EPOD - a service of USRA
The Earth Science Picture of the Day (EPOD) highlights the diverse processes and phenomena which shape our planet and our lives. EPOD will collect and archive photos, imagery, graphics, and artwork with short explanatory
captions and links exemplifying features within the Earth system. The
community is invited to contribute digital imagery, short captions and
relevant links.
Archive - Explaining Ring Patterns in a Frozen Puddle
January 26, 2020
IceRingsIMG_2777 (2)
Each Sunday we present a notable item from our archives. This EPOD was
originally published January 28, 2014.
Photographer: Douglas Stith
Summary Authors: Douglas Stith; Steven Arcone; Zachary Stith
My son, Zachary, found this curious frozen puddle in Concord, New
Hampshire on the afternoon of February 1, 2013. January 31 had
unseasonably warm temperatures (in the 50’s F, about 12 C) and heavy
rain, but temperatures plummeted after sundown. The official morning
temperature on February 1 was 16 F (-9 C), but the temperature was
still well below freezing later in the day. The puddle’s diameter was
approximately 6 ft (2 m). Upon closer inspection, we found that the
ice wasn't completely frozen to the puddle's shallow bottom. We
easily picked up the thin frozen layers on the puddle that were no more
than about a quarter-inch (5 mm) thick. We also observed slight bulges
below the rings of ice. The overall milky-white color resulted from the
presence of minute air bubbles, but some clear bubbles were also
present.
How various ice features form, change shape and melt is rarely
straightforward and sometimes quite confounding. Factors such as water
purity, the rate of cooling, the preferred growth of ice in crystalline
planes, etc., all play a role.
The shallowness of this puddle suggests that it rapidly froze; only a
thin water layer remained below the puddle. Then the fast-falling
temperatures likely caused the ice to contract, which produced the
cracking. Continued cooling widened the cracks. The ring pattern shows
that the main direction of the stress force was radial, but the
scalloped pattern along the rings shows that some stress varied with
angle around the center. The small amount of water that didn't freeze
rose into the cracks due to the hydrostatic pressure of the ice
above and capillary action. Water in the rings then froze and
expanded, and as it did it widened the rings and also directed the
remaining small amount of liquid to the top of the ice. The slight
bulges on the bottom of the rings were remnants of its last contact
with the deepest water. In other words, the unfrozen water at the
bottom of the puddle was, in essence, pushed and suctioned into the
cracks.
Photo Details: Camera: Canon PowerShot SX120 IS; Lens: 6.0-60.0 mm;
Focal Length: 6mm; Aperture: f/2.8; Exposure Time: 0.033 s (1/30); ISO
equiv: 250.
* Concord, New Hampshire Coordinates: 43.2067, -71.5381
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Cryosphere Links
* Guide to Frost
* What is the Cryosphere?
* Bentley Snow Crystals
* Glaciers of the World
* Ice, Snow, and Glaciers: The Water Cycle
* The National Snow and Ice Data Center Google Earth Images
* Snow and Ice Crystals
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