Playlearn Snow, White

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If the Customer opts for replacement or exchange of Products, the affected Products MUST be returned in person to the selected Azim Bakery stores within Malaysia as directed by Azim Bakery pursuant to Item is most commonly used as a dressing due to its ability to remain on hot or warm goods, even in moist environments. It is considered a superior topping and holds up under plastic and ice cream. A snow bridge is an arch formed by snow that has drifted across a crevasse, forming first a cornice, and ultimately a covering which may completely obscure the crevasse. Frozen precipitation includes snow, snow pellets, snow grains, ice crystals, ice pellets, and hail. [12] Falling snow comprises ice crystals, growing in a hexagonal pattern and combining as snowflakes. [13] Ice crystals may be "any one of a number of macroscopic, crystalline forms in which ice appears, including hexagonal columns, hexagonal platelets, dendritic crystals, ice needles, and combinations of these forms". [14] Terms that refer to falling snow particles include:

Spring snow – Spring snow describes a variety of temperature and moisture conditions with corn snow. [38] Avery, Martin (2 February 2016). Canada, I Love You: The Canadian Dream. Lulu.com. ISBN 9781329874862. Watermelon snow – Watermelon snow is reddish pink, caused by a red-colored green algae called Chlamydomonas nivalis. [43]

Kaplan, Larry (2003). "Inuit Snow Terms: How Many and What Does It Mean?". Building Capacity in Arctic Societies: Dynamics and Shifting Perspectives. Proceedings from the 2nd IPSSAS Seminar. Nunavut, Canada: May 26-June 6, 2003. Montreal: Alaska Native Language Center . Retrieved 2 January 2019. Hail – Forms in cumulonimbus clouds as irregular spheres of ice ( hailstones) with a diameter of 5mm or more. In the US, the intensity of snowfall is characterized by visibility through the falling precipitation, as follows: [13]

National Weather Service, NOAA. "Glossary - Snow flurry". w1.weather.gov . Retrieved 29 December 2018. Snowsquall – A brief but intense period of moderate to heavy snowfall with strong, gusty surface winds and measurable snowfall. [9] Snow most frequently appears white, but deep snow can act as a filter, absorbing more of one color and less of another. Deep snow tends to absorb red light, reflecting the blue tints often seen in snow. — Credit: Pixabay Lliboutry, L. (1954b). "The origin of penitentes". Journal of Glaciology. 2 (15): 331–338. Bibcode: 1954JGlac...2..331L. doi: 10.1017/S0022143000025181. Column and plate combination (CP): Snow crystals may be a column with plane crystal at both ends, a bullet with plane crystals, a plane crystal with spatial extensions at ends.Pillow drift – A pillow drift is a snow drift crossing a roadway and usually 3 to 4.5 metres (10–15 feet) in width and 30cm to 90cm (1–3 feet) in depth. [28] Different parts of the world have their own avalanche classifications. In the United States, a number is given to rate avalanche destructiveness, where volumes and impact pressures go up exponentially like earthquake magnitude scales. Avalanches range in size from one to five, or low to extreme, with one unlikely to cause damage or bury a person. Any avalanche above a two has the potential to kill someone. The volume grows from 100 cubic meters (131 cubic yards) to 100,000 cubic meters (131,000 cubic yards) in terms of size. Snow pellets (also soft hail, graupel, tapioca snow) – Spherical or conical ice particles, based on a snowlike structure, with diameters between 2mm and 5mm. They form by accretion of supercooled droplets near or slightly below the freezing point and rebound off hard surfaces upon landing. [19]

Classification of snow on the ground comes from two sources: the science community and the community of those who encounter it in their daily lives. Snow on the ground exists both as a material with varying properties and as a variety of structures, shaped by wind, sun, temperature, and precipitation. Lopez, Barry; Gwartney, Debra (14 April 2011). Home Ground: Language for an American Landscape. Trinity University Press. p.136. ISBN 9781595340887. Trube, L.L. (1978). "The Various Russian Words for Snowstorm". Soviet Geography. 19 (8): 572–575. doi: 10.1080/00385417.1978.10640252.Sastrugi – Sastrugi are snow surface features sculpted by wind into ridges and grooves up to 3 meters high, [29] with the ridges facing into the prevailing wind. [30] Yukimarimo – Yukimarimo are balls of fine frost, formed at low temperatures on the Antarctic Plateau during light or calm winds. [37] National Weather Service, NOAA. "Glossary - Lake effect snow". w1.weather.gov . Retrieved 29 December 2018. Snow Today examines where snow is present, where it has snowed recently, and how much water is in the snow, while also comparing between snow today, snow yesterday, snow last year, and snow over the last few decades. Data