Articles | Volume 17, issue 20
Atmos. Chem. Phys., 17, 12743–12778, 2017
https://doi.org/10.5194/acp-17-12743-2017

Special issue: The SPARC Reanalysis Intercomparison Project (S-RIP) (ACP/ESSD...

Atmos. Chem. Phys., 17, 12743–12778, 2017
https://doi.org/10.5194/acp-17-12743-2017
Research article
26 Oct 2017
Research article | 26 Oct 2017

Assessment of upper tropospheric and stratospheric water vapor and ozone in reanalyses as part of S-RIP

Sean M. Davis et al.

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Cited articles

Abalos, M., Legras, B., Ploeger, F., and Randel, W. J.: Evaluating the advective Brewer–Dobson circulation in three reanalyses for the period 1979–2012, J. Geophys. Res.-Atmos., 120, 7534–7554, https://doi.org/10.1002/2015JD023182, 2015.
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Bhartia, P. K. and Wellemeyer, C. W.: TOMS-V8 total O3 algorithm, in: OMI Algorithm Theoretical Basis Document: OMI Ozone Products, edited by: Bhartia, P. K., NASA Goddard Space Flight Center, Greenbelt, Maryland, ATBD-OMI-02, 15–32, 2002.
Bhartia, P. K., McPeters, R. D., Flynn, L. E., Taylor, S., Kramarova, N. A., Frith, S., Fisher, B., and DeLand, M.: Solar Backscatter UV (SBUV) total ozone and profile algorithm, Atmos. Meas. Tech., 6, 2533–2548, https://doi.org/10.5194/amt-6-2533-2013, 2013.
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Short summary
Ozone and water vapor in the stratosphere are important gases that affect surface climate and absorb incoming solar ultraviolet radiation. These gases are represented in reanalyses, which create a complete picture of the state of Earth's atmosphere using limited observations. We evaluate reanalysis water vapor and ozone fidelity by intercomparing them, and comparing them to independent observations. Generally reanalyses do a good job at representing ozone, but have problems with water vapor.
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