Physics
Scientific paper
Mar 1990
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990georl..17..525d&link_type=abstract
Geophysical Research Letters, Supplement (ISSN 0094-8276), vol. 17, March 1990, p. 525-528.
Physics
21
Arctic Regions, Atmospheric Composition, Ozonometry, Spatial Distribution, Stratosphere, Three Dimensional Models, Atmospheric Models, Temperature Distribution, Vorticity
Scientific paper
The success of three-dimensional simulations of stratospheric constituent variability depends critically on the initialization of the constituent fields within the global model. This paper describes a technique for generating global three-dimensional fields from vertical constituent proflies. The technique uses potential vorticity (q) and potential temperature (theta) to map the profiles onto the global domain. The profiles used here are obtained from a two-dimensional model calculation that reproduces the relationship between theta, q, N2O and O3 observed during the Airborne Arctic Stratospheric Expedition. The method is verified by comparison with satellite data, aircraft data, and model simulations.
Douglass Anne R.
Loewenstein Max
Margitan James J.
Podolske James R.
Proffitt Michael H.
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