Search results

Filters

  • Journals
  • Authors
  • Keywords
  • Date
  • Type

Search results

Number of results: 19
items per page: 25 50 75
Sort by:
Download PDF Download RIS Download Bibtex

Abstract

Recently, the topic of ontologies has growing attention from the IT community. Various processes of ontology creation, integration, and deployment have been proposed. As a consequence there appeared an urgent need for evaluating the resulting ontologies in a quantitative way. A number of metrics has been defined along with different approaches to measuring the properties of ontologies. In the first part of this paper we review the state of the art in this domain. Special attention is devoted to discussing differences between syntactic measures (referring to various properties of graphs that represent ontologies) and semantic measures (reflecting the properties of the space of ontology models). In the second part we propose an alternative approach to quantification of semantics of an ontology. The original proposal presented here exploits specific methods of representing the space of semantic models used for optimization of reasoning. We argue that this approach enables us to capture different kinds of relations among ontology terms and offers possibilities of devising new useful measures.

Go to article

Authors and Affiliations

Sylwester Kaczmarek
Magdalena Młynarczuk
Marcin Narloch
Maciej Sac
Download PDF Download RIS Download Bibtex

Abstract

Recently, the topic of ontologies has growing attention from the IT community. Various processes of ontology creation, integration, and deployment have been proposed. As a consequence there appeared an urgent need for evaluating the resulting ontologies in a quantitative way. A number of metrics has been defined along with different approaches to measuring the properties of ontologies. In the first part of this paper we review the state of the art in this domain. Special attention is devoted to discussing differences between syntactic measures (referring to various properties of graphs that represent ontologies) and semantic measures (reflecting the properties of the space of ontology models). In the second part we propose an alternative approach to quantification of semantics of an ontology. The original proposal presented here exploits specific methods of representing the space of semantic models used for optimization of reasoning. We argue that this approach enables us to capture different kinds of relations among ontology terms and offers possibilities of devising new useful measures.

Go to article

Authors and Affiliations

Wojciech Waloszek
Download PDF Download RIS Download Bibtex

Abstract

Cartography is the study and practice of making maps. Although originally defined for Earth, the term is also a perfect description of the aims of the VIPERS team, whose members include Polish astronomers.

Go to article

Authors and Affiliations

Katarzyna Małek
Małgorzata Siudek
Janusz Krywult
Agnieszka Pollo
Download PDF Download RIS Download Bibtex

Abstract

Permanent renewal of measurements of phenomena occuring on Earth sufrace — the main task of geodesy and cartography — is the important element of geodynamic studies of the Arctic and Antarctic regions. Insitute of Geodesy and Cartography participates in the program of research led by Polish Academy of Sciences for over 10 years, using conventional geodetic methods, as well as new types of data, acquired from satellite observations and through remote sensing techniques. This activity is evidenced by setting-up astronomical main points close to Hornsund Station in 1958, as well as at Arctowski Station in 1976, where cyclic astronomical and satellite measurements were performed on these points. Geodynamic test site was organized in the Hornsund Region. As a result of these works numerous topographic and thematic maps were produced and many scientific publications were prepared by Institute specialists.

Go to article

Authors and Affiliations

Jan Cisak
Stanisław Dąbrowski
Download PDF Download RIS Download Bibtex

Abstract

The subject matter of this article constitutes the semiotic mapping of human of knowledge which results from cognition. Departing from the presentation of human subjects as world-model-builders, it places epistemology among the sciences of science and the sciences of man. As such the understanding of epistemology is referred either to a static state of knowledge or to a dynamic acquisition of knowledge by cognizing subjects. The point of arrival, in the conclusive part of a this article, constitutes the substantiation of the two understandings of epistemology, specified, firstly, as a set of investigative perspectives, which the subject of science has at his/her disposal as a knower on the metascientific level, or, secondly, as a psychophysiological endowment of a cognizing subject who possesses the ability of learning and/or knowing a certain kind of information about cognized reality.

Go to article

Authors and Affiliations

Zdzisław Wąsik
Download PDF Download RIS Download Bibtex

Abstract

The applications of the machine learning and programming approaches in cartography has been increasing in recent years. This paper presents a case study of the scripting techniques used for cartographic mapping using Generic Mapping Tools (GMT) and R language (raster and tmaps packages). The aim of the study is environmental mapping of Ghana. The materials include high-resolution raster grids: topography by the General Bathymetric Chart of the Oceans (GEBCO), climate and environmental datasets (TerraClimate) and Shuttle Radar Topography Mission (SRTM) Digital Elevation Model (DEM) for geomorphometric analysis (slope, aspect, hillshade and elevations). The methodology includes code snippets commented and explained with details of scripts. It is argued that using consolebased scripting tools for mapping is effective for cartographic workflow due to the logical structure and repeatability of scripts. The results include eight new thematic maps of Ghana performed using scripting approach inGMTscripting toolset and R language for quantitative and qualitative environmental assessment. Maps show correlations between the landforms of Ghana and certain environmental variables (drought index and soil moisture) showing the effects of the topographic relief on the distribution of the continuous geographic fields. These varied in several geographically distinct regions of Ghana: Ashanti (Kumasi), Volta, Savannah, coastal and northern regions. Demonstrated maps show that scripting method works effectively on a wide range of geosciences including environmental, topographic and climate studies. In such a way, this paper contributes both to the regional studies of Ghana and development of cartographic techniques.
Go to article

Authors and Affiliations

Polina Lemenkova
1
ORCID: ORCID

  1. Université Libre de Bruxelles, Brussels, Belgium
Download PDF Download RIS Download Bibtex

Abstract

Modern geological maps are 3D, or even 4D models representing the complex structure of the Earth. They interpret a variety of geological information and represent it in graphical form.
Go to article

