Lidar measurements of gravity wave saturation effects in the sodium layer

1985 ◽  
Vol 12 (11) ◽  
pp. 765-768 ◽  
Author(s):  
C. S. Gardner ◽  
D. G. Voelz
2015 ◽  
Vol 8 (11) ◽  
pp. 4645-4655 ◽  
Author(s):  
B. Ehard ◽  
B. Kaifler ◽  
N. Kaifler ◽  
M. Rapp

Abstract. This study evaluates commonly used methods of extracting gravity-wave-induced temperature perturbations from lidar measurements. The spectral response of these methods is characterized with the help of a synthetic data set with known temperature perturbations added to a realistic background temperature profile. The simulations are carried out with the background temperature being either constant or varying in time to evaluate the sensitivity to temperature perturbations not caused by gravity waves. The different methods are applied to lidar measurements over New Zealand, and the performance of the algorithms is evaluated. We find that the Butterworth filter performs best if gravity waves over a wide range of periods are to be extracted from lidar temperature measurements. The running mean method gives good results if only gravity waves with short periods are to be analyzed.


2020 ◽  
Vol 13 (2) ◽  
pp. 479-499
Author(s):  
Irina Strelnikova ◽  
Gerd Baumgarten ◽  
Franz-Josef Lübken

Abstract. An advanced hodograph-based analysis technique to derive gravity-wave (GW) parameters from observations of temperature and winds is developed and presented as a step-by-step recipe with justification for every step in such an analysis. As the most adequate background removal technique the 2-D FFT is suggested. For an unbiased analysis of fluctuation whose amplitude grows with height exponentially, we propose applying a scaling function of the form exp (z∕(ςH)), where H is scale height, z is altitude, and the constant ς can be derived by a linear fit to the fluctuation profile and should be in the range 1–10. The most essential part of the proposed analysis technique consists of fitting cosine waves to simultaneously measured profiles of zonal and meridional winds and temperature and subsequent hodograph analysis of these fitted waves. The linear wave theory applied in this analysis is extended by introducing a wave packet envelope term exp⁡(-(z-z0)2/2σ2) that accounts for limited extent of GWs in the observational data set. The novelty of our approach is that its robustness ultimately allows for automation of the hodograph analysis and resolves many more GWs than can be inferred by the manually applied hodograph technique. This technique allows us to unambiguously identify upward- and downward-propagating GWs and their parameters. This technique is applied to unique lidar measurements of temperature and horizontal winds measured in an altitude range of 30 to 70 km.


2016 ◽  
Vol 59 (8) ◽  
pp. 1707-1708 ◽  
Author(s):  
Xiao Liu ◽  
JiYao Xu

2018 ◽  
Vol 53 ◽  
pp. 01016
Author(s):  
Xiaodong Wang ◽  
Fan Yi

Based on the 6-s resolution Na lidar measurements during ~395 hours on 47 different nights from May to November 2011 in Beijing(40.2°N, 116°E), China, it was found that the Na density at altitude 83-98 km always exhibited strong short-term fluctuations. The magnitude of the mean absolute increasing and decreasing rates for these short-term fluctuations ranged from ~8 to ~16 cm-3s-1. Their profiles were close to each other with the increasing rate being slightly larger than that of decreasing rate at most altitudes. This difference coincided with the earlier observations that the Na layer column abundance mostly tends to have a slow net increase during night [2]. The characteristic time for the short-term Na density fluctuations had a magnitude ranging from 46 to 118 s at altitudes between 83 and 98 km, which was apparently shorter than the Brunt-Väisälä period (~5 min). The gravity wave seems difficultly to induce observed Na fluctuations.


1987 ◽  
Vol 92 (A8) ◽  
pp. 8781 ◽  
Author(s):  
K. H. Kwon ◽  
C. S. Gardner ◽  
D. C. Senft ◽  
F. L. Roesler ◽  
J. Harlander

2014 ◽  
Vol 32 (11) ◽  
pp. 1395-1405 ◽  
Author(s):  
B. Ehard ◽  
P. Achtert ◽  
J. Gumbel

Abstract. This paper presents an analysis of gravity wave activity over northern Sweden as deduced from 18 years of wintertime lidar measurements at Esrange (68° N, 21° E). Gravity wave potential energy density (GWPED) was used to characterize the strength of gravity waves in the altitude regions 30–40 km and 40–50 km. The obtained values exceed previous observations reported in the literature. This is suggested to be due to Esrange's location downwind of the Scandinavian mountain range and due to differences in the various methods that are currently used to retrieve gravity wave parameters. The analysis method restricted the identification of the dominating vertical wavelengths to a range from 2 to 13 km. No preference was found for any wavelength in this window. Monthly mean values of GWPED show that most of the gravity waves' energy dissipates well below the stratopause and that higher altitude regions show only small dissipation rates of GWPED. Our analysis does not reproduce the previously reported negative trend in gravity wave activity over Esrange. The observed inter-annual variability of GWPED is connected to the occurrence of stratospheric warmings with generally lower wintertime mean GWPED during years with major stratospheric warmings. A bimodal GWPED occurrence frequency indicates that gravity wave activity at Esrange is affected by both ubiquitous wave sources and orographic forcing.


1982 ◽  
Vol 30 (2) ◽  
pp. 169-177 ◽  
Author(s):  
C. Granier ◽  
G. Megie

Sign in / Sign up

Export Citation Format

Share Document