Smoothing radio occultation bending angles above 40 km

The 'statistically optimal' approach to smoothing bending angles derived from radio occultation (RO) measurements is outlined. This combines a measured bending angle profile with an <i>a priori </i>or background estimate derived from climatology, in order to obtain the most...

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Main Author: S. B. Healy
Format: Article
Language:English
Published: Copernicus Publications 2001-04-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/19/459/2001/angeo-19-459-2001.pdf
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author S. B. Healy
author_facet S. B. Healy
author_sort S. B. Healy
collection DOAJ
description The 'statistically optimal' approach to smoothing bending angles derived from radio occultation (RO) measurements is outlined. This combines a measured bending angle profile with an <i>a priori </i>or background estimate derived from climatology, in order to obtain the most probable bending angle profile. However, the method is only optimal if the error statistics of both the measured and background profiles are known and applied accurately. In this work it is shown that correlations in the background estimate have a significant role in determining the degree of smoothing in the solution. We find that smooth profiles, consistent with the measured values, can be derived if the correlations are approximated analytically with a Gaussian, assuming a scale length of 6km. In regions where the observed and background error levels are comparable, the solutions take the general shape from the background estimate, centred on the observation data. The effects of correlated observation errors are also considered. It is shown that the quality of the temperature retrievals can be significantly affected by the choice of climatology used for background estimate.<br><br><b>Key words. </b>Atmosphere composition and structure (pressure, density and temperature) – Radio science (remote sensing)
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spelling doaj.art-cefd4eff640d49db83970911247ab8082022-12-21T23:26:19ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762001-04-011945946810.5194/angeo-19-459-2001Smoothing radio occultation bending angles above 40 kmS. B. Healy0NWP Division, The Met Office, London Road, Bracknell, RG12 2SZ, UKThe 'statistically optimal' approach to smoothing bending angles derived from radio occultation (RO) measurements is outlined. This combines a measured bending angle profile with an <i>a priori </i>or background estimate derived from climatology, in order to obtain the most probable bending angle profile. However, the method is only optimal if the error statistics of both the measured and background profiles are known and applied accurately. In this work it is shown that correlations in the background estimate have a significant role in determining the degree of smoothing in the solution. We find that smooth profiles, consistent with the measured values, can be derived if the correlations are approximated analytically with a Gaussian, assuming a scale length of 6km. In regions where the observed and background error levels are comparable, the solutions take the general shape from the background estimate, centred on the observation data. The effects of correlated observation errors are also considered. It is shown that the quality of the temperature retrievals can be significantly affected by the choice of climatology used for background estimate.<br><br><b>Key words. </b>Atmosphere composition and structure (pressure, density and temperature) – Radio science (remote sensing)https://www.ann-geophys.net/19/459/2001/angeo-19-459-2001.pdf
spellingShingle S. B. Healy
Smoothing radio occultation bending angles above 40 km
Annales Geophysicae
title Smoothing radio occultation bending angles above 40 km
title_full Smoothing radio occultation bending angles above 40 km
title_fullStr Smoothing radio occultation bending angles above 40 km
title_full_unstemmed Smoothing radio occultation bending angles above 40 km
title_short Smoothing radio occultation bending angles above 40 km
title_sort smoothing radio occultation bending angles above 40 km
url https://www.ann-geophys.net/19/459/2001/angeo-19-459-2001.pdf
work_keys_str_mv AT sbhealy smoothingradiooccultationbendinganglesabove40km