Height-latitude structure of the vertical wind in the upper mesosphere and lower thermosphere (70–110 km)

Author:

Portnyagin Yu. I.,Solov’eva T. V.,Merzlyakov E. G.,Pogorel’tsev A. I.,Savenkova E. N.

Publisher

Pleiades Publishing Ltd

Subject

Atmospheric Science,Oceanography

Reference18 articles.

1. Yu. I. Portnyagin and T. V. Solov’eva, “Regular Motions in the Mesopausal-Lower Thermospheric Area,” Geomagn. Aeron. 22(2), 229–232 (1982).

2. Yu. I. Portnyagin and T. V. Solov’eva, “Height-Latitude Structure of Fields of Meridional and Vertical Widns in the Mesopause-Lower Thermosphere Area,” Meteorol. Gidrol., No. 9, 25–30 (1985).

3. V. Fauliot, G. Thuiller, and F. Vial, “Mean Vertical Wind in the Mesosphere-Lower Thermosphere Area (80–120 km) Deduced from the WINDII Observations on Board UARS,” Ann. Geophys. 15, 1221–1231 (1997).

4. Portnyagin et al. “Mesosphere Lower Thermosphere Prevailing Wind Model,” Adv. Space Res. 34, 1755–1762 (2004).

5. Xun Zhu, et al., “An Algorithm for Extracting Zonal Mean and Migrating Tidal Fields in the Middle Atmosphere from space-based Measurements: Applications to TIMED/SABER-Measured Temperature and Tidal Modeling,” J. Geophys. Res. 110 D02105, 1–14 (2005).

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