首页> 外文会议>2011 30th URSI General Assembly and Scientific Symposium >VHF radar studies of the migrating and nonmigrating diurnal and semidiurnal tides over a tropical and an equatorial station
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VHF radar studies of the migrating and nonmigrating diurnal and semidiurnal tides over a tropical and an equatorial station

机译:VHF雷达研究热带和赤道站上正在迁移和不迁移的日,半日潮

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摘要

VHF radar measurements of winds are utilized to study the diurnal and semi-diurnal tides over Gadanki and Kotatabang. The tidal amplitudes exhibit maxima in UTLS region during June-September over Gadanki and during March and September over Kotatabang. The vertical wavelength is 3–5 km (Gadanki) and 25–30 km (Kotatabang), which reveal the existence of nonmigrating and migrating tides, respectively. Brightness temperature shows that over Gadanki(deep) and Kotatabang(shallow) convective clouds. Release of latent heat due to deep-clouds is found to be the main source mechanism for nonmigrating tides. The present study brings out the differences in tides over equatorial and low latitude.
机译:利用甚高频雷达对风的测量来研究盖丹基和哥打t邦的日潮和半日潮。在Gadanki的6月至9月以及Kotatabang的3月和9月,潮汐振幅在UTLS地区表现出最大值。垂直波长为3–5 km(Gadanki)和25–30 km(Kotatabang),分别揭示了非迁徙潮汐和迁徙潮汐的存在。亮度温度表明在对流云层上有深浅的Gadanki和浅层的Kotatabang。发现由于深云而释放潜热是非迁移潮汐的主要来源机制。本研究揭示了赤道和低纬度在潮汐方面的差异。

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