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Abstract

The observations made on the Ebbaelva and measurements of water stages and discharge provide the basis of determination of runoff variations and amount for its catchment. The results of simultaneous measurements of suspended sediment load are used for calculating the magnitude of denudation. The present article, whilst covering the above aspects, describes thermal properties of the Petuniabukta waters as well as considers whether inland water can desalt them.

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Authors and Affiliations

Adam Choiński

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