BROWSE - VOLUME LIST
- A - Physics of the Earth's Interior
- B - Seismology
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C - Geomagnetism
C-119, 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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Browse - Volume list
Macroseismic Intensities Observed in Czechoslovakia and Poland *** Makrosejsmiczne Intensywności w Czechosłowacji i Polsce
Author(s):
Volume: 122
Series: B-3
Volume: 122
Series: B-3
The macroseismic map of the maximum observed intensities in Czechoslovakia and Poland was constructed for the period from about 1000 A.D. to 1973. There were given isoseismals of degrees VII, VI and V. The whole Bohemian Massif, the central part and the south-eastern part of Slovakia can be shaken with the intensity of III to IV degrees at least and locally with intensity from V to VII. The north-eastern Slovakia can be shaken with the intensity of V to VIII degrees and the southern Poland with intensity of V to VI degrees. There were given also lists of the maximum observed intensity in Bohemia, Slovakia and Poland.
Électricité Atmosphérique et Météorologie Observatoire Géophysique de St. Kalinowski à Świder 1976
Author(s): Warzecha S.
Volume: 121
Series: D-6
Volume: 121
Series: D-6
This volume contains the results of recordings of some elements of atmospheric electricity and daily observations of major meteorological factors, noted at the S. Kalinowski Geophysical Observatory of the Polish Academy of Sciences at Świder in 1976.
Atmospheric Ozone, Solar Radiation and Radiation Balance, 1976
Author(s):
Volume: 120
Series: D-5
Volume: 120
Series: D-5
CONTENTS
P. Barański - Model of the vertical ozone transport in the lower troposphere, ...3
J. Podogrocki - Spatial distribution of global solar radiation in Poland, ...7
A. Michałowska-Smak - Relations between the net long-wave radiation and the meteorological elements in the climatic conditions
of the Polish Lowland, ...31
Methods of the Optimal Planning of Regional Seismic Networks
Author(s): Kijko A.
Volume: 119
Series: A-7
Volume: 119
Series: A-7
General principles for the optimum distribution of any nuber of regional seismic stations are formulated. The distribution of seismic activity i.e. the probability of an earthquake occurrence in a given point of a seismic region, and travel times of seismic waves used for earthquake location must be known. To define the optimum distribution of a regional network, some generalization of A and D-planning (minimization of the function of the ellipsoid volume of earthquake location errors) was applied. The optimum criterions are generalized for a case where equations describing the process are nonlinear and when the most probable values of the sought parameters (origin time and earthquake focus coordinates) are not known.
Bulletin Séismologique 1976
Author(s):
Volume: 118
Series: B-2
Volume: 118
Series: B-2
Cette publication contient une elaboration des tremblements de terre distants enregistres par les observatoires seismologiques de l'Institut de Geophysique de l'Academie Polonaise des Sciences en 1976.