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Salty meet up

Computer renderings of a lab-grown sea ice crystal show how brine pockets (gold) connect to form channels as temperatures increase from -15 degrees Celsius (left) to -6 degrees Celsius (middle) to -3 degrees Celsius (bottom). The amount of brine flowing through the ice can affect melting and freezing rates. Credit: K.M. Golden et al./Geophysical Research Letters 2007

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