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Introduction Instrument
Data
References Links
Contact
In 1995, a DOAS instrument was set-up in the NDSC building at the Ny-Ålesund
(79°N, 10°E) station in Svalbard. The Ny-Ålesund
station is an Arctic
NDACC station with polar night from October to February,
rapidly changing solar elevation angles in spring and fall and polar day in
summer. The focus of the measurements at this site is stratospheric chemistry in
arctic regions, in particular ozone chemistry. As a result of its geographical
location, Ny-Ålesund experiences
both time periods with the polar vortex located above the station, and
situations when non vortex air is probed.
A second focus of the Ny-Ålesund
measurements is polar tropospheric halogen chemistry, in particular bromine
chemistry. Depending on the meteorological conditions, air masses from the polar
ice cap are transported to Ny-Ålesund,
and episodes of rapid ozone destruction in the boundary layer (low ozone events)
can frequently be observed in spring.
Originally, the DOAS instrument in Ny-Ålesund
was a simple zenith-viewing grating spectrometer using a 1024 pixel cooled
Reticon diode array as a detector. To minimize wavelength drift, the
spectrometer is temperature stabilized. Calibration measurements (line lamp,
white light source) are automatically performed every day. The telescope of the
instrument is integrated in a roof window, leaving all parts inside the
building.
In spring 1998, a flip mirror was
integrated in the telescope, facilitating alternating zenith-sky and off-axis
(horizon viewing) measurements. The latter are directed towards the Fjord, and
had an elevation angle of 4°. With this viewing geometry, the light path
through the troposphere is strongly enhanced, increasing the sensitivity of the
measurements towards tropospheric absorbers such as BrO. By combining
measurements from both viewing directions, stratospheric and tropospheric
contributions to the observed total column can be separated.
In spring 2002, the telescope was
replaced by an improved version, allowing sequential measurements in up to 4
directions above the horizon (3°, 6°, 10° and 18°) and to the zenith with a motorized mirror. At the
same time, the spectrometer and detector were replaced by a new system using a CCD
detector to decrease noise at low sun.
In March 2003
a second spectrometer with a CCD was installed to extend the observed wavelength range
to include the visible spectrum. Both spectrometers are connected to the same
telescope.
In April 2011, the telescope was again replaced by a new
version on a pan tilt head allowing measurements in various azimuthal directions,
now providing
measurements towards and away from the Fjord. At the same time, the UV
instrument was replaced by a system with better signal to noise characteristics.
More on the instrument and measurement method can be found on our
MAXDOAS page.
Some data from the Ny-Alesund measurements is available on the
data products page.
All stratospheric measurements from Ny-Alesund are available through the NDACC
data base. If you have any
other data requests, please
contact
Folkard Wittrock.
- SCIAMACHY validation with ground-based DOAS observations
final report (in
German)
- F. Wittrock, H. Oetjen, A. Richter, S. Fietkau, T. Medeke, A. Rozanov, J.
P. Burrows
MAX-DOAS measurements of atmospheric trace gases in Ny-Ålesund - Radiative transfer
studies and their application, Atmos. Chem. Phys., 4, 955-966,
2004
- J. Sommar, I. Wängberg, T. Berg, K. Gårdfeldt, J. Munthe, A. Richter, A. Urba,
F. Wittrock, W. H. Schroeder,
Circumpolar transport and air-surface exchange of atmospheric mercury at Ny-Ålesund
(79° N), Svalbard, spring 2002,Atmos. Chem. Phys. Discuss., 4, 1727-1771,
2004H. Oetjen,
Messungen atmosphärischer Spurengase in Ny-Ålesund,
Diploma-Thesis, University of Bremen, September 2002 (in German)
- F. Wittrock, H. Oetjen, A. Richter, S. Fietkau, T. Medeke, A. Rozanov, J.
P. Burrows
MAX-DOAS measurements of atmospheric trace gases in Ny-Ålesund - Radiative transfer
studies and their application, Atmos. Chem. Phys., 4, 955-966,
2004 Müller, R.W., H. Bovensmann, J. W. Kaiser, A.
Richter, A. Rozanov, F. Wittrock, and J. P. Burrows, Consistent Interpretation
of Ground based and GOME BrO Slant Column Data,
Adv. Space Res., 29(11) ,1655-1660, 2002
- Aliwell, S. R., M. Van Roozendael, P. V. Johnston, A. Richter, T. Wagner,
D. W. Arlander, J. P. Burrows, D. J. Fish, R. L. Jones, K. K. Tornkvist,
J.-C. Lambert, K. Pfeilsticker, and I. Pundt, Analysis for BrO in zenith-sky
spectra; An intercomparison exercise for
analysis improvement, JGR, doi:10.1029/2001JD000329, 2002
- Sinnhuber, B.-M., D. W. Arlander, H. Bovensmann, J. P. Burrows, M. P.
Chipperfield, C.-F. Enell, U. Frieß, F. Hendrick, P. V. Johnston, R. L. Jones,
K. Kreher, N. Mohamed-Tahrin, R. Müller, K. Pfeilsticker, U. Platt, J.-P.
Pommereau, I. Pundt, A. Richter, A. M. South, K. K. Toernkvist, M. Van
Roozendael, T. Wagner, and F. Wittrock,
Comparison of measurements
and model calculations of stratospheric bromine monoxide, JGR, doi:10.1029/2001JD000940,
2002
- S. Schlieter,
Spurengasmessungen während der Nacht mittels Mondlichtspektroskopie im
Vergleich mit Modellrechnungen, PhD-Thesis, University of Bremen, June
2001 (in german)
- Wittrock, F., R. Müller, A. Richter, H. Bovensmann, and J.P. Burrows, Observations of
Iodine monoxide above Spitsbergen, Geoph. Res. Let., Vol. 27, No. 10, p1471-1474, 2000.
- Bruns, M., H. Bovensmann, R. Müller, A. Richter, F. Wittrock and J. P.
Burrows, Modelling of BrO slant columns over Ny-Ålesund (79°N) and Bremen
(53°N), Fifth European Workshop on Stratospheric Ozone, St. Jean de Luz,
France, 1999.
- Schlieter, S., M. Bruns, R. Müller, A. Richter, F. Wittrock and J. P.
Burrows, NO3 measurements in polar and midlatitudes and comparison with model
calculations, Fifth European Workshop on Stratospheric Ozone, St. Jean de Luz,
France, 1999.
- Wittrock, F., H. Altmeyer, M. Bruns, M. Laue, K. Munderloh, A. Richter, S. Schlieter and J. P.
Burrows, Observations of O3, NO2, BrO and OClO at different latitudes, Fifth European Workshop on Stratospheric Ozone, St. Jean de Luz,
France, 1999.
If
you are interested in more information or would like to have access to our
data, please contact Folkard
Wittrock.
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