
| Background | Detection | Limitations | Case Study | Preparation | Bottom Line | References |
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Flash Flood Case Study
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Navajo Lake State Park: August 2003
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Here is an example of an unwarned flash flood with significant human impact that occurred at a long range (about 125 miles) from the Albuquerque radar in a portion of the New Mexico back country hydrologically favored for flash flooding.
Rugged Canyons and Arroyos Surround Navajo Lake
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The steep and rocky terrain makes this a hydrologically favored area for flash flooding; especially in normally dry arroyos and washes, where gravity forces flood waters to drain.
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Navajo Lake is Located in Northwest New Mexico on the Colorado Border
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C = Campsite in Cottonwood Canyon
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Radar Images of Evening Storms
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Taken around 915 pm, this series of composite reflectivity images depicted a couple of ordinary summer thunderstorms gradually decreasing in intensity as they passed from northeast to southwest across Navajo Lake. Also depicted are cloud-to-ground lightning strikes, mostly as small white dashes and a few white plus signs. |
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903 PM
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915 PM
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926 PM
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C = Campsite in Cottonwood Canyon
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D = Navajo Lake Dam
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Satellite Estimated Precipitable Water
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The 1201 pm geostationary satellite precipitable water estimate indicated late-day thunderstorms would be capable of producing around 25 cm (nearly 1 inch) of rain.
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Radar Precipitation Tally
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Three-hour precipitation estimates from the Albuquerque radar, and other data, indicated the late afternoon storms developed in an environment of greater instability and produced significantly more rain near the Cottonwood Canyon drainage basin than the evening storms. Although the evening storms probably produced less rain into the canyon, they may have produced greater runoff into the wash due to the already saturated ground. |
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*Approximate location
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4-7 PM
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7-10 PM
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Case Study Conclusions
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