使用探地雷达对菲律宾中部比科尔湾湾口最近风暴历史的调查

Jeremy Pile, A. Switzer, L. Soria, F. Siringan, A. Daag
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引用次数: 2

摘要

菲律宾群岛位于季节性热带气旋的路径上,由于风暴潮,大部分海岸容易遭受周期性的淹没。台风榴莲就是一个例子,它是2006年11月30日登陆菲律宾中东部海岸比科尔省的三级风暴。2007年5月的卫星图像显示,榴莲造成了严重的侵蚀,并破坏了一个沙口,从海湾湾村的奎纳尔河口向东南方向流向塔巴科城。图像还显示,尽管决口处显示出部分恢复的迹象,但与台风榴莲相关的洪水事件的地貌证据仍然存在。2012年,我们绘制了榴莲的地貌特征。2013年6月,我们再次对Bay-Bay吐槽进行探地雷达(GPR)调查,以调查之前风暴事件的潜在地下证据。探地雷达调查包括5条1.5公里的海岸剖面和12条50 -200米长的跨海岸剖面。本研究使用的探地雷达系统是一个带有100兆赫天线的传感器和软件脑洞。利用双曲线匹配确定近地表速度,以估计深度。使用dGPS系统收集地形和位置数据。经过最小的处理,在测量过程中,穿透深度从2-8米不等。岸线GPR剖面显示,在2006年台风榴莲之前,至少发生了两次侵蚀事件,每次侵蚀面之间的恢复和进积距离约为10 m。在这里,我们展示了探地雷达剖面捕获了侵蚀特征。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
An investigation of recent storm histories using ground penetrating radar at Bay-Bay spit, Bicol, Central Philippines
The Philippine archipelago lies in the path of seasonal tropical cyclones, and much of the coast is prone to periodic inundation due to storm surges. One example is typhoon Durian, a category 3 storm that made landfall on the 30th November 2006, in Bicol province, on the east central Philippine coast. Satellite imagery from May 2007 reveal that Durian caused significant erosion and breached a sandy spit that runs southeast from the mouth of the Quinale River at Bay-Bay village towards Tabaco City. The imagery also showed that, although the breach site showed signs of partial recovery, geomorphological evidence of the inundation event associated with typhoon Durian still remains. In 2012 we mapped the geomorphological features of Durian. In June 2013 we returned to conduct Ground Penetrating Radar (GPR) surveys on the Bay-Bay spit to investigate potential subsurface evidence of previous storm events. The GPR surveys comprised five, 1.5 km, longshore profiles and 12 cross-shore profiles, of 50 m-200 m in length. The GPR system used for this study was a Sensors and Software Noggin with 100 Mhz antennas. Near surface velocities were determined using hyperbolas matching in order to estimate depth. Topographic and positional data were collected using a dGPS system. After minimal processing, depth of penetration during the survey varied from 2-8 m. The cross-shore GPR profiles reveal at least two erosional events prior to 2006 typhoon Durian, with approximately 10 m of recovery and progradation between each erosion surface. Here we show that the GPR profiles captured the erosional features.
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