VHF radar measurements of momentum flux using summer polar mesopause echoes
Autor: | Rüdiger Rüster, Andrew J. Spargo, Peter Czechowsky, Iain M. Reid |
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Jazyk: | angličtina |
Rok vydání: | 2018 |
Předmět: |
010504 meteorology & atmospheric sciences
Polar mesosphere summer echoes Doppler radar lcsh:Geodesy Flux 010502 geochemistry & geophysics Momentum flux 01 natural sciences law.invention symbols.namesake law Sensitivity (control systems) Radar Very high-frequency radar Physics::Atmospheric and Oceanic Physics 0105 earth and related environmental sciences Physics Momentum (technical analysis) lcsh:QB275-343 Scattering lcsh:QE1-996.5 lcsh:Geography. Anthropology. Recreation Geology Computational physics lcsh:Geology lcsh:G Space and Planetary Science Mesopause symbols Doppler effect |
Zdroj: | Earth, Planets and Space, Vol 70, Iss 1, Pp 1-15 (2018) |
ISSN: | 1880-5981 |
DOI: | 10.1186/s40623-018-0902-9 |
Popis: | We revisit previously unpublished analysis of observations of the dynamics of the mesopause region over the Norwegian Island of Andoya (69°N, 16°E) made during a 1-week period in summer 1987 during the Middle Atmosphere Cooperation-Summer in Northern Europe (MAC-SINE) campaign using the mobile SOUSY VHF (53.5 MHz) Doppler radar operating in a six-beam mode. We do this in the light of: (1) more recent developments in the measurement of the components of the density-normalized Reynolds stress tensor using meteor radars, and with medium-frequency partial reflection radars using the hybrid Doppler interferometric technique, and (2) satellite measurements of the absolute upward flux of horizontal momentum. We consider of the density-normalized total upward flux of horizontal momentum $$\left( {\overline{{u^{\prime}w^{\prime}}} + \overline{{v^{\prime}w^{\prime}}} } \right)$$ for the 83–90 km height interval. Values of the component of the density-normalized flux for the 6 min to 12.8 h period range, after the tidal components have been removed, and the effects of the aspect sensitivity on the radar beam look directions have been accounted for vary between 5 m2 s−2 below 86 km and 13 m2 s−2 above 86 km. The major contribution is from the 6 to 12.8 h period range. The results of the analysis have implications for meteor radar estimates of momentum flux and also for Doppler radar measurements of the same term in the presence of aspect-sensitive scattering. |
Databáze: | OpenAIRE |
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