The accuracy of United States precipitation data

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Abstract

When these measurements are used to obtain areal averages, particularly in mountainous terrain, additional biases may be introduced because most stations are at lower elevations in exposed sites. Gauge measurements tend to be underestimates of the true precipitation, largely because of wind-induced turbulence at the gauge orifice and wetting losses on the internal walls of the gauge. These are not trivial as monthly estimates of this bias often vary from 5% to 40%. Biases are larger in winter than in summer and increase to the north in the US due largely to the deleterious effect of the wind on snowfall. -from Authors

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APA

Groisman, P. Y., & Legates, D. R. (1994). The accuracy of United States precipitation data. Bulletin - American Meteorological Society, 75(2), 215–227. https://doi.org/10.1175/1520-0477(1994)075<0215:TAOUSP>2.0.CO;2

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