103, https://doi.org/10.5194/amt-4-1077-2011, 2011.
Berrisford, P., Kållberg, P., Kobayashi, S., Dee, D., Uppala, S., Simmons, A., Poli, P., and Sato, H.: Atmospheric conservation properties in ERA-Interim, Q. J. Roy. Meteorol. Soc., 137, 1381–1399, https://doi.org/10.1002/qj.864, 2011.
Brown, R. G. and Zhang, C.: Variability of midtropospheric moisture and its effect on cloud-top height distribution during TOGA COARE, J. Atmos. Sci., 54, 2760–2774, https://doi.org/10.1175/1520-0469(1997)054<2760:VOMMAI>2.0.CO;2, 1997.
Casey, S. P. F., Dessler, A. E., and Schumacher, C.: Five-Year Climatology of Midtroposphere Dry Air Layers in Warm Tropical Ocean Regions as Viewed by AIRS/Aqua, J. Appl. Meteorol. Clim., 48, 1831–1842, https://doi.org/10.1175/2009JAMC2099.1, 2009.
Cau, P., Methven, J., and Hoskins, B.: Representation of dry tropical layers and their origins in ERA-40 data, J. Geophys. Res., 110, D06110, https://doi.org/10.1029/2004JD004928, 2005.
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We use GPS radio occultation (RO) data to investigate the structure and temporal behavior of extremely dry, high-ozone tropospheric air in the tropical western Pacific and compare them to various data sets (research aircraft, radiosonde, infrared sounder, and model reanalyses). All these data sets have limitations. We show that the RO data contribute significant information on the water vapor content. Our results also verify the quality of the reanalyses.
We use GPS radio occultation (RO) data to investigate the structure and temporal behavior of...
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