BROWSE - VOLUME LIST
- A - Physics of the Earth's Interior
- B - Seismology
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C - Geomagnetism
C-118, 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-79, 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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Online First
Browse - Volume list
Results of Geomagnetic Observations, Hel 2000
Author(s): Czyszek A., Czyszek J.
Volume: 330
Series: C-81
Volume: 330
Series: C-81
This volume contains the results of observations of the Earth magnetic field for the year 2000, carried out at the Geophysical Observatory at Hel near Gdańsk. It is a consecutive twenty-fourth report of similar results published since 1966.
Results of Geomagnetic Observations, Polish Polar Station, Hornsund, Spitsbergen 2000
Author(s): Glegolski W., Gnoiński A.
Volume: 329
Series: C-80
Volume: 329
Series: C-80
This volume contains the results of observations of the Earth's magnetic field carried out at the Polish Polar Station Hornsund in Spitsbergen in the year 2000.
Results of Geomagnetic Observations, Belsk 2000
Author(s): Marianiuk J., Reda J.
Volume: 328
Series: C-79
Volume: 328
Series: C-79
This publication contains results of geomagnetic observations performed in 2000; it is a consecutive, thirty-fifth issue in the series of yearbooks listing observations of the natural magnetic field of the Earth at the Central Geophysical Observatory at Belsk.
Stochastic Inversion Method for Modeling the Electrical Conductivity Distribution within the Earth´s Mantle
Author(s): Jóźwiak W.
Volume: 327
Series: C-78
Volume: 327
Series: C-78
The gist of the study of the Earth's interior is to make observations of natural physical processes at the surface and then to construct such models of the structure that would explain the observations in the best way. It is only in the case of the crust and partly the upper mantle that we are able to artificially generate phenomena to get information about their structure. Thus, unlike in other natural sciences, we cannot use repeatable experiments designed to study the nature of a specific phenomenon.
Study of Relationships Between Local Seismic Activity and Magnetotelluric Field Changes
Author(s): Rozłuski C.
Volume: 326
Series: C-77
Volume: 326
Series: C-77
The goal was to find possible confirmation of the fact that in the magnetotelluric recordings in seismic zones there are signals associated with seismic activity in the region. This is claimed by many authors for the purpose of earthquake prediction or in order to find earthquake precursors. Superpositions of transformation functions from the physical observables space into the hypothetical model space, where correlation can be observed, have been defined. Unfortunately, these superpositions and functions are irreversible, limiting the possibility for earthquake prediction. The single scalar function of magnetotelluric field, calculated in frequency domain, has been introduced with simple physical interpretation related to energy transmission through the Earth's surface. For the seismic events set of observables, two different, discrete in time-space, transformations have been introduced, arising from two models: for Greek and Japanese data.