BROWSE - VOLUME LIST
- A - Physics of the Earth's Interior
- B - Seismology
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C - Geomagnetism
C-117, C-116, C-115, C-114, C-113, C-112, C-111, C-110, C-109, C-108, C-107, C-106, C-105, C-104, C-103, C-102, C-101, C-100, C-99, C-98, C-97, C-96, C-95, C-94, C-93, C-92, C-91, C-90, C-89, C-88, C-87, C-86, C-85, C-84, C-83, C-82, C-81, C-80, C-79, C-78, C-77, C-76, C-75, C-74, C-73, C-72, C-71, C-70, C-69, C-68, C-67, C-66, C-65, C-64, C-63, C-62, C-61, C-60, C-59, C-58, C-57, C-56, C-55, C-54, C-53, C-52, C-51, C-50, C-49, C-48, C-47, C-46, C-45, C-44, C-43, C-42, C-41, C-40, C-39, C-38, C-37, C-36, C-35, C-33, C-32, C-31, C-30, C-29, C-28, C-27, C-26, C-25, C-24, C-23, C-22, C-21, C-20, C-19, C-18, C-17, C-16, C-15, C-14, C-13, C-12, C-11, C-10, C-9, C-8, C-7, C-6, C-5, C-4, C-3, C-2, C-1
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D - Physics of the Atmosphere
D-78, D-77, D-76, D-75, D-74, D-73, D-72, D-71, D-70, D-69, D-68, D-67, D-66, D-65, D-64, D-63, D-62, D-61, D-60, D-59, D-58, D-57, D-56, D-55, D-54, D-53, D-52, D-51, D-50, D-49, D-48, D-47, D-46, D-44, D-45, D-43, D-42, D-41, D-40, D-39, D-38, D-37, D-35, D-34, D-33, D-32, D-31, D-30, D-28, D-27, D-26, D-25, D-24, D-23, D-22, D-21, D-20, D-19, D-18, D-17, D-16, D-15, D-14, D-13, D-12, D-11, D-10, D-9, D-8, D-7, D-6, D-5, D-4, D-3, D-2, D-1
- E - Hydrology
- P - Polar Research
- M - Miscellanea
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Browse - Volume list
Potential Climate Changes and Sustainable Water Management
Editor(s): Liszewska M.
Volume: 377
Series: E-4
Volume: 377
Series: E-4
In recent years it has become obvious that operational use of natural resources assuming their stationarity represents too narrow view of this complex issue. A change of paradigm seems to be developing, the two main principles of which are: the increased role of geo-sciences in assessing non-stationarity of resources potential, and postulate for their sustainable exploitation in the face of global change. Sustainability criteria provide a framework for prioritising competing interests and for making decision about safe and stable use of resources.
Local Earthquakes Recorded by Polish Seismological Stations 2003
Author(s): Zuchniak M., Niewiadomski J., Guterch B.
Volume: 376
Series: B-37
Volume: 376
Series: B-37
The majority of seismic events recorded in Poland are caused by mining activity in the Upper Silesian Coal Basin and Lubin Copper Basin. Induced seismicity is observed less frequently in the Rybnik Coal District and Bełchatów Open-Pit Mining Area. In 2003, a few local tectonic earthquakes occurred in the Western Carpathians at distances up to about 30 km from station Niedzica.
Seismological Bulletin 2002. Local Earthquakes Recorded by Polish Seismological Stations
Author(s): Draber D., Niewiadomski J., Zuchniak M.
Volume: 375
Series: B-36
Volume: 375
Series: B-36
The majority of seismic events recorded in Poland are caused by mining activity in the Upper Silesian Coal Basin and Lubin Copper Basin. Induced seismicity is observed less frequently in the Rybnik Coal District and Belchatów Open-Pit Mining area. In 2002, a few local tectonic earthquakes occurred in the Western Carparhians at distances up to about 30 km from station Niedzica.
Seismological Bulletin 2003. Polish Broadband Seismic Stations SUW, KWP, WAR, KSP, OJC, RAC
Author(s): Jankowska W., Kowalski P., Wiejacz P.
Volume: 374
Series: B-35
Volume: 374
Series: B-35
This is the eighth yearly report of activity of Polish broadband seismic stations. Since the reinstallation of the STS-2 seismometer at KSP on January 22, during 2003 the stations worked normally, except for occasional problems that are listed in section 3.
Meteorological Conditions, Hornsund, Spitsbergen, 2003/2004
Author(s):
Volume: 373
Series: D-66
Volume: 373
Series: D-66
The Polish Polar Station of the Institute of Geophysics is located nearby the entrance to the Hornsund fiord (Spitsbergen). It is situated at the northern shore of the fiord, by the Isbjornhamna bay, at a height of about 10 m a.m.s.l. The meteorological measurements and observations at the Polish Polar Station Hornsund had been initiated in 1957, during the International Geophysical Year, and carried out until the fall of 1958. They were resumed in July 1978, when the Polar Station was reactivated, and since then the station has been in incessant operation.