Initial Observations for Precipitation Cores With X-Band Dual Polarized Phased Array Weather Radar

被引:18
|
作者
Kikuchi, Hiroshi [1 ]
Suezawa, Taku [2 ]
Ushio, Tomoo [3 ]
Takahashi, Nobuhiro [4 ]
Hanado, Hiroshi [5 ]
Nakagawa, Katsuhiro [5 ]
Osada, Masahiko [6 ]
Maesaka, Tsuyoshi [7 ]
Iwanami, Koyuru [7 ]
Yoshimi, Kazuhiro [8 ]
Mizutani, Fumihiko [8 ]
Wada, Masakazu [8 ]
Hobara, Yasuhide [9 ]
机构
[1] Univ Electrocommun, Ctr Space Sci & Radio Engn SSRE, Tokyo 1828585, Japan
[2] Tokyo Metropolitan Univ, Grad Sch Syst Design, Tokyo 5650871, Japan
[3] Osaka Univ, Grad Sch Engn, Suita, Osaka 5650871, Japan
[4] Nagoya Univ, Grad Sch Environm Studies, Nagoya, Aichi 4648601, Japan
[5] Natl Inst Informat & Commun Technol, Koganei, Tokyo 1848795, Japan
[6] Saitama Univ, Grad Sch Sci & Engn, Saitama 3388570, Japan
[7] Natl Res Inst Earth Sci & Disaster Resilience HIE, Tsukuba, Ibaraki 3050006, Japan
[8] Toshiba Infrastruct Syst & Solut Corp, Kawasaki, Kanagawa 2128585, Japan
[9] Univ Electrocommun, Grad Sch Informat & Engn, Tokyo 1828585, Japan
来源
关键词
Phased array radar; polarimetric radar observations; remote sensing; POLARIMETRIC RADAR; DIFFERENTIAL REFLECTIVITY; RAINFALL ESTIMATION; DISTRIBUTIONS; SIGNATURES; SUPERCELL; MOBILE;
D O I
10.1109/TGRS.2019.2959628
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The first X-band dual polarized phased array weather radar (DP-PAWR), which simultaneously transmits pulses of horizontal and vertical polarized radiation, was developed and installed at Saitama University, Japan, in December 2017. The DP-PAWR uses mechanical and electronic scanning at azimuth and elevation angles, respectively. It provides polarimetric precipitation measurements via 3-D volume scanning with an update rate between 10 and 60 s, for a range of up to 80 km. Here, we describe the initial DP-PAWR observation results. To evaluate the DP-PAWR observation accuracy, we compared the observational data with radar variables derived from Parsivel disdrometer data. In comparison with the disdrometer, the relative observation accuracy for the DP-PAWR radar reflectively factor had a standard deviation of 1.1 dB and mean value of 0.4 dB. We also conducted detailed observations of a developing thunderstorm using a specific differential phase ( $K_{\mathrm {dp}}$ ) column, focusing on the $K_{\mathrm {dp}}$ core during the storm. The $K_{\mathrm {dp}}$ core movements provided useful information about the convection flow during the storm.
引用
收藏
页码:3657 / 3666
页数:10
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