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AGU: Journal of Geophysical Research, Atmospheres

 

Keywords

  • satellite data
  • stratospheric dynamics

Index Terms

  • Atmospheric Composition and Structure: Middle atmosphere: constituent transport and chemistry
  • Atmospheric Composition and Structure: Middle atmosphere: composition and chemistry
  • Atmospheric Processes: Middle atmosphere dynamics
  • Atmospheric Processes: Remote sensing
Abstract
Cited By (6)
 

Abstract

Solar occultation satellite data and derived meteorological products: Sampling issues and comparisons with Aura Microwave Limb Sounder

Gloria L. Manney

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

William H. Daffer

Columbus Technologies and Services Inc., Pasadena, California, USA

Joseph M. Zawodny

NASA Langley Research Center, Hampton, Virginia, USA

Peter F. Bernath

Department of Chemistry, University of Waterloo, Waterloo, Ontario, Canada

Department of Chemistry, University of York, Heslington, York, United Kingdom

Karl W. Hoppel

Naval Research Laboratory, Washington, D. C., USA

Kaley A. Walker

Department of Chemistry, University of Waterloo, Waterloo, Ontario, Canada

Department of Physics, University of Toronto, Toronto, Ontario, Canada

Brian W. Knosp

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

Chris Boone

Department of Chemistry, University of Waterloo, Waterloo, Ontario, Canada

Ellis E. Remsberg

NASA Langley Research Center, Hampton, Virginia, USA

Michelle L. Santee

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

V. Lynn Harvey

Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, Colorado, USA

Steven Pawson

NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

David R. Jackson

Met Office, Exeter, UK

Lance Deaver

GATS, Inc., Newport News, Virginia, USA

C. Thomas McElroy

Environment Canada, Toronto, Ontario, Canada

Chris A. McLinden

Environment Canada, Toronto, Ontario, Canada

James R. Drummond

Department of Physics, University of Toronto, Toronto, Ontario, Canada

Department of Physics and Atmospheric Science, Dalhousie University, Halifax, Nova Scotia, Canada

Hugh C. Pumphrey

School of Geosciences, University of Edinburgh, Edinburgh, UK

Alyn Lambert

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

Michael J. Schwartz

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

Lucien Froidevaux

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

Sean McLeod

Department of Chemistry, University of Waterloo, Waterloo, Ontario, Canada

Lawrence L. Takacs

NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

Max J. Suarez

NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

Charles R. Trepte

NASA Langley Research Center, Hampton, Virginia, USA

David C. Cuddy

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

Nathaniel J. Livesey

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

Robert S. Harwood

Environment Canada, Toronto, Ontario, Canada

Joe W. Waters

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

Derived Meteorological Products (DMPs, including potential temperature, potential vorticity (PV), equivalent latitude (EqL), horizontal winds and tropopause locations) from several meteorological analyses have been produced for the locations and times of measurements taken by several solar occultation instruments and the Aura Microwave Limb Sounder (MLS). MLS and solar occultation data are analyzed using DMPs to illustrate sampling issues that may affect interpretation and comparison of data sets with diverse sampling patterns and to provide guidance regarding the kinds of studies that benefit most from analyzing satellite data in relation to meteorological conditions using the DMPs. Using EqL or PV as a vortex-centered coordinate does not alleviate all sampling problems, including those in studies using “vortex averages” of solar occultation data and in analyses of localized features (such as polar stratospheric clouds) and other fields that do not correlate well with PV. Using DMPs to view measurements with respect to their air mass characteristics is particularly valuable in studies of transport of long-lived trace gases, polar processing in the winter lower stratosphere, and distributions and transport of O3 and other trace gases from the upper troposphere through the lower stratosphere. The comparisons shown here demonstrate good agreement between MLS and solar occultation data for O3, N2O, H2O, HNO3, and HCl; small biases are attributable to sampling effects or are consistent with detailed validation results presented elsewhere in this special section. The DMPs are valuable for many scientific studies and to facilitate validation of noncoincident measurements.

Received 27 March 2007; accepted 5 November 2007; published 25 December 2007.

Citation: Manney, G. L., et al. (2007), Solar occultation satellite data and derived meteorological products: Sampling issues and comparisons with Aura Microwave Limb Sounder, J. Geophys. Res., 112, D24S50, doi:10.1029/2007JD008709.

Cited By

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