𝔖 Bobbio Scriptorium
✦   LIBER   ✦

Evaportation-loss per month from two drainage areas

✍ Scribed by David Lloyd

Book ID
104570161
Publisher
John Wiley and Sons
Year
2007
Tongue
English
Weight
833 KB
Volume
66
Category
Article
ISSN
0035-9009

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✦ Synopsis

Abstract

Monthly data of the apparent loss by evaporation, etc., of moisture from Vyrnwy and Rivington drainage areas are examined in relation to the rainfall and the temperature.

After discussing the subject matter, the association and the degree of association are determined on the hypothesis that variations in evaporation‐loss can be associated with the variations in rainfall and temperature in a joint functional manner. The regressions have been computed together with the formal evaluation of the significance of the statistics.

The results show that, when the temperature is constant, the evaporation‐loss is proportional to the rainfall; when the rainfall has a given value, the loss increases in relation to the temperature; while the loss is reduced according to the previous rainfall. There is similarity in the relations at Vyrnwy and Rivington.

πŸ“œ SIMILAR VOLUMES

Evaporation-loss per month over drainage
Evaporation-loss per month over drainage areas, III
✍ David Lloyd πŸ“‚ Article πŸ“… 1942 πŸ› John Wiley and Sons 🌐 English βš– 541 KB

## Abstract Evidence is brought forward of curvilinearity in the partial relation between evaporation‐loss and the period rainfall; this is shown by diagrams. The joint functional causation of rainfall and temperature is further advanced. It is inferred statistically that rain experienced in three

Evaporation-loss per month over drainage
Evaporation-loss per month over drainage areas, II. Loss over three areas
✍ David Lloyd πŸ“‚ Article πŸ“… 2007 πŸ› John Wiley and Sons 🌐 English βš– 352 KB

## Abstract The data from three more large drainage areas are examined by the same method as in the former paper on this subject. The results show again that the variations in loss can be largely associated with variations in rainfall and temperature. It is also demonstrated that, with similar clim