英语翻译Geological Component of COMPSThe coastal data-monitoring
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英语翻译
Geological Component of COMPS
The coastal data-monitoring program presents an important opportunity for studying the response of our coastal and shelf systems to storm activity.Key elements of the geological component are to characterize the coastal and seafloor environments,and their changes related to storm events.The West Florida Shelf and coastal systems contain geologically diverse environments,having economic importance for marine resources and coastal land use.It is important to know how,under what conditions,and on what time scales are sediments transported and the coastal morphology altered as a result of erosion and land loss.
The nearshore seafloor environments may be linked to some degree with the stability and behavior of the barrier-island coastline.Recent sonar images of two small areas on the inner shelf have revealed extensive hardgrounds and complex sand wave structures indicating active sediment transport.Sonar images collected one year apart suggested some migration of large offshore sand ridges (kilometers in scale) may occur.However,what is missing is an explanation of the physical forcing mechanism that produced this seabed geomorphology.The real-time oceanographic data system will provide this essential data so that we can explain how and when the seabed is in motion and how the seabed interacts with the beach,either providing sand to the beach or storing it temporarily or permanently offshore.
The long-term monitoring of offshore sediment distribution patterns will help verify transport rates and identify potential response of the adjacent coastline.This could lead to predictions of coastal site prone toward erosion.Along the marsh coast,is sediment cover on the adjacent shelf providing sediment to the marsh thus allowing it to keep up with sea-level,or is the eroding marsh providing sediment to the shelf?Simply put,we do not know the sediment transport pathways and exchanges between the coastal and inner shelf system.
We do not know the extent of seagrass cover on the adjacent shelf and to what extent this retards sediment transport during storms or how this benthic community response to storm activity.The seagrasses are vitally important to the marine benthic ecology of this region.
In summary,the geological monitoring program is designed to measure the changes and response of nearshore and coastal environments that can be directly related to the primary driving mechanism - the physical oceanographic data sets generated by the real-time monitoring program.This provides an unprecedented opportunity to identify physical mechanisms driving coastal change.
Geological Component of COMPS
The coastal data-monitoring program presents an important opportunity for studying the response of our coastal and shelf systems to storm activity.Key elements of the geological component are to characterize the coastal and seafloor environments,and their changes related to storm events.The West Florida Shelf and coastal systems contain geologically diverse environments,having economic importance for marine resources and coastal land use.It is important to know how,under what conditions,and on what time scales are sediments transported and the coastal morphology altered as a result of erosion and land loss.
The nearshore seafloor environments may be linked to some degree with the stability and behavior of the barrier-island coastline.Recent sonar images of two small areas on the inner shelf have revealed extensive hardgrounds and complex sand wave structures indicating active sediment transport.Sonar images collected one year apart suggested some migration of large offshore sand ridges (kilometers in scale) may occur.However,what is missing is an explanation of the physical forcing mechanism that produced this seabed geomorphology.The real-time oceanographic data system will provide this essential data so that we can explain how and when the seabed is in motion and how the seabed interacts with the beach,either providing sand to the beach or storing it temporarily or permanently offshore.
The long-term monitoring of offshore sediment distribution patterns will help verify transport rates and identify potential response of the adjacent coastline.This could lead to predictions of coastal site prone toward erosion.Along the marsh coast,is sediment cover on the adjacent shelf providing sediment to the marsh thus allowing it to keep up with sea-level,or is the eroding marsh providing sediment to the shelf?Simply put,we do not know the sediment transport pathways and exchanges between the coastal and inner shelf system.
We do not know the extent of seagrass cover on the adjacent shelf and to what extent this retards sediment transport during storms or how this benthic community response to storm activity.The seagrasses are vitally important to the marine benthic ecology of this region.
In summary,the geological monitoring program is designed to measure the changes and response of nearshore and coastal environments that can be directly related to the primary driving mechanism - the physical oceanographic data sets generated by the real-time monitoring program.This provides an unprecedented opportunity to identify physical mechanisms driving coastal change.
comps沿海地质组成数据监控程序提出了一个重要的机会,为研究我国沿海和响应 货架系统风暴活动.地质要素构成的特点和沿海海底环境 暴风变化及其相关活动.西佛罗里达陆架和沿海系统含有多种地质环境 具有重要的经济和沿海土地利用海洋资源.必须懂得,在什么情况下,什么时间、规模和沿海运输的沉积物形态改变所造成水土流失和土地 损失.近岸海底环境可能与某种程度的稳定和行为障碍岛屿海岸线.最近声纳图象的内在两个小地区发现货架hardgrounds广泛和复杂的沙浪搭建 显示输沙活跃.声纳图像采集一年除了建议一些大型远洋沙脊迁移(公里规模)可能发生.不过,解释什么是失踪的物理机制产生,迫使这个海底地貌.实时海洋学数据系统将提供必要的数据,使我们可以这样解释,当床 在运行时,如何与在沙滩床、 或者提供的砂滩或它暂时或永久存放境外.长期监测海洋沉积物分布格局将有助于查明核实率和运输潜力响应毗邻 海岸线.这可能导致对易受侵蚀预言沿海地盘.沿海岸沼泽、 泥沙复盖在相邻的货架上,提供给泥沙沼泽从而使它跟上海平面,或者是侵蚀泥沙马什提供给货架?简单的说,我们不知道输沙通路与交流沿海和内陆架体系.我们不知道程度和海草复盖的货架旁多大程度上阻碍泥沙 暴风雨或运输期间如何回应风暴底栖社区活动.至关重要的海草对海洋底栖生态区.总之,地质监测计划,旨在改变和响应措施近岸和沿海环境,可以 直接相关的主要驱动机制所产生的物理海洋学数据的实时监控程序.这提供了一个难得的机会,找出物理机制驱动沿岸转变.
英语翻译Geological Component of COMPSThe coastal data-monitoring
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