Multistatic meteor radar observations of gravity-wave–tidal interaction over southern Australia
Autor: | Iain M. Reid, Andrew D. MacKinnon, Andrew J. Spargo |
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Jazyk: | angličtina |
Rok vydání: | 2019 |
Předmět: |
Meteor (satellite)
Atmospheric Science 010504 meteorology & atmospheric sciences Meteoroid lcsh:TA715-787 lcsh:Earthwork. Foundations Forcing (mathematics) Geodesy 01 natural sciences law.invention lcsh:Environmental engineering Bistatic radar Amplitude law 0103 physical sciences Mesopause Astrophysics::Earth and Planetary Astrophysics Gravity wave Radar lcsh:TA170-171 010303 astronomy & astrophysics Geology 0105 earth and related environmental sciences |
Zdroj: | Atmospheric Measurement Techniques, Vol 12, Pp 4791-4812 (2019) |
ISSN: | 1867-8548 1867-1381 |
Popis: | This paper assesses the ability of a recently installed 55 MHz multistatic meteor radar to measure gravity-wave-driven momentum fluxes around the mesopause and applies it in a case study of measuring gravity wave forcing on the diurnal tide during a period following the autumnal equinox of 2018. The radar considered is in the vicinity of Adelaide, South Australia (34.9∘ S, 138.6∘ E), and consists of a monostatic radar and bistatic receiver separated by approximately 55 km. The assessment shows that the inclusion of the bistatic receiver reduces the relative uncertainty of the momentum flux estimate from about 75 % to 65 % (for a flux magnitude of ∼20 m2 s−2, 1 d's worth of integration, and for a gravity wave field synthesized from a realistic spectral model). This increase in precision appears to be entirely attributable to the increased number of meteor detections associated with the combined monostatic and bistatic receivers rather than changes in the meteors' spatial distribution. The case study reveals large modulations in the diurnal tidal amplitudes, with a maximum tidal amplitude of ∼50 m s−1 and an associated maximum zonal wind velocity of around 140 m s−1. While the observed gravity wave forcing exhibits a complex relationship with the tidal winds during this period, the components of the forcing are seen to be approximately out of phase with the tidal winds above 88 km. No clear phase relationship has been observed below 88 km. |
Databáze: | OpenAIRE |
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