High-Resolution Doppler Lidar for Boundary Layer and Cloud Research

By C. Grund, R. Banta, Joanne George, J. Howell, M. Post, R. Richter, A. Weickmann. 2001

241 citations recorded by the source corpus.

Subfields: Earth-Surface Processes, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/0a91670ab062e8719605804cb1029e5be8f815b3

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Earth-Surface Processes

1. B. Galperin
2. A. Grachev
3. R. Banta

In Global and Planetary Change

1. R. Banta
2. Y. Pichugina
3. R. Newsom
4. Jielun Sun
5. B. Grisogono
6. B. Galperin
7. Xuhui Lee
8. A. Grachev

Citations in the corpus

• Intermittent Turbulence Associated with a Density Current Passage in the Stable Boundary Layer (2002, methodology): “Similar wave disturbances above density currents were also observed from numerical simulations of propagating internal bores by Klemp et al. (1997), from ambient shear flow on density currents by Liu and Moncrieff (1996), and from thunderstorm outflow by Droegemeier and Wilhelmson (1986).”
• Stable-boundary-layer regimes from the perspective of the low-level jet (2008, methodology): “One of the instruments deployed was the high-resolution Doppler lidar (HRDL) described by Grund et al. (2001) and Wulfmeyer et al. (2000).”
• High-energy 2μm Doppler lidar for wind measurements (2007, methodology): “Wind profiling with 2-μm lidar has already shown merit using low-energy (1-10 mJ) laser transmitters based on thulium.(1,2,3) And the addition of stronger energy lasers promises to boost the applicability of the coherent Doppler technique to farther distances and higher altitudes.”
• Turbulence Regimes and Turbulence Intermittency in the Stable Boundary Layer during CASES-99 (2012, unknown): “High-resolution Doppler lidar (HRDL), a scanning, coherent Doppler lidar system designed for atmospheric boundary layer research (Grund et al. 2001; Pichugina et al. 2008), was located 1.45 km southeast of the 60-m tower.”
• Review of wave‐turbulence interactions in the stable atmospheric boundary layer (2015, background): “With a horizontal scan, Doppler lidars are typically capable of making radial velocity measurements to distances from 1 to 10 km depending on the aerosol backscatter conditions [Grund et al., 2001; Pearson et al., 2009].”
• 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.”
• Relationship between Low-Level Jet Properties and Turbulence Kinetic Energy in the Nocturnal Stable Boundary Layer (2003, background): “For example, Mahrt (1987) found similar behavior for the vertical velocity variance calculated from aircraft data, although at a higher critical Ri.”