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Surface Water Hydrology
Learning Objectives To be able to quantify watershed attributes (7.1) To be able to describe the role of atmospheric and ocean circulation in hydrology and the formation of precipitation (7.1) To be able to quantify the variability of precipitation, calculate area average precipitation and determine design storm amounts (7.2) To be able to calculate evaporation from an open water surface (7.3)
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Watershed delineated on a topographic map
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Water Budget in a Watershed
From Mays, 2011, Ground and Surface Water Hydrology
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Streamstats
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Normal monthly distribution of precipitation in the US in inches
From Mays, 2011, Ground and Surface Water Hydrology
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From Dingman, 1994
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General Circulation of the Atmosphere
From Simon Wang
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Coriolis Effect
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Formation of Precipitation
Source of moisture Lifting mechanism (frontal, orographic, convective) Phase change from vapor to water - Energy Small nuclei or dust for droplet formation Droplets must grow as they fall to earth From Bedient
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Lifting Mechanisms From Bedient
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Ralph, F. M. , P. J. Neiman, G. A. Wick, S. I. Gutman, M. D
Ralph, F. M., P. J. Neiman, G. A. Wick, S. I. Gutman, M. D. Dettinger, D. R. Cayan, and A. B. White (2006), Flooding on California's Russian River: Role of atmospheric rivers, Geophys. Res. Lett., 33, L13801, doi: /2006GL
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Hurricane Katrina in the Gulf - 8/29/2005
From Bedient Katrina at 17:00 UTC
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Measuring Rainfall - Tipping
Bucket Recording gage Collector and Funnel Bucket and Recorder Accurate to .01 ft Telemetry- computer From Bedient
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Shielded and Unshielded weighing Precip (Rain and Snow Gages
Snow Pillow
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RADAR Rainfall Estimates
NEXRAD provides real-time data on a ~16 km2 (6 mi2) grid Each estimate represents an average rainfall amount over the entire 4 x 4 km2 area NEXRAD rainfall estimates compare well with point rain gage measurements (r2 ~ 0.9) From Bedient
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Normal monthly distribution of precipitation in the US in inches
From Mays, 2011, Ground and Surface Water Hydrology
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Rainfall Averaging Methods
From Bedient Rainfall Averaging Methods
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