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[1]
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Rao, T. N., J. Arvelius and S. Kirkwood: Climatology of tropopause
folds over a european arctic station - Esrange. J.Geophys. Res., vol. 113:D00B03, 10.1029/2007JD009638, 2008.
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DOI ]
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[2]
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Robinson, A. D., G. A. Millard, F. Danis, M. Guirlet, N. R. P. Harris, A. M.
Lee, J. D. McIntyre, J. A. Pyle, J. Arvelius, S. Dagnesjo, S. Kirkwood,
H. Nilsson, D. W. Toohey, T. Deshler, F. Goutail, J-P. Pommereau, J. W.
Elkins, F. Moore, E. Ray, U. Schmidt, A. Engel and M. Müller:
Ozone loss derived from balloon-borne tracer measurements in the
1999/2000 arctic winter. Atmos.Chem.Phys., vol. 5(5):1423-1436,
ISSN 1680-7316, SRef-ID:1680-7324/acp/2005-5-1423, 2005.
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[3]
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Hooper, D., J. Arvelius and K. Stebel: Retrieval of atmospheric static
stability from radar return signal power. Ann.Geophys.,
vol. 22(11):3781-3788, SRef-ID:1432-0576/ag/2004-22-3781, 2004.
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[4]
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Rao, T. Narayana, J. Arvelius, S. Kirkwood and P. von der Gathen:
Climatology of ozone in the troposphere and lower stratosphere over
the european arctic. Adv.Space Res., vol. 34(4):754-758,
10.1016/j.asr.2003.05.055, 2004.
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DOI ]
A brief climatology of ozone using more than 8 years
of ozonesonde data in the troposphere and lower
stratosphere at two northern high latitude stations,
Sodankyla and Ny-Ålesund, is presented. The
climatology of ozone clearly shows a significant
seasonal cycle with the ozone maxima changing with
height. The monthly variability of ozone as well as
its seasonal maximum is found near the
tropopause. Variation in tropopause height is due
mainly to the passage of tropospheric weather
systems and is responsible for the large monthly
variability of ozone near the tropopause. In the
lower stratosphere, interannual variations are at a
maximum in winter and spring, and are the result of
variations in wave driven stratospheric circulation,
which peaks in winter. The present climatology forms
a basis for 3-D chemistry transport models to test
its ability at high latitudes.
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[5]
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Rao, T. Narayana, S. Kirkwood, J. Arvelius, P. von der Gathen and R. Kivi:
Climatology of UTLS ozone and the ratio of ozone and potential
vorticity over northern Europe. J.Geophys.Res., vol.
108(D22):4703, 10.1029/2003JD003860, 2003.
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DOI |
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[6]
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Müller, Rolf, Simone Tilmes, Jens-Uwe Groß, Daniel S. McKenna, Melanie
Müller, Ulrich Schmidt, Geoffrey C. Toon, Robert A. Stachnik, James J.
Margitan, James W. Elkins, Johan Arvelius and James M. Russel III:
Chlorine activation and chemical ozone loss deduced from HALOE and
balloon measurments in the arctic during the winter of 1999-2000. J. Geophys.Res., vol. 108(D5), 10.1029/2001JD001423, 2002.
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DOI ]
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[1]
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Arvelius, J., S. Roslin, H. Nilsson and S. Kirkwood: Adsorption
efficiency of a molecular sieve in low pressure. In: Proceedings of
the XX quadrennial ozone symposium, C. Zerefos, ed., pp. 515-516
(International Ozone Commission), 2004.
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DESCARTES is a balloon-borne grab-sampler instrument
sampling stratospheric trace gases. Sampling and
pre-concentration is done by adsorption traps and
analysis by gas chromatography. In order to get good
focusing for the chromatography the traps should be
as small as possible and the lower limit is set by
the breakthrough of the adsorbate during
sampling. This study focuses on the adsorption
behaviour of these traps under different
circumstances. The results show that simple theory
does not explain adsorption at high flow speed.
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[2]
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Hooper, D., J. Arvelius and K. Stebel: Retrieval of atmospheric static
stability from radar return signal power. In: Proceedings of MST10,
13-20 May 2003, Piura, Peru, 2003.
