GOME NRT Total Ozone and Profiles


Please note that these maps are small versions and that each map is clickable. A new window will appear with the normalsized jpg-version of the map. You should use a browser with activated JavaScript. Otherwise go to the Archive section down below, where a data page for each day is available. A brief introduction can also be found further down below. The results on this page are preliminary!
 

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Archive

December
  06 13 20 27
  07 14 21 28
01 08 15 22 29
02 09 16 23 30
03 10 17 24 31
04 11 18 25  
05 12 19 26  
January
  03 10 17 24 31
  04 11 18 25  
  05 12 19 26  
  06 13 20 27  
  07 14 21 28  
01 08 15 22 29  
02 09 16 23 30  
February
  07 14 21 28
01 08 15 22 29
02 09 16 23  
03 10 17 24  
04 11 18 25  
05 12 19 26  
06 13 20 27  
March
  06 13 20 27
  07 14 21 28
01 08 15 22 29
02 09 16 23 30
03 10 17 24 31
04 11 18 25  
05 12 19 26  
April
  03 10 17 24
  04 11 18 25
  05 12 19 26
  06 13 20 27
  07 14 21 28
01 08 15 22 29
02 09 16 23 30
May
01 08 15 22 29
02 09 16 23 30
03 10 17 24  
04 11 18 25  
05 12 19 26  
06 13 20 27  
07 14 21 28  


Introduction

GOME near real time (NRT) total ozone data are directly processed by the GDP installed at ESA's Kiruna ground station, by applying the DOAS (Differential Optical Absorption) algorithm to GOME Level-1 spectra. From correlative studies it has been shown that the differences between NRT and final version total ozone are fairly small.
GOME NRT ozone profiles are produced at the Institute of Environmental Physics and Remote Sensing, University of Bremen using the FURM algorithm on GOME NRT Level-1 radiances and irradiances.
FURM (FUll Retrieval Method) is an advanced Optimal Estimation inversion scheme to derive ozone profiles from the UV spectra. FURM consists of two major parts: (a) a forward model: the pseudo-spherical multiple scattering radiative transfer model (RTM) GOMETRAN++, calculating the top of atmosphere (TOA) radiance for a given state of the atmosphere, and (b) an iterative inversion scheme, that adjusts this state to match the calculated with the measured TOA radiance, utilizing the so-called weighting functions also provided by GOMETRAN. Because this inversion problem is under-constrained, an optimal estimation approach was chosen, which combines the information from the measurement with statistical a-priori information from a climatology.
For good results, reliable information about the meteorological conditions, e.g. temperature and pressure profile are needed. We usually use UKMO - UARS assimilated data for this purpose, because data are available up to about 55km. For NRT profile retrieval, this is not possible, because the UKMO data are not available until the next day. Instead, we use the 24hour forecast provided by ECMWF. Because these data reach only up to 30km altitude, the profiles are extended by UKMO data of the previous day.
FURM profile retrieval is currently limited to solar zenith angles less then 75 degree, thus the most nothern GOME pixel are not usable.

References:

  • K. Bramstedt, K.-U. Eichmann, M. Weber, R. Hoogen, V. Rozanov, and J.P. Burrows, Ozone depletion in the Arctic spring calculated from GOME Ozone Profiles, European Symposium on Atmospheric Measurements from Space, Proc. ESAMS'99, ESA-WPP-161, 225-229, 1999.
  • K.-U. Eichmann, K. Bramstedt, M. Weber, R. Hoogen, V.V. Rozanov, and J.P. Burrows, Structure of ozone mini-holes from GOME, European Symposium on Atmospheric Measurements from Space, Proc. ESAMS'99, ESA-WPP-161, 231-236, 1999.
  • K.-U. Eichmann, K. Bramstedt, M. Weber, V.V. Rozanov, R. Hoogen and J.P. Burrows, O3 profiles from GOME satellite data - II: Observations in the Arctic spring 1997 and 1998, Physics and Chemistry of the Earth 24, 453-457, 1999.
  • R. Hoogen, V.V. Rozanov, J.P. Burrows, Ozone Profiles from GOME Satellite Data: Algorithm Description and First Validation,J. Geophysical Research, 1999, vol.104, p. 8263-8280.
  • R. Hoogen, V.V. Rozanov, K. Bramstedt, K.-U. Eichmann, M. Weber, and J.P. Burrows, Ozone profiles from GOME satellite data-I: Comparison with ozonesonde measurements, Physics and Chemistry of the Earth 24, 447-452, 1999.

Responsible: Klaus Bramstedt / Kai-Uwe Eichmann / Last Change.

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