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The seasonal characteristics of the breeze circulation at a coastal Mediterranean site in South Italy

机译:意大利南部地中海沿岸微风环流的季节性特征

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We present a study on the characteristics of the sea breeze flow at acoastal site located in the centre of the Mediterranean basin at thesouthern tip of Italy. This study is finalized to add new data on breezecirculations over a narrow peninsula and present a unique experimentalcoastal site at about 600 m from the coastline in a flat open area at the foot ofa mountain chain located in a region of complex orography. We study theseasonal behaviour of the sea-land breeze circulation by analysing two yearsof hourly data of wind speed and direction, temperature, radiation andrelative humidity from a surface meteorological station, eighteen-monthsdata from a wind profiler, and two-year data from the ECMWF analysis.Results show that breezes dominate the local circulation and play a majorrole for the local climate. They are modulated by the season, through thesea-land temperature difference and the large-scale flow. The large-scaleforcing acts in phase with the diurnal breeze and opposes the nocturnalbreeze.In summer, the daytime difference between the land surface temperature and the SST (Sea Surface Temperature)reaches its maximum, while the nigh-time difference has its minimum. This causes a strong, frequent and intense diurnal breeze and a weak nocturnal breeze.In winter and fall the nocturnal difference between the sea and land surface temperature reaches amaximum value, while the diurnal difference is at its minimum value. This causes a strong, frequentand intense nocturnal breeze despite of the large-scale forcing that is usually opposed to local-scale flow.
机译:我们对位于意大利南端地中海盆地中心的沿海站点的海风流动特征进行了研究。这项研究最终完成,目的是为狭窄半岛上的微风环流增加新的数据,并在距地形复杂的山区链脚下的平坦开放区域中,距海岸线约600 m处呈现一个独特的实验性沿海地区。我们通过分析来自地面气象站的风速和方向,温度,辐射和相对湿度的两年每小时数据,来自风廓线仪的十八个月数据以及来自ECMWF的两年数据来研究海陆风循环的季节性行为分析。 结果表明,微风主导着当地的循环,并为当地的气候起到了重要作用。它们是通过季节,海陆温差和大规模流量来调节的。大型强迫与昼夜微风同相,并与夜间微风相反。 夏季,陆地表面温度与SST(海表温度)之间的白天差异达到最大,而夜间则达到最大。差异有其最小值。这会导致强烈的,频繁的和强烈的昼间微风,而夜间的微弱微风。 在冬季和秋季,海面和陆地表面温度之间的夜间差异达到最大值,而昼夜差异则达到最小值。尽管通常与局部规模流动相反的大规模强迫作用,却造成强烈,频繁和强烈的夜间微风。

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