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首页> 外文期刊>Shore and beach >Beach kelp wrack surveys following construction of Wheeler North Reef in San Clemente, California
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Beach kelp wrack surveys following construction of Wheeler North Reef in San Clemente, California

机译:在加利福尼亚州圣克莱门特的惠勒北礁建设之后,对海滩海带残骸进行了勘测

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摘要

The accumulation of drift kelp (kelp wrack) along the shoreline is documented at five 500-foot transects spanning a 3.7-mile study area on the beach at San Clemente, California, 1999-2005 and 2008-2013. Large amounts of kelp wrack were found to accumulate on the beach immediately after some, but not all, large wave storm/swell events. Evidence was found that a combination of swell size and directionality shift had as much to do with kelp breaking free from its substrate as mere wave height (Hs). Further, there were larger volumes of kelp wrack during southern California's dry summer season than during its rainy winter season, even though it is usually during the winter that most of the large storm events occur. This may have been due to the fact that kelps ability to stay attached to the bottom weakens as a function of increasing temperatures over the summer season, as well as to large southern swell events that occasionally arise from early spring through fall. Overall, higher average kelp wrack amounts were observed during the spring, summer, and fall months than during the winter months of January-March. On an annual basis, the largest amount of kelp wrack appeared in the last two years of both the initial six-year study, from 1999 to 2005, and the later five-year study from 2008 to 2013. This is most likely because individual giant kelp plants (Macrocystis pyrifera) in southern California have a life expectancy of 4-6 years. Two of the five 500-ft transects, San Clemente Pier and San Mateo Point, consistently showed the greatest amount of kelp wrack per survey. This is likely due to the trapping abilities of the pier pilings of San Clemente Pier and the focusing of wave energy by San Mateo Point.
机译:1999-2005年和2008-2013年,在加利福尼亚州圣克莱门特海滩上一个3.7英里研究区域的五个500英尺横断面上,记录了沿海岸线的海带(海带残骸)堆积。发现一些(但不是全部)大浪风暴/骤升事件后,大量海带残骸立即堆积在海滩上。有证据表明,膨胀大小和方向性变化的组合与海带从其基底上脱离出来的程度与单纯的波高(Hs)一样大。此外,尽管大部分大风暴事件通常发生在冬季,但在南加州的干燥夏季,海带残骸的数量要多于其冬季的雨季。这可能是由于以下事实:海带保持附着在底部的能力随夏季温度升高而减弱,以及由于早春至秋季偶尔发生的南方南部隆起事件。总体而言,春季,夏季和秋季的海带残骸平均数量要高于1-3月的冬季。从每年的角度来看,海带残骸的数量最多,出现在最初的六年研究(从1999年至2005年)和后来的五年研究(从2008年至2013年)的最后两年中。这很可能是因为个体巨人南加州的海带植物(Macrocystis pyrifera)的预期寿命为4-6年。在五个500英尺长的断面中,有两个,圣克莱门特码头和圣马特奥角,每次调查都一致显示出最大的海带残骸。这可能是由于San Clemente Pier码头桩的陷井能力和San Mateo Point对波能的聚焦。

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  • 来源
    《Shore and beach》 |2017年第1期|17-24|共8页
  • 作者单位

    Coastal Environments, Inc. 2166 Avenida de la Playa, Suite E La Jolla, CA 92037;

    Coastal Environments, Inc. 2166 Avenida de la Playa, Suite E La Jolla, CA 92037;

    Coastal Environments, Inc. 2166 Avenida de la Playa, Suite E La Jolla, CA 92037;

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