Results 291 to 300 of about 1,272,248 (329)
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Nature, 1971
DURING the winter 1969–1970 we installed an 8 inch tipping-bucket recording rain gauge on a large spar-buoy, Totem, located at 45° 04′ N latitude 124° 44′ W longitude. This is about 56 km west of Cascade Head, Oregon. The water caught in the gauge was retained on the buoy and measured at intervals of approximately 1 month.
W P, Elliott, R, Egami, G, Rossknecht
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DURING the winter 1969–1970 we installed an 8 inch tipping-bucket recording rain gauge on a large spar-buoy, Totem, located at 45° 04′ N latitude 124° 44′ W longitude. This is about 56 km west of Cascade Head, Oregon. The water caught in the gauge was retained on the buoy and measured at intervals of approximately 1 month.
W P, Elliott, R, Egami, G, Rossknecht
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The effect of rainfall changes on economic production
Nature, 2022M. Kotz, A. Levermann, L. Wenz
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Extreme rainfall reduces one-twelfth of China’s rice yield over the last two decades
Nature Food, 2023Jin Fu +18 more
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Rainfall Generator for Nonstationary Extreme Rainfall Condition
Journal of Hydrologic Engineering, 2019AbstractStochastic weather generators are generally used to produce scenarios of climate variability on a daily timescale for hydrological modeling and water resource planning applications.
V. Agilan, N. V. Umamahesh
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Estimating actual rainfall from satellite rainfall products
Atmospheric Research, 2009Abstract The lack of uncertainty measures in operational satellite rainfall (SR) products leads to a situation where users of the SR products know that there are significant errors in the products, but they have no quantitative information about the distribution of these errors.
Jun Yan, Mekonnen Gebremichael
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Separation of Rainfall Excess from Total Rainfall
Water Resources Research, 1969Twenty‐seven unit hydrographs from the Ralston Creek basin in Iowa are used to develop a general dimensionless unit hydrograph. A dimensionless unit hydrograph procedure is used with excess rainfall rates to synthesize historic hydrographs of Ralston Creek.
David R. Scully, Donald L. Bender
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Raindrop size distribution and terminal velocity for rainfall erosivity studies. A review
Journal of Hydrology, 2019The knowledge of the rainfall drop size distribution (DSD) at the land surface is essential for understanding precipitation mechanisms affecting soil erosion processes. Rainfall erosivity is defined as the potential of rain to cause erosion and it can be
M. A. Serio, F. Carollo, V. Ferro
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The effects of rainfall on rainfall
Science, 2016Atmospheric Science![Figure][1] In the United States, soil moisture in the east or west has opposite effects on future rainfall. PHOTO: GEORGE RANALLI/SCIENCE SOURCE Soil moisture, which is controlled in part by past rainfall, can affect the probability of future rainfall over large areas.
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Effective and efficient global optimization for conceptual rainfall‐runoff models
, 1992Q. Duan, S. Sorooshian, V. Gupta
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