February on Kilimanjaro is typically a rather dry month, a mini dry season sandwiched between the short-rains of roughly November-December, and the long-rains during the March-April-May period. Last month followed this pattern, excepting a brief, important event occurring mid-month.
At the summit, snowfall began late on the 14th and appears to have
continued all day on the 15th. The 16th may have been dry in the
morning, but by evening telemetry data suggest that snowfall began
again, with increased wind speed that may have caused drifting of the
fresh snow. Reports from climbers on the mountain mention heavy snowfall at Arrow Glacier Camp and in the Western Breach. By early on the 18th the event was over and dry conditions
again prevailed on into early March.
This February event is important because it was the largest snowfall
event since the long-rains of 2014, totaling 16.5 cm. This is ~2 cm
greater than the event of late-November into early-December 2014.
Although events of this magnitude pale in comparison with those on other
mountains, they must be viewed in context; the summit of Kilimanjaro is
very dry. Snowfall on the summit glaciers adds mass to horizontal
surfaces, and more importantly - a bright, smooth snow surface changes
the energy balance both on the glaciers and on surrounding caldera
surfaces adjacent to the vertical walls.