We are pleased to share that AUC Geographica was awarded an Impact Factor of 0.5 in the 2023 Journal Citation Reports™ released by Clarivate in June 2024. AUC Geographica ranks in Q3 in the field of Geography.
AUC Geographica (Acta Universitatis Carolinae Geographica) is a scholarly academic journal continuously published since 1966 that publishes research in the broadly defined field of geography: physical geography, geo-ecology, regional, social, political and economic geography, regional development, cartography, geoinformatics, demography and geo-demography.
AUC Geographica also publishes articles that contribute to advances in geographic theory and methodology and address the questions of regional, socio-economic and population policy-making in Czechia.
Periodical twice yearly.
Release dates: June 30, December 31
All articles are licenced under Creative Commons Attribution 4.0 International licence (CC BY 4.0), have DOI and are indexed in CrossRef database.
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The journal has been covered in the SCOPUS database since 1975 – today
https://www.scopus.com/source/sourceInfo.uri?sourceId=27100&origin=recordpage
The journal has been selected for coverage in Clarivate Analytics products and services. Beginning with V. 52 (1) 2017, this publication will be indexed and abstracted in Emerging Sources Citation Index.
The journal has been indexed by the Polish Ministry of Science and Higher Education (MSHE) on the list of scientific journals recommended for authors to publish their articles. ICI World of Journals; Acta Universitatis Carolinae, Geographica.
Journal metrics 2023
Web of Science
Impact factor (JCR®): 0.5
Journal Citation Indicator (JCI): 0.20
Rank (JCI): Q3 in Geography
Scopus
Cite Score: 1.2
Rank (ASJC): Q3 in Geography, Planning and Development; Q3 in General Earth and Planetary Sciences
The journal is archived in Portico.
AUC GEOGRAPHICA, Vol 45 No 2 (2010), 53–71
Regional correlation of the Earth Gravitational Model 08 with morphogenetic patterns of the Nepal Himalaya
Jan Kalvoda, Jaroslav Klokočník, Jan Kostelecký
DOI: https://doi.org/10.14712/23361980.2015.48
published online: 02. 06. 2019
abstract
Results of the correlation of regional features of the Earth Gravitational Model 2008 (EGM 08) with morphogenetic and orographical patterns of the Nepal Himalaya are presented. Strong coincidences between large-scale morphogenetic styles of the Nepal Himalaya and the extension of regions with very high positive values of the radial second derivative of the disturbing gravitational potential Tzz and the most likely in combination with conspicuous areas of high negative values of Tzz in their close neighbourhood, have been identified. These variable values of Tzz display significant gravitational signatures of extensive differences and changes in mass density and/or rock massif and regolith distributions which occurred during very dynamic landform evolution of the Nepal Himalaya in the late Cenozoic. Regionální korelace modelu gravitačního pole Země 2008 s morfogenetickými styly Nepálského Himálaje V práci jsou předloženy výsledky korelace regionálních rysů modelu gravitačního pole Země 2008 (EGM 08) s morfogenetickými styly Nepálského Himálaje. Byly zjištěny podstatné shody mezi oblastmi s vysokými kladnými hodnotami radiální složky druhé derivace poruchového gravitačního potenciálu Tzz, které jsou často doprovázeny blízkými areály výrazně záporných hodnot Tzz, a specifickými morfogenetickými styly pohoří. Tyto variabilní hodnoty Tzz představují významný gravitační záznam značných rozdílů a změn hustoty hmoty resp. rozčlenění horninových masivů a regolithu, které jsou důsledkem velmi dynamického vývoje povrchových tvarů Nepálského Himálaje v mladším kenozoiku.
keywords: Earth Gravitational Model 2008; geodynamics; landform evolution; Nepal Himalaya
Regional correlation of the Earth Gravitational Model 08 with morphogenetic patterns of the Nepal Himalaya is licensed under a Creative Commons Attribution 4.0 International License.
210 x 297 mm
periodicity: 2 x per year
print price: 200 czk
ISSN: 0300-5402
E-ISSN: 2336-1980
