ON BOUCHET'S COMPLEMENTARY HYPOTHESIS

dc.contributor.author	Szilagyi J.
dc.date.accessioned	2021-02-13T00:51:52Z
dc.date.available	2021-02-13T00:51:52Z
dc.date.issued	2001
dc.identifier	https://www.elibrary.ru/item.asp?id=606589
dc.identifier.citation	Journal of Hydrology, 2001, 246, 1-4, 155-158
dc.identifier.issn	0022-1694
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/24816
dc.description.abstract	Morton's proof of Bouchet's complementary hypothesis has been revisited. The proof's central assumption is that an increase in sensible heat from the surface to the air induces a similar increment in the sensible heat transfer from the air to a hypothetical potential evaporimeter. It is shown that this assumption is not necessary in the derivation. Instead, the complementary hypothesis under simplified conditions can be obtained with the help of the mass conservation equation for water vapor.
dc.subject	COMPLEMENTARY HYPOTHESIS
dc.subject	AREAL EVAPORATION
dc.subject	POTENTIAL EVAPORATION
dc.subject	WET SURFACE EVAPORATION
dc.title	ON BOUCHET'S COMPLEMENTARY HYPOTHESIS
dc.type	Статья

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