Agata Wielgosz, Monika Tercjak and Aleksander Brzeziński
., Heinkelmann, R., Karbon, M., Raposo-Pulido, V., Soja, B., & Schuh, H. (2014). Earthorientation parameters estimated from VLBI during the CONT11 campaign. Journal of Geodesy, 88(5), 491-502. doi: 10.1007/s00190-014-0700-5
Petit, G., & Luzum, B. (Eds.). (2010). IERS Conventions (2010). IERS Technical Note 36, Verlag des Bundesamts für Kartographie und Geodäsie, Frankfurt am Main, Germany.
Petrachenko, W., Behrend, D., Hase, H., Ma, C., Niell, A., Schuh, H., & Whitney, A. (2013). The VLBI2010 Global Observing System (VGOS). In EGU General
processing of geographic and Cartesian data sets. Several grid and vector layers are embedded in the GMT, such as the world coastline ( Wessel and Smith, 1996 ) that can be visualized directly using coordinates and choosing projection. A variety of cartographic projections and transformations (over 30) are presented in the GMT enabling cartographer to select coordinates, suitable map orientation and additional elements (e.g., standard parallels, meridian). The effectiveness of the GMT consists in flexibility and variety of the modules that enables to perform high
Aleksander Brzeziński, Mieczysław Jóźwik, Marek Kaczorowski, Maciej Kalarus, Damian Kasza, Wiesław Kosek, Jolanta Nastula, Zbigniew Szczerbowski, Małgorzata Wińska, Roman Wronowski, Ryszard Zdunek and Janusz B. Zieliński
maximum entropy spectral analysis - Part II: Fortran program, Geophysics, 45, 433-446.
IERS, 2016, Earthorientation parameters, http://hpiers.obspm.fr/iers/eop/eopc04_05/
Jin S.G., Chambers P. , and Tapley D. (2010). Hydrological and oceanic effects on polar motion from GRACE and models, Journal of Geophysical Research, doi: 10.1029/2009JB006635.
Jin S.G., Hassan A., and Feng G.P. (2012). Assessment of terrestrial water contributions to polar motion from GRACE and hydrological models, Journal of Geodynamics, 62, 40
Aleksandra Bujakiewicz, Jakub Markiewicz, Krzysztof Bakuła and Dorota Zawierska
., Remote Sensing, Vol. XXXVI, Part 5
Hao, X., & Mayer, H. (2003). Orientation and Auto-Calibration of Image Triplets and Sequences, IAPRSSIS, 34(3/W8), pp. 73-78
Kraus, K. (2007). Photogrammetry, vol.1, Fundamentals and Standard Processes, Bonn: Dümmlers
Kurczyński, Z. (2006). Aerial and satellite imagery of Earth. Warsaw: Warsaw University of Technology Publishing House
Lisowska, P. (2007). Use of Digital Photogrammetry for Architectural Inventory (Eng. Diploma thesis), Warsaw University of Technology
Land and urban management require detecting changes in topography and urban areas. Topography changes in rural areas are generally the results of natural processes such as landslides, earthquakes, coastal erosion de- or afforestation. Urban changes consist of new constructions, extensions, destructions, excavation work and earth fill formed by natural or human effects. Change detection in urban areas is essential for planning, management, building and discovering unauthorized construction activities. In addition, the results of earthquakes can
, S., Haney, M., Dannemiller, N. (2004): Comprehensive approaches to the inversion of magnetic data with strong remanent magnetization, 74th Ann. Internat. Mtg., Soc. Explor. Geophys ., Expanded Abstracts.
 Telford, W. M., Geldart, L. P., Sheriff, R. G., Keys, D. A. (1976): Applied Geophysics : Cambridge University Press, Cambridge, pp. 7–215, 632–692.
 Medeiros, W. E., Silva, J. B. C. (1995): Simultaneous estimation of total magnetization direction and spatial orientation: Geophysics , 50, 1365–1377.
 Helbig, K. (1963): Some integrals
observations, some frequent directions were distinguished without seasonal effects. In many stations, the analysed directions of detrended displacement vectors correspond to the orientation of tectonic lines. So, the statistical distribution of daily solutions of GNSS stations located in the Sudetes and adjacent areas including the analysed further on stations in the area of LGCD are not random, and in most stations, are oriented accordingly towards the Sudetes. It was concluded that the directions of temporal stations’ position changes can be an indication of the impulse