BROWSE - VOLUME LIST
- A - Physics of the Earth's Interior
- B - Seismology
C - Geomagnetism
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-34, 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
D - Physics of the Atmosphere
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-36, D-35, D-34, D-33, D-32, D-31, D-30, D-29, 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
Browse - Volume list
Atmospheric Ozone, Solar Radiation and Atmospheric Electricity Measurements in the Years 2006-2007
The present issue, with subtitle Monographic Volume, is published in place of the former yearbooks entitled: Atmospheric Ozone, Solar Radiation, Belsk and Results of Atmospheric Electricity and Meteorological Observations, S. Kalinowski Geophysical Observatory at Świder.
Results of Geomagnetic Observations; Belsk, Hel, Hornsund, 2006
Poland has three magnetic observatories: Belsk, Hel and Hornsund. Yearbooks for these observatories have been published regularly since 1966 for Belsk and Hel, and since 1978 for Hornsund. During the years, formats of yearbooks have been changing.
Transport Phenomena in Hydraulics
This volume concerns various aspects of research that contributes to the knowledge of a large number of engineering processes and also some natural processes that involve the transformation and transport of momentum, matter and energy. Those problems constitute the basis of the studies performed within the Project of the Ministry of Higher Education and Science Grant No. 2 P04D 026 29; it has also been the basic theme of the 27th International School of Hydraulics held from 18th to 21st September 2007 in Hucisko in the Jura Region in Southern Poland. It has been decided to combine the experience gained by the participants of the meeting and the results achieved within the project to provide the reader with a broad overview of the mentioned problems.
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.
Seismological Bulletin 2005. Local Earthquakes Recorded by Polish Seismological Stations
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 observedless frequently in the Rybnik Coal District and Bełchatów Open-Pit Mining area. The series of local earthquakes that began on November 30, 2004, of local magnitude M = 4.4, macroseismic intensity Io = 7 in the southern margin of the intramontane Orawa-Nowy Targ Basin, Western Carpathians, have been still recorded in 2005, mainly in January and February (Guterch 2006, 2007). The strongest after shocks did not exceed macroseismic intensity 5 in the EMS scale.