日本地球惑星科学連合2016年大会

講演情報

ポスター発表

セッション記号 A (大気水圏科学) » A-AS 大気科学・気象学・大気環境

[A-AS13] ミクロスケール気象現象解明にむけた稠密観測・予報の新展開

2016年5月23日(月) 17:15 〜 18:30 ポスター会場 (国際展示場 6ホール)

コンビーナ:*古本 淳一(京都大学生存圏研究所)、常松 展充(東京都環境科学研究所)、荒木 健太郎(気象研究所)

17:15 〜 18:30

[AAS13-P10] 地上デジタルテレビ放送波を用いた水蒸気変動推定に関する研究

*西田 圭吾1古本 淳一1津田 敏隆1 (1.京都大学生存圏研究所)

キーワード:水蒸気、テレビ放送、大気遅延、大気境界層、局地的豪雨

This paper is devoted to develop the humidity estimation method by using the atmospheric propagation delay of digital television (DTV) radio-wave. Detailed structure of refractive index is dominantly determined by the temporal and spatial variation of atmospheric water vapor by detecting the propagation delay between DTV transmission and receiving antennas. Previous studies was severely annoyed by the oscillator noise of the transmitter and receiver. Due to the strong phase noise, the propagation delay has not been derived precisely.
This study invented a breakthrough method to solve these problems by detecting two DTV stations signal simultaneously. This method uses two receivers nearby and far away from DTV antenna.
Firstly, each receiver processes the subtraction of pilot signal between two DTV stations. In the next step, the subtraction of the above differential signal between two receivers removes the most of error due to oscillator fluctuations. The receiver system is consisted of software radio receivers and Rubidium oscillators. CP (continuous pilot) and SP (scattering pilot) is extracted from OFDM (orthogonal frequency-division multiplexing) carrier of DTV signal.
Prior to field experiment, the precision of receiver is investigated by comparing the results of two collocated receiver systems at Uji Campus of Kyoto University. Three evaluation test was conducted by detecting DTV signal transmitted from Ikoma station. In the first test, phase difference of CP signals neighboring DTV channel is detected, and found the system noise is much larger by 30 dB than the atmospheric propagation delay.
In order to decrease the system noise, this study developed two new methods to integrate many differential signals of SP from single or double station(s), whose frequency is separated by a constant value of 6 MHz or 3 MHz. Both method show excellent improvement of phase error reduction. The system error of propagation delay significantly decreased to 5.47 mm and 7.80 mm, respectively.
This promising method is very useful to monitor horizontal variation of humidity in the boundary layer and expected to proceed to field test very soon.