Frontal Motion in the Atmosphere
Frontal Motion in the Atmosphere
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In our eReader you can find the full English version of the book. Read Frontal Motion in the Atmosphere 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 Frontal Motion in the Atmosphere
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Now the front remains closer to its initial value and even moves somewhat southward to the west of the front. This movement Increases the length of the cold front where we have the steep slope.
In case II we change the initial velocities and height distribution to conform to the condition of a geostro- phic wind. The position of the front is again initially sinusoidal and since the initial wind field is geostrophic we have -rr- = and -tt- = 0. Thus, the initial slope of the height of the cold a...ir, -5—, is constant with respect to y but is variable with respect to x. The boundary conditions are the same as in our original formulation, case I. These initial conditions are physically more reasonable than those of initially constant velocities. However, this prolem was more difficult to handle numerically. Figure 15 shows the position of the front after 11 hours and 18 hours have elapsed. As in the previous cases the entire frontal system progresses eastward relative to the moving coordinate system.
What to read after Frontal Motion in the Atmosphere?
You can find similar books in the "Read Also" column, or choose other free books by Eli L Turkel to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Now the front remains closer to its initial value and even moves somewhat southward to the west of the front. This movement Increases the length of the cold front where we have the steep slope.
In case II we change the initial velocities and height distribution to conform to the condition of a geostro- phic wind. The position of the front is again initially sinusoidal and since the initial wind field is geostrophic we have -rr- = and -tt- = 0. Thus, the initial slope of the height of the cold a...ir, -5—, is constant with respect to y but is variable with respect to x. The boundary conditions are the same as in our original formulation, case I. These initial conditions are physically more reasonable than those of initially constant velocities. However, this prolem was more difficult to handle numerically. Figure 15 shows the position of the front after 11 hours and 18 hours have elapsed. As in the previous cases the entire frontal system progresses eastward relative to the moving coordinate system.
What to read after Frontal Motion in the Atmosphere?
You can find similar books in the "Read Also" column, or choose other free books by Eli L Turkel to read onlineMoreLess
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