Breaks in Ice on the Volga River
acquired January 29, 2004

acquired January 29, 2004 download large simulated natural color (15 m resolution) image (3 MB, JPEG, 2400x1800)
acquired January 29, 2004 download simulated natural color (15 m resolution) GeoTIFF file (12 MB, TIFF, 2400x2400)
acquired January 29, 2004 download large thermal imagery (90 m resolution) image (142 KB, JPEG, 600x450)
acquired January 29, 2004 download thermal imagery (90 m resolution) GeoTIFF file (238 KB, TIFF, 400x400)
acquired January 29, 2004 download Google Earth file (KML)

With most of the country located at high northern latitudes, far from the temperature-moderating influence of oceans, much of Russia experiences bitterly cold winters. Wintertime temperatures are usually cold enough to freeze rivers and lakes with ice crusts that are thick enough to walk and even drive on. In this image of the ice-bound Volga River in southern Russia, however, two major ice-free areas contrast sharply with the surrounding wintry landscape. These dark blue areas of open water result from different technologies, but they have a common cause: generating electricity.

This image of the Balakovo Nuclear Power Station and the Saratov Hydroelectric Power Station was captured by the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on NASA’s Terra satellite on January 29, 2004. The top, photo-like image is almost all white: the fields surrounding the city of Balakovo are snow-covered, the Volga River is ice-covered, and small puffs of clouds hang over the Balakovo Nuclear Power Plant cooling pond. The cooling pond and the stretch of open water downriver of the dam at the Saratov Hydroelectric Station are the only places free of winter’s grip.

The bottom image shows surface temperatures that ASTER observed. Both of the ice-free areas are warmer than the rest of the ice-bound river, but the area downstream of the dam is chillier than the water in the nuclear plant cooling pond. Just below the dam, the water is just barely above freezing (pink). Farther downriver, the water appears to be cold enough to freeze (blue), but turbulence from the flow of water over the dam prevents it from icing over. In the cooling pond, the temperatures are nearly 10 degrees Celsius in places. The water in the pond is not radioactive; it is part of a secondary “closed” cooling loop for the reactor. The water temperature in this cooling pond varies with the seasons and power demands, but usually is lukewarm and well above freezing even in the depth of winter.

The 40-meter- (131-foot-) high dam at Balakovo holds back the Saratov Reservoir, which extends upriver more than 350 kilometers (217 miles). In addition to generating electricity, the reservoir provides irrigation water in the Saratov Oblast (province), one of the major agricultural areas in Russia. Near the bottom of the image, the city of Balakovo is divided by a shipping channel that separates the newer island section of the city from the older city center. Though the city predates the creation of the hydroelectric power station, it grew tremendously with the arrival of engineers and construction experts in the 1960s.

You can download a 15-meter-resolution KMZ file comparing simulated natural color and thermal imagery (90-meter resolution) of the Saratov Hydroelectric Station and Balakovo Nuclear Power Plant suitable for use with Google Earth.

NASA image created by Jesse Allen, using data provided courtesy of NASA/GSFC/METI/ERSDAC/JAROS, and U.S./Japan ASTER Science Team.

Instrument(s): 
Terra - ASTER

Breaks in Ice on the Volga River

January 6, 2008
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Image Location
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