An observation of hot air downwelling over Pantelleria Island in the Strait of Sicily |
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Authors: | David H Shonting |
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Institution: | (1) NATO SACLANT ASW Research Centre, La Spezia, Italy;(2) Naval Underwater Systems Center, 02840 Newport, Rhode Island, U.S.A. |
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Abstract: | During a period of strong SW winds, a local anomalous hot air mass was observed at sea level on the lee side of Pantelleria
Island in the Strait of Sicily. The hot air, some 10 °C above ambient, was produced by downward transport or mixing from an
intense inversion layer occurring above 500 m. This rapidly moving layer, associated with a flow from the Libyan Desert, was
apparently perturbed by the 836-m high volcanic cone of the island. Laboratory models suggest that such an interaction could
produce phenomena, i.e., vortex shedding and lee waves, all of which would mix or advect the upper warm air downward. This,
together with the adiabatic heating effect, would produce the hot air phenomena. |
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