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The North Pole is technically a "cold desert". Very little snow falls there but it is so cold that what does fall seldom melts. In fact it is generally cold enough that the primary means by which the snow dissipates is sublimation - the direct transition of ice to water vapor without melting. It is akin to evaporation.

Monthly precipitation totals at the North Pole average less than 5 mm (0.2 in) from November through May (with a surge to about 20 mm in January), and rise to 10 to 20 mm June through October. If you average it out, daily snowfall at the North Pole would work out to be less than 1 mm.

It should be noted that much of the precipitation is actually in the form of snow that has already fallen elsewhere and then is swept up and entrained by the wind to fall again. High winds often stir up snow, creating the illusion of continuous snowfall. Since it is difficult - if not impossible - to distinguish between new snowfall and snow that fell somewhere else and then was picked up by the winds and redeposited (still frozen) at the North Pole, the total precipitation reported suggests more snow accumulation than is actually observed.

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