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[3]
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Arvelius, Johan, H. Nilsson, S. Kirkwood, A. Robinson, N. Harris, J. Pyle,
O. Morgenstern, F. Goutail and J.-P. Pommereau: Measured tracer
profiles from the polar stratosphere covering all seasons 2000. In:
Proceedings of the Sixth European workshop on stratospheric ozone,
N. R. P Harris, G. T. Amanatidis and J. G. Levine, eds., no. 79 in Air
Pollution Research Report, pp. 217-220 (European Commission), 2002.
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DESCARTES is a lightweight balloon-borne
grab-sampler instrument for the long-lived chemical
tracer CFC-11 developed at the University of
Cambridge. From Dec 3, 1999 and throughout 2000 it
made 15 flights from Esrange and Andø
ya. Simultaneous balloon-borne ozone measurements
were made during most flights. The evolution of the
polar airmass over the whole year is studied from
these flights and compared to model profiles at
Kiruna and other subsidence studies.
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[4]
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Arvelius, Johan, Hans Nilsson, Sheila Kirkwood, François Danis, Neil R.P.
Harris and John A. Pyle: CFC measurements with DESCARTES during
the THESEO campaign in Kiruna spring 1999. In: Proceedings of the
Fifth European workshop on stratospheric ozone, N. R. P Harris, M. Guirlet
and G. T. Amanatidis, eds., no. 73 in Air Pollution Research Report, pp.
459-462 (European Commission), ISBN 92-827-5672-6, 2000.
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DESCARTES is a lightweight instrument for in-situ
measurements of long-lived stratospheric tracers
from balloons. The instrument is designed to fly
piggyback on other payloads; it weighs 16kg and
there is no need for telemetry. The instrument
collects samples by letting a measured amount of air
pass though a tube containing a carboxen
adsorbent. The instrument can measure CFC-11,
CFC-113, CCl4 and CH3CCl3
quantitatively. Results from the four flights with
DESCARTES during the THESEO-O3-loss campaign in
the spring of 1999 are presented.
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[5]
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Hooper, D. A. and J. Arvelius: Monitoring of the arctic winter
tropopause: A comparison of radiosonde, ozonesonde and MST radar
observations. In: Proceedings of the Ninth International Workshop on
Technical and Scientific Aspects of MST Radar, combined with COST76 Final
Profiler Workshop, 2000.
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[6]
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Arvelius, Johan, Hans Nilsson, Sheila Kirkwood, François Danis, Neil R. P.
Harris and John A. Pyle: CFC measurements with DESCARTES during
the THESEO campaign in Kiruna spring 1999 - early results. In:
Proceedings 14th ESA Symposium on Rocket and Balloon Programmes and
Related Research, B. Kaldeich-Schürmann, ed., no. 437 in SP, pp.
353-358, Eurpoean Space Agency (ESA Publications Division), 1999.
[ bib |
.pdf ]
DESCARTES is a lightweight instrument for in-situ
measurements of long-lived stratospheric tracers
from balloons. The instrument is designed to fly
piggyback on other payloads; it weighs 16kg and
there is no need for telemetry. The instrument
collects samples by letting a measured amount of air
pass though a tube containing a carboxen
adsorbent. The instrument can measure CFC-11 and
CFC-113 quantitatively, CCl4 and CH3CCl3 is
adsorbed and might give quantitative results after
further laboratory analysis. Preliminary results
from the four flights with DESCARTES during the
THESEO-O3-loss campaign in the spring of 1999 are
presented.
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[7]
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Pommereau, J. P., F. Goutail, I. Pundt, J. A. Pyle, F. Danis, G. Hansford,
R. Freshwater, A. Robinson, R. L. Jones, N. R. P. Harris, A. Adriani,
F. Cairo, L. Pulvirenti, G. Difrancesco, S. Kirkwood, H. Nilsson,
J. Arvelius, P. Woods, N. R. Swann, I. H. Howeison, S. Garcelon, T. D.
Gardiner, T. Deshler and A. Buivan: Small balloons for stratospheric
ozone research and satellite validation. In: Proceedings 14th ESA
Symposium on Rocket and Balloon Programmes and Related Research,
B. Kaldeich-Schürmann, ed., no. 437 in SP, pp. 609-614, Eurpoean Space
Agency (ESA Publications Division), 1999.
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