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Development of New Type Frost Point Zonde (Electric Cooling Method)

Development of New Type Frost Point Zonde (Electric Cooling Method)
新型霜点Zonde(电冷却方式)的开发
批准号:
03554012
负责人:
IWASAKA Y
金额:
$9.15万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Developmental Scientific Research (B)
财政年份:
1991
资助国家:
日本
项目状态:
已结题
起止时间:
1991 至 1992

项目摘要

项目成果

相关文献

中文摘要
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英文摘要
Frost Point Sonde was world-widely used for routine upper air measurements, but is now inhibited to use since this type of sonde containes lots of CFCs to cool mirror surface. Therefore there are few data on water vapor content in the upper troposphere and stratosphere although water vapor content in the upperair is very important information to study on upper atmospheric physics and develope weather forcasting technique. In this research, we tried to make new type frost point zonde which does not contain CFCs and furthermore some technical problems which were pointed concerning old type frost point zonde. According to the research.1. Thermomodule is very effective to cool mirror surface and heat capacity is extremely small when we use the metal vapor deposited surface of the thermomodule as the mirror.2. The proto-type instrumnts suggest that the shape, total weight, and capacity of electric power of the new type sonde will be approximately same comparing with the old type sonde.3. Use of solid state source light and receiver of scattering light contributes to the stability of the optics of sonde and increasc in S/N.4 It was hard to identify whether droplets of water or ice crystals forms on the mirror surface under the condition of the lower atmosphere. It is desired to more measurements on this problem under various atmospheric condition.Summarizing the research, it can be concluded that the new type frost point sonde is very hopeful for routine measurements on upper air humidity.
期刊论文(1)
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科研奖励(0)
会议论文
Y.Iwasaka: "Water Vapor Measurements with New Type Frost-Point Sonde" Proc.NIPR Symp.Upper Atmospheric Physics. 6. (1993)
Y.Iwasaka:“使用新型霜点探测器进行水蒸气测量”Proc.NIPR Symp.高层大气物理。
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