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National Report of Sweden to the NKG General ... - Lantmäteriet

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43Kiamehr R. and Eshagh M. (2008)Estimation <strong>of</strong> variancecomponents Ellipsoidal, Geoidaland orthometrical heights, J Earth& Space Phys., 34(3) : 1-13.Kiamehr R. and Eshagh M. (2008)EGMlab, a scientific s<strong>of</strong>tware fordetermining <strong>the</strong> gravity andgradient components from globalgeopotential models, Earth Sci.Inf. 1 : 93-103.Kiamehr R., Eshagh M. and Sjöberg LE,(2008) Interpretation <strong>of</strong> <strong>the</strong>general geophysical patterns <strong>of</strong>Iran based on <strong>the</strong> gradientcomponents analysis <strong>of</strong> <strong>the</strong>GRACE , Acta Geophys., 56(2) :440-454.Kiamehr R. and Sjöberg L.E. (2010) Anoptimum way <strong>to</strong> determine aprecise gravimetric geoid basedon <strong>the</strong> least-squares modification<strong>of</strong> S<strong>to</strong>kes’ formula-A case study <strong>of</strong><strong>Sweden</strong>, Acta Geod. Geophys.Hung. 45:148-164.Sjöberg L. E. (2007) The <strong>to</strong>pographicbias by analytical continuation inphysical geodey. J Geod. 81:345-350.Sjöberg L. E. (2007) Precisedetermination <strong>of</strong> <strong>the</strong> Clairautconstant in ellipsoidal geodesy.Surv. Rev. 39:81-86.Sjöberg L. E. (2007) Answers <strong>to</strong> <strong>the</strong>comments by M. Vermeer on L.E.Sjöberg (2007) The <strong>to</strong>pographicbias by analytical continuation inphysical geodesy. J Geod. 81:345-350.Sjöberg L. E. (2008) A stricttransformation from Cartesian <strong>to</strong>Geodetic coordinate, Surv. Rev.40:156-163.Sjöberg L.E. (2008) Geodeticintersection on <strong>the</strong> ellipsoid, JGeod, 82:565-567.Sjöberg L.E. (2008) New solutions <strong>to</strong>classical geodetic problems on <strong>the</strong>ellipsoid. In M Sideris (Ed.):Observing our changing Earth.IAG Symposia Vol. 133:781-784.Sjöberg L.E. (2009) The terraincorrection in gravimetric geoidcomputation-is it needed?Geophys. J. Int. 176:14-18.Sjöberg L.E. (2009) On <strong>the</strong> <strong>to</strong>pographicbias in geoid determination by <strong>the</strong>external gravity field, J Geod.83:967-972.Sjöberg L. E. (2009) Solving Vening-Meinesz-Moritz inverse problemin isostasy, Geophys. J. Int. 179:1527-1536.Sjöberg L.E. (2010) Solving <strong>the</strong><strong>to</strong>pographic potential bias as aninitial value problem, Art. Sat.44(3): 75-84.Sjöberg L. E. (2010) A strict formula forgeoid-<strong>to</strong>-quasigeoid separation, JGeod (in press).Sjöberg L.E. and Eshagh M. (2009) Ageoid solution for airborne gravitydata, Stud. Geophys. Geod. 53:359-374.Sjöberg L.E. and Eshagh M. (2010)Considering data gaps in geoidmodelling by modifying S<strong>to</strong>kes'sformula, Acta Geod. Geophys.Hung. 45:165-183.Ågren J., Sjöberg L.E. and Kiamehr R.(2009) The new gravimetricquasigeoid model KTH08 over<strong>Sweden</strong>, J. Applied Geod.3(3):143-153.

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