Authors and Affiliations

Joanna Rychel
1
Łukasz Nowacki
1
Mirosław Kamiński
1

  1. Polish Geological Institute – National Research Institute in Warsaw
Download PDF Download RIS Download Bibtex

Abstract

The paper concerns GMT application for studies of the geophysical and geomorphological settings of the Weddell Sea. Its western part is occupied by the back-arc basin developed during geologic evolution of the Antarctic. The mapping presents geophysical settings reflecting tectonic formation of the region, glaciomarine sediment distribution and the bathymetry. The GlobSed grid highlighted the abnormally large thickness of sedimentary strata resulted from the long lasting sedimentation and great subsidence ratio. The sediment thickness indicated significant influx (>13,000m) in the southern segment. Values of 6,000–7,000 m along the peninsula indicate stability of the sediments influx. The northern end of the Filchner Trough shows increased sediment supply. The topography shows variability -7,160–4,763 m. The ridges in the northern segment and gravity anomalies (>75 mGal) show parallel lines stretching NW-SE (10°–45°W, 60°–67°S) which points at the effects of regional topography. The basin is dominated by the slightly negative gravity >-30 mGal. The geoid model shows a SW-NE trend with the lowest values <18 m in the south, the highest values >20m in the NE and along the Coats Land. The ripples in the north follow the geometry of the submarine ridges and channels proving correlation with topography and gravitational equipotential surface.
Go to article

