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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Online First
C - Geomagnetism
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.
Results of Geomagnetic Observations, Hel Geophysical Observatory 1999
Author(s): Czyszek A., Czyszek J.
Volume: 320
Series: C-76
Volume: 320
Series: C-76
This volume contains the results of observations of the Earth magnetic field for the year 1999, carried out at the Geophysical Observatory at Hel near Gdańsk. It is a consecutive twenty-second report of similar results published since 1966.
Results of Geomagnetic Observations, Polish Polar Station, Hornsund, Spitsbergen 1999
Author(s): Glegolski W., Gnoiński A.
Volume: 319
Series: C-75
Volume: 319
Series: C-75
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 1999.
Results of Geomagnetic Observations, Belsk 1999
Author(s): Reda J.
Volume: 318
Series: C-74
Volume: 318
Series: C-74
This publication contains results of geomagnetic observations performed in 1999; it is a consecutive, thirty-fourth issue in the series of yearbooks listing observations of the natural magnetic field of the Earth at the Central Geophysical Observatory at Belsk.
Signatures of Dual Mechanism of Plasma Sheet Formation and Structuring: A Study Based on Prognoz-8 Plasma Data
Author(s): Popielawska B.
Volume: 317
Series: C-73
Volume: 317
Series: C-73
A unique orbit of Prognoz-8 satellite allowed for the near Earth (X > -20 RE) tail crossings below the lowest latitudes accessible for polar orbiting satellites like Heos, Hawkeye, or Prognoz-7 and above those accessible for satellites with an ecliptic orbit like ISEE-1, 2 or AMPTE satellites. By the same, Prognoz-8 provided plasma merasurements in the magnetotail region that has not been well investigated yet. Previous survey of Prognoz-8 plasma measurements in the tail by Jimenez et al. (1984) used the SKS instrument data. Another plasma instrument aboard was PROMICS-2 with wider angular and energy range coverage and a supplementary ion mass composition diagnosis (oxygen ions).