SCOSTEP - Report - Ground-Based Observations
Ground-Based Observations The ground-based observations of the Sun are continuously
realized at the Skalnaté Pleso Solar Observatory (20.24° E, 49.19° N) being managed within the frame of
AISAS. In the IEPSAS, the Department of Space Physics community has long-term experience with measurements of corpuscular radiation in the Earth's environment. Ground-based observations are carried out under the unique high altitude conditions of High Tatras mountains. At the observatory Lomnický tít (Lomnicky Peak) the IGY neutron monitor was initially used. That was later reconstructed as NM64. This device has been providing continuous data on primary cosmic rays since December 1, 1981 (vertical cutoff rigidities 4GV, average count rate 1.6 x 106 hr-1). The data are at disposal of World Data Centers. The Lomnický tít station was among those three stations (together with Jungfraujoch, Swiss and Rome, Italy) which detected the first GLE of solar neutrons on June 3, 1982. This fact motivated the efforts for a better temporal resolution, which is 10 sec now. The joint experiment (in cooperation with Turku University, Finland) has been running since 1989. High statistical accuracy of NM data allowed to investigate variability of power spectra of NM time series (Kudela et al. 1995, Kudela et al. 1996a, b). Geomagnetic observation are carried out on a continuous basis at the Hurbanovo Geomagnetic Observatory (j =47.87° N, l =18.18° E; F =46.89° N, L =101.12° E) of the GISAS. The recent modernization of the equipment includes the installation of digital variometers from Poland (1996) and magnetoregistration device DI Fluxgate (1997) gained on the basis of co-operation with GeoForschungsZentrum Potsdam and VW Stiftung (Germany). To keep international standards comparative measurements are realized on a regular basis since 1953 in cooperation with European observatories (e.g. Niemegk, Tihany, Moscow, Wien-Kobenzl). The long time series data make it possible to study the profiles of secular changes in the total field and its components (Váczyová 1997d). The observational results are pubIished (e. g. Váczyová 1997a, b, c) in annual reports (database since 1949) and submitted (recently also on diskettes) to WDC-A in Boulder, USA. The Hurbanovo Geomagnetic Observatory has gained the status of the IMO observatory and contributes to the realization of the INTERMAGNET programme. Micropulsation measurements within the frame of the international network supported study have been started. The investigation of the non-linear character of the evolution of geomagnetic pulsations and their interaction with the background plasma at different levels of magnetospheric activity is under way in co-operation with US Geological Survey. Earlier observations of Pc3 pulsations were used to analyse their statistical regularities (Stoetík & Prigancová 1996). The IXth IAGA WORKSHOP ON GEOMAGNETIC OBSERVATORY INSTRUMENTS, DATA ACQUISITION AND PROCESSING will be held at Hurbanovo on June 12-18, 2000. The workshop has longstanding traditions in testing geomagnetic instrumentation and at this time it will be dedicated to the 100th anniversary of the Hurbanovo Geomagnetic Observatory. The importance of observational activities realized by the DGCU is growing. The Complex Astronomical and Geophysical Observatory has been built at Modra-Piesok near Bratislava. At this observatory the measurements of the geomagnetic field elements are carried out with high time resolution (1-min data) since 1992. The modernization of data processing is under way. According to the new project the measurements of Schumann resonances at the Modra - Piesok Observatory are carried out. The measurements without utilization of cryogenic apparatus have been also preparing.
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