radiate less of his internal heat? The most interesting example of Polar colouring here is the increased proportion of albinos amongst the giant petrels found in high latitudes.
To-day have had our first game of football; a harassing southerly wind sprang up, which helped my own side to the extent of three goals.
This same wind came with a clear sky and jumped up and down in force throughout the afternoon, but has died away to-night. In the afternoon I saw an ominous lead outside the Island which appeared to extend a long way south. I'm much afraid it may go across our pony track from Hut Point. I am getting anxious to have the hut party back, and begin to wonder if the ice to the south will ever hold in permanently now that the Glacier Tongue has gone.
Wednesday, May 3.—Another calm day, very beautiful and clear. Wilson and Bowers took our few dogs for a run in a sledge. Walked myself out over ice in North Bay—there are a good many cracks and pressures with varying thickness of ice, showing how tide and wind shift the thin sheets—the newest leads held young ice of 4 inches.
The temperature remains high, the lowest yesterday −13°; it should be much lower with such calm weather and clear skies. A strange fact is now very commonly noticed: in calm weather there is usually a difference of 4° or 5° between the temperature at the hut and that on Wind Vane Hill (64 feet), the latter being the higher. This shows an inverted temperature.
As I returned from my walk the southern sky seemed
