Turbulent Mixing Theory Applied to Radio Scattering
Turbulent Mixing Theory Applied to Radio Scattering
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The meteorological equation for the dielectric constant is"- -' e - 1 = £ ["2. 11 X 10-^ + a( 2£^ - 0. 293) x 10"^], T *- where p is the pressure in mm. Of mercury, T is the temperature in degjTees Kelvin, and a is the percentage ratio of the partial pressure of water vapor - ID - to that of dry air. Neglecting the teim -0, 293, we find that the change in 6 due to a change in temperature is where A = 2, 11 x 10~, so that values of a of about 3 percent are inquired to double the effective value ...of Ao The change in e due to a change in a is T Thus, the relation between the structure function of the dielectric constant field and the structure functions of the temperature and humidity fields is D^(r) ^ (1 . ^f ( ^)2 D^(r) + 2300( ^ )\(r), where it is assumed that temperature fluctuations are independent of humidity fluctuations o The corresponding formula for the scattering cross section is 1 (Ag)2r(i. 96a)2 2^^3^32-j -OX^ T*^ L T ^ "^ J (8) ^ -fl ( ^ ^' '(1 * — )' S"' * 230OBf 1 L^/3 For comparison with experiment, we have chosen the South Dartmouth, Mass.
What to read after Turbulent Mixing Theory Applied to Radio Scattering?
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To quickly assess the difficulty of the text, read a short excerpt:
The meteorological equation for the dielectric constant is"- -' e - 1 = £ ["2. 11 X 10-^ + a( 2£^ - 0. 293) x 10"^], T *- where p is the pressure in mm. Of mercury, T is the temperature in degjTees Kelvin, and a is the percentage ratio of the partial pressure of water vapor - ID - to that of dry air. Neglecting the teim -0, 293, we find that the change in 6 due to a change in temperature is where A = 2, 11 x 10~, so that values of a of about 3 percent are inquired to double the effective value ...of Ao The change in e due to a change in a is T Thus, the relation between the structure function of the dielectric constant field and the structure functions of the temperature and humidity fields is D^(r) ^ (1 . ^f ( ^)2 D^(r) + 2300( ^ )\(r), where it is assumed that temperature fluctuations are independent of humidity fluctuations o The corresponding formula for the scattering cross section is 1 (Ag)2r(i. 96a)2 2^^3^32-j -OX^ T*^ L T ^ "^ J (8) ^ -fl ( ^ ^' '(1 * — )' S"' * 230OBf 1 L^/3 For comparison with experiment, we have chosen the South Dartmouth, Mass.
What to read after Turbulent Mixing Theory Applied to Radio Scattering?
You can find similar books in the "Read Also" column, or choose other free books by Richard a Silverman to read onlineMoreLess
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