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contributor authorZhu, Xun
date accessioned2017-06-09T14:29:35Z
date available2017-06-09T14:29:35Z
date copyright1990/03/01
date issued1989
identifier issn0022-4928
identifier otherams-20289.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4156500
description abstractA new algorithm for calculating CO2 15-?m band cooling rate is suggested following a similar idea proposed by Fels and Schwarzkopf in 1981. Since the Curtis matrix is more useful in cooling rate calculations, we show in this paper that it is possible to calculate the Curtis matrix by direct interpolation with precomputed Curtis matrices. The algorithm is applied to the calculation of the CO2 15-?m band cooling rate in the upper-middle atmosphere (64?106 km). The stored Curtis matrices are off-line computed by escape functions with an appropriate treatment of the nearby layer calculations. These escape functions are calculated by line-by-line integrations. With precomputed Curtis Matrices an accurate atmospheric cooling rate by CO2 can be calculated more objectively than with transmission functions. A multi-energy-level model to treat the non-LTE problem in this region is also derived systematically. It is shown that when vibration?vibration (V?V) transitions are neglected cooling rate calculations of the multi-energy-level model could be approximated by the usual two-energy-level model with the revised ratio of relaxation rates. Since the complete solution of the non-LTE problem including V?V transitions requires tremendous amounts of computation time due to nonlinearity, it is suggested that such a two-energy-level model can be used in GCMs to approximate the total cooling rate by the whole band.
publisherAmerican Meteorological Society
titleCarbon Dioxide 15-μm Band Cooling Rates in the Upper Middle Atmosphere Calculated by Curtis Matrix Interpolation
typeJournal Paper
journal volume47
journal issue6
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1990)047<0755:CDBCRI>2.0.CO;2
journal fristpage755
journal lastpage774
treeJournal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 006
contenttypeFulltext


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