Mesosphere/lower thermosphere prevailing wind model

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dc.contributor.author Portnyagin, Yu.
dc.contributor.author Solovjova, T.
dc.contributor.author Merzlyakov, E.
dc.contributor.author Forbes, J.
dc.contributor.author Palo, S.
dc.contributor.author Ortland, D.
dc.contributor.author Hocking, W.
dc.contributor.author MacDougall, J.
dc.contributor.author Thayaparan, T.
dc.contributor.author Manson, A.
dc.contributor.author Meek, C.
dc.contributor.author Hoffmann, P.
dc.contributor.author Singer, W.
dc.contributor.author Mitchell, N.
dc.contributor.author Pancheva, D.
dc.contributor.author Igarashi, K.
dc.contributor.author Murayama, Y.
dc.contributor.author Jacobi, Ch.
dc.contributor.author Kuerschner, D.
dc.contributor.author Fahrutdinova, A.
dc.contributor.author Korotyshkin, D.
dc.contributor.author Clark, R.
dc.contributor.author Taylor, M.
dc.contributor.author Franke, S.
dc.contributor.author Fritts, D.
dc.contributor.author Tsuda, T.
dc.contributor.author Nakamura, T.
dc.contributor.author Gurubaran, S.
dc.contributor.author Rajaram, R.
dc.contributor.author Vincent, R.
dc.contributor.author Kovalam, S.
dc.contributor.author Batista, P.
dc.contributor.author Poole, G.
dc.contributor.author Malinga, S.
dc.contributor.author Fraser, G.
dc.contributor.author Murphy, D.
dc.contributor.author Riggin, D.
dc.contributor.author Aso, T.
dc.contributor.author Tsutsumi, M.
dc.date.accessioned 2024-04-16T08:04:12Z
dc.date.available 2024-04-16T08:04:12Z
dc.date.issued 2004
dc.identifier.citation Advances in Space Research Volume 34, Issue 8, 2004, Pages 1755-1762, https://doi.org/10.1016/j.asr.2003.04.058 en_US
dc.identifier.uri http://library.iigm.res.in:8080/xmlui/handle/123456789/1844
dc.description.abstract The mesosphere/lower thermosphere (MLT) wind data from the 46 ground-based (GB) MF and meteor radar (MR) stations, located at the different latitudes over the globe, and the space-based (SB) HRDI data were used for constructing of the empirical global climatic 2-D prevailing wind model at 80–100 km heights for all months of the year. The main data set is obtained during 1990–2001 period. It is shown that the three datasets (MF, MR, HRDI) are mainly well correlated. However, a certain systematic bias between the GB and SB data at 96 km exists, as well as that between the MF and MR data higher 88 km. Simple correction factors are proposed to minimize these biases. The 2-D distant-weighted least-square interpolation procedure for some arbitrary collection of points was used for drawing model contour plots. The model is available in the computer readable form and may be used for construction of the new CIRA model. en_US
dc.language.iso en en_US
dc.subject Mesosphere/lower thermosphere (MLT) en_US
dc.subject Prevailing wind model en_US
dc.title Mesosphere/lower thermosphere prevailing wind model en_US
dc.type Article en_US


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