Bibliography

1. Aleshkova, N. D., Golynsky, A. V, Kurinin, R.G., Mandrikov, V.S., 1997. Gravity Mapping in the Southern Weddell Sea Region. (Explanatory note for free-air and Bouguer anomalies maps). Polarforschung, 67 (3), 163–177.
2. Anderson, J.B., 1972a. The Marine Geology of the Weddell Sea. Florida State University Sedimentological Research Laboratory, Publication Number 35, Florida State University, Tallahassee, p. 222.
3. Anderson, J.B., 1972b. Nearshore glacial-marine deposition from modern sediments of the Weddell Sea. Nature 240, 189–192.
4. Anderson, J.B., Andrews, B.A., Bartek, L.R., Truswell, E.M., 1991. Petrology and palynology of glacial sediments: implications for subglacial geology of the eastern Weddell Sea, Antarctica. In: Thomson, M.R.A., Crame, J.A., Thomson, J.W. (Eds.), Geological Evolution of Antarctica. Cambridge University Press, Cambridge (UK), 231–235.
5. Barker, P.F., Dalziel, I.W.D., Storey, B.C., 1991. Tectonic evolution of the Scotia Arc region. In: Tingey, R.J. (Ed.), Antarctic Geology. Oxford University Press, 215–248.
6. Bart, P.J., DeBatist, M., Jokat, W., 1999. Interglacial collapse off Crary Trough Mouth Fan, Weddell Sea, Antarctica: implications for Antarctic glacial history. Journal of Sedimentary Research 69, 1276–1289.
7. Bell, R.E., Brozena, J.M., Haxby, W.F., Labrecque, J.L., 1990. Continental Margins of the Western Weddell Sea: Insights from Airborne Gravity and Geosat‐Derived Gravity. Contributions to Antarctic Research I, 50, doi: 10.1029/AR050p0091.
8. Bentley, M.J., Anderson, J.B., 1998. Glacial and marine geological evidence for the ice sheet configuration in the Weddell Sea Antarctic Peninsula region during the Last Glacial Maximum. Antarctic Science 10, 309–325.
9. Bentley, M., Fogwill, C., Le Brocq, A., Hubbard, A., Sugden, D., Dunai, T., Freeman, S., 2010. Deglacial history of the West Antarctic Ice Sheet in the Weddell Sea Embayment: constraints on past ice volume change. Geology 38, 411–414.
10. Bentley, M.J., Hein, A., Sugden, D.E., Whitehouse, P., Vieli, A., Hindmarsh, R.C.A., 2012. Post-glacial thinning history of the Foundation Ice Stream, Weddell Sea embayment, Antarctica. In: Abstract C51C-0787 Presented at 2012 Fall Meeting, AGU, San Francisco, California, 3–7 December 2012.
11. Bentley, M.J., Hein, A.S., Sugden, D.E., Whitehouse, P.L., Shanks, R., Xu, S., Freeman, S.P.H.T., 2017. Deglacial history of the Pensacola mountains, Antarctica from glacial geomorphology and cosmogenic nuclide surface exposure dating. Quaternary Science Reviews 158, 58–76.
12. Bradley, S.L., Hindmarsh, R.C.A., Whitehouse, P.L., Bentley, M.J., King, M.A., 2015. Low post-glacial rebound rates in the Weddell Sea due to late Holocene ice-sheet readvance. Earth and Planetary Science Letters 413, 79–89.
13. Carsey, F.D., 1980. Microwave observation of the Weddell Polynya. Monthly Weather Review 108, 2032–2044.
14. Clark, P.U., 2011. Deglacial history of the West Antarctic Ice Sheet in the Weddell Sea Embayment: constraints on past ice volume change: comment. Geology 39, 239, doi: 10.1130/G31533C.1.
15. Collares, L.L., Mata, M.M., Kerr, R., Arigony-Neto, J., Barbat, M.M., 2018. Iceberg drift and ocean circulation in the northwestern Weddell Sea, Antarctica. Deep Sea Research Part II: Topical Studies in Oceanography 149, 10–24.
16. Crawford, K., Kuhn, G., Hambrey, M.J., 1996. Changes in the character of glaciomarine sedimentation in the southwestern Weddell Sea, Antarctica: evidence from the core PS1423-2. Annals of Glaciology 22, 200–204.
17. Cunningham, W.D., Dalziel, I.W.D., Lee, T.-Y., Lawver, L.A., 1995. Southernmost South America-Antarctic Peninsula relative plate motions since 84 Ma: implications for the tectonic evolution of the Scotia Arc region. Journal of Geophysical Research 100, 8257–8266.
18. Curtis, M.L., Storey, B.C. 1996. A review of geological constraints on the pre-break-up position of the Ellsworth Mountains within Gondwana: implications for Weddell Sea evolution. Geological Society, London, Special Publications 108, 11–30, doi: 10.1144/ GSL.SP.1996.108.01.02.
19. DeConto, R., Pollard, D., 2016. Contribution of Antarctica to past and future sea-level rise. Nature 531, 591–597.
20. Eagles, G., Jokat, W. 2014. Tectonic reconstructions for paleobathymetry in Drake Passage. Tectonophysics 611, 28–50.
21. Elverhøi, A., 1981. Evidence for a late Wisconsin glaciation of the Weddell Sea. Nature 293, 641–642.
22. Elverhøi, A., Roaldset, E., 1983. Glaciomarine sediments and suspended particulate matter, Weddell Sea shelf, Antarctica. Polar Research 1, 1–21.
23. Fahrbach, E., Rohardt, G., Scheele, N., Schröder, M., Strass, V., Wisotzki, A., 1995. Formation and discharge of deep and bottom water in the northwestern Weddell Sea. Journal of Marine Research 53, 515–538.
24. Fretwell, P., Pritchard, H.D., Vaughan, D.G., Bamber, J.L., Barrand, N.E., et al., 2013. Bedmap2: improved ice bed, surface and thickness datasets for Antarctica. Cryosphere 7, 375–393.
25. Gales, J., Leat, P., Larter, R., Kuhn, G., Hillenbrand, C.D., Graham, A., Mitchell, N., Tate, A., Buys, G., Jokat, W., 2014. Large-scale submarine landslides, channel and gully systems on the southern Weddell Sea margin, Antarctica. Marine Geology 348, 73–87.
26. Gauger, S., Kuhn, G., Gohl, K., Feigl, T., Lemenkova, P., Hillenbrand, C., 2007. Swath-bathymetric mapping. Reports on Polar and Marine Research 557, 38–45.
27. GEBCO Compilation Group, 2020. GEBCO 2020 Grid, doi: 10.5285/ a29c5465-b138-234d-e053-6c86abc040b9.
