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首页> 外文期刊>Earth, planets and space: EPS >Radar observations of the diurnal tide in the tropical mesosphere-lower thermosphere region: Longitudinal variabilities
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Radar observations of the diurnal tide in the tropical mesosphere-lower thermosphere region: Longitudinal variabilities

机译:热带中层低层热圈地区日潮的雷达观测:纵向变化

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Significant attention is being paid in recent times by several observational and modeling studies to quantify the spatial and temporal variabilities of diurnal tide in the mesosphere and lower thermosphere (MLT) region. These variabilities are ascribed to spatial and temporal variations in the tidal forcing or interactions between the propagating tides and background wind, planetary waves or gravity waves. The present work makes USC of simultaneous ground-based radar wind observations of different durations from five equatorial/low latitude sites in the Indian. Indonesian and Pacific sectors: Tirunelveli (8.7 degrees N, 77.8 degrees E), Jakarta (6.4 degrees S. 106.7 degrees E). Ponlianak (0.03 degrees N 109 degrees E), Kauai (22 degrees N, 160 degrees W) and Christmas Island (2 degrees N. 157 degrees W). This study delineates the longitudinal differences in the tidal characteristics in (i) interannual time scales over Tirunelveli and Kauai during 1993-2002, (ii) seasonal time scales over Christmas Island, Jakarta and Tirunelveli for the years 1993-1997 and (iii) shorter than seasonal time scales over Christmas Island, Pontianak and Tirunelveli during 1996-1997. An important observational feature noticed in this work is the differing behavior of the long-term tidal fields over Tirunelveli and Kauai. The monthly tidal amplitudes over Tirunelveli reveal a strong QBO signature whereas it similar, strong QBO signal could not be traced in the long-term observations front Kauai.
机译:最近,一些观测和模型研究引起了人们的极大关注,以量化中层和低热层(MLT)区域昼夜潮的时空变化。这些变化归因于潮汐强迫的时空变化或传播的潮汐与背景风,行星波或重力波之间的相互作用。目前的工作使USC可以同时从印度的五个赤道/低纬度地点同时观测不同持续时间的地基雷达风。印度尼西亚和太平洋地区:Tirunelveli(北纬8.7度,东经77.8度),雅加达(南纬6.4度。东经106.7度)。 Ponlianak(北纬0.03度,东经109度),Kauai(北纬22度,西经160度)和Christmas Island(北纬2度(北纬157度))。这项研究描述了(i)1993-2002年Tirunelveli和Kauai的年际时间尺度,(ii)1993-1997年圣诞节岛,雅加达和Tirunelveli的季节性时间尺度以及(iii)较短的潮汐特征的纵向差异。比1996-1997年圣诞节岛,坤甸和蒂鲁内尔维利的季节性时标大。这项工作中注意到的一个重要观测特征是Tirunelveli和Kauai上的长期潮汐场的行为不同。 Tirunelveli上的每月潮汐振幅显示出很强的QBO信号,而在考艾岛前线的长期观测中却没有类似的,很强的QBO信号。

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