JpGU-AGU Joint Meeting 2017

Presentation information

[EE] Poster

A (Atmospheric and Hydrospheric Sciences) » A-AS Atmospheric Sciences, Meteorology & Atmospheric Environment

[A-AS09] [EE] Stratosphere - Troposphere Interaction

Wed. May 24, 2017 10:45 AM - 12:15 PM Poster Hall (International Exhibition Hall HALL7)

convener:Nawo Eguchi(Kyushu University), Rei Ueyama(NASA Ames Research Center), Sean M Davis(NOAA Boulder), Seok Woo Son(Seoul National University)

[AAS09-P20] Development of a cloud particle sensor for radiosonde sounding

*Masatomo Fujiwara1, Takuji Sugidachi2, Kensaku Shimizu2, Mayumi Hayashi3, Kazuo Sagara3, Yoichi Inai4, Takashi Shibata5, Suginori Iwasaki6, Atsushi Shimizu7, Yasuhisa Noma3, Hideaki Kawagita3, Taro Nakagawa8, Satoshi Okumura8 (1.Faculty of Environmental Earth Science, Hokkaido University, 2.Meisei Electric Co. Ltd , 3.Shinyei Technology Co., Ltd, 4.Tohoku University, 5.Nagoya University, 6.National Defense Academy, 7.National Institute for Environmental Studies, 8.Shinyei Kaisha)

Keywords:cloud, radiosonde

A meteorological balloon-borne cloud sensor called the cloud particle sensor (CPS) has been developed. The CPS is equipped with a diode laser at ~790 nm and two photodetectors, with a polarization plate in front of one of the detectors, to count the number of particles per second and to obtain the cloud-phase information (i.e. liquid, ice, or mixed). The lower detection limit for particle size was evaluated in laboratory experiments as ~2 micro m diameter for water droplets. For the current model the output voltage often saturates for water droplets with diameter equal to or greater than ~80 micro m. The upper limit of the directly measured particle number concentration is ~2 cm^−3 (2 × 10^3 L^−1), which is determined by the volume of the detection area of the instrument. In a cloud layer with a number concentration higher than this value, particle signal overlap and multiple scattering of light occur within the detection area, resulting in a counting loss, though a partial correction may be possible using the particle signal width data. The CPS is currently interfaced with either a Meisei RS-06G radiosonde or a Meisei RS-11G radiosonde that measures vertical profiles of temperature, relative humidity, height, pressure, and horizontal winds. In the presentation, results from four flights, two in Japan and two in Indonesia, are discussed in detail.