On the Structure of Moving Cyclones
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In our eReader you can find the full English version of the book. Read On the Structure of Moving Cyclones Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book On the Structure of Moving Cyclones
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The back of the head has, as far as we know, an almost horizontal course interrupted only by some small waves. Data concerning its continuation to greater heights are not yet to hand.
Fig. 4 b shows the horizontal field of flow in the nearest vicinity af the squall surface, and Fig. 4 a gives a vertical section of the same motion, under the supposition that the head has the same character as in W. Schmidt's experiment. The sqall surface itself is represented by the dotted line on both figures. ...The cold air flowing in from the left displaces the warm air in front of it. The warm air is forced rapidly to ascend the abrupt front of the head, in order afterwards to perform only occasional ascensions and descensions.
At the centre of the cyclone the steering and the squall surface join into one. The entire surface, cutting the ground along the steering and squall line, forms a wide flat valley, conveying the warm air current upwards over the underlying cold air.
Fig. 4. Squall line.
*) . 1.
What to read after On the Structure of Moving Cyclones?
You can find similar books in the "Read Also" column, or choose other free books by Jakob Bjerknes to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
The back of the head has, as far as we know, an almost horizontal course interrupted only by some small waves. Data concerning its continuation to greater heights are not yet to hand.
Fig. 4 b shows the horizontal field of flow in the nearest vicinity af the squall surface, and Fig. 4 a gives a vertical section of the same motion, under the supposition that the head has the same character as in W. Schmidt's experiment. The sqall surface itself is represented by the dotted line on both figures. ...The cold air flowing in from the left displaces the warm air in front of it. The warm air is forced rapidly to ascend the abrupt front of the head, in order afterwards to perform only occasional ascensions and descensions.
At the centre of the cyclone the steering and the squall surface join into one. The entire surface, cutting the ground along the steering and squall line, forms a wide flat valley, conveying the warm air current upwards over the underlying cold air.
Fig. 4. Squall line.
*) . 1.
What to read after On the Structure of Moving Cyclones?
You can find similar books in the "Read Also" column, or choose other free books by Jakob Bjerknes to read onlineMoreLess
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