Gravity wave instability structures and turbulence from more than 1.5 years of OH* airglow imager observations in Slovenia

• Published in: Atmospheric Measurement Techniques
• Main Authors: R. Sedlak, P. Hannawald, C. Schmidt, S. Wüst, M. Bittner, S. Stanič
• Format: Article
• Language: English
• Published: Copernicus Publications 2021-10-01
• Online Access: https://amt.copernicus.org/articles/14/6821/2021/amt-14-6821-2021.pdf
• ISSN: 1867-1381; 1867-8548

<p>We analysed 286 nights of data from the OH* airglow imager FAIM 3 (Fast Airglow IMager) acquired at Otlica Observatory (45.93<span class="inline-formula">^∘</span> N, 13.91<span class="inline-formula">^∘</span> E), Slovenia, between 26 October 2017 and 6 June 2019. Measurements have been performed with a spatial resolution of 24 m per pixel and a temporal resolution of 2.8 s.</p> <p>A two-dimensional fast Fourier transform is applied to the image data to derive horizontal wavelengths between 48 m and 4.5 km in the upper mesosphere/lower thermosphere (UMLT) region. In contrast to the statistics of larger-scale gravity waves (horizontal wavelength up to ca. 50 km; Hannawald et al., 2019), we find a more isotropic distribution of directions of propagation, pointing to the presence of wave structures created above the stratospheric wind fields. A weak seasonal tendency of a majority of waves propagating eastward during winter may be due to instability features from breaking secondary gravity waves that were created in the stratosphere. We also observe an increased southward propagation during summer, which we interpret as an enhanced contribution of secondary gravity waves created as a consequence of primary wave filtering by the meridional mesospheric circulation.</p> <p>We present multiple observations of turbulence episodes captured by our high-resolution airglow imager and estimated the energy dissipation rate in the UMLT from image sequences in 25 cases. Values range around 0.08 and 9.03 W kg<span class="inline-formula">⁻¹</span> and are on average higher than those in recent literature. The values found here would lead to an approximated localized maximum heating of 0.03–3.02 K per turbulence event. These are in the same range as the daily chemical heating rates for the entire atmosphere reported by Marsh (2011), which apparently stresses the importance of dynamical energy conversion in the UMLT.</p>