首页> 外文会议>International Conference on Coastal Engineering 2006(ICCE 2006); 20060903-08; San Diego,CA(US) >LARGE AMPLITUDE SEICHE IN ST. JOSEPH BAY, FL- OBSERVATIONS AND IMPLICATIONS
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LARGE AMPLITUDE SEICHE IN ST. JOSEPH BAY, FL- OBSERVATIONS AND IMPLICATIONS

机译:圣安普特大公馆。约瑟夫湾,佛罗里达州-观察与启示

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St Joseph Bay, FL is on the northern shore of the Gulf of Mexico. It is formed by St. Joseph Peninsula, a curving, rapidly - eroding sand spit with the prominent Cape San Blas located at its southern tip. A section of the peninsula at a site called Stump Hole will likely breach in the near future. The new inlet will bisect the only road available to peninsula residents and visitors to St Joseph Peninsula State Park. Tidal hydraulic data were collected to identify and quantify the hydrodynamic processes governing the bay system and to calibrate and verify a numerical hydrodynamic circulation model (ADCIRC) for predicting the long-term fate of a new inlet. Instruments were placed in the Gulf of Mexico offshore of Stump Hole, in the bay behind Stump Hole, and in the bay near its entrance. Data were collected for four days, capturing spring tides and, coincidentally, passage of a strong cold front. Raw pressure data were reduced to water elevation time series relative to NGVD. Local conversions to NAVD and mean seal level were calculated from analysis of regional spatial and temporal trends in MSL. The tidal circulation model predicted that an inlet, once formed, would be stable over the long term under tidal forcing alone. However, measurements showed that sub-tidal long wave energy (associated with the passage of the cold front) occurred with periods near the resonant seiche modes of the bay. This could have significant impacts on the flow regime through any new inlet over short time scales. The phase lag of one component between the outside and the inside of the bay at the potential breach site was near 180 deg, resulting in a much larger hydraulic head across Stump Hole than tidal analysis alone would predict. Potential impacts include short term scour of the inlet beyond the equilibrium size during certain meteorological events (including hurricanes), and introduction of water with much higher sediment loads, discharged from adjacent Apalachicola Bay, into the relatively clear waters of St Joseph Bay.
机译:佛罗里达州圣约瑟夫湾位于墨西哥湾的北岸。它由圣约瑟夫半岛(St. Joseph Peninsula)形成,它是一条弯曲的,侵蚀迅速的沙嘴,其南端有著名的圣布拉斯角。在不久的将来,半岛上一个名为“树桩洞”(Stump Hole)的区域可能会破裂。新的入口将平分半岛居民和圣约瑟夫半岛州立公园游客的唯一道路。收集了潮汐水力数据,以识别和量化控制海湾系统的水动力过程,并校准和验证数值水动力循环模型(ADCIRC),以预测新进口的长期命运。仪器放置在树桩洞近海的墨西哥湾,树桩洞后面的海湾以及入口附近的海湾。收集了为期四天的数据,捕获了春季潮汐,并恰巧捕获了一个强冷锋。相对于NGVD,原始压力数据减少到水高程时间序列。通过对MSL的区域时空趋势进行分析,可以计算出向NAVD的局部转换和平均海豹的水平。潮汐循环模型预测,一旦形成入口,仅靠潮汐强迫就可以长期保持稳定。但是,测量结果表明,潮汐下的长波能量(与冷锋通过有关)的发生周期与海湾的共振seiche模式接近。这可能会对短时间内通过任何新入口的流动状态产生重大影响。潜在突破点处海湾外部与内部之间的一种成分的相位滞后接近180度,从而导致横跨树桩孔的水头比单独进行潮汐分析所预测的要大得多。潜在的影响包括在某些气象事件(包括飓风)期间短期冲刷入水口超过平衡尺寸,以及将沉积物含量高得多的水从相邻的Apalachicola湾排放到相对较清澈的圣约瑟夫湾。

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