Quantification of waves in lidar observations of noctilucent clouds at scales from seconds to minutes

• Main Authors: Kaifler, N., Baumgarten, G., Fiedler, J.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Göttingen : Copernicus 2013
• Subjects: amplitude; brightness temperature; displacement; gravity wave; lidar; Mie theory; polar mesospheric cloud; Raman spectroscopy; Rayleigh wave; Norway; 550; Alomar; Northern Norway
• Online Access: https://doi.org/10.34657/4267; https://oa.tib.eu/renate/handle/123456789/5638

We present small-scale structures and waves observed in noctilucent clouds (NLC) by lidar at an unprecedented temporal resolution of 30 s or less. The measurements were taken with the Rayleigh/Mie/Raman lidar at the ALOMAR observatory in northern Norway (69 N) in the years 2008-2011. We find multiple layer NLC in 7.9% of the time for a brightness threshold of δ β 12 × 10-10 m-1 sr-1. In comparison to 10 min averaged data, the 30 s dataset shows considerably more structure. For limited periods, quasi-monochromatic waves in NLC altitude variations are common, in accord with ground-based NLC imagery. For the combined dataset, on the other hand, we do not find preferred periods but rather significant periods at all timescales observed (1 min to 1 h). Typical wave amplitudes in the layer vertical displacements are 0.2 km with maximum amplitudes up to 2.3 km. Average spectral slopes of temporal altitude and brightness variations are-2.01 ± 0.25 for centroid altitude,-1.41 ± 0.24 for peak brightness and-1.73 ± 0.25 for integrated brightness. Evaluating a new single-pulse detection system, we observe altitude variations of 70 s period and spectral slopes down to a scale of 10 s. We evaluate the suitability of NLC parameters as tracers for gravity waves. publishedVersion