28. GDAL/OGR contributors, 2020. GDAL/OGR Geospatial Data Abstraction software Library. Open Source Geospatial Foundation. https://gdal.org.
29. Grobe, H., Huybrechts, P., Fütterer, D.K., 1993. Late Quaternary record of sea-level changes in the Antarctic. Geologische Rundschau 82, 263–275, doi: 10.1007/BF00191832.
30. Grikurov, G.E., Ivanov, V.L., Traube, V.V., Leitchenkov G.L., Aleshkova, N.D., Golynsky, A.V., Kurinin, R.G., 1991. Structure and evolution of sedimentary basins in the Weddell province. Abstract 6th International Symposium Antarctic Earth Sciences, Tokyo, 185–190.
31. Haase, G.M., 1986. Glaciomarine sediments along the Filchner/Ronne Ice Shelf. southern Weddell Sea e first results of the 1983/84 ANTARKTIS- II/4 expedition. Marine Geology 72, 241–258.
32. Haid, V., Timmermann, R., 2013. Simulated heat flux and sea ice production at coastal polynyas in the southwestern Weddell Sea. Journal of Geophysical Research 118, 2640–2652.
33. Haugland, K., Kristoffersen, Y., Velde, A., 1985. Seismic investigations in the Weddell Sea embayment. Tectonophysics 114 (1–4), 1–21.
34. Haugland, K., 1982. Seismic reconnaissance survey in the Weddell Sea. In: Craddock, C. (Ed.), Antarctic Geoscience. University of Wisconsin Press, Madison (U.S.A.), 405–413.
35. Hegland, M., Vermeulen, M., Todd, C., Balco, G., Huybers, K., Campbell, S., Conway, H., Simmons, C., 2012. Glacial geomorphology of the Pensacola mountains, Weddell Sea sector, Antarctica. In: Abstracts of the WAIS Workshop 2012, 21.
36. Hein, A.S., Marrero, S.M., Woodward, J., Dunning, S.A., Winter, K., Westoby, M.J., Freeman, S.P.H.T., Shanks, R.P., Sugden, D.E., 2016. Mid-Holocene pulse of thinning in the Weddell Sea sector of the West Antarctic ice sheet. Nature Communications 7, 12511, doi: 10.1038/ncomms12511.
37. Hein, A.S., Fogwill, C.J., Sugden, D.E., Xu, S., 2011. Glacial/Interglacial ice-stream stability in the Weddell Sea embayment, Antarctica. Earth and Planetary Science Letters 307, 211–221.
38. Hillenbrand, C.-D., Melles, M., Kuhn, G., Larter, R.D., 2012. Marine geological constraints for the grounding-line position of the Antarctic Ice Sheet on the southern Weddell Sea shelf at the Last Glacial Maximum. Quaternary Science Reviews 32, 25–47.
39. Hillenbrand, C.-D., Bentley, M.J., Stolldorf, T.D., Hein, A.S., Kuhn, G., Graham, A.G.C., Fogwill, C.J., Kristoffersen, Y., Smith, J.A., Anderson, J.B., Larter, R.D., Melles, M., Hodgson, D.A., Mulvaney, R., Sugden D.E., 2014. Reconstruction of changes in the Weddell Sea sector of the Antarctic Ice Sheet since the Last Glacial Maximum. Quaternary Science Reviews 100, 111–136.
40. Huang, X., Gohl, K. Jokat, W., 2014. Variability in Cenozoic sedimentation and paleo-water depths of the Weddell Sea basin related to pre-glacial and glacial conditions of Antarctica. Global and Planetary Change 118, 25–41.
41. Huang, X., Jokat, W., 2016. Middle Miocene to present sediment transport and deposits in the Southeastern Weddell Sea, Antarctica. Global and Planetary Change 139, 211–225.
42. Johnson, J.S., Nichols, K.A., Goehring, B.M., Balco, G., Schaefer, J.M., 2019. Abrupt mid-Holocene ice loss in the western Weddell Sea Embayment of Antarctica. Earth and Planetary Science Letters 518, 127–135.
43. Jokat, W., Fechner, N., Studinger, M., 1997. Geodynamic models of the Weddell Sea embayment in view of new geophysical data. In: Ricchi, C.A. (Ed.), The Antarctic Region: Geological Evolution and Processes. Terra Antarctica Publication, Siena (Italy), 453– 459.
44. Kerr, R., Dotto, T.S., Mata, M.M., Hellmer, H.H., 2018. Three decades of deep water mass investigation in the Weddell Sea (1984–2014): Temporal variability and changes. Deep Sea Research Part II: Topical Studies in Oceanography 149, 70–83.
45. King, E.C., Bell, A.C., 1996. New seismic data from the Ronne Ice Shelf, Antarctica. In: Storey, B.C., King, E.C., Livermore, R.A. (Eds), Weddell Sea tectonics and Gondwana break-up. London, Geological Society of London, 213–226. (Geological Society special publication, 108), doi: 10.1144/GSL.SP.1996.108.01.16.
46. Kjellsson, J., Holland, P.R., Marshall, G.J., Mathiot, P., Aksenov, Y., Coward, A.C., Bacon, S., Megann, A.P., Ridley, J., 2015. Model sensitivity of the Weddell and Ross seas, Antarctica, to vertical mixing and freshwater forcing. Ocean Modelling 94, 141–152.
47. Klaučo, M., Gregorová, B., Stankov, U., Marković, V., Lemenkova, P., 2013. Determination of ecological significance based on geostatistical assessment: a case study from the Slovak Natura 2000 protected area. Open Geosciences 5 (1), 28–42.
48. Klaučo, M., Gregorová, B., Stankov, U., Marković, V., Lemenkova, P., 2014. Landscape metrics as indicator for ecological significance: assessment of Sitno Natura 2000 sites, Slovakia. Ecology and Environmental Protection. Proceedings of the International Conference. March 19–20, 2014. Minsk, Belarus, 85–90.
49. Klaučo, M., Gregorová, B., Stankov, U., Marković, V., Lemenkova, P., 2017. Land planning as a support for sustainable development based on tourism: A case study of Slovak Rural Region. Environmental Engineering and Management Journal 2 (16), 449–458.
50. König, M., Jokat, W., 2006. The Mesozoic breakup of the Weddell Sea. Journal of Geophysical Research Solid Earth (1978–2012), 111 (B12).
51. Kristoffersen, Y., Hinz, K., 1991. Evolution of the Gondwana plate boundary in the Weddell Sea area. In: Thomson, M.R. A., Crame, J.A., Thomson, J.W. (Eds), Geological evolution of Antarctica. Cambridge University Press, Cambridge, 225–223.
