Footprints in Micrometeorology and Ecology

Format: Hardcover

Language: English

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An increase in water velocity is caused by either an increase in the slope of the streambed or an increase in the volume of water flowing in the stream. (1) Friction along the banks decreases the velocity of the water in contact with the banks. Our main suppliers of freshwater are rivers and lakes – the visible segment of a complex hydrological process that cycles water between the land and the sea. Fieldwork is supported by a well-equipped technical workshop.

Pages: 239

Publisher: Springer; 2014 edition (June 18, 2014)

ISBN: 3642545440

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