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Validation of Ife-1.6 Sciamachy Limb Ozone Profiles : Volume 5, Issue 11 (15/11/2005)

By Segers, A. J.

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Book Id: WPLBN0003994289
Format Type: PDF Article :
File Size: Pages 8
Reproduction Date: 2015

Title: Validation of Ife-1.6 Sciamachy Limb Ozone Profiles : Volume 5, Issue 11 (15/11/2005)  
Author: Segers, A. J.
Volume: Vol. 5, Issue 11
Language: English
Subject: Science, Atmospheric, Chemistry
Collections: Periodicals: Journal and Magazine Collection (Contemporary), Copernicus GmbH
Historic
Publication Date:
2005
Publisher: Copernicus Gmbh, Göttingen, Germany
Member Page: Copernicus Publications

Citation

APA MLA Chicago

M. Piter, A. J., Savigny, C. V., Brinksma, E. J., & Segers, A. J. (2005). Validation of Ife-1.6 Sciamachy Limb Ozone Profiles : Volume 5, Issue 11 (15/11/2005). Retrieved from http://www.ebooklibrary.org/


Description
Description: Royal Dutch Meteorological Institute (KNMI), P.O. Box 201, 3730 AE De Bilt, The Netherlands. The IFE-1.6 scientific data set of SCIAMACHY limb ozone profiles is validated for the period August–December 2002. The data set provides ozone profiles over an altitude range of 15–45 km. The main uncertainty in the profiles is the imprecise knowledge of the pointing of the instrument, leading to retrieved profiles that are shifted in altitude direction. To obtain a first order correction for the pointing error and the remaining uncertainties, the retrieved profiles are compared to their a-priori value and ozone sondes based on absolute distance and equivalent latitude criteria. A vertical shift of the satellite profiles with 2 km downward is found to be an appropriate correction for the data set studied. A total root-mean-square difference between limb profiles and sondes of 10–15% remains for the stratospheric ozone profile after application of the correction. Small biases are left above and below the ozone maximum at mid latitudes, where the vertical gradients in the retrieved product are in general too strong.

Summary
Validation of IFE-1.6 SCIAMACHY limb ozone profiles

 

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