GOME NRT Nitrogen Dioxide


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 NO2 maps are created at the University of Bremen by applying the DOAS (Differential Optical Absorption) algorithm to GOME lv1 near real time spectra received from the Kiruna ground station.
In the DOAS retrieval, atmospheric absorbers are identified by their characteristic spectral absorption signature. In order to separate molecular absorptions from broad band scattering features, only the differential part of the absorption is used. In the case of NO2, the absorption bands in the 425 to 450 nm region are used for the detection. As GOME is essentially a nadir viewing instrument, the result of the DOAS analysis is the absorber column integrated along the line of sight. To convert this into a vertical column, the light path through the atmosphere is modelled using radiative transfer calculations, and a correction factor (airmass factor or AMF) is applied to the measurements. This airmass factor depends on the assumed vertical profile of the absorber, in particular in the UV.
All NO2 plots on this page are derived using a standard airmass factor derived using the profiles from the US standard atmosphere. This implies, that tropospheric NO2 pollution over industrialised regions are underestimated, in particular during winter. The NO2 columns in these regions are therefore to be interpreted in a qualitative way only.
More detailed information on the GOME NO2 analysis at the University of Bremen and the validation of GOME measurements can be found in the following publication:
  • Richter, A., Kreher, K., Johnston, P. V., Wittrock, F., and J. P. Burrows, Validation of GOME O3, NO2, BrO, and OClO Measurements in Southern High Latitudes, Fifth European Workshop on Stratospheric Ozone, 1999 zipped PS-File

More on NO2 from GOME can be found in the following publication:

  • Leue, C., Quantitative analysis of NOx emissions from GOME satellite images, Phd Thesis, University of Heidelberg, 1999 (in German)

Responsible: Andreas Richter / Last Change.

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