Trace gas transport in the 1999/2000 Arctic winter: comparison of nudged GCM runs with observations

We have compared satellite and balloon observations of methane (CH<sub>4</sub>) and hydrogen fluoride (HF) during the Arctic winter 1999/2000 with results from the MA-ECHAM4 middle atmospheric general circulation model (GCM). For this purpose, the meteorology in the model was nudged t...

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Main Authors: M. K. van Aalst, M. M. P. van den Broek, A. Bregman, C. Brühl, B. Steil, G. C. Toon, S. Garcelon, G. M. Hansford, R. L. Jones, T. D. Gardiner, G. J. Roelofs, J. Lelieveld, P.J. Crutzen
Format: Article
Language:English
Published: Copernicus Publications 2004-01-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/4/81/2004/acp-4-81-2004.pdf
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author M. K. van Aalst
M. M. P. van den Broek
A. Bregman
C. Brühl
B. Steil
G. C. Toon
S. Garcelon
G. M. Hansford
R. L. Jones
T. D. Gardiner
G. J. Roelofs
J. Lelieveld
P.J. Crutzen
author_facet M. K. van Aalst
M. M. P. van den Broek
A. Bregman
C. Brühl
B. Steil
G. C. Toon
S. Garcelon
G. M. Hansford
R. L. Jones
T. D. Gardiner
G. J. Roelofs
J. Lelieveld
P.J. Crutzen
author_sort M. K. van Aalst
collection DOAJ
description We have compared satellite and balloon observations of methane (CH<sub>4</sub>) and hydrogen fluoride (HF) during the Arctic winter 1999/2000 with results from the MA-ECHAM4 middle atmospheric general circulation model (GCM). For this purpose, the meteorology in the model was nudged towards ECMWF analyses. This nudging technique is shown to work well for this middle atmospheric model, and offers good opportunities for the simulation of chemistry and transport processes. However, caution must be used inside the polar vortex, particularly late in the winter. The current study focuses on transport of HF and CH<sub>4</sub>, initialized with satellite measurements from the HALOE instrument aboard the UARS satellite. We have compared the model results with HALOE data and balloon measurements throughout the winter, and analyzed the uncertainties associated with tracer initialization, boundary conditions and the passive tracer assumption. This comparison shows that the model represents some aspects of the Arctic vortex well, including relatively small-scale features. However, while profiles outside the vortex match observations well, the model underestimates HF and overestimates CH<sub>4</sub> concentrations inside the vortex, particularly in the middle stratosphere. This problem is also evident in a comparison of vortex descent rates based upon vortex average tracer profiles from MA-ECHAM4, and various observations. This could be due to an underestimate of diabatic subsidence in the model, or due to too much mixing between vortex and non-vortex air.
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spelling doaj.art-b47b8b9d7ce743b380c469dddf5a95c32022-12-22T00:48:11ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242004-01-01418193Trace gas transport in the 1999/2000 Arctic winter: comparison of nudged GCM runs with observationsM. K. van AalstM. M. P. van den BroekA. BregmanC. BrühlB. SteilG. C. ToonS. GarcelonG. M. HansfordR. L. JonesT. D. GardinerG. J. RoelofsJ. LelieveldP.J. CrutzenWe have compared satellite and balloon observations of methane (CH<sub>4</sub>) and hydrogen fluoride (HF) during the Arctic winter 1999/2000 with results from the MA-ECHAM4 middle atmospheric general circulation model (GCM). For this purpose, the meteorology in the model was nudged towards ECMWF analyses. This nudging technique is shown to work well for this middle atmospheric model, and offers good opportunities for the simulation of chemistry and transport processes. However, caution must be used inside the polar vortex, particularly late in the winter. The current study focuses on transport of HF and CH<sub>4</sub>, initialized with satellite measurements from the HALOE instrument aboard the UARS satellite. We have compared the model results with HALOE data and balloon measurements throughout the winter, and analyzed the uncertainties associated with tracer initialization, boundary conditions and the passive tracer assumption. This comparison shows that the model represents some aspects of the Arctic vortex well, including relatively small-scale features. However, while profiles outside the vortex match observations well, the model underestimates HF and overestimates CH<sub>4</sub> concentrations inside the vortex, particularly in the middle stratosphere. This problem is also evident in a comparison of vortex descent rates based upon vortex average tracer profiles from MA-ECHAM4, and various observations. This could be due to an underestimate of diabatic subsidence in the model, or due to too much mixing between vortex and non-vortex air.http://www.atmos-chem-phys.net/4/81/2004/acp-4-81-2004.pdf
spellingShingle M. K. van Aalst
M. M. P. van den Broek
A. Bregman
C. Brühl
B. Steil
G. C. Toon
S. Garcelon
G. M. Hansford
R. L. Jones
T. D. Gardiner
G. J. Roelofs
J. Lelieveld
P.J. Crutzen
Trace gas transport in the 1999/2000 Arctic winter: comparison of nudged GCM runs with observations
Atmospheric Chemistry and Physics
title Trace gas transport in the 1999/2000 Arctic winter: comparison of nudged GCM runs with observations
title_full Trace gas transport in the 1999/2000 Arctic winter: comparison of nudged GCM runs with observations
title_fullStr Trace gas transport in the 1999/2000 Arctic winter: comparison of nudged GCM runs with observations
title_full_unstemmed Trace gas transport in the 1999/2000 Arctic winter: comparison of nudged GCM runs with observations
title_short Trace gas transport in the 1999/2000 Arctic winter: comparison of nudged GCM runs with observations
title_sort trace gas transport in the 1999 2000 arctic winter comparison of nudged gcm runs with observations
url http://www.atmos-chem-phys.net/4/81/2004/acp-4-81-2004.pdf
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