Meteorology, Weather, And Methods of Forecasting, Description of ...
Meteorology, Weather, And Methods of Forecasting, Description of ...
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To quickly assess the difficulty of the text, read a short excerpt:
A wind of this kind is the Fohn-wind of Switzerland.
It is warm and very dry and comes down over the mountains with great violence. It blows from the south-east and south. Its direction depends on the valleys through which it comes. The intensity of the wind diminishes with distance from the mountains. It is the southerly current of air moving from Italy toward a centre of low pressure north of the Alps.
Cause of Fohn. — As the air ascends the mountains, it is cooled dynamically by expansion. T...his cooling condenses the vapour, and there is rain on the side of the mountain from which the wind comes. The latent heat in the vapour is set free. The air in descending the moun- tain on the other side is dynamically heated by compression. Air going over without any condensation of vapour would remain unaltered in tem- perature, for it would have been warmed in the descent just as much as it had been cooled in rising. But when there is condensation of vapour the latent heat is added, so that it is much warmer after its descent than before.
What to read after Meteorology, Weather, And Methods of Forecasting, Description of ...?
You can find similar books in the "Read Also" column, or choose other free books by Thomas Russell to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
A wind of this kind is the Fohn-wind of Switzerland.
It is warm and very dry and comes down over the mountains with great violence. It blows from the south-east and south. Its direction depends on the valleys through which it comes. The intensity of the wind diminishes with distance from the mountains. It is the southerly current of air moving from Italy toward a centre of low pressure north of the Alps.
Cause of Fohn. — As the air ascends the mountains, it is cooled dynamically by expansion. T...his cooling condenses the vapour, and there is rain on the side of the mountain from which the wind comes. The latent heat in the vapour is set free. The air in descending the moun- tain on the other side is dynamically heated by compression. Air going over without any condensation of vapour would remain unaltered in tem- perature, for it would have been warmed in the descent just as much as it had been cooled in rising. But when there is condensation of vapour the latent heat is added, so that it is much warmer after its descent than before.
What to read after Meteorology, Weather, And Methods of Forecasting, Description of ...?
You can find similar books in the "Read Also" column, or choose other free books by Thomas Russell to read onlineMoreLess
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