. "1"^^ . "Earth gravity field" . . "0"^^ . . "2014-03-31+02:00"^^ . . "0"^^ . . . "2013-02-01+01:00"^^ . "Study of the Earth's gravity field by means of data from the GOCE satellite"@en . "2016-12-31+01:00"^^ . . . . "GA13-36843S" . . . . "2015-04-23+02:00"^^ . "ESA\u2019s Gravity field and steady-state Ocean Circulation Explorer (GOCE) is the most challenging space mission for mapping the Earth's gravitational field ever launched. The mission duration is planned until end of 2012, with possible prolongation. Our project is dedicated to multipurpose GOCE data processing with two main topics. The first topic deals with the gravity field modelling based on the GOCE data. The aim is to develop new methods to compute geopotential models. The long wavelength part of the models come from the inversion of the GOCE kinematic orbits, the shortwave part is based on the gradiometer measurements of the gravity gradients in space. We will also study the problem of resolvability of the gravity field solution for a given resonant orbit. The second topic deals with various geoapplications (impact craters, regional geomorphological processes, interpretation of the gravity field invariants and others)."@en . . . . "5"^^ . "Studium gravita\u010Dn\u00EDho pole Zem\u011B na z\u00E1klad\u011B dat dru\u017Eice GOCE" . "http://www.isvav.cz/projectDetail.do?rowId=GA13-36843S"^^ . "5"^^ . "Dru\u017Eicov\u00E1 mise %22Gravity field and steady-state Ocean Circulation Explorer%22(GOCE) je nejmodern\u011Bj\u0161\u00EDm p\u0159\u00EDstrojem ke studiu gravita\u010Dn\u00EDho pole Zem\u011B, jak\u00FD kdy byl na ob\u011B\u017Enou dr\u00E1hu vynesen. Jej\u00ED \u017Eivotnost pl\u00E1nuje Evropsk\u00E1 kosmick\u00E1 agentura (ESA) do konce roku 2012 s mo\u017En\u00FDm prodlou\u017Een\u00EDm. P\u0159edkl\u00E1dan\u00FD projekt ur\u010Den\u00FD k anal\u00FDze dat dru\u017Eice GOCE m\u00E1 dv\u011B hlavn\u00ED t\u00E9mata. Prvn\u00ED t\u00E9ma se t\u00FDk\u00E1 modelov\u00E1n\u00ED gravita\u010Dn\u00EDho pole z dat GOCE. C\u00EDlem je v\u00FDvoj nov\u00FDch metod pro v\u00FDpo\u010Det modelu gravita\u010Dn\u00EDho pole. Dlouhovlnn\u00E1 \u010D\u00E1st modelu je zalo\u017Eena na inverzi kinematick\u00FDch drah GOCE, kr\u00E1tkovlnn\u00E1 \u010D\u00E1st pou\u017E\u00EDv\u00E1 m\u011B\u0159en\u00ED prvn\u00EDho kosmick\u00E9ho gravita\u010Dn\u00EDho gradientometru. Budeme tak\u00E9 studovat probl\u00E9m \u0159e\u0161itelnosti gravita\u010Dn\u00EDho pole pro danou rezonan\u010Dn\u00ED dr\u00E1hu. Do druh\u00E9ho t\u00E9matu spadaj\u00ED r\u016Fzn\u00E9 geoaplikace (impaktn\u00ED kr\u00E1tery, region\u00E1ln\u00ED geomorfologick\u00E9 procesy, interpretace invariant\u016F gravita\u010Dn\u00EDho pole a jin\u00E9)." . . " gradiometry" . "Earth gravity field, gradiometry, geopotential"@en . .