52. Kuhn, G., Weber, M., 1993. Acoustical characterization of sediments by Parasound and 3.5 kHz systems: related sedimentary processes on the southeastern Weddell Sea continental slope, Antarctica. Marine Geology 113, 201–217.
53. Kuhn, G., Hass, C., Kober, M., Petitat, M., Feigl, T., Hillenbrand, C.D., Kruger, S., Forwick, M., Gauger, S., Lemenkova, P., 2006. The response of quaternary climatic cycles in the South-East Pacific: development of the opal belt and dynamics behavior of the West Antarctic ice sheet. In: Gohl, K. (Ed.), Expeditions programm Nr. 75 ANT XXIII/4, AWI, doi: 10.13140/RG.2.2.11468.87687.
54. Larter, R.D., Graham, A.G.C., Hillenbrand, C.-D., Smith, J.A., Gales, J.A., 2012. Late Quaternary grounded ice extent in the Filchner Trough, Weddell Sea, Antarctica: new marine geophysical evidence. Quaternary Science Reviews 53, 111–122.
55. Lemenkova, P., 2011. Seagrass Mapping and Monitoring Along the Coasts of Crete, Greece. M.Sc. Thesis. Netherlands: University of Twente, 158 pp., doi: 10.13140/RG.2.2.16945.22881.
56. Lemenkova, P., 2018. R scripting libraries for comparative analysis of the correlation methods to identify factors affecting Mariana Trench formation. Journal of Marine Technology and Environment 2, 35–42.
57. Lemenkova, P., 2019a. Statistical Analysis of the Mariana Trench Geomorphology Using R Programming Language. Geodesy and Cartography 45 (2), 57–84.
58. Lemenkova, P., 2019b. Automatic Data Processing for Visualising Yap and Palau Trenches by Generic Mapping Tools. Cartographic Letters 27 (2), 72–89.
59. Lemenkova, P., 2019c. AWK and GNU Octave Programming Languages Integrated with Generic Mapping Tools for Geomorphological Analysis. GeoScience Engineering 65 (4), 1–22.
60. Lemenkova, P., 2019d. Topographic surface modelling using raster grid datasets by GMT: example of the Kuril-Kamchatka Trench, Pacific Ocean. Reports on Geodesy and Geoinformatics 108, 9–22.
61. Lemenkova, P., 2019e. GMT Based Comparative Analysis and Geomorphological Mapping of the Kermadec and Tonga Trenches, Southwest Pacific Ocean. Geographia Technica 14 (2), 39–48.
62. Lemenkova, P., 2019f. Geomorphological modelling and mapping of the Peru-Chile Trench by GMT. Polish Cartographical Review 51 (4), 181–194.
63. Lemenkova, P., 2020a. Variations in the bathymetry and bottom morphology of the Izu-Bonin Trench modelled by GMT. Bulletin of Geography. Physical Geography Series 18 (1), 41–60.
64. Lemenkova, P., 2020b. GMT Based Comparative Geomorphological Analysis of the Vityaz and Vanuatu Trenches, Fiji Basin. Geodetski List 74 (1), 19–39.
65. Lemenkova, P., 2020c. Integration of geospatial data for mapping variation of sediment thickness in the North Sea. Scientific Annals of the Danube Delta Institute 25, 129–138.
66. Lemenkova, P., 2020d. R Libraries {dendextend} and {magrittr} and Clustering Package scipy.cluster of Python For Modelling Diagrams of Dendrogram Trees. Carpathian Journal of Electronic and Computer Engineering 13 (1), 5–12.
67. Lemenkova, P., Promper, C., Glade, T., 2012. Economic Assessment of Landslide Risk for the Waidhofen a.d. Ybbs Region, Alpine Foreland, Lower Austria. In: Eberhardt, E., Froese, C., Turner, A.K., Leroueil, S. (Eds), Protecting Society through Improved Understanding. 11th International Symposium on Landslides & the 2nd North American Symposium on Landslides & Engineered Slopes (NASL), June 2–8, 2012. Banff, AB, Canada, 279–285, doi: 10.6084/m9.figshare.7434230.
68. Lemoine, F.G., Kenyon, S.C., Factor, J.K., Trimmer, R.G., Pavlis, N.K., Chinn, D.S., Cox, C.M., Klosko, S.M., Luthcke, S.B., Torrence, M.H., Wang, Y.M., Williamson, R.G., Pavlis, E.C., Rapp R.H., Olson, T.R., 1998. The Development of the Joint NASA GSFC and the National Imagery and Mapping Agency (NIMA) Geopotential Model EGM96. NASA/TP-1998-206861.
69. Lindeque, A., Martin, Y., Gohl, K., Maldonado, A., 2013. Deep sea pre-glacial to glacial sedimentation in the Weddell Sea and southern Scotia Sea from a cross-basin seismic transect. Marine Geology 336, 61–83.
70. Livermore, R.A., Woollett, R.W., 1993. Seafloor spreading in the Weddell Sea and southwest Atlantic since the Late Cretaceous. Earth and Planetary Science Letters 117, (3–4), 475–495.
71. Livermore, R.A., Hunter, R., 1996. Mesozoic seafloor spreading in the southern Weddell Sea. In: Storey, B., King, E., Livermore, R. (Eds.), Weddell Sea Tectonics and Gondwana Breakup. Geological Society, London, Special Publications 108, 227–241.
72. Maldonado, A., Barnolas, A., Bohoyo, F., Escutia, C., Galindo-Zaldívar, J., Hernández-Molina, J., Jabaloy, A., Lobo, F.J., Nelson, C.H., Rodríguez- Fernández, J., Somoza, L., Vázquez, J.T., 2005. Miocene to recent contourite drifts development in the northern Weddell Sea (Antarctica). Global and Planetary Change 45 (1), 99–129.
73. Maldonado, A., Barnolas, A., Bohoyo, F., Escutia, C., Galindo-ZaldÍvar, J., Hernández-Molina, J., Jabaloy, A., Lobo, F.J., Nelson, C.H., RodrÍguez-Fernández, J., Somoza, L., Suriñach, E., Vázquez, J.T., 2006. Seismic Stratigraphy of Miocene to Recent Sedimentary Deposits in the Central Scotia Sea and Northern Weddell Sea: Influence of Bottom Flows (Antarctica). In: Fütterer, D.K., Damaske, D., Kleinschmidt, G., Miller, H., Tessensohn, F. (Eds), Antarctica. Springer, Berlin, Heidelberg, 441–446, doi: 10.1007/3-540-32934- X_56.
74. Michels, K.H., Rogenhagen, J., Kuhn, G., 2001. Recognition of contour- current influence in mixed contourite-turbidite sequences of the western Weddell Sea, Antarctica. Marine Geophysical Research 22, 465–485.
