Abstract
In recent studies of stream‐flow determination from rainfall‐records much emphasis has been placed on antecedent weather. The soil‐moisture deficiencies that occur on a watershed as a result of weather preceding rainfall could be rather closely estimated if the amount of moisture lost by evaporation and transpiration between storms were known. Instruments designed to secure measurements of such losses are only now being perfected [see 5 of “References” at end of paper] and it was in anticipation of them that a proposed method has been developed for calculating contributions of runoff to stream‐flow by reference to soil‐moisture deficiencies at the beginning of rainfall. The details of the method are tentative. Only a brief outline of the procedure and of the results obtained is therefore presented in this paper.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
