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  3. File:February 08-09, 2013 Blizzard Storm Total Snow ...

    en.wikipedia.org/wiki/File:February_08-09,_2013...

    File:February 08-09, 2013 Blizzard Storm Total Snow Accumulation.gif. Add languages. Page contents not supported in other languages. ... Download QR code ...

  4. Precipitation - Wikipedia

    en.wikipedia.org/wiki/Precipitation

    The relationship between snow height and water equivalent depends on the water content of the snow; the water equivalent can thus only provide a rough estimate of snow depth. Other forms of solid precipitation, such as snow pellets and hail or even sleet (rain and snow mixed), can also be melted and measured as their respective water ...

  5. Freshet - Wikipedia

    en.wikipedia.org/wiki/Freshet

    Freshets are the result of the mass delivery of water to the landscape, either by snowmelt, heavy rains, or a combination of the two. Specifically, freshets occur when this water enters streams and results in flooding and high flow conditions. When freshets occur in the winter or early spring, the frozen ground can contribute to rapid flooding.

  6. Watch: Feet of lake-effect snow piles up along Great Lakes ...

    www.aol.com/videos-chaos-ensues-along-great...

    A high-impact lake-effect snowstorm has brought feet of snow to communities along the Great Lakes from Michigan to New York, and another foot or more of snow is likely to fall in some of those ...

  7. Snow forecast: Great Lakes bracing for heavy snowfall this ...

    www.aol.com/news/snow-forecast-great-lakes...

    Lake effect snow is set to hit parts of the Great Lakes region, including Michigan and western New York, throughout the week. Snow forecast: Great Lakes bracing for heavy snowfall this week as ...

  8. Accretion (meteorology) - Wikipedia

    en.wikipedia.org/wiki/Accretion_(meteorology)

    Accretion is defined as the gradual collection of something over time. [1] In meteorology or atmospheric science it is the process of accumulation of frozen water as precipitation over time as it descends through the atmosphere, in particular when an ice crystal or snowflake hits a supercooled liquid droplet, which then freeze together, increasing the size of the water particle.

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