Identification of large-scale billow-like structure in the neutral sodium layer over Arecibo

We present a rare event that was recorded over Arecibo using sodium (Na) lidar. Billow‐like structures with periods of ∼60 min were seen in the Na layer above 102 km on the night of 7–8 July 2010. The absence of any high‐altitude structure was noted on the following night. Spectral analysis using th...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Journal of Geophysical Research: Space Physics 2012-10, Vol.117 (A10), p.n/a
Hauptverfasser: Sarkhel, S., Raizada, Shikha, Mathews, John D., Smith, Steve, Tepley, Craig A., Rivera, Francisco J., Gonzalez, Sixto A.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:We present a rare event that was recorded over Arecibo using sodium (Na) lidar. Billow‐like structures with periods of ∼60 min were seen in the Na layer above 102 km on the night of 7–8 July 2010. The absence of any high‐altitude structure was noted on the following night. Spectral analysis using the Lomb‐Scargle technique reveals periods with larger power on the first night as compared to the adjacent one. The keograms derived from a sequence of 557.7 nm airglow images show the passage of a large frontal wave on 7–8 July 2010. Further investigation on the occurrence of neutral instabilities was carried out using mesospheric temperature and horizontal wind obtained from the Sounding of Atmosphere using Broadband Emission Radiometry (SABER) and TIMED Doppler Interferometer (TIDI) instruments onboard the TIMED satellite. A good agreement is observed between the temperatures derived from SABER and ground‐based airglow instruments. The mesospheric temperature and horizontal wind profiles allowed the determination of square of the Brunt‐Väisälä frequency and Richardson number to quantitatively evaluate the possible role of different instabilities in generating this structure. The profile of the former entity reveals that the region is convectively stable during the time when the event was observed. However, the presence of strong shears in the region, where billow‐like structures are observed on 7–8 July 2010, is noted along with a Richardson number of 0.22, indicating the likely occurrence of dynamical instability. Thus, the present work suggests that dynamical instability make conditions conducive for billow‐like structures in the Na layer above 102 km. The possible role of plasma processes in generating these structures is also discussed. Key Points Identification of high altitude billow‐like structure in Na layer Dynamical instability is the cause for generating this structure Apparently, plasma is not playing any role in creating this structure
ISSN:0148-0227
2169-9380
2156-2202
2169-9402
DOI:10.1029/2012JA017891