The Climate of Australasia in Reference to Its Control By the Southern Ocean
The Climate of Australasia in Reference to Its Control By the Southern Ocean
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1 1 ). If now we look at the rainfall curve for one of those localities and contrast it with that of Sydney, we find that the conditions are reversed (fig. 1 2). When the rainfall is heavy THE WEATHER CYCLE 59 1 6O THE CLIMATE OF AUSTRALASIA Sydney, it is light in the interior. This fact is illustrated for the whole of New South Wales by the instructive rainfall maps of that State, prepared by Dr. Russell. The shaded areas in the maps (figs. 13 and 14) are the districts where the rainfall was a...bove the average ; and the plain areas are districts where the rainfall was below the average. In the FIG. 1 2. Departures from average rainfall on coast and interior of New South Wales.
year 1894, the whole of the inland or western district had a heavier rainfall than usual, while the coastlands had less than their average. The reverse arrangement is shown for the year 1899. The balance of the coastal and inland conditions is not always shewn with such diagrammatic simplicity, for in some years the coastal and continental rainfalls are both above the average, owing no doubt to an increase in THE WEATHER CYCLE 6l the amount of rain raised from the sea by evaporation.
What to read after The Climate of Australasia in Reference to Its Control By the Southern Ocean?
You can find similar books in the "Read Also" column, or choose other free books by J W John Walter Gregory to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
1 1 ). If now we look at the rainfall curve for one of those localities and contrast it with that of Sydney, we find that the conditions are reversed (fig. 1 2). When the rainfall is heavy THE WEATHER CYCLE 59 1 6O THE CLIMATE OF AUSTRALASIA Sydney, it is light in the interior. This fact is illustrated for the whole of New South Wales by the instructive rainfall maps of that State, prepared by Dr. Russell. The shaded areas in the maps (figs. 13 and 14) are the districts where the rainfall was a...bove the average ; and the plain areas are districts where the rainfall was below the average. In the FIG. 1 2. Departures from average rainfall on coast and interior of New South Wales.
year 1894, the whole of the inland or western district had a heavier rainfall than usual, while the coastlands had less than their average. The reverse arrangement is shown for the year 1899. The balance of the coastal and inland conditions is not always shewn with such diagrammatic simplicity, for in some years the coastal and continental rainfalls are both above the average, owing no doubt to an increase in THE WEATHER CYCLE 6l the amount of rain raised from the sea by evaporation.
What to read after The Climate of Australasia in Reference to Its Control By the Southern Ocean?
You can find similar books in the "Read Also" column, or choose other free books by J W John Walter Gregory to read onlineMoreLess
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