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A case study of sea breeze blocking regulated by sea surface temperature along the English south coast

机译:英国南海岸海面温度调节海风阻塞的案例研究

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pstrongAbstract./strong The sensitivity of sea breeze structure to sea surface temperature (SST) and coastal orography is investigated in convection-permitting Met Office Unified Model simulations of a case study along the south coast of England. Changes in SST of 1 K are shown to significantly modify the structure of the sea breeze immediately offshore. On the day of the case study, the sea breeze was partially blocked by coastal orography, particularly within Lyme Bay. The extent to which the flow is blocked depends strongly on the static stability of the marine boundary layer. In experiments with colder SST, the marine boundary layer is more stable, and the degree of blocking is more pronounced. Although a colder SST would also imply a larger landa??sea temperature contrast and hence a stronger onshore wind a?? an effect which alone would discourage blocking a?? the increased static stability exerts a dominant control over whether blocking takes place. The implications of prescribing fixed SST from climatology in numerical weather prediction model forecasts of the sea breeze are discussed./p.
机译:> >摘要。在英格兰南部沿海对流允许的Met Office统一模型模拟中,研究了海风结构对海表温度(SST)和沿海地形的敏感性。 SST的变化为1 K,表明可以显着改变紧邻海面的海风的结构。在案例研究的当天,海风被沿海地形特别是莱姆湾内的沿海地形所阻挡。流动受阻的程度在很大程度上取决于海洋边界层的静态稳定性。在海温较低的实验中,海洋边界层更稳定,阻塞程度更明显。尽管较冷的海面温度也意味着较大的陆地温度与海水温度的反差,因此也意味着陆上风能更强。单独阻止阻塞的效果?更高的静态稳定性可控制是否发生阻塞。讨论了从气候学中规定固定的海温对海风数值天气预报模型预报的意义。

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