The Structure of the Atmosphere in Clear Weather a Study of Soundings With Pilo
The Structure of the Atmosphere in Clear Weather a Study of Soundings With Pilo
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In our eReader you can find the full English version of the book. Read The Structure of the Atmosphere in Clear Weather a Study of Soundings With Pilo 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 The Structure of the Atmosphere in Clear Weather a Study of Soundings With Pilo
What reading level is The Structure of the Atmosphere in Clear Weather a Study of Soundings With Pilo book?
To quickly assess the difficulty of the text, read a short excerpt:
M.
6-3 a * 5 6. 43 10-2 a 94 292 6 10. 33 a. M.
2-8 c 197 310 6 0. 27 p. M.
8-0 a * 6 6. 25 12-8 a;f 81 305 7 2. 52 13-0 c;f 41 290 * 7 6. 29 15-0 c;f 46 272 16 6. 22 3-0 e2 31 0. 13 4-3 b June 1 10. 23 a. M.
2-4 d , 3 0. 5 p. M.
1-2 c 3 0. 59 3-6 e2 21 7. 0 4-2 b Aug. 5 0. 8 2-8 a 5 2. 30 8-0 a 5 6. 33 185 a;f 19 254 1910 *Mar. 3 4. 30 p. M.
15-2 c;f 20 265 * Ballon sonde.
112 84 THE STRUCTURE OF THE ATMOSPHERE IN CLEAR WEATHER TABLE OF THE ASCENTS GIVING THE WIND VELOCITIES IN METRES PER SECO...ND AND THE WIND DIRECTIONS IN DEGREES FROM NORTH (THROUGH EAST, SOUTH, AND WEST) FOR EVERY HALF KILOMETRE.
Figures in square brackets indicate that the height opposite the figures has been nearly but not quite reached.
All ascents are from Ditcham and observed with one theodolite unless otherwise stated.
The cause of cessation of observations when it has been recorded, is given by the words distance, clouds, etc. , in the notes at the foot of the column of observations.
CLASS (a).
''Solid" current; little change in velocity or direction, wind reaches the gradient value and does not increase very much at greater altitudes.
What to read after The Structure of the Atmosphere in Clear Weather a Study of Soundings With Pilo?
You can find similar books in the "Read Also" column, or choose other free books by C J P Charles John Philip Cave to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
M.
6-3 a * 5 6. 43 10-2 a 94 292 6 10. 33 a. M.
2-8 c 197 310 6 0. 27 p. M.
8-0 a * 6 6. 25 12-8 a;f 81 305 7 2. 52 13-0 c;f 41 290 * 7 6. 29 15-0 c;f 46 272 16 6. 22 3-0 e2 31 0. 13 4-3 b June 1 10. 23 a. M.
2-4 d , 3 0. 5 p. M.
1-2 c 3 0. 59 3-6 e2 21 7. 0 4-2 b Aug. 5 0. 8 2-8 a 5 2. 30 8-0 a 5 6. 33 185 a;f 19 254 1910 *Mar. 3 4. 30 p. M.
15-2 c;f 20 265 * Ballon sonde.
112 84 THE STRUCTURE OF THE ATMOSPHERE IN CLEAR WEATHER TABLE OF THE ASCENTS GIVING THE WIND VELOCITIES IN METRES PER SECO...ND AND THE WIND DIRECTIONS IN DEGREES FROM NORTH (THROUGH EAST, SOUTH, AND WEST) FOR EVERY HALF KILOMETRE.
Figures in square brackets indicate that the height opposite the figures has been nearly but not quite reached.
All ascents are from Ditcham and observed with one theodolite unless otherwise stated.
The cause of cessation of observations when it has been recorded, is given by the words distance, clouds, etc. , in the notes at the foot of the column of observations.
CLASS (a).
''Solid" current; little change in velocity or direction, wind reaches the gradient value and does not increase very much at greater altitudes.
What to read after The Structure of the Atmosphere in Clear Weather a Study of Soundings With Pilo?
You can find similar books in the "Read Also" column, or choose other free books by C J P Charles John Philip Cave to read onlineMoreLess
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