An Annotated Bibliography of Evaporation
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223-8.) Haslam, B.
Measurement of evaporation.. Nature, 1885, 32:357.
Describes a differential evaporometer in which water flows from a reservoir through an evaporating tank into an overflow receiver. The loss from the reservoir minus the gain in tne receiver equals the evaporation from the exposed surface.
Houdaille, F.
Etudes des pluies de 1885. Bui. m6t. Herault, 1885, (— ):41-60.
A comparison of monthly rainfall with the simultaneous evaporation furnishes a factor expressing the relative hu...midity of each month.
68 Houdaille, F.
Sur les lois d'evaporation. Oompt. rend., 1885, 100:170-2.
Dalton's formula, M=^B?^^, where E= evaporation from a unit surface in a unit of time, Fzsfhe vapor pressure at the surface of the liquid, /= the vapor pressure of the air, If ^ the atmospheric pressure, and B^a. constant determined by the extent of the evapor- ating surface, is found not to apply to observations with the Fiohe evaporometer when the wind effect is considered. Confirms Dalton's discovery that evaporation from large evaporating surfaces is proportional to F—f.
What to read after An Annotated Bibliography of Evaporation?
You can find similar books in the "Read Also" column, or choose other free books by United States. Weather Bureau to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
223-8.) Haslam, B.
Measurement of evaporation.. Nature, 1885, 32:357.
Describes a differential evaporometer in which water flows from a reservoir through an evaporating tank into an overflow receiver. The loss from the reservoir minus the gain in tne receiver equals the evaporation from the exposed surface.
Houdaille, F.
Etudes des pluies de 1885. Bui. m6t. Herault, 1885, (— ):41-60.
A comparison of monthly rainfall with the simultaneous evaporation furnishes a factor expressing the relative hu...midity of each month.
68 Houdaille, F.
Sur les lois d'evaporation. Oompt. rend., 1885, 100:170-2.
Dalton's formula, M=^B?^^, where E= evaporation from a unit surface in a unit of time, Fzsfhe vapor pressure at the surface of the liquid, /= the vapor pressure of the air, If ^ the atmospheric pressure, and B^a. constant determined by the extent of the evapor- ating surface, is found not to apply to observations with the Fiohe evaporometer when the wind effect is considered. Confirms Dalton's discovery that evaporation from large evaporating surfaces is proportional to F—f.
What to read after An Annotated Bibliography of Evaporation?
You can find similar books in the "Read Also" column, or choose other free books by United States. Weather Bureau to read onlineMoreLess
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