Geodesy, the Concepts |
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Page 207
... linear model by its linear approximation . When analysing this problem , POPE [ 1974 ] employed the Newton- Gauss iterative method for solving non - linear problems and discovered that the non - linear solution can be arrived at by a ...
... linear model by its linear approximation . When analysing this problem , POPE [ 1974 ] employed the Newton- Gauss iterative method for solving non - linear problems and discovered that the non - linear solution can be arrived at by a ...
Page 249
... linear filter , where the smoothed series is a linear function of the original series . It can be written as l ' = Fl , ( 14.16 ) where the filter F is simply a matrix . It can easily be understood that , again , the least - squares ...
... linear filter , where the smoothed series is a linear function of the original series . It can be written as l ' = Fl , ( 14.16 ) where the filter F is simply a matrix . It can easily be understood that , again , the least - squares ...
Page 677
... linear equation 28 linear filter 249 linear form 245 linear implicit model 180 linear integral equation : Fredholm 37 linear model explicit in x 178 linear model explicit in / 180 linear operator 26 linear orbital perturbation 555 ...
... linear equation 28 linear filter 249 linear form 245 linear implicit model 180 linear integral equation : Fredholm 37 linear model explicit in x 178 linear model explicit in / 180 linear operator 26 linear orbital perturbation 555 ...
Contents
HISTORY OF GEODESY | 6 |
GEODESY AND OTHER DISCIPLINES | 20 |
STRUCTURE OF GEODESY | 46 |
Copyright | |
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accuracy adjustment angle approximation astronomical axis azimuth C₁ called Chapter coefficients components computed considered coordinate system correction covariance matrix CT system datum defined deflection deformation denoted derived design matrix determined direction displacement earth earth's gravity field earth's surface effect ellipse equipotential surfaces error estimated evaluated filter formula frequency geocentric geodesy geodetic geoid geoidal height given global gradient gravity anomalies height differences horizontal networks integral inverse known least-squares linear lithosphere mass mathematical model mean measured meridian motion normal equations normal gravity nutation observations obtained orbital orthometric height plane plumb line polar motion position potential probability density function problem quadratic form quantities reference ellipsoid refraction relative residual satellite sea level shown in FIG solution space spherical spin statistically dependent statistically independent techniques tidal transformation unknown parameters VANÍČEK variance variations vector velocity vertical