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首页> 外文期刊>African Journal of Marine Science >Short-term variability in alongshore winds and temperature off Swakopmund, Namibia, during a non-upwelling event in 1998-1999
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Short-term variability in alongshore winds and temperature off Swakopmund, Namibia, during a non-upwelling event in 1998-1999

机译:在1998-1999年的一次非上升流事件中,纳米比亚斯瓦科普蒙德附近沿海风和温度的短期变化

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摘要

Swakopmund Is a popular coastal resort in Namibia, especially during the summer holiday season when daily sea temperatures can fluctuate several degrees in a short period. Hourly measurements of the near-bottom water temperature were collected off theSwakopmund Jetty to investigate the thermal variability in relation to local winds. The thermal regime of this coastal region appears to be controlled by the locally forced Ekman offshore transport. Related changes in offshore transport led those of thesurf-zone temperature by about one day. A transfer of kinetic energy from the alongshore wind into the temperature field of the nearshore zone dominated relative short time scales (hourly). The longer periods (7-9 days) are associated with the forcing of poleward-directed continental shelf waves. The origin of the 24-25 day frequencies is not clearly understood. However, it characterises the near-shore wind field as well as the water temperature of the surf zone. These relatively long quasi-cycles could originate from rhythmic changes in the regional wind field as a result of changes in the thermal contrast between sea and land areas.
机译:斯瓦科普蒙德(Swakopmund)是纳米比亚最受欢迎的沿海度假胜地,尤其是在暑假期间,每天的海水温度在短期内会波动几度。从斯瓦科普蒙德码头(Swakopmund Jetty)每小时收集一次接近底部水温的测量数据,以研究与局部风有关的热变率。该沿海地区的热力状况似乎受到当地强迫的埃克曼海上运输的控制。离岸运输的相关变化导致冲浪区温度上升了约一天。动能从沿岸风向近岸带温度场的转移主要是相对较短的时间尺度(每小时)。较长的时间(7-9天)与极向性大陆架波的强迫有关。 24-25天频率的起源尚不清楚。但是,它表征了近岸风场以及冲浪区的水温。这些相对较长的准周期可能是由于海陆区域之间的热反差发生变化而导致区域风场的节奏变化所致。

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