Windy flats development on the untidal Ukrainian Black Sea

dc.contributor.author	Shuiskyi, Yurii D.
dc.contributor.author	Шуйский, Юрий Дмитриевич
dc.contributor.author	Шуйський, Юрій Дмитрович
dc.date.accessioned	2018-06-14T13:16:47Z
dc.date.available	2018-06-14T13:16:47Z
dc.date.issued	2002
dc.description.abstract	The Black Sea is untidal because the maximum value of tide near the Nothem shoreline is not greater than 0.08 m. That is why there are no typical tidal flats there. Nevertheless short-term changes of sea level take place. They are caused not by tides but by winds of gale force. If the wind is blowing landward, the water level near the shoreline is rising, if the wind is of the opposite direction, the level lowers relatively the average long-term value. The higher the wind velocity and the time of its action, the greater the amplitude of windy fluctuations of the level. It reaches the maximum in the tops of bays and harbours when windy vector acts along the normal to the shoreline, when land surfaces and nearshore sea bottom are the gentlest.	uk
dc.identifier.citation	Annals Valahia Univ. (Rom.).	uk
dc.identifier.uri	https://dspace.onu.edu.ua/handle/123456789/16976
dc.relation.ispartofseries	Geography;Vol. 2.
dc.subject	Coastal zone	uk
dc.subject	Windy flats	uk
dc.subject	Set up	uk
dc.subject	Beach	uk
dc.subject	Sediment	uk
dc.subject	Bench	uk
dc.subject	Abrasion	uk
dc.subject	Ukraine	uk
dc.title	Windy flats development on the untidal Ukrainian Black Sea	uk
dc.type	Article	uk

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