75. Mueller, R.D., Timmermann, R., 2017. Weddell Sea Circulation. Journal of Atmospheric and Solar-Terrestrial Physics 161, 105–117.
76. Nankivell, A.P., 1997. Tectonic Evolution of the Southern Ocean Between Antarctica, South America and Africa Over the Last 84 Ma. Ph.D. thesis University of Oxford, Oxford, UK.
77. Nicholls, K.W., Østerhus, S., Makinson, K., Gammelsrød, T., Fahrbach, E., 2009. Ice-ocean processes over the continental shelf of the southern Weddell Sea, Antarctica: a review. Reviews of Geophysics 47, RG3003, doi: 10.1029/2007RG000250.
78. Pavlis, N.K., Holmes, S.A., Kenyon, S.C., Factor, J.K., 2012. The development and evaluation of the Earth Gravitational Model 2008 (EGM2008). Journal of Geophysical Research 117, B04406, doi: 10.1029/2011JB008916.
79. Paxman, G.J.G., Jamieson, S.S.R., Hochmuth, K., Gohl, K., Bentleya, M.J., Leitchenkov, G., Ferracciolif, F., 2019. Reconstructions of Antarctic topography since the Eocene–Oligocene boundary. Palaeogeography, Palaeoclimatology, Palaeoecology 535. 109346, doi: 10.1016/j.palaeo.2019.109346.
80. Riley, T.R., Jordan, T.A., Leat, P.T., Curtis, M.L., Millar, I.L., 2020. Magmatism of the Weddell Sea rift system in Antarctica: Implications for the age and mechanism of rifting and early stage Gondwana breakup. Gondwana Research 79, 185–196, doi: 10.1016/j. gr.2019.09.014.
81. Sandwell, D.T., Müller, R.D., Smith, W.H.F., Garcia, E., Francis, R., 2014. New global marine gravity model from CryoSat-2 and Jason- 1 reveals buried tectonic structure. Science 346 (6205), 65–67.
82. Scheinert, M., Ferraccioli, F., Schwabe, J., Bell, R., Studinger, M., Damaske, D., Jokat, W., Aleshkova, N., Jordan, T., Leitchenkov, G., Blankenship, D.D., Damiani, T.M., Young, D., Cochran, J.R., Richter, T.D., 2016. New Antarctic gravity anomaly grid forenhanced geodetic and geophysical studies in Antarctica. Geophysical Research Letters 43 (2), doi: 10.1002/2015GL067439.
83. Schenke, H.W., Lemenkova, P., 2008. Zur Frage der Meeresboden-Kartographie: Die Nutzung von AutoTrace Digitizer für die Vektorisierung der Bathymetrischen Daten in der Petschora-See. Hydrographische Nachrichten 81, 16–21.
84. Siegert, M., Ross, N., Corr, H., Kingslake, J., Hindmarsh, R., 2013. Late Holocene ice-flow reconfiguration in the Weddell Sea sector of West Antarctica. Quaternary Science Reviews 78, 98–107.
85. Smith, W.H.F., 1993. On the accuracy of digital bathymetric data. Journal of Geophysical Research 98, B6, 9591–9603.
86. Snyder, J.P., 1987. Map Projections – A Working Manual. U.S. Geological Survey Professional Paper 1395. Washington, DC: U.S. Government Printing Office, 124–137.
87. Snyder, J.P., 1993. Flattening the Earth: Two Thousand Years of Map Projections. ISBN 0-226-76747-7.
88. Storey, B.C., Dalziel, I.W.D., Garrett, S.W., Grunow, A.M., Pankhurst, R.J., Vennum, W.R., 1988. West Antarctica in Gondwanaland: crustal blocks, reconstruction and breakup processes. In: Scotese, C.R., Sager, W.W. (Eds), 8th Geodynamics Symposium, Mesozoic and Cenozoic Plate Reconstructions. Elsevier, 381–390. (Tectonophysics, 155, 1–4).
89. Storey, B.C., Vaughan, A.P.M., Millar I.L., 1996. Geodynamic evolution of the Antarctic Peninsula during Mesozoic times and its bearing on Weddell Sea history. In: Storey, B.C., King, E.C., Livermore, R.A. (Eds), Weddell Sea Tectonics and Gondwana Break-up. Geological Society Special Publication, London, 108, 87–103.
90. Stolldorf, T., Schenke, H.-W., Anderson, J.B., 2012. LGM ice sheet extent in the Weddell Sea: evidence for diachronous behavior of Antarctic Ice Sheets. Quaternary Science Reviews 48, 20–31.
91. Stow, D.A.V., Faugères, J.C., Howe, J.A., Pudsey, C.J., Viana, A.R., 2002. Bottom currents, contourites and deep-sea sediment drifts: Current state-of-the-art. In: Stow, D.A.V., Pudsey, C.J., Howe, J.A., Faugeres, J.C., Viana, A.R. (Eds.), Deep-Water Contourite Systems: Modern Drifts and Ancient Series. Memoir. Geological Society of London, London, 7–20.
92. Straume, E.O., Gaina, C., Medvedev, S., Hochmuth, K., Gohl, K., Whittaker, J.M., Abdul Fattah, R., Doornenbal, J.C., Hopper, J.R., 2019. GlobSed: Updated total sediment thickness in the world’s oceans. Geochemistry, Geophysics, Geosystems 20 (4), 1756– 1772.
93. Suetova, I.A., Ushakova, L.A., Lemenkova P., 2005. Geoinformation mapping of the Barents and Pechora Seas. Geography and Natural Resources 4, 138–142.
94. Tingey, R.J., 1991. The regional geology of Archean and Proterozoic rocks in Antarctica. In: Tingey, RJ. (Ed.), The Geology of Antarctica, Clarendon Press, Oxford, 1–58.
95. Uenzelmann-Neben, G., 2006. Depositional patterns at Drift 7, Antarctic Peninsula: along-slope versus down-slope sediment transport as indicators for oceanic currents and climatic conditions. Marine Geology 233, 49–62.
96. Weber, M.E., Bonani, G., Fütterer, K.D., 1994. Sedimentation processes within channel ridge systems, southern Weddell Sea, Antarctica. Palaeoceanography 9, 1027–1048.
97. Wessel, P., Smith, W.H.F., 1991. Free software helps map and display data. Eos Transactions of the American Geophysical Union 72 (41), 441.
98. Wessel, P., Smith, W.H.F., 1995. New version of the Generic Mapping Tools released. Eos Transactions of the American Geophysical Union 76 (33), 329.
99. Wessel, P., Smith, W.H.F., 1996. A Global Self-consistent, Hierarchical, High-resolution Shoreline Database. Journal of Geophysical Research 101, 8741-8743.
100. Wessel, P., Smith, W.H.F., Scharroo, R., Luis, J.F., Wobbe, F., 2013. Generic mapping tools: Improved version released. Eos Transactions American Geophysical Union 94 (45), 409–410.
Go to article

