Graupel

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Graupel (/ˈɡraʊpəl/; German: [ˈɡʁaʊpl̩]), also called soft hail, corn snow, hominy snow, or snow pellets,^[1] is precipitation that forms when supercooled water droplets are collected and freeze on falling snowflakes, forming 2–5 mm (0.08–0.20 in) balls of crisp, opaque rime.^[2]

Graupel is distinct from hail and ice pellets. Hail is common in thunderstorms, while graupel typically falls in winter storms and in convective showers especially at higher elevations.^[3] The METAR code for graupel is GS.

Formation[]

Falling graupel

Graupel pellets in morning, having fallen the previous day

Under some atmospheric conditions, snow crystals may encounter supercooled water droplets. These droplets, which have a diameter of about 10 μm (0.00039 in), can exist in the liquid state at temperatures as low as −40 °C (−40 °F), far below the normal freezing point. Contact between a snow crystal and the supercooled droplets results in freezing of the liquid droplets onto the surface of the crystal. This process of crystal growth is known as accretion. Crystals that exhibit frozen droplets on their surfaces are often referred to as rimed. When this process continues so that the shape of the original snow crystal is no longer identifiable, the resulting crystal is referred to as graupel.^[4]

Graupel was formerly referred to by meteorologists as "soft hail." However, graupel is easily distinguishable from hail in both the shape and strength of the pellet and the circumstances in which it falls. Ice from hail is formed in hard, relatively uniform layers and usually falls only during thunderstorms. Graupel forms fragile, oblong crystals and falls in place of typical snowflakes in wintry mix situations, often in concert with ice pellets. Graupel is also fragile enough that it will typically fall apart when touched.^[5]

Microscopic structure[]

The frozen droplets on the surface of rimed crystals are difficult to see, and the topography of a graupel particle is not easy to record with a light microscope because of the limited resolution and depth of field in the instrument.

However, observations of snow crystals with a low-temperature scanning electron microscope (LT-SEM) clearly show cloud droplets measuring up to 50 μm (0.002 in) on the surface of the crystals. The rime has been observed on all four basic forms of snow crystals, including plates, dendrites, columns and needles. As the riming process continues, the mass of frozen, accumulated cloud droplets eventually obscures the form of the original snow crystal, thereby giving rise to graupel.^[4]

• 

  Graupel encasing and hiding a snow crystal from view

• 

  Rime on both ends of a columnar snow crystal

Graupel and avalanches[]

Graupel commonly forms in high-altitude^[quantify] climates and is both denser and more granular than ordinary snow, due to its rimed exterior. Macroscopically, graupel resembles small beads of polystyrene. The combination of density and low viscosity makes fresh layers of graupel unstable on slopes, and layers of 20–30 cm (8–12 in) present a high risk of dangerous slab avalanches. In addition, thinner layers of graupel falling at low temperatures can act as ball bearings below subsequent falls of more naturally stable snow, rendering them also liable to avalanche.^[6] Graupel tends to compact and stabilise ("weld") approximately one or two days after falling, depending on the temperature and the properties of the graupel.^[7]

Gallery[]

• 

  Snowflakes can turn into graupel

• 

  Almost graupel

• 

  Graupel in shape of snowflake

See also[]

• Sleet - term variously used for frozen precipitation

References[]

External links[]

Look up graupel in Wiktionary, the free dictionary.

Wikimedia Commons has media related to Graupel.

Dictionaries[]

• 3 results for:graupel. Dictionary.com, accessed September 12, 2006.
• Graupel. Merriam-Webster Online Dictionary, accessed September 12, 2006.

Weather glossaries[]

• Weather Glossary, G. The Weather Channel, accessed September 12, 2006.
• All About Snow. National Snow and Ice Data Center (NSIDC), accessed September 12, 2006.
• Terms used by meteorologists, forecasters, weather observers, and in weather forecasts. National Oceanic and Atmospheric Administration (NOAA), accessed September 12, 2006.
• About.com Weather Glossary. Weather at About.com, accessed December 21, 2008.