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291.
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293.
2011年贵州两次降雪天气过程的多普勒雷达产品特征分析 总被引:1,自引:0,他引:1
利用常规观测和新一代多普勒天气雷达回波资料对2011年1月17日至20日贵州省出现的两次降雪天气进行详细的特征分析。结果表明:贵州降雪回波强度一般〈30dBz,中心强度普遍在30-40dBz之间,反射率因子的分布梯度不大;但降雪过程中夹杂冰粒的时候,回波中心强度能达到50dBz。降雪回波的顶高一般在7km以下,其中顶高5-7km的情况占到60%左右,发展旺盛时回波顶高可达到8km以上。降雪回波径向速度的等值线比较密集,沿径向梯度变化大。“牛眼”状回波是降雪回波的一个典型特征,“牛眼”状回波正负速度中心值的大小与降雪量存在一定的正比关系。风廓线产品的近地面层风向对于预报降水类型有明显的指示意义,当风廓线产品上近地面1.5km高度的风向由东偏南转为东偏北时,地面冷平流取代暖平流,雨夹雪向纯雪转换,反之,暖平流取代冷平流,则是纯雪向雨夹雪转换,或者降雪减弱消失。 相似文献
294.
This paper presents the results of a 3-year-long (November 2004–November 2007) study based on the use of acoustic Doppler current profilers (ADCPs) to estimate the solid transport through the three inlets of Venice lagoon. In each of the three inlets instruments were mounted both on survey boats and deployed on the channel bed. The three bottom-mounted ADCPs were positioned in the central part of the inlets, continuously monitoring vertical profiles in the water column. Periodic transects along the investigated sections were collected by the boat-mounted ADCP. Both installations measured current speed and acoustic backscatter intensity. The latter expresses the attenuation of acoustic energy due to material in the water column. 相似文献
295.
利用差分测速和Kalman滤波估计相位变率方法对某次航空重力测量的飞行数据进行了解算,通过与GT-1A自带的GPS高精度定位测速软件和WAY-Point软件比对分析,结果表明:采用Kalman滤波估计相位变率的GPS差分测速,能够适应较复杂的运动模式,定速精度达到mm/s级,高于WAY-Point软件的动态测速精度。 相似文献
296.
2017年8月11日下午,三个EF4级龙卷袭击了内蒙古自治区赤峰市的地形复杂地区,造成5人死亡,58人受伤。这是1961年以来中国有记录的最强山地龙卷事件。首先给出了此次龙卷过程的灾情调查结果,接下来分析了此次龙卷母体风暴-龙卷超级单体产生的天气背景、关键环境参数以及多普勒天气雷达观测特征。本次龙卷事件发生在东北冷涡东南象限的地面锋前和干线向湿侧发展处,CAPE(对流有效位能)值为1 800 J/kg,0~6 km风垂直切变为12.9 m/s,0~1 km风垂直切变达到10.8 m/s;同时,0~1 km相对风暴螺旋度达到67.3 m2/s2,接近美国龙卷发生环境的中位数,有利于超级单体龙卷的发生。现场灾害调查发现,灾害路径具有多涡旋和不连续的特点,可能与当地的复杂地形有关。基于多普勒天气雷达相对径向速度图识别出三个龙卷涡旋特征(TVS),TVS径向速度差最大达到38 m/s。三个龙卷及对应TVS出自同一个超级单体的同一个中气旋,其中两个TVS出现时间重叠。 相似文献
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298.
Nearshore directional wave measurements by surface-following buoy and acoustic Doppler current profiler 总被引:1,自引:0,他引:1
Directional energy spectra of nearshore surface waves were measured for a 3-year period (2004–2007) at a site with mean depth 14 m and mean tidal range 2.1 m. Triaxys surface-following wave buoys reported hourly directional wave energy spectra and wave parameters near the offshore end of the Savannah River Entrance Channel, Georgia, USA. An acoustic Doppler current profiler (ADCP) was located beside the wave buoy for 3 months. Directional and non-directional surface wave energy spectra and the corresponding bulk wave parameters (height, period, and direction) are compared for the two systems. Most parameters derived from the spectra agree closely; the most significant differences were found at the upper and lower frequency measurement limits, where signal-to-noise ratios were lower. The wave buoy consistently reports a small amount of energy below 0.05 Hz that does not appear in the ADCP-derived spectra and does not appear to be related to the mooring system. This leads to larger mean and peak periods reported by the buoy. All directional spectra were computed using the Maximum Entropy Method for both instruments, but the buoy, with spectra derived from six independent time series, provides lower directional resolving power than the ADCP, which utilizes twelve time series. Both systems gave similar results defining mean and peak wave directions, with the primary difference being that the ADCP indicates energy to be more tightly concentrated around the peak direction. 相似文献
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300.
Volume transport of the Soya Warm Current revealed by bottom-mounted ADCP and ocean-radar measurement 总被引:2,自引:2,他引:0
Yasushi Fukamachi Iori Tanaka Kay I. Ohshima Naoto Ebuchi Genta Mizuta Hideo Yoshida Shiro Takayanagi Masaaki Wakatsuchi 《Journal of Oceanography》2008,64(3):385-392
The vertical structure of the Soya Warm Current (SWC) was observed by a bottom-mounted acoustic Doppler current profiler (ADCP)
in the region of the SWC axis near the Soya Strait during a 1-year period from May 2004. The ADCP data revealed a marked seasonal
variability in the vertical structure, with positive (negative) vertical shear in summer and fall (winter and spring). The
volume transport of the SWC is estimated on the basis of both the vertical structure observed by the ADCP and horizontal structure
observed by the ocean radars near the strait. The transport estimates have a minimum in winter and a maximum in fall, with
the yearly-averaged values in the range of 0.94–1.04 Sv (1 Sv = 106 m3 s−1). These lie within a reasonable range in comparison to those through other straits in the Japan Sea. 相似文献