"Alpine" pond

 

One of the ponds we studied was high on the flank of the big ridge and did not appear to be in direct contact with the ocean. The water level in this pond waxed and waned throughout the melt season. To observe these changes, we strung a reference line across the pond and periodically measured the water depth and the distance to the ice bottom. Measurement uncertainties were mainly due to the string sagging, giving errors of 2-3 cm in height. Fortunately we can correct for these errors since we know that the surface of the pond is flat. The results of these measurements are shown in the animation below. The gray shaded area is ice, the blue is water, and the light blue is snow. The overall ice melt is shown, along with changes in pond depth. By 26 August the pond surface was frozen and snow began to accumulate.  There is also an animation for the evolution of a pond at Seattle. There is also a photo showing this pond and its neighors.

 

Press Stop button on browser to end animation.

 

 

Selected profiles from the "alpine" pond.

 

 

 

 

 

 

 

 

 

 

 

 

 
                                          

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