Combined characterisation of GOME and TOMS total ozone measurements from space using ground-based observations from the NDSC

  • J.-C. Lambert
  • , M. Van Roozendael
  • , P.C. Simon
  • , J.-P. Pommereau
  • , F. Goutail
  • , J.F. Gleason
  • , S.B. Andersen
  • , D.W. Arlander
  • , N.A. Bui Van
  • , H. Claude
  • , J. de La Noë
  • , M. De Mazière
  • , V. Dorokhov
  • , P. Eriksen
  • , A. Green
  • , K. Karlsen Tornkvist
  • , B.A. Kåstad Hoiskar
  • , E. Kyrö
  • , J. Leveau
  • , M.-F. Merienne
  • G. Milinevsky, H.K. Roscoe, A. Sarkissian, J.D. Shanklin, J. Stähelin, C. Wahlstrom Tellefsen, G. Vaughan

Publikation: Bidrag til tidsskriftArtikelForskningpeer review

28 Citationer (Scopus)

Resumé

Several years of total ozone measured from space by the ERS-2 GOME, the Earth Probe TOMS, and the ADEOS TOMS, are compared with high-quality ground-based observations associated with the Network for the Detection of Stratospheric Change (NDSC), over an extended latitude range and a variety of geophysical conditions. The comparisons with each spaceborne sensor are combined altogether for investigating their respective solar zenith angle (SZA) dependence, dispersion, and difference of sensitivity. The space- and ground-based data are found to agree within a few percent on average. However, the analysis highlights for both GOME and TOMS several sources of discrepancies: (i) a SZA dependence with TOMS beyond 80° SZA; (ii) a seasonal SZA dependence with GOME beyond 70° SZA; (iii) a difference of sensitivity with GOME at high latitudes; (iv) a difference of sensitivity to low ozone values between satellite and SAOZ sensors around the southern tropics; (v) a north/south difference of TOMS with the ground-based observations; and (vi) internal inconsistencies in GOME total ozone.

OriginalsprogEngelsk
Sider (fra-til)1931-1940
Antal sider10
TidsskriftAdvances in Space Research
Vol/bind26
Udgave nummer12
DOI
StatusUdgivet - dec. 2000
Udgivet eksterntJa

Emneord

  • Atmosphere

Programområde

  • Programområde 5: Natur og klima

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