Meteorology An Introductory Treatise
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In our eReader you can find the full English version of the book. Read Meteorology An Introductory Treatise 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 Meteorology An Introductory Treatise
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To an observer at the point A, the ray from the first position of the cloud passes along the line GCA, and from the second position along HDA, so that the angular 170 METEOROLOGY motion is measured by the angle GA'H. Thus, the velocity-height ratio is given by GH ^ LM ^ CD ^ CD ^ a < X GK « X KL « X A'B « X AB h£ The Comb Nephoscope. — The Besson Comb Nephoscope serves as an example of the direct vision nephoscope. The principle is the same as in the reflection type, but instead of watching the image, the cloud itself is observed. The comb, which consists of a number of spikes placed at equal distances apart, is adjusted so that the cloud appears to travel along the line of the spikes. Thus, the direction is obtained. The velocity-height ratio is determined by noting the time taken to travel from one spike to the next. If a is the distance between the spikes, 6 the height of the tips of the spikes above the observer's eye, and t the time in seconds, then the velocity-height ratio = ajht.
What to read after Meteorology An Introductory Treatise?
You can find similar books in the "Read Also" column, or choose other free books by A E M Alexander Ebenezer Mclean Geddes to read online
To quickly assess the difficulty of the text, read a short excerpt:
To an observer at the point A, the ray from the first position of the cloud passes along the line GCA, and from the second position along HDA, so that the angular 170 METEOROLOGY motion is measured by the angle GA'H. Thus, the velocity-height ratio is given by GH ^ LM ^ CD ^ CD ^ a < X GK « X KL « X A'B « X AB h£ The Comb Nephoscope. — The Besson Comb Nephoscope serves as an example of the direct vision nephoscope. The principle is the same as in the reflection type, but instead of watching the image, the cloud itself is observed. The comb, which consists of a number of spikes placed at equal distances apart, is adjusted so that the cloud appears to travel along the line of the spikes. Thus, the direction is obtained. The velocity-height ratio is determined by noting the time taken to travel from one spike to the next. If a is the distance between the spikes, 6 the height of the tips of the spikes above the observer's eye, and t the time in seconds, then the velocity-height ratio = ajht.
What to read after Meteorology An Introductory Treatise?
You can find similar books in the "Read Also" column, or choose other free books by A E M Alexander Ebenezer Mclean Geddes to read online
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