Page:Hunt - The climate and weather of Australia - 1913.djvu/133

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73

Synchronous observations are received by telegraph from a number of stations from as wide an area as possible.

The following table gives the number and equipment of stations reporting daily to the Central Bureau:—

9 a.m. Reports. 3 p.m. Reports. 6 p.m. Reports.
Stations
with
Instruments.
Wind,
Weather,
and Rain
Report.
Rain only
(when any).
Instrument
Stations.
Wind and
Weather.
Rain only.
Western Australia 34 .. 72   1 .. ..
South Australia 18    4 72   4 .. ..
Queensland 40 .. 59   1 .. ..
New South Wales 15    1 99   2 .. ..
Victoria 45 150 10 27 5 158
Tasmania 12 .. 19   1 .. ..
New Zealand   3 .. .. .. .. ..
New Caledonia   2 .. .. .. .. ..
Norfolk Islands   1 .. .. .. .. ..
Cocos Islands   1 .. .. .. .. ..
Rodriguez   1 .. .. .. .. ..
Batavia   1 .. .. .. .. ..
Singapore   1 .. .. .. .. ..
Hong Kong   1 .. .. .. .. ..
  175 155 331 36 5 158

Note.—Extra 3 p.m. and 6 p.m. reports are also received at the Divisional Offices in each State.

Stations with Instruments.

Wireless.
Port Moresby (Papua) 1
Macquarie Island 1
Adelie Land 1
Ships (average) 9 to 10 weekly

The barometer readings after being reduced to sea—level, to freezing point, and for standard gravity, are plotted on a separate chart, together with wind direction and wind velocity.

All readings of the same height are then connected up by lines or isobars, thus we have invariably presented on the charts a number of contour curves which represent graphically the different pressures of the atmosphere prevailing over those portions of the earth's surface under review.

Other secondary charts are also compiled for discussion. On one is shown by figures and shading the synchronous weather throughout Australasia, the amount of cloud, rain recorded, and temperatures; on a second, the variations of pressure for the 24 hours, which indicate in a measure the probable direction of atmospheric drift; on a third, the variation in temperature for the same interval of time, and this is useful in suggesting the probable route of hot and cold waves.

All these factors are discussed together with the conditions assumed to be normal for the time of the year, and from them the forecast deductions are made.