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Tropospheric NO2 from SCIAMACHY limb-nadir matching
Introduction Data Documentation PROMOTE
References Links
Contact
Nitrogen dioxide (NO2) is a key species in tropospheric chemistry and air
quality. It usually is measured by in-situ surface networks, but the total
amount of tropospheric NO2 can also be measured from space, providing a global
view.
As an air pollution monitoring demonstration project for
PROMOTE, the University of Bremen provides
tropospheric NO2 columns derived from measurements of the SCIAMACHY on ENVISAT for a
selected time period. The approach taken is the novel limb-nadir matching
technique, that promises higher accuracy and less dependence on external a
priori information on the stratospheric amount of NO2.
Coverage of the SCIAMACHY limb-nadir columns is limited by three parameters:
- the orbit and alternating limb-nadir pattern of the instrument
- availability of SCIAMACHY lv0 data which is not always guaranteed
- selection of cloud free scenes
Coverage has improved as lv1 data is now also included in the data analysis.
However, for the data presented here, only lv0 NRT data has been used.
More details on the analysis procedures used can be found in the
Documentation given below.
As a demonstration product, tropospheric NO2 columns derived from SCIAMACHY limb-nadir
measurements for 2004 have been derived. In principle, the data set could be
extended to the complete SCIAMACHY time series, but transition from the
demonstration service to a continuous service depends on funding.
Daily and monthly images are accessible via our
SCIAMACHY data browser pages by selecting NO2 and limb Nadir Trop. Column.
ASCII data files with monthly global data can be downloaded below.
Daily values will be added soon. These files are
encrypted. Please contact
Andreas Heckel for
the password.
The file format is plain ASCII with CR LF delimiters and no EOF:
- 20 lines of ASCII header with information on file format and content
- 1440 blocks of data for the 0.125° latitude bands starting at the south
pole
- each block starts with a line indicating the centre of the latitude band
- followed by 2880 values for the longitudes starting at -179.9375°E with a
line break after every 10 values
- units are 1E14 molec/cm2
- error flag is -999.99
If you experience any problems, please contact
Andreas Heckel.
More data is available in our group off-line. If you have any requests, please
contact
Andreas
Heckel.
What is limb-nadir matching?
The
SCIAMACHY instrument on ENVISAT is alternating between two measurement modes: a
nadir measurement that provides total columns in good spatial resolution and a
limb sounding that takes a stratospheric profile. The two measurements are
synchronized (matched) in a way that for each nadir measurement, a corresponding
stratospheric profile has been measured a couple of minutes earlier (see
animation). Thus, in principle the tropospheric amount of a species can be
determined by subtracting the integrated limb stratospheric column from
the total nadir column.
How is the tropospheric NO2 column determined?
Determination of the tropospheric NO2 column is a multi-step analysis briefly
outlined below:
- Determination of the total nadir NO2 slant column using the DOAS method
- Determination of the stratospheric NO2 profile from the limb measurements
- Computation of the stratospheric nadir NO2 slant column from the limb
profile
- Subtraction of the stratospheric nadir slant column from the total nadir
slant column to derive the tropospheric nadir slant column
- Application of a tropospheric airmass factor (AMF) to derive tropospheric
vertical columns
For more details, have a look at our
limb-nadir documentation.
What does it look like in practice?
The data analysis is illustrated in the three pictures below which are monthly
averages of July 2004 for clarity although the method works on a measurement by measurement
basis.
How does it compare to other tropospheric NO2 products?
The main difference between tropospheric NO2 columns from limb-nadir matching
and other products is the treatment of stratospheric NO2. Many other
tropospheric column products just assume that the stratosphere is zonally
homogeneous, and while this is often correct, it sometimes fails and leads to
large errors in the tropospheric product.
An example is shown below for February 16th, 2004 without cloud screening. On the left hand side, the
result of a standard analysis using the reference sector method (RSM) is shown,
on the right hand side the same data analysed with the limb-nadir matching (LNM)
are plotted. Although the overall pattern is similar, it is clear that the
number of negative values is much reduced.
 
Validation
TBD
PROMOTE,
PROtocol MOniToring for the GMES Service Element on
Atmospheric Composition, is an ambitious proposal covering the atmosphere part
of System Earth. It proposes GMES services relevant to the ozone layer,
UV-exposure on the ground, air pollution and climate change. These services are
directed at the needs for information on environment and climate by public
authorities and governmental agencies.
- Richter, A., Burrows, J. P., Nüß, H., Granier, C, Niemeier, U.,
Increase in tropospheric nitrogen dioxide over China observed from space,
Nature, 437, 129-132, doi: 10.1038/nature04092, 2005
-
Sierk, B., Richter, A., Rozanov, A., v. Savigny, C.,
Schmoltner, A.M., Buchwitz, M., Bovensmann, H., and J. P. Burrows,
Retrieval and Monitoring of Atmospheric
Trace Gas Concentrations in Nadir and Limb Geometry using the Space-Borne
SCIAMACHY Instrument, Environmental Monitoring and Assessment, DOI:
10.1007/s10661-005-9049-9, 2006
-
Richter, A. and J.P. Burrows,
Retrieval of Tropospheric NO2
from GOME Measurements, Adv. Space Res., 29(11) ,1673-1683,
2002
.
If you are interested in more information or GOME and SCIAMACHY tropospheric
NO2 data from the University of Bremen, please contact
Andreas Heckel or
Andreas Richter.
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