TY - JOUR
T1 - Mesospheric Wind Estimation With the Jicamarca MST Radar Using Spectral Mainlobe Identification
AU - Lee, Kiwook
AU - Kudeki, Erhan
AU - Reyes, Pablo M.
AU - Lehmacher, Gerald A.
AU - Milla, Marco
N1 - We thank the staff and engineers of the Jicamarca Radio Observatory for their assistance with the observations. Jicamarca Observatory is operated by the Instituto Geofísico del Perú, with support from the National Science Foundation. This work was supported by the Aeronomy Program, Division of Atmospheric and Geospace Sciences of the NSF, through Grants AGS 0422661 and 1143523. Results from the entire set of MST‐ISR and MST‐ISR‐EEJ observations made at Jicamarca since 2005 are on display at this site ( http://remote1.ece.illinois.edu/MST_ISR/uvw.py ).
We thank the staff and engineers of the Jicamarca Radio Observatory for their assistance with the observations. Jicamarca Observatory is operated by the Instituto Geof?sico del Per?, with support from the National Science Foundation. This work was supported by the Aeronomy Program, Division of Atmospheric and Geospace Sciences of the NSF, through Grants AGS 0422661 and 1143523. Results from the entire set of MST-ISR and MST-ISR-EEJ observations made at Jicamarca since 2005 are on display at this site (http://remote1.ece.illinois.edu/MST_ISR/uvw.py).
PY - 2019/12/1
Y1 - 2019/12/1
N2 - MST (mesosphere, stratosphere, troposphere) radar observations at Jicamarca use four antenna beams, one vertical, others tilted to the east, west, and south, to detect the scattered pulse returns from mesospheric heights (∼55–85 km). Doppler shifts of scattered returns, estimated by fitting the observed signal spectra by generalized Gaussian-shaped models, are used to estimate mesospheric wind vectors. At some heights two spectral peaks are seen in which case a dual-peaked model is fitted the spectrum. Dual peaks are more common for returns from the east and west tilted beams with stronger sidelobes. When sidelobe-caused peaks are dominant and are mistaken for mainlobe peaks, wind errors occur since the estimation algorithm uses the pointing angle of the mainbeam. To avoid such errors we implemented a clustering-based machine learning procedure to identify and use only the mainbeam components of dual-peaked spectra. Wind estimates made before and after the procedure will be presented to assess the improvements achieved by this new method to be used routinely in Jicamarca mesospheric wind measurements and applied to past MST data.
AB - MST (mesosphere, stratosphere, troposphere) radar observations at Jicamarca use four antenna beams, one vertical, others tilted to the east, west, and south, to detect the scattered pulse returns from mesospheric heights (∼55–85 km). Doppler shifts of scattered returns, estimated by fitting the observed signal spectra by generalized Gaussian-shaped models, are used to estimate mesospheric wind vectors. At some heights two spectral peaks are seen in which case a dual-peaked model is fitted the spectrum. Dual peaks are more common for returns from the east and west tilted beams with stronger sidelobes. When sidelobe-caused peaks are dominant and are mistaken for mainlobe peaks, wind errors occur since the estimation algorithm uses the pointing angle of the mainbeam. To avoid such errors we implemented a clustering-based machine learning procedure to identify and use only the mainbeam components of dual-peaked spectra. Wind estimates made before and after the procedure will be presented to assess the improvements achieved by this new method to be used routinely in Jicamarca mesospheric wind measurements and applied to past MST data.
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U2 - 10.1029/2019RS006892
DO - 10.1029/2019RS006892
M3 - Article
AN - SCOPUS:85076228029
SN - 0048-6604
VL - 54
SP - 1222
EP - 1239
JO - Radio Science
JF - Radio Science
IS - 12
ER -