BROWSE - VOLUME LIST
- A - Physics of the Earth's Interior
- B - Seismology
C - Geomagnetism
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
- D - Physics of the Atmosphere
- E - Hydrology
P - Polar Research
G - Numerical Methods in Geophysics
- M - Miscellanea
M - Miscellanea
BOOK OF EXTENDED ABSTRACTS. “Electromagnetic ULF/ELF Fields on Earth and in Space” Conference, Warsaw, Poland, 3-5 July 2019
Editor(s): Kułak A., Odzimek A.
A common topic of the conference are issues related to physics and geophysics of naturalsystems generating fields of frequencies in the ULF (Ultra Low Frequency – 0.003 to 3 Hz) range and ELF (Extremely Low Frequency – 3 to 3000 Hz) range. In the range below 3 Hz, atypical geophysical division of the pulsation phenomena in the Pc1-Pc6 ranges was used. Currently, after the International Telecommunication Union (ITU) introduced a new division of frequency bands, there was chaos, because the former ELF range was divided into three ranges, and one of them is called a ULF range. The division currently used includes the following bands: ELF (Extremely Low Frequency – 3 to 30 Hz), SLF (Super Low Frequency – 30 to 300 Hz) and ULF (Ultra Low Frequency 300 to 3000 Hz).
Bibliography of Polish Research in Spitsbergen Archipelago. Part II: 1997-2006
We are giving to the still growing community of people interested in Spitsbergen and its surroundings a second part of the Bibliography of Polish Research in Spitsbergen Archipelago, covering the years from 1997 to 2006. The aim of the editors was to gather bibliographic information on scientific papers of Polish researchers. In some cases, we took into account foreign authors who closely cooperated with Polish teams in the area of Spitsbergen and around: Greenland, Iceland, Greenland Sea, Barents Sea, and the Russian Arctic. We also included publications of popular-science and informative character, which contribute to the history of research in the period covered by the Bibliography.
Rola Procesów Fizyczno-Chemicznych w Kształtowaniu Struktury Wewnętrznej i Obiegu Masy Lodowców Spitsbergenu (Role of Physical and Chemical Processes in the Internal Structure Formation and Mass Circulation of Spitsbergen Glacier)
W globalnym obiegu wody i energii na Ziemi lodowce spełniają rolę, której nie można pominąć. Chociaż powierzchnia zlodzenia na Ziemi wynosi niespełna 16,3 mln km2 (Szumski, Krenke 1965), co stanowi 11% powierzchni lądów naszego globu, to obszary pokryte lodowcami znacząco oddziaływują nie tylko na tereny przyległe, ale również,co należy podkreślić, na klimat w sensie globalnym. Jednocześnie lodowce podlegają wpływom zmieniającego się klimatu.
Mining and Environmental Geophysics. Selected and Revised Contributions to the XXX Polish-Czech-Slovakian Symposium held at Lądek Zdrój on June 6-8, 2005
The XXX Polish-Czech-Slovakian Symposium on Mining and Environmental Geophysics was held at Lądek spa (the Sudety Mts., Poland) from 6 to 8 June 2005. It was organized by the Faculty of Earth Sciences, University of Silesia, together with the Institute of Geophysics, Polish Academy of Sciences. The Symposium was attended by 71 participants which presented 44 original papers.
Geology, Geophysics, Geothermics and Deep Structure of the West Carpathians and Their Basement
Editor(s): Golonka J., Lewandowski M.
The Carpathians form a great arc of mountains, which stretches more than 1300 km from the Vienna Forest to the Iron Gate on the Danube. On the west the Carpathians are linked with the eastern Alps and on the east pass into the Balkan chain. Traditionally, the Carpathians are subdivided into the West and East Carpathians. The Carpathian Fold Belt system offers an outstanding opportunity to study the dynamics of astenosphere and lithosphere during volcanic arc and related fore- and back-arc basin development in the context of the Alpine orogenesis.