Shear-Flow Instability in the Stable Nocturnal Boundary Layer as Observed by Doppler Lidar during CASES-99

By R. Newsom, R. Banta. 2003

160 citations recorded by the source corpus.

Subfields: Atmospheric Science, Environmental Engineering, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/f2f153194eeb73306139df466e788e3364c45b68

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Citations in the corpus

The structure of the near neutral atmospheric surface layer as observed during the CASES'99 experiment (2004, methodology): “2002) and properties of a shear-instability wave event (Newsom and Banta 2003).”
Stable-boundary-layer regimes from the perspective of the low-level jet (2008, methodology): “…propagating gravity-wave and density-current activity (18 October 1999: Sun et al. 2002, 2004), and another night with a 9 m s-1 jet was interrupted by a traveling shear-instability (Kelvin–Helmholtz-type) wave packet (5 October 1999: Blumen et al. 2001, Poulos et al. 2002, Newsom and Banta 2003).”
Turbulence Regimes and Turbulence Intermittency in the Stable Boundary Layer during CASES-99 (2012, unknown): “In addition to these two regimes, moderate turbulence is often generated above the observation level and diffuses downward, such as the case analyzed by Blumen et al. (2001) and Newsom and Banta (2003).”
Turbulent Velocity-Variance Profiles in the Stable Boundary Layer Generated by a Nocturnal Low-Level Jet (2006, background): “However, as pointed out in Newsom and Banta (2003), scan data were sometimes tilted as a result of topographic slope effects, and sometimes the Lamar data indicated dips or humps in the jet maximum across a scan, which were probably also related to local topography.”
An Analysis of the Performance of the UFAM Pulsed Doppler Lidar for Observing the Boundary Layer (2009, background): “In addition, long-term observations of the dynamics and particulate levels in urban and rural environments offer a valuable climatological record with uses in predicting and analyzing phenomena such as convection, waves, dispersion of pollution, wind resource availability, and mesoscale meteorology ”
Atmospheric Disturbances that Generate Intermittent Turbulence in Nocturnal Boundary Layers (2004, methodology): “, 1998), a scanning High Resolution Doppler Lidar (HRDL) (Wulfmeyer et al., 2000; Grund et al., 2001; Banta et al., 2002; Newsom and Banta, 2003), a Tethered Lifting System (TLS) (Balsley et al.”