At DGFI individual geophysical excitation mechanisms of the Earth rotation are determined from space-geodetic observation techniques. Until now the individual contributions of the subsystems of the Earth could be only estimated from geophysical models. Due to the combination of different space-geodetic observations in terms of Earth rotation, gravity field and sea level changes the atmospheric, oceanic and hydrological mass effects can be determined as well as the integral motion effect. We assume that the combined geodetic results are more realistic than the geophysical model solutions because they are based on precise space-geodetic measurements.
Funding: DFG-Research Group Earth Rotation (DFG-FOR 584)
Period: 04/2009 - 05/2012
Project partners: TU Munich (IAPG), Leibniz University Hannover (GIH)
Responsible persons at DGFI: Michael Schmidt, Franziska Göttl
Göttl F.: Earth rotation variations from geometric, gravimetric and altimetric observations and geophysical models. DGFI Report 84, Deutsches Geodätisches Forschungsinstitut (DGFI), München, 2008
Göttl F., Seitz F.: Contribution of non-tidal oceanic mass variations to polar motion determined from space geodesy and ocean data. in: Sideris, M.G. (eds.) Observing our Changing Earth, IAG Symposia, Vol. 133, pp 439-445, Springer, ISBN (Print) 978-3-540-85425-8, ISBN (Online) 978-3-540-85426-5, ISSN 0939-9585, DOI: 10.1007/978-3-540-85426-5_53, 2008
Mladek F. (2006): Hydrostatische Isostasie, Schriftreihe IAPG/FESG No.24, Institut für Astronomische und Physikalische Geodäsie, München
Schmidt M., Angermann D., Bloßfeld M., Göttl F., Richter B., Seitz M.: Erdrotation und geophysikalische Anregungsmechanismen. Zeitschrift für Vermessungswesen, 135, Heft 2, 2010