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Satellite observations of cold filaments and surface jets in the Mediterranean Sea

机译:地中海在地中海的冷丝和表面喷射的卫星观察

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Thermal satellite images relative to the years 1997-2000 are analyzed in this study, in order to infer cold filament and surface jet dynamics in the Mediterranean Sea. The main zones in which these phenomena are seen to occur, are characterised by upwelling and/or the funnelling of strong cold winds by a somewhat irregular coastal orography. Indeed, intense air-sea interaction in the coastal zone is known to generate a particularly strong input of potential vorticity into the sea, and this in turn gives origin to upwellings, cold filaments and jets. In the Mediterranean Sea the geographical zones with a higher frequency in these jets are the two lobes of the southern Sicilian coast, the sea off Olbia in Eastern Sardinia, that south of the island of Crete where a particularly intense large scale turbulence field is evident, and the Balkanic coast of the Adriatic Sea. In addition the theoretical analysis of these jets' evolution using a modern version of the potential vorticity conservation, valid even if friction and entrainment are considered, gives further insight into these systems' dynamics.
机译:在本研究中分析了相对于1997-2000年的热卫星图像,以推断出地中海的冷灯丝和地表喷射动力学。看到这些现象发生的主要区域,其特征在于通过稍微不规则的沿海或沿线地区的升高和/或强大的冷风漏斗。实际上,众所周知,沿海地区的强烈的海海相互作用产生了特别强大的潜在涡流进入大海,这反过来又为升值,冷丝和喷气机造成了原点。在地中海在地中海,这些喷气机频率较高的地理区域是西西里岛南部的两个裂片,海外奥尔比亚在撒丁岛的奥尔比亚,克里特岛南部,其中一个特别强大的大规模湍流场是明显的,和亚得里亚海的南非海岸。此外,这些喷气机的潜在涡度保护的潜在涡度保护的理论分析,即使考虑摩擦和夹带,也有效地介绍了这些系统的动态。

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