Handy Book of MeteorologyW. Blackwood and Sons, 1868 - 371 sider |
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Side 106
... coast , from which , owing to the labours of the Scottish Meteorological Society , we have sys- tematic observations during the last ten years . From these observations we learn that the mean annual temperature at the mouth of Loch Fyne ...
... coast , from which , owing to the labours of the Scottish Meteorological Society , we have sys- tematic observations during the last ten years . From these observations we learn that the mean annual temperature at the mouth of Loch Fyne ...
Side 107
... coast of Scotland . The sea is also 1 ° .0 warmer than the air , and among the islands in the north it is 3 ° .0 warmer . But it is during winter that the difference between the temperature of the Atlantic and the North Sea is most ...
... coast of Scotland . The sea is also 1 ° .0 warmer than the air , and among the islands in the north it is 3 ° .0 warmer . But it is during winter that the difference between the temperature of the Atlantic and the North Sea is most ...
Side 110
... coast of North America are caused by the well - known current from the frozen seas of the arctic regions which flows southward on the great bank of Newfoundland . 237. On the west coast of North America , the temperature of the sea ...
... coast of North America are caused by the well - known current from the frozen seas of the arctic regions which flows southward on the great bank of Newfoundland . 237. On the west coast of North America , the temperature of the sea ...
Side 111
... coast of South America , thus raising the whole temperature of that coast . The effect of the two opposite currents on the coasts of this continent , is to raise the temperature on the east coast from 8 ° to 10 ° above that on the west ...
... coast of South America , thus raising the whole temperature of that coast . The effect of the two opposite currents on the coasts of this continent , is to raise the temperature on the east coast from 8 ° to 10 ° above that on the west ...
Side 112
... - land was passed . Was the low temperature of the sea on the British coast from the Wash to Berwick , caused by a cold current from the Baltic Sea ( where the temperature 112 THE DISTRIBUTION OF TERRESTRIAL TEMPERATURE .
... - land was passed . Was the low temperature of the sea on the British coast from the Wash to Berwick , caused by a cold current from the Baltic Sea ( where the temperature 112 THE DISTRIBUTION OF TERRESTRIAL TEMPERATURE .
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