کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
4580024 | 1630149 | 2007 | 12 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Comparisons of measured stream flow with drainage and runoff simulated by a soil-vegetation-atmosphere transport model parameterized with GLOBE student data
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کلمات کلیدی
SVATActual evaporationUSGSpotential evapotranspiration - تبخیر تبخیری بالقوهEvapotranspiration - تبخیر و تعرقPotential evaporation - تبخیر پتانسیلStream flow - جریان جریانRunoff - رونابDrainage - زهکشیUnited States Geological Survey - سازمان زمین شناسی ایالات متحدهSimulation model - مدل شبیه سازیPET - پتGlobe - گلوب
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
فرآیندهای سطح زمین
پیش نمایش صفحه اول مقاله
چکیده انگلیسی
Predicting runoff and drainage from landscapes and correlating these with stream flow can be a powerful watershed management tool. We examined the feasibility of using runoff and drainage output of a simple soil-vegetation-atmosphere (SVAT) model as a predictor of monthly and daily changes in measured stream flow. Six watersheds in the eastern US were analyzed, located from approximately 35°N to 43°N. They ranged in area from 23 to 2463 km2 and were 35-65% forested. The SVAT model was parameterized with weather, soils and phenological data largely obtained from a secondary school in each watershed that is participating in the Global Learning and Observations to Benefit the Environment (GLOBE) program. This program is a United States government science education effort promoting scientific inquiry in grades K-12 by providing protocols for collecting environmental data. Monthly measured stream flow and simulated runoff + drainage over a one year period were normalized to the largest value in that period and were compared using linear regression. Simulated monthly runoff + drainage explained between 37% and 76% of the variability in monthly stream flow. Changes in daily simulated runoff + drainage and measured stream flow depended on the simulated volumetric soil water content (θv). At low θv, large precipitation events (>20 mm) did not result in increased daily simulated runoff + drainage or measured stream flow. At high or saturating θv, large precipitation events resulted in increased daily simulated runoff + drainage followed by increased measured stream flow within two days.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Journal of Hydrology - Volume 333, Issues 2â4, 15 February 2007, Pages 214-225
Journal: Journal of Hydrology - Volume 333, Issues 2â4, 15 February 2007, Pages 214-225
نویسندگان
Jeffrey Melkonian, Susan J. Riha, Jessica Robin, Elissa Levine,