Authors and Affiliations

Polina Lemenkova
1
ORCID: ORCID

  1. Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Department of Natural Disasters, Anthropogenic Hazards and Seismicity of the Earth, Laboratory of Regional Geophysics and Natural Disasters, Bolshaya Gruzinskaya Str. 10, Bld. 1, Moscow, 123995, Russian Federation;
Download PDF Download RIS Download Bibtex

Abstract

On the basis of about 12500 depth measurements of which 6700 were taken from r/v Profesor Siedlecki, 1300 from r/v Polarstern and the remainder from British navigation charts, a bathymetric chart of the Bransfield Strait in the scale 1:500 000 has been prepared. Within the assumed boundaries the total area of the Bransfield Strait covers 65308.6 square kilometres, of which the Western Basin covers 23.5%, Central Basin — 47.3%, and Eastern Basin 29.2%. Capacity of the whole Bransfield Strait amounts to 38451 km3 . The average depth of the Bransfield Strait is 592 m.

Go to article

Authors and Affiliations

Jan Szeliga
Stanisław Rakusa-Suszczewski
Download PDF Download RIS Download Bibtex

Abstract

Lexical knowledge sources are indispensable for research, education and general information. The transition of the reference works to the digital world has been a gradual one. This paper discusses the basic principles and structure of knowledge presentation, as well as user access and knowledge acquisition with specific consideration of contributions in German. The ideal reference works of the future should be interactive, optimally adapted to the user, reliable, current and quotable.
Go to article

Authors and Affiliations

Wolf Günther Koch
Download PDF Download RIS Download Bibtex

Abstract

Eye tracking constitutes a valuable tool for the examination of human visual behavior since it provides objective measurements related to the performed visual strategies during the observation of any type of visual stimuli. Over the last decade, eye movement analysis contributed substantially to the better understanding of how visual attention processes work in different types of maps. Considering the clear need for the examination of map user reaction during the observation of realistic cartographic products (i.e. static maps, animated maps, interactive and multimedia maps), a critical amount of experimental studies were performed in order to study different aspects related to map reading process by the cartographic community. The foundation of these studies is based on theories and models that have been developed in similar research domains (i.e. psychology, neuroscience etc.), while the research outcomes that produced over these years can be used directly for the design of more effective and efficient maps. The aim of the present article is to summarize and present the current panorama of the existing eye tracking studies in cartographic research appeared over the last decade. Additionally, methodological contributions (including analysis tools) of cartographic society in the field of eye movement analysis are reported, while existing challenges and future perspectives are also discussed.

Go to article

Authors and Affiliations

Vassilios Krassanakis
Paweł Cybulski
Download PDF Download RIS Download Bibtex

Abstract

In this paper, the climate and environmental datasets were processed by the scripts of Generic Mapping Tools (GMT) and R to evaluate changes in climate parameters, vegetation patters and land cover types in Burkina Faso. Located in the southern Sahel zone, Burkina Faso experiences one of the most extreme climatic hazards in sub-saharan Africa varying from the extreme floods in Volta River Basin, to desertification and recurrent droughts.. The data include the TerraClimate dataset and satellite images Landsat 8-9 Operational Land Imager (OLI) and Thermal Infrared (TIRS) C2 L1. The dynamics of target climate characteristics of Burkina Faso was visualised for 2013-2022 using remote sensing data. To evaluate the environmental dynamics the TerraClimate data were used for visualizing key climate parameter: extreme temperatures, precipitation, soil moisture, downward surface shortwave radiation, vapour pressure deficit and anomaly. The Palmer Drought Severity Index (PDSI) was modelled over the study area to estimate soil water balance related to the soil moisture conditions as a prerequisites for vegetation growth. The land cover types were mapped using the k-means clustering by R. Two vegetation indices were computed to evaluate the changes in vegetation patterns over recent decade. These included the Normalized Difference Vegetation Index (NDVI) and the Soil-Adjusted Vegetation Index (SAVI) The scripts used for cartographic workflow are presented and discussed. This study contributes to the environmental mapping of Burkina Faso with aim to highlight the links between the climate processes and vegetation dynamics in West Africa.
Go to article

Authors and Affiliations

Polina Lemenkova
1
ORCID: ORCID
Olivier Debeir
2
ORCID: ORCID

  1. Universität Salzburg, Salzburg, Austria
  2. Université Libre de Bruxelles, Brussels, Belgium
Download PDF Download RIS Download Bibtex

Abstract

The paper outlines the methodological issues connected to national statistics, their cartographical representations, and the methods of conducting censuses. During the Paris Peace Conference representatives of new Central- and Eastern European states vehemently criticized the ethnic statistics developed by the empires, mostly Russian and Austro-Hungarian. The censuses, conducted in these new states in early 1920s, were criticized along similar lines by the minorities. Among the most vociferous critics were German geographers. Pointing out to the results of the plebiscites in Silesia, Carinthia and other regions they argued, that national identity did not have to correspond to the mother tongue, and census authorities should have taken it into account. Paradoxically, they considered this point valid only to the Central and Eastern Europe, not Western Europe. In the final part of the paper the position of geographers and statisticians in post-war debates are confronted with information on the behaviour of respondents during the censuses in Poland and Czechoslovakia.

Go to article

Authors and Affiliations

Maciej Górny
Download PDF Download RIS Download Bibtex

Abstract

Bogdan Ney was born on 3 February 1935 in Pinsk. After graduating from high school in Tarnow in 1952, he attended the AGH University of Science and Technology in Cracow, where at the Department of Mining Surveying he received his MSc degree in 1957. At the same faculty he obtained his PhD degree in 1963 and habilitation in 1977. Two years later he was awarded the title of extraordinary professor of technical sciences, and in 1989 – the title of full professor.

