Preliminary VHF radar and high-data-rate optical turbulence profile observations using a balloon-ring platform
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Wiley T. Black | Frank D. Eaton | Demos T. Kyrazis | G. D. Nastrom | Don G. Black | R. Alastair Black | F. Eaton | R. Black | D. Kyrazis | D. Black | W. Black | Gregory D. Nastrom
[1] Frank D. Eaton,et al. Radar and aircraft observations of a layer of strong refractivity turbulence , 1998, Defense, Security, and Sensing.
[2] K. S. Gage,et al. Vertical profiles of refractivity turbulence structure constant: Comparison of observations by the Sunset Radar with a new theoretical model , 1978 .
[3] Frank D. Eaton,et al. Middle atmosphere slant-path optical turbulence conditions derived from very high frequency radar observations , 1999 .
[4] G. D. Nastrom,et al. Persistent layers of enhanced C2N in the lower stratosphere from VHF radar observations , 2001 .
[5] R. Stephenson. A and V , 1962, The British journal of ophthalmology.
[6] Roy L. Lamberth,et al. Ambient Temperature Measurements from Radiosondes Flown on Constant-Level Balloons , 1966 .
[7] G. D. Nastrom,et al. Turbulence eddy dissipation rates from radar observations at 5-20 km at White Sands Missile Range, New mexico , 1997 .
[8] Helmut K. E. Tiefenau,et al. Influence of Meteorological Balloons on Temperature Measurements with Radiosondes: Nighttime Cooling and Daylight Heating , 1989 .
[9] G. D. Nastrom,et al. Onset of the summer monsoon over White Sands Missile Range, New Mexico, as seen by VHF radar , 1993 .
[10] G. D. Nastrom,et al. A Case Study of Atmospheric Conditions at 4-19 km over Vandenberg Air Force Base during Passage of a Cyclone , 2003 .
[11] G. D. Nastrom,et al. Variations of Winds and Turbulence Seen by the 50-MHz Radar at White Sands Missile Range, New Mexico , 1995 .
[12] Frank D. Eaton,et al. Preliminary estimates of the vertical profiles of inner and outer scales from White Sands Missile Range, New Mexico, VHF radar observations , 1998 .
[13] Frank D. Eaton,et al. A new frequency‐modulated continuous wave radar for studying planetary boundary layer morphology , 1995 .
[14] Frank D. Eaton,et al. Seasonal variation of gravity wave activity at 5–20 km observed with VHF radar at White Sands Missile Range, New Mexico , 2001 .
[15] Wiley T. Black,et al. The balloon ring: a high-performance low-cost instrumentation platform for measuring atmospheric turbulence profiles , 2009, Optical Engineering + Applications.
[16] Frank D. Eaton,et al. MST Radar Observations of Gravity Waves and Turbulence near Thunderstorms , 2002 .
[17] G. D. Nastrom,et al. The Coupling of Gravity Waves and Turbulence at White Sands, New Mexico, from VHF Radar Observations , 1993 .
[18] G. D. Nastrom,et al. The frequency of occurrence of quasi-monochromatic inertia-gravity waves in the lower stratosphere from MST radar observations , 2005 .
[19] G. D. Nastrom,et al. A brief climatology of eddy diffusivities over White Sands Missile Range, New Mexico , 1997 .
[20] G. D. Nastrom,et al. Seasonal variability of turbulence parameters at 2 to 21 km from MST radar measurements at Vandenberg Air Force Base, California , 2005 .
[21] Ronald J. Hugo,et al. Turbulence observations over a desert basin using a kite'tethered-blimp platform , 2000 .