A Study of the Lunar Atmospheric Tidal Wave

碩士 === 輔仁大學 === 物理學研究所 === 86 === The study tends to analyze geopotential which measured by radiosondes using the vertical phase and group velocities calculation methods within Taiwan area. There are oscillations phenomenon in 29. 5 day period from January 1996 to February 1998. We also noticed th...

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Main Author: 李鍾嵐
Other Authors: 呂秀鏞
Format: Others
Language:zh-TW
Published: 1998
Online Access:http://ndltd.ncl.edu.tw/handle/07216023440513274958
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spelling ndltd-TW-086FJU031980092015-10-13T11:03:30Z http://ndltd.ncl.edu.tw/handle/07216023440513274958 A Study of the Lunar Atmospheric Tidal Wave 大氣月潮波動之研究 李鍾嵐 碩士 輔仁大學 物理學研究所 86 The study tends to analyze geopotential which measured by radiosondes using the vertical phase and group velocities calculation methods within Taiwan area. There are oscillations phenomenon in 29. 5 day period from January 1996 to February 1998. We also noticed the phenomenon is caused by the interaction of gravity between the earth and moon. We named the phenomenon as lunar atmospheric tidal. From the calculation of vertical group velocities, we find that the vertical group velocities is upward behind the troposphere; the direction of vertical group velocities below troposphere is downward. This shows us the energy of the waving should generate from stir up of atmosphere near troposphere. Furthermore through the characteristics of transmission of wave, we can understand more about mechanism of waves caused by lunar atmospheric tidal in lower atmosphere. 呂秀鏞 劉正彥 1998 學位論文 ; thesis 72 zh-TW
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description 碩士 === 輔仁大學 === 物理學研究所 === 86 === The study tends to analyze geopotential which measured by radiosondes using the vertical phase and group velocities calculation methods within Taiwan area. There are oscillations phenomenon in 29. 5 day period from January 1996 to February 1998. We also noticed the phenomenon is caused by the interaction of gravity between the earth and moon. We named the phenomenon as lunar atmospheric tidal. From the calculation of vertical group velocities, we find that the vertical group velocities is upward behind the troposphere; the direction of vertical group velocities below troposphere is downward. This shows us the energy of the waving should generate from stir up of atmosphere near troposphere. Furthermore through the characteristics of transmission of wave, we can understand more about mechanism of waves caused by lunar atmospheric tidal in lower atmosphere.
author2 呂秀鏞
author_facet 呂秀鏞
李鍾嵐
author 李鍾嵐
spellingShingle 李鍾嵐
A Study of the Lunar Atmospheric Tidal Wave
author_sort 李鍾嵐
title A Study of the Lunar Atmospheric Tidal Wave
title_short A Study of the Lunar Atmospheric Tidal Wave
title_full A Study of the Lunar Atmospheric Tidal Wave
title_fullStr A Study of the Lunar Atmospheric Tidal Wave
title_full_unstemmed A Study of the Lunar Atmospheric Tidal Wave
title_sort study of the lunar atmospheric tidal wave
publishDate 1998
url http://ndltd.ncl.edu.tw/handle/07216023440513274958
work_keys_str_mv AT lǐzhōnglán astudyofthelunaratmospherictidalwave
AT lǐzhōnglán dàqìyuècháobōdòngzhīyánjiū
AT lǐzhōnglán studyofthelunaratmospherictidalwave
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