His scientific career started in 1957 at the AGH University of Science and Technology in Cracow working as an assistant at the Department of the Descriptive Geometry, which from 1960 he continued in the Department of Geodesy and Surveying Data Processing. In 1969–1974 he served as the deputy director at the Institute of Mining and Engineering Surveying of the AGH University of Science and Technology in Cracow. His scientific interest focused on the problems of errors in surveying measurements, adaptation of some statistical techniques to the needs of surveying and development of surveying calculation methods, and methods and techniques of inventory, implementation and control measurements in engineering and engineering surveying. In 1974 Bogdan Ney was transferred to the Institute of Geodesy and Cartography (IGiK) in Warsaw for the position of director of the Institute which he held until 1991. In 1986, he was elected a corresponding member of the Polish Academy of Sciences (PAS), and in 2002 a full member of PAS. As the director and then the head of the System Research Laboratory of IGiK he was further involved in research, providing valuable contributions in the following fields: the use of principles and techniques of aerial and satellite remote sensing in various fields of science and applications; general, organizational and economic problems of surveying and mapping as well as related disciplines; spatial information systems; scientific and scientific-technical policy. In 1991–1997 he continued his educational activity lecturing at the Military University of Technology. The entire scientific achievements of Bogdan Ney consist of more than 300 publications, and many presentations on national and international conferences and seminars. His was the author/coauthor of 24 monographs, 6 textbooks and many other scientific reports. He successfully supervised 10 PhD students.

Bogdan Ney had great achievements in organizational and social activities. He was active in numerous committees, councils, societies and associations. In 1998 the Agriculture-Technical Academy in Olsztyn honoured Bogdan Ney awarding him an honorary doctor degree. Bogdan Ney enjoyed widespread recognition of the scientific community due to his high culture, responsibility in carrying out numerous duties, supporting young scientists, outstanding ability to solve conflict situations and sincere kindness towards all people. He was not only a respected scientist and authority, but also a wonderful man, full of tact and warmth, admired and liked by colleagues. Professor Bogdan Ney, age 85, passed away in Warsaw, on 23 March 2020. He was one of the outstanding surveyors with wide reputation in the scientific community.

Go to article

Authors and Affiliations

Jan Kryński
Download PDF Download RIS Download Bibtex

Abstract

Research of semiotic aspects Lithuanian military air navigation charts was based on the semantic, graphic and information load analysis. The aim of semantic analysis was to determine how the conventional cartographical symbols, used in air navigation charts, correspond with carto-linguistic and carto-semiotic requirements. The analysis of all the markings was performed complex and collected by questionnaire were interviewed various respondents: pilots, cartographers and other chart users. The researches seek two aims: evaluate information and graphical load of military air navigation charts. Information load evaluated to calculate all objects and phenomenon, which was in 25 cm² of map. Charts analysis showed that in low flight charts (LFC) average information load are 4 – 5 times richer than in the operational maps. Map signs optimization on LFC has to be managed very carefully, choosing signs that can reduce the load of information and helps for the information transfer process. Graphical load of maps evaluated of aeronautical maps is not great (5 – 12%) and does not require reduction the information load and generalization of charts. Air navigation charts analysis pointed that not all air navigation sings correspond carto-semiotic requirements and must be improved. The authors suggested some new sings for military air navigation chart, which are simpler, equivalent to human psychophysical perception criteria, creates faster communication and less load on the chart.
Go to article

Authors and Affiliations

Donatas Ovodas
Algimantas Česnulevičius
Download PDF Download RIS Download Bibtex

Abstract

In the present research, a scripting cartographic technique for the environmental mapping of Ethiopia using climate and topographic datasets is developed. The strength of the Generic Mapping Tools (GMT) is employed for the effective visualisation of the seven maps using high-resolution data: GEBCO, TerraClimate, WorldClim, CRUTS 4.0 in 2018 by considering the solutions of map design. The role of topographic characteristics for climate variables (evapotranspiration, downward surface shortwave radiation, vapour pressure, vapour pressure deficit and climatic water deficit) is explained. Topographic variability of Ethiopia is illustrated for geographically dispersed and contrasting environmental setting in its various regions: Afar, Danakil Depression, Ethiopian Highlands, Great Rift Valley, lowlands and Ogaden Desert. The relationships between the environmental and topographic variables are investigated with aid of literature review and the outcomes are discussed. The maps are demonstrated graphically to highlight variables enabling to find correlations between the geographic phenomena, their distribution and intensity. The presented maps honor the environmental and topographic data sets within the resolution of the data. Integration of these results in the interpretation maps presented here brings new insights into both the variations of selected climate variables, and the topography of Ethiopia.
Go to article

Authors and Affiliations

Polina Lemenkova
1
ORCID: ORCID

  1. Université Libre de Bruxelles (ULB), École polytechnique de Bruxelles (Brussels Faculty of Engineering), Laboratory of Image Synthesis and Analysis, Building L, Campus de Solbosch, Avenue Franklin Roosevelt 50, Brussels 1000, Belgium
Download PDF Download RIS Download Bibtex

Abstract

The article raises the issue of zoning of the central area of Zamosc based on downtown unrealized projects. It also explains the genesis of the formation of its range and the spatial layout, which affected the functioning of nineteenth-century fortress. As early as 1804. Entailer Stanisław Kostka Zamoyski planned to demolish the decaying fortifications and sell strip of land fortress for development. Change the situation on the political arena of Europe made Zamosc under Tsarist Russia became a fortress – a closed town, where civilian activity have been pushed to the back burner and separated from the historical center of strategic cordoned off the circuit. It was not until 24 years after the dissolution of the fortress, in 1880. returned to the development concept of post-fortress area in connection with the planned development of the city, but this met with opposition the military commission – the owner of the land. After regaining independence, the magistrate put forward ambitious building projects realization in the esplanade of the formerly fