File:Fundy High & Low tide.jpg

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Summary

Description
English: "This pair of images from the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on NASA’s Terra satellite shows the dramatic difference in the amount of water-covered land at the head of the southeast corner of the bay during a high tide on April 20, 2001, and a low tide on September 30, 2002. Vegetation is green, and water ranges from dark blue (deeper water) to light purple (shallow water)."
Date
Source NASA Earth Observatory, url=http://earthobservatory.nasa.gov/IOTD/view.php?id=6650
Author NASA/GSFC/METI/ERSDAC/JAROS, and U.S./Japan ASTER Science Team
Permission
(Reusing this file)
Images from NASA are usually free of copyright and are in the PUBLIC Domain.

"The large tides in the Bay of Fundy result from tidal resonance. Tidal resonance occurs when the amount of time it takes a large wave to travel from the mouth of a bay to the far shore and back to the mouth is the same, or nearly the same, as the time between the high and low tides. This coincidence means that the general sloshing of the water around the bay can become synchronized with the lunar tides, amplifying their effect. When other factors come into play, such as storm surges, the tides in the Bay of Fundy have exceeded 20 meters."

Licensing

Public domain This file is in the public domain in the United States because it was solely created by NASA. NASA copyright policy states that "NASA material is not protected by copyright unless noted". (See Template:PD-USGov, NASA copyright policy page or JPL Image Use Policy.)
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14 June 2006

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Date/TimeThumbnailDimensionsUserComment
current00:35, 28 May 2012Thumbnail for version as of 00:35, 28 May 2012540 × 720 (126 KB)Marshallsumter{{Information |Description ={{en|1="This pair of images from the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on NASA’s Terra satellite shows the dramatic difference in the amount of water-covered land at the head of the ...