Penetration of sea breeze inland




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Observational results of the structure of the sea breeze over the urban and suburban areas of yeddo for quaternion summertime days are presented. On two of these days, the inland penetration of the sea breeze head-on could be clear traced. In one case, the sea breeze was first observed along the shores of national capital Bay around 0900 JST, and propagated in three unit of time done the Tokyo metropolis area, the breadth of which is about 20 km. Prior to the arrival of the sea breeze at the suburban site, the mixing height had remained at about 600 m for four hours.




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PROJECT OBJECTIVES AND ACCOMPLISHMENTS The sea cinch commonly occurs along the southern Maine coastal zone during the spring, summer, and fall months. Passage of the sea-breeze front is often accompanied by a exhalation shift, drop in temperature, and change in wet content. Therefore, the sea labour plays an important role in controlling the maximum somesthesia an inland location realizes during the day and its attendant wind shift is an important aviation hazard.


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Characteristics of sea breeze circulations over a tropical Indian station have been studied, based on one year of observations, by Doppler Sound Detection and Ranging (SODAR) method at internal Atmospheric Research Laboratory, Gadanki (13.5°N, 79.2°E), India. The effect of sea breeze circulations on the dynamics of low level flow patterns in atmospherical boundary layer over complex terrain in tropics is investigated. The study reveals that a sea-breeze foremost develops healed on the eastern coastal plain of austral peninsular India and propagates over inland up to the distance about 80 km.

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