. . "S" . "Parameters of the gravity field harmonics outside the geoid are sought in solving the Stokes boundary-value problem while harmonics outside the Earth in solving the Molodensky boundary-value problem. The gravitational field generated by the atmosphere is subtracted from the Earth?s gravity field in solving either the Stokes or Molodensky problem. The computation of the atmospheric effect on the ground gravity anomaly is of a particular interest in this study." . "[2A16F05D49AF]" . . "Studia Geophysica et Geodaetica" . . "CZ - \u010Cesk\u00E1 republika" . "Moore, Philip" . "1"^^ . . "Atmospheric effects in the derivation of of geoid-generated gravity anomalies" . . "Nov\u00E1k, Pavel" . . . "4"^^ . . . "Vajda, Peter" . . "Atmosf\u00E9rick\u00E9 vlivy p\u0159i odvozen\u00ED t\u00EDhov\u00FDch anom\u00E1li\u00ED generovan\u00FDch geoidem"@cs . "466275" . "50" . "Atmospheric effects in the derivation of of geoid-generated gravity anomalies"@en . "Tenzer, Robert" . . . "Atmosf\u00E9rick\u00E9 vlivy p\u0159i odvozen\u00ED t\u00EDhov\u00FDch anom\u00E1li\u00ED generovan\u00FDch geoidem"@cs . "4" . "23520" . "Atmospheric effects in the derivation of of geoid-generated gravity anomalies"@en . . "Atmospheric effects in the derivation of of geoid-generated gravity anomalies" . "Parametry t\u00EDhov\u00E9ho pole harmonick\u00E9 vn\u011B geoidu jsou odvozov\u00E1ny v kontextu Stokesovy okrajov\u00E9 \u00FAlohy. Gravita\u010Dn\u00ED potenci\u00E1l generovan\u00FD atmosf\u00E9rou je ode\u010D\u00EDt\u00E1n od t\u00EDhov\u00E9ho pole Zem\u011B p\u0159i \u0159e\u0161en\u00ED Stokesovy \u010Di Molod\u011Bnsk\u00E9ho \u00FAlohy. V\u00FDpo\u010Det atmosf\u00E9rick\u00E9ho vlivu na pozemn\u00ED t\u00EDhov\u00E1 data je studov\u00E1n v tomto p\u0159\u00EDsp\u011Bvku."@cs . "RIV/49777513:23520/06:00501397!RIV09-MSM-23520___" . "0039-3169" . "RIV/49777513:23520/06:00501397" . "atmosphere; boundary-value problem; gravity anomaly; Newton?s integral"@en . . "Parameters of the gravity field harmonics outside the geoid are sought in solving the Stokes boundary-value problem while harmonics outside the Earth in solving the Molodensky boundary-value problem. The gravitational field generated by the atmosphere is subtracted from the Earth?s gravity field in solving either the Stokes or Molodensky problem. The computation of the atmospheric effect on the ground gravity anomaly is of a particular interest in this study."@en . "11"^^ .