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-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
Ozone Content Variability in the Ground-level Atmosphere Layer in the Mazowieckie Voivodeship, Central Poland
Author(s): Pawlak I., Jarosławski J.
Volume: 429
Series: D-76
DOI: 10.25171/InstGeoph_PAS_Publs-2020-004
Volume: 429
Series: D-76
DOI: 10.25171/InstGeoph_PAS_Publs-2020-004
This publication presents an analysis of the variability of ground-level ozone in the Mazowieckie Voivodeship, Central Poland, in 2005−2012 and the forecast of ground-level ozone for the next day using artificial neural network models. The content of ground-level ozone in a given area is mainly determined by meteorological conditions and the presence of appropriate chemical compounds, i.e. ozone precursors.
Analysis of Measurements and Modelling of the Biologically Active UV Solar Radiation for Selected Sites in Poland – Assessment of Photo-medical Effects
Author(s): Czerwińska A., Krzyścin J.
Volume: 428
Series: D-75
DOI: 10.25171/InstGeoph_PAS_Publs-2020-002
Volume: 428
Series: D-75
DOI: 10.25171/InstGeoph_PAS_Publs-2020-002
This publication presents scenarios how to balance pro-health and detrimental effects of the UV radiation during controlled heliotherapy in order to minimize harm (erythema appearance and DNA damage) and maximize gain (increase of vitamin D level, psoriasis clearance). Referring to the literature, there is a need of finding a methodology to assess the potential risk and benefit at the moment of exposition to natural UV radiation.
The Microscopic Insight into Fracturing of Brittle Materials with the Discrete Element Method
Author(s): Klejment P.
Volume: 427
Series: A-31
DOI: 10.25171/InstGeoph_PAS_Publs-2020-001
Volume: 427
Series: A-31
DOI: 10.25171/InstGeoph_PAS_Publs-2020-001
In this work, the analysis of the issue of material fracturing in geophysical applications was undertaken. The Discrete Element Method was used, which is ideally suited for simulating the fracturing process, because it assumes a discrete model of matter (consisting of particles), and also allows to considerate all kinds of issues related to particle rotations and movements.
Results of Geomagnetic Observations: Belsk, Hel, Hornsund, 2018
Author(s): Reda J., Neska M., Wójcik S., Czubak P.
Volume: 426
Series: C-113
DOI: 10.25171/InstGeoph_PAS_Publs-2019-019
Volume: 426
Series: C-113
DOI: 10.25171/InstGeoph_PAS_Publs-2019-019
This publication contains basic information on geomagnetic observations carried out in 2018 in three Polish geophysical observatories: Belsk (BEL), Hel (HLP), and Hornsund (HRN). All these observatories belong to the Institute of Geophysics, Polish Academy of Sciences. Observatories Belsk and Hel are located on the territory of Poland, while Hornsund is in Spitsbergen archipelago, under Norwegian administration.In 2018, like in the previous years, the Belsk, Hel, and Hornsund observatories have kept a close collaboration with the world network of geomagnetic observatories INTERMAGNET. The Belsk Observatory joined INTERMAGNET in 1992, Hel in 1999, and Hornsund in 2002.
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.
Volume: 425
Series: M-32
DOI: 10.25171/InstGeoph_PAS_Publs-2019-002
Volume: 425
Series: M-32
DOI: 10.25171/InstGeoph_PAS_Publs-2019-002
A common topic of the conference are issues related to physics and geophysics of natural systems 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).