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    A Direct Method for Deriving Drop-Size Distribution and Vertical Air Velocities from VHF Doppler Radar Spectra 

    Source: Journal of Atmospheric and Oceanic Technology:;1986:;volume( 003 ):;issue: 004:;page 623
    Author(s): Wakasugi, Koichiro; Mizutani, Akiyoshi; Matsuo, Masaru; Fukao, Shoichiro; Kato, Susumu
    Publisher: American Meteorological Society
    Abstract: In precipitation environments, sensitive VHF Doppler radars have a capability to detect echoes from both refractive index irregularities and precipitation particles. The purpose of this paper is to propose a direct method ...
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    Further Discussion on Deriving Drop-Size Distribution and Vertical Air Velocities Directly from VHF Doppler Radar Spectra 

    Source: Journal of Atmospheric and Oceanic Technology:;1987:;volume( 004 ):;issue: 001:;page 170
    Author(s): Wakasugi, Koichiro; Mizutani, Akiyoshi; Matsuo, Masaru; Fukao, Shoichiro; Kato, Susumu
    Publisher: American Meteorological Society
    Abstract: Raindrop size distribution and vertical air velocity are directly derived from VHF Doppler radar spectra in precipitation environments. As was first proposed by Wakasugi et al., we use a least-squares fitting parametric ...
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    Observations of Tropospheric Temperature Fluctuations with the MU Radar-RASS 

    Source: Journal of Atmospheric and Oceanic Technology:;1994:;volume( 011 ):;issue: 001:;page 50
    Author(s): Tsuda, Toshitaka; Adachi, Tatsuhiro; Masuda, Yoshihisa; Fukao, Shoichiro; Kato, Susumu
    Publisher: American Meteorological Society
    Abstract: Applying the RASS (radio acoustic sounding system) technique to the MU (middle and upper atmosphere) radar, profiles of both temperature and wind velocity were observed every 90 s in the height range of about 1.5?7.0 km, ...
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    Observational Evidence of a Saturated Gravity Wave Spectrum in the Troposphere and Lower Stratosphere 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 012:;page 1741
    Author(s): Fritts, David C.; Tsuda, Toshitaka; Kato, Susumu; Sato, Toru; Fukao, Shoichiro
    Publisher: American Meteorological Society
    Abstract: Radial velocity and temperature data obtained at the MU Radar Observatory during October and November 1986 are used to examine the character of the motion spectrum in the troposphere and lower stratosphere. It is found ...
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    Winds Measured by a UHF Doppler Radar and Rawinsondes: Comparisons Made on Twenty-Six Days (August-September 1977) at Arecibo, Puerto Rico 

    Source: Journal of Applied Meteorology:;1982:;volume( 021 ):;issue: 009:;page 1357
    Author(s): Fukao, Shoichiro; Sato, Toru; Yamasaki, Norikazu; Harper, Robert M.; Kato, Susumu
    Publisher: American Meteorological Society
    Abstract: Vertical profiles of horizontal winds in the lower stratosphere and upper troposphere were measured by the UHF Doppler radar at Arecibo, Puerto Rico (18.35°N, 66.75°W) on 26 days in August and September 1977. On comparing ...
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    VHF Doppler Radar Determination of the Momentum Flux in the Upper Troposphere and Lower Stratosphere: Comparison between the Three- and Four-Beam Methods 

    Source: Journal of Atmospheric and Oceanic Technology:;1988:;volume( 005 ):;issue: 001:;page 57
    Author(s): Fukao, Shoichiro; Sato, Toru; Tsuda, Toshitaka; Kato, Susumu; Inaba, Motoyuki; Kimura, Iwane
    Publisher: American Meteorological Society
    Abstract: The vertical flux of horizontal momentum in the upper troposphere and lower stratosphere can be measured by VHF Doppler radars using the mesosphere-stratosphere-troposphere (MST) radar technique. Two methods have been used: ...
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    Radar Measurement of Tidal Winds at Stratospheric Heights over Arecibo 

    Source: Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 011:;page 2540
    Author(s): Fukao, Shoichiro; Sato, Toru; Yamasaki, Norikazu; Harper, Robert M.; Kato, Susumu
    Publisher: American Meteorological Society
    Abstract: Wind oscillations of tidal periods that showed a marked downward phase progression were detected at the lower stratosphere using the Arecibo radar. The amplitudes of 1?5 m s?1 were inferred for both diurnal and semidiurnal ...
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    Errors in the Determination of Wind Speed by Doppler Radar 

    Source: Journal of Atmospheric and Oceanic Technology:;1989:;volume( 006 ):;issue: 002:;page 235
    Author(s): May, Peter Thomas; Sato, Toru; Yamamoto, Mamoru; Kato, Susumu; Tsuda, Toshitaka; Fukao, Shoichiro
    Publisher: American Meteorological Society
    Abstract: A numerical model to simulate radar data is used for testing various estimators of the Doppler shift in Doppler radar echoes. Five estimators for the Doppler shift are considered: the pulse pair and poly-pulse pair algorithms ...
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    A Typhoon Observed with the MU Radar 

    Source: Monthly Weather Review:;1990:;volume( 119 ):;issue: 003:;page 755
    Author(s): Sato, Toru; Ao, Naoki; Yamamoto, Mamoru; Fukao, Shoichiro; Tsuda, Toshitaka; Kato, Susumu
    Publisher: American Meteorological Society
    Abstract: During the passage of Typhoon 8719 a 60-h continuous observation was made of the troposphere and the lower stratosphere with the MU (middle and upper atmosphere) radar. Height profiles of the wind velocity vector were ...
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    Internal Inertia–Gravity Waves in the Tropical Lower Stratosphere Observed by the Arecibo Radar 

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 015:;page 2359
    Author(s): Maekawa, Yasuyuki; Fukao, Shoichiro; Sato, Toru; Kato, Susumu; Woodman, Ronald F.
    Publisher: American Meteorological Society
    Abstract: High-resolution upper tropospheric and lower stratospheric (5?30 km) wind data were obtained during three periods from 1979 to 1981 with the aid of the high-power UHF radar at Arecibo, Puerto Rico (18.4°N, 66.8°W). A ...
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