scholarly journals Quality Evaluation of Wind Vectors from UHF Wind Profiler using Radiosonde Measurements

2015 ◽  
Vol 24 (1) ◽  
pp. 133-150 ◽  
Author(s):  
Kwang-Ho Kim ◽  
Min-Seong Kim ◽  
Seong-Woon Seo ◽  
Park-Sa Kim ◽  
Dong-Hwan Kang ◽  
...  
2000 ◽  
Author(s):  
Chaiwat Somboonlarp ◽  
Nipha Leelaruji ◽  
Narong Hemmakorn ◽  
Apinan Manyanon ◽  
Yuichi Ohno

2002 ◽  
Vol 103 (3) ◽  
pp. 361-389 ◽  
Author(s):  
Sandra Jacoby-Koaly ◽  
B. Campistron ◽  
S. Bernard ◽  
B. Bénech ◽  
F. Ardhuin-Girard ◽  
...  

2001 ◽  
Vol 129 (8) ◽  
pp. 1968-1986 ◽  
Author(s):  
Gregor S. Lehmiller ◽  
Howard B. Bluestein ◽  
Paul J. Neiman ◽  
F. Martin Ralph ◽  
Wayne F. Feltz

2007 ◽  
Vol 69 (4-5) ◽  
pp. 419-430 ◽  
Author(s):  
Madhu Chandra Reddy Kalapureddy ◽  
K. Kishore Kumar ◽  
V. Sivakumar ◽  
A.K. Ghosh ◽  
A.R. Jain ◽  
...  

2012 ◽  
Vol 5 (3) ◽  
pp. 4447-4472 ◽  
Author(s):  
T. V. Chandrasekhar Sarma ◽  
P. Srinivasulu ◽  
T. Tsuda

Abstract. A UHF wind profiler operating at 1280 MHz has been developed at NARL for atmospheric studies in the planetary boundary layer. In order to explore application of radio acoustic sounding system (RASS) technique to this profiler, a suitable acoustic attachment was designed and preliminary experiments were conducted on 27–30 August 2010. Height profiles of virtual temperature, Tv, in the planetary boundary layer were derived with 1 μs and 0.25 μs pulse transmission, corresponding to a height resolution of 150 m and about 40 m, respectively. Diurnal variation of Tv is clearly recognized, and perturbations of Tv are also seen in association with a precipitation event. Simultaneous profiles obtained from the MST Radar-RASS and an onsite 50 m tower demonstrate the capability to continuously profile the atmospheric temperature from near the ground to upper tropospheric altitudes.


2009 ◽  
Vol 26 (9) ◽  
pp. 1940-1955 ◽  
Author(s):  
Michihiro S. Teshiba ◽  
Phillip B. Chilson ◽  
Alexander V. Ryzhkov ◽  
Terry J. Schuur ◽  
Robert D. Palmer

Abstract A method is presented by which combined S-band polarimetric weather radar and UHF wind profiler observations of precipitation can be used to extract the properties of liquid phase hydrometeors and the vertical velocity of the air through which they are falling. Doppler spectra, which contain the air motion and/or fall speed of hydrometeors, are estimated using the vertically pointing wind profiler. Complementary to these observations, spectra of rain drop size distribution (DSD) are simulated by several parameters as related to the DSD, which are estimated through the two polarimetric parameters of radar reflectivity (ZH) and differential reflectivity (ZDR) from the scanning weather radar. These DSDs are then mapped into equivalent Doppler spectra (fall speeds) using an assumed relationship between the equivolume drop diameter and the drop’s terminal velocity. The method is applied to a set of observations collected on 11 March 2007 in central Oklahoma. In areas of stratiform precipitation, where the vertical wind motion is expected to be small, it was found that the fall speeds obtained from the spectra of the rain DSD agree well with those of the Doppler velocity estimated with the profiler. For those cases when the shapes of the Doppler spectra are found to be similar in shape but shifted in velocity, the velocity offset is attributed to vertical air motion. In convective rainfall, the Doppler spectra of the rain DSD and the Doppler velocity can exhibit significant differences owing to vertical air motions together with atmospheric turbulence. Overall, it was found that the height dependencies of Doppler spectra measured by the profiler combined with vertical profiles of Z, ZDR, and the cross correlation (ρHV) as well as the estimated spectra of raindrop physical terminal fall speeds from the polarimetric radar provide unique insight into the microphysics of precipitation. Vertical air motions (updrafts/downdrafts) can be estimated using such combined measurements.


2016 ◽  
Vol 25 (2) ◽  
pp. 267-280
Author(s):  
Kwang-Ho Kim ◽  
◽  
Park-Sa Kim ◽  
Min-Seong Kim ◽  
Dong-Hwan Kang ◽  
...  

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