Boundary-Value Problems for Gravimetric Determination of a by Zdenek Martinec

By Zdenek Martinec

This ebook bargains a simultaneous therapy of the speculation and numerical software of boundary-value difficulties relating to the decision of an exact geoid from gravimetric info. the subsequent matters are mentioned: topographical results and their computations in unique gravimetric geoid selection, the downward continuation of a harmonic functionality, Stokes' challenge formulated on an ellipsoid of revolution, round Stokes' challenge with ellipsoidal corrections fascinated with boundary stipulations for an anomalous power, and the altimetry-gravimetry boundary-value challenge. the reply to a couple of medical difficulties, raised and mentioned in geodetic literature during the last years, are available the following. The ebook is meant for scientists and complex graduate scholars.

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Extra resources for Boundary-Value Problems for Gravimetric Determination of a Precise Geoid (Lecture Notes in Earth Sciences)

Example text

18) for the Airy-Heiskanen compensation model may be simplified as f fR-D(a) r 12 v~,~(~, a) = czx~o~o J~o J~,:~-~(~,) L(~, ¢, ~,) denS'. 27) The last integral may be readily evaluated yielding V ~'B(r, ~) = -, 4rrG~(a) -R2r r>R, 4~rG~(~)R , r < R . 28) The 2-D condensation density c~(~t) can be chosen in a variety of ways. , we will assume that. 29) Chapter 3 40 where VB(r, ~t) is the Bouguer term of topographical potential V t. 29), the condensation density a(fl) reads a(ft)--~(a)H(ft) 1+~+ 3R 2 ] .

31) where A*(Ft) . 32) are the radial components of the gravitational attraction induced by the topographical and compensated masses at the point on the Earth's surface. t2 L - l ( r , ¢ , r ') := f , L(r,¢,r,)dr' . , when V ~ = V e, the attraction of compensated masses can be derived taking the radial derivatives of eqn. 16). 19), then AB(gt) = A~'B(~) . 39) -G£ :~(a') i)L-l(r'~b'r') o OL-l(r'¢'r') 07" -- ~0c(~¢~) Or da'. 40) dgt' . 41) ~LOMohoOL-l(r, ¢, r') ~00 Or d~'. 26). 29), we get dB(a) = A~'B(a) .

7) Under the assumption that the condensation of the topographical masses conserves the topographical masses, the Cartesian. coordinates of the mass-center of the Helmert body of the mass M ~ := M a + M c = M are x~ = ~ 0~=0 e(r, ft)e,,(~)Pdrdft + o ~(~)e~(a)r~(f~)df~ . (a)+H(a) 3 G(a)er(fl)r3(a)da] . S) for ~,(a), we finally get 1 [ /rg(a)+H(a) xh = M Jao Jr=~(a) g(r, f~) [rg(Ft) - r] e~(f~)r2drda. 1o) To estimate the magnitude of the vector xhT, we approximate the density ~(r, fl) of topographical masses by a mean value ~o and the radius rg(f~) of Chapter 2 30 the geoid by a mean radius R of the Earth.

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