Semi-empirical model of middle atmosphere wind from the ground to the lower thermosphere

被引：22

作者：

Jacobi, Ch. ^{[1
]}

Froehlich, K. ^{[2
]}

Portnyagin, Y. ^{[3
]}

Merzlyakov, E. ^{[3
]}

Solovjova, T. ^{[3
]}

Makarov, N. ^{[3
]}

Rees, D. ^{[4
]}

Fahrutdinova, A. ^{[5
]}

Guryanov, V. ^{[5
]}

Fedorov, D. ^{[5
]}

Korotyshkin, D. ^{[5
]}

Forbes, J. ^{[6
]}

Pogoreltsev, A. ^{[7
]}

Kuerschner, D. ^{[1
]}

机构：

[1] Univ Leipzig, Inst Meteorol, D-04103 Leipzig, Germany

[2] Business Area Res & Dev, D-63067 Offenbach, Germany

[3] Inst Expt Meteorol, Obninsk 249020, Kaluga Region, Russia

[4] Hovemere Ltd, Tonbridge, Kent, England

[5] Kazan VI Lenin State Univ, Dept Phys, Kazan 420008, Russia

[6] Univ Colorado, Dept Aerosp Engn Sci, Boulder, CO 80309 USA

[7] Russian State Hydrometeorol Univ, Dept Meteorol Forecasts, St Petersburg 195196, Russia

来源：

ADVANCES IN SPACE RESEARCH | 2009年 / 43卷 / 02期

关键词：

Winds; Middle atmosphere; Lower thermosphere; Semi-empirical model; RESOLUTION DOPPLER IMAGER/UARS; DIURNAL MIGRATING TIDE; MF RADAR OBSERVATIONS; MESOSPHERE/LOWER THERMOSPHERE; SEMIDIURNAL TIDE; SEASONAL-VARIATIONS; EMPIRICAL WIND; UARS; MLT; SATELLITE;

D O I：

10.1016/j.asr.2008.05.011

中图分类号：

V [航空、航天];

学科分类号：

08 ; 0825 ;

摘要：

During recent years, special attention has been paid to understanding the background circulation of the middle atmosphere. Particularly in the mesosphere/lower thermosphere (MLT) region, this has involved including data from a range of new radar measurements. It has also involved the comparison of existing empirical middle atmosphere wind models, such as CIRA-86 and HWM-93 to the new data. This has led to the construction of empirical models of MLT winds such as the Global Empirical Wind Model (GEWM). Further investigations are aimed at the construction of new empirical and semi-empirical wind models of the entire middle atmosphere including these new experimental results. The results Of a new wind climatology (0-100 km) are presented here, based upon the GEWM, a reanalysis of stratospheric data, and a numerical model which is used to fill the gap between data from the stratospheric and MLT regions. (C) 2008 COSPAR. Published by Elsevier Ltd. All rights reserved.

引用

页码：239 / 246

页数：8

共 35 条

[1] Barnet J.J., 1985, Handbook for MAP, 16: Atmospheric structure and its variation in the region 20-120 km: Draft of a new reference middle atmosphere, P47
[2] LATITUDE AND SEASONAL DEPENDENCE OF THE SEMIDIURNAL TIDE OBSERVED BY THE HIGH-RESOLUTION DOPPLER IMAGER
BURRAGE, MD
WU, DL
SKINNER, WR
ORTLAND, DA
HAYS, PB
[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1995, 100 (D6) : 11313 - 11321
[3] *COLE AE, 1972, CIRA72 COSPAR INT RE
[4] Planetary wave activity and rotational effects in the mid-latitudes of the lower and middle atmosphere (0-100km).
Fahrutdinova, AN
Guryanov, VV
Korotyshkin, DV
Manson, AH
Meek, CE
Jacobi, C
Kürschner, D
[J]. MIDDLE ATMOSPHERE STRUCTURE AND DYNAMICS, 2003, 32 (05): : 869 - 874
[5] Fauliot V, 1997, ANN GEOPHYS-ATM HYDR, V15, P1221
[6] Fleming E. L., 1990, Advances in Space Research, V10, P11, DOI 10.1016/0273-1177(90)90386-E
[7] Climatological mean wind observations from the UARS high-resolution Doppler imager and wind imaging interferometer: Comparison with current reference models
Fleming, EL
Chandra, S
Burrage, MD
Skinner, WR
Hays, PB
Solheim, BH
Shepherd, GG
[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D6) : 10455 - 10473
[8] SEMIDIURNAL TIDE IN THE 80-150 KM REGION - AN ASSIMILATIVE DATA-ANALYSIS
FORBES, JM
MANSON, AH
VINCENT, RA
FRASER, GJ
VIAL, F
WAND, R
AVERY, SK
CLARK, RR
JOHNSON, R
ROPER, R
SCHMINDER, R
TSUDA, T
KAZIMIROVSKY, ES
[J]. JOURNAL OF ATMOSPHERIC AND TERRESTRIAL PHYSICS, 1994, 56 (10): : 1237 - 1249
[9] Planetary wave transience effects on the zonal mean flow:: simulations with the COMMA-LIM model
Fröhlich, K
Jacobi, C
Pogoreltsev, AI
[J]. COUPLING PROCESSES IN THE MLT REGION, 2005, 35 (11): : 1900 - 1904
[10] GROVES GV, 1969, JBIS-J BRIT INTERPLA, V22, P285

← 1 2 3 4 →