it was learned afterwards that none of them had been received by any station.]
"June 13.—The temperature in the chart-room ranges from zero to a little above freezing-point. This is a very disturbing factor in rates of the chronometers (five in number, 3 G.M.T. and 2 Sid.T.), which are kept in cases in a padded box, each case covered by a piece of blanket, and the box covered by a heavy coat. In any enclosed place where people pass their time, the niches and places where no heat penetrates are covered with frozen breath. There will be a big thaw-out when the temperature rises.
"June 14.—Mount Melbourne is bearing north 14° W (true). Our approximate position is forty miles east-north-east of Nordenskjold Ice Tongue. At 9 p.m. Hooke called Cape Evans and sent weather reports to Wellington and Melbourne via Macquarie Island. Hooke and Ninnis on several evenings at about 11 o'clock have heard what happened to be faint messages, but unreadable. He sent word to Macquarie Island of this in hopes that they would hear and increase the power.
"June 20.—During this last blow with its accompanying drift-snow there has been much leakage of current from the aerial during the sending of reports. This is apparently due to induction caused by the snow accumulating on the insulators aloft, and thus rendering them useless, and probably to increased inductive force of the current in a body of snowdrift. Hooke appears to be somewhat downhearted over it, and, after discussing the matter, gave me a written report on the non-success (up to the present time) of his endeavours to establish communication. He thinks that the proximity of the Magnetic Pole and Aurora Australis might affect things. The radiation is good and sufficient for normal conditions. His suggestion to lead the down lead wires out to the ahead and astern would increase scope, but I cannot countenance it owing to unsettled state of ice and our too lofty poles.
"June 21.—Blowing gale from south-west throughout day, but for short spell of westerly breeze about 5 p.m. Light drift
