1971
DOI: 10.1029/rs006i003p00357
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Tropospheric Effect on Electromagnetically Measured Range: Prediction from Surface Weather Data

Abstract: Knowledge of the height integral of atmospheric refractivity (n — 1), where n is the refractive index, is essential for prediction of atmospheric range effect at any elevation angle. Observed values of the height integral for the lower, nonionized atmosphere can be obtained from weather balloon ascent data. Year‐long collections of data from widely separated locations were used to relate this integral to surface data. Although (n — 1) at any point in a dry atmosphere depends on both pressure and temperature (t… Show more

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Cited by 229 publications
(124 citation statements)
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“…Analyzing the percentage of successful baselines we can establish that while for the 2D case, in all strategies and for each class, the success increases with session length, in 1D that trend is not clear. Applying the Hopfield model [5] for baselines in class R 3 and higher do not appear to produce better results with longer sessions. By adopting the strategy of computing the troposphere the benefits of longer sessions are only significant to baselines up to class R 3 and, even yet, 12 hours sessions are required (74% of success with BC, 65% with PC).…”
Section: Numerical Results and Final Remarksmentioning
confidence: 99%
“…Analyzing the percentage of successful baselines we can establish that while for the 2D case, in all strategies and for each class, the success increases with session length, in 1D that trend is not clear. Applying the Hopfield model [5] for baselines in class R 3 and higher do not appear to produce better results with longer sessions. By adopting the strategy of computing the troposphere the benefits of longer sessions are only significant to baselines up to class R 3 and, even yet, 12 hours sessions are required (74% of success with BC, 65% with PC).…”
Section: Numerical Results and Final Remarksmentioning
confidence: 99%
“…The wet mapping functions derived by Black are based on the quartic profiles developed by Hopfield and use the equivalent heights proposed by Hopfield [3]. This mapping function was recommended for elevation angles above 5å nd the slant wet delay is [17]:…”
Section: Black Modelmentioning
confidence: 99%
“…Additionally, electromagnetic waves are refracted in the neutral, lower part of the Earth's atmosphere. Influence of the neutral atmosphere is commonly referred to as the tropospheric refraction [3]. In detail, the GNSS signal slows down and its path is getting curved.…”
Section: Introductionmentioning
confidence: 99%
“…In past research, several tropospheric models have been established, such as the Modified Saastamoinen Model (Saastamoinen, 1972;1973), the Modified Hopfield Model (Hopfield, 1969;1970;. These can correct up to 90% of the tropospheric effect.…”
Section: Introduction Fast High Precision Relative Globamentioning
confidence: 99%