Abstract

A dense precipitation network was operated for 45 mo in three remote watersheds in the Adirondack Park of New York State. The network consisted of 4 to 7 wet/dry collectors spaced 3 m to 30 km apart; network operation was on an event basis. The chief objective was an accurate determination of atmospheric inputs into the three watersheds and an assessment of intra- and interbasin variability. Approximately 96% of all possible events were captured. One of the watersheds, Sagamore, received from 6 to 36% less precipitation on a seasonal basis. The capture efficiency relationship between volume collected and standard rain gauge was quantified and shown to be a function of precipitation quantity, type, and sampler location.

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 call

Disclaimer: 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.