What Passes for Weather
We’re guaranteed to have a white Christmas (of sorts) here at the South Pole. But it won’t snow. It is normally too cold here for any form of precipitation. The snow on the ground here is different from the December snows back home. It squeaks when you step in it, and the particles in the air are not snowflakes but tiny, diamond-like fragments of solid ice swept up by the wind. We do get days when the wind whips enough ice into the air that you can see no more than ten feet in front of you. On these “white out” days, the array of flags peppering the landscape begins to make a lot of practical sense, marking the paths back to the station. The wind causes massive snow drifts, and after a large wind storm, the flags above the snow may be the only way to know where the carefully groomed roads once were.
Every few minutes, television screens in the galley display the current weather. This consists of the temperature, the wind chill, the wind speed and direction, and the physiological altitude (mainly a function of the air pressure).
Wind determines the “weather” here. Lately, it has been warm and the winds have been mild, but irregular. Last night while I was working, it seemed that every time I looked out the window the landscape had completely changed character. One moment it was blue and sunny, the next it was grey and the sky was threatening to consume the horizon and merge with the ice below. In the space of an hour the view through the science lab window changed colors and moods several times.