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Hydrologic Applications: Snow Cover; Flooding

These views of frozen water carry us naturally into the last topic - hydrology - in this Section. In this context, hydrology refers to aspects of water distribution and management on land surfaces. We will discuss here two of the three principal uses of satellites for hydorlogic applications: runoff prediction and flood monitoring/damage assessment. The third - drainage basin characterization - will not be considered.

Obviously, metsats can provide near real time indications of weather conditions that can be interpreted as forecasts of severe storms and heavy rainfall. Over a longer period, potential flooding from spring thaws can be predicted, and estimates of expected quantities of water runoff made by repetitive monitoring snow cover over large regions. Satellite observations of surfaces blanketed by snow - in the U.S. principally in mountains and high prairies - suffice to measure the areal extent of the masses likely to melt. Seasonal variation in snow cover from year to year is illustrated by this pair of Landsat-1 images of the central Sierra Nevada highlands.

Thickness variations and packing densities must, however, be determined from onsite ground measurements in order to fix anticipated volumes. This information is important not only for flood warnings and control but also as an estimator of water supply from reservoir fillings, river channeling, and aqueduct retrieval.

Images from both the NOAA and the GOES satellites are used routinely to determine extent of snow cover (snow can be separated from clouds - both being highly reflective in the visible and photographic IR - because of differences in spectral absorption in longer wavelength bands; TM Band 5 also can distinguish snow/clouds, and thermal responses vary as well). Here is a color composite made from three NOAA-12 AVHRR bands (1,3,4 = RGB) showing snow in April 1995 in the northwestern U.S. as red:

Major snow storms can bring about heavy cover that can cause extensive flooding if a thaw sets in rapidly. Look (top, below) at this GOES-8 coverage of a massive storm that hit the northeastern U.S. on January 7, 1996; the bottom image taken after storm passage and return of clear skies shows the extent of snow cover.



Its damaging effects were brought home to the writer (NMS) very quickly. A combination of ice followed by more than 50 cm (20 inches) of snow and then a rapid thaw led to basement flooding in his house (located on the side of a hill away from any floodplain). While the above images didn't play a role in this instance, it is almost "comforting" to see afterwards how violent was this storm and vast its output of snow.

The National Weather Service keeps an up-to-date map of snow cover for the U.S. as exemplified here for March 9-12 of 1997. This map encompasses areas with snow but not every part of the blue-area surface actually has a cover.


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Code 935, Goddard Space Flight Center, NASA
Written by: Nicholas M. Short, Sr. email: nmshort@epix.net
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Updated: 1999.03.15.