The Everest Experience

"Snow Snow" Avalanche and Mountaineering Period
Everest is extremely cold, and the water vapor in the atmosphere is extremely low. The annual precipitation may be only tens of millimeters. The accumulation of snow is caused by the low temperature after snowfall. And the snowfall at low temperatures is not a "snowflake" but a "snowshake" and cannot be shaped into snowballs.

Similar to the low temperature of the Antarctic inland. The snow on the slope exceeds a certain thickness, overcomes the friction, and falls down to form an avalanche. In the rainy season in the Everest region, the amount of snow is the highest in the summer, so the summer is also the season with the highest number of avalanches in the whole year. The avalanche is extremely fast, and thousands of tons of snow are spreading quickly and electrically. Therefore, Dengzhufeng has severe cold and windy winds in the winter months and frequent avalanches in the summer months. Nature only gives Everest climbers about two months in the Spring and Autumn Period. So far, the successful Everest summit time has been within these two periods of time. Most of them were in May because the wind speed was already small and the temperature rose. The rain (snow) season has not yet begun.

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