It has been said that Australia is practically Southern
Europe, and to a very great extent this is perfectly true. It
will be seen, however, on reference to the preceding tables,
that the Australian climate is more equable than that of
Southern Europe, for there is not such a marked difference
between the hot and the cooler months. In the New
England States of North America, as exemplified by New
York, there are intensely hot summers and extremely cold
winters — to which fact attention has already been drawn.
And lastly, in India, the thermometer stands at such a
height, winter as well as summer, that Ave can only be
thankful our lines are cast in more pleasant places.
THE CLIMATE OF AUSTRALIA. 9
Having thus compared the summer and winter tempera-
tures of the Australian capitals with those of other cities in
different parts of the world, it will be advisable to direct our
attention to some details connected with the climate of these
capitals, and of the corresponding colonies generally. Com-
mencing with Sydney we find that the climate is charac-
terized by the absence of very violent changes of tempera-
ture, owing in great measure to its proximity to the ocean,
which in winter is about 10° warmer than the air. Its
summer climate is marked by the absence of hot winds,
whichrdo not come more than three or four times, and then
are short-lived, seldom lasting more than five or six hours.
For a short time in the midsummer of each year, Sydney is
visited regularly by moist sea breezes, which are enervating
to many j^ersons. While these continue the temperature
seldom rises to 80°, but there is so much moisture that they
are very oppressive. Otherwise the climate is one of the
most enjoyable in the world. In other parts of New South
Wales towns may be found varying in mean tempera-
ture from 45*8° at Kiandra to G9'l° at Bourke. Speak-
ing generally it is a fact that for the same mean
annual temperature in New South Wales the range be-
tween summer and winter temperature is less than it is
in Europe.
The climate of Melbourne is characterized by a low
average humidity, moderate rainfall, and moderate winds,
strong gales being of rather rare occurrence. The most
marked feature is the summer hot wind. A hot wind is
always a northerly Avind, and the highest temperature
generally occurs a little before the wind changes to west or
south-west. When this takes place a sudden drop to a
comparatively low temperature sometimes follows within a
few minutes. These hot winds, however, are not frequent,
only averaging eight or nine per annum. These charac-
10 THE ART OF LIVING IN AUSTRALIA.
Page 18
Presented as published in 1893. Historical recipes may not meet modern food-safety standards. Cook from the modern interpretation, not the original instructions.
AI-modernized reading of the original text
It has been said that Australia is practically Southern Europe, and to a very great extent this is perfectly true. It will be seen, however, on reference to the preceding tables, that the Australian climate is more equable than that of Southern Europe, for there is not such a marked difference between the hot and the cooler months. In the New England States of North America, as exemplified by New York, there are intensely hot summers and extremely cold winters — to which fact attention has already been drawn. And lastly, in India, the thermometer stands at such a height, winter as well as summer, that Ave can only be thankful our lines are cast in more pleasant places.
Having thus compared the summer and winter temperatures of the Australian capitals with those of other cities in different parts of the world, it will be advisable to direct our attention to some details connected with the climate of these capitals, and of the corresponding colonies generally. Commencing with Sydney we find that the climate is characterized by the absence of very violent changes of temperature, owing in great measure to its proximity to the ocean, which in winter is about 10° warmer than the air. Its summer climate is marked by the absence of hot winds, which do not come more than three or four times, and then are short-lived, seldom lasting more than five or six hours. For a short time in the midsummer of each year, Sydney is visited regularly by moist sea breezes, which are enervating to many j^ersons. While these continue the temperature seldom rises to 80°, but there is so much moisture that they are very oppressive. Otherwise the climate is one of the most enjoyable in the world. In other parts of New South Wales towns may be found varying in mean temperature from 45*8° at Kiandra to G9'l° at Bourke. Speaking generally it is a fact that for the same mean annual temperature in New South Wales the range between summer and winter temperature is less than it is in Europe.
The climate of Melbourne is characterized by a low average humidity, moderate rainfall, and moderate winds, strong gales being of rather rare occurrence. The most marked feature is the summer hot wind. A hot wind is always a northerly Avind, and the highest temperature generally occurs a little before the wind changes to west or south-west. When this takes place a sudden drop to a comparatively low temperature sometimes follows within a few minutes. These hot winds, however, are not frequent, only averaging eight or nine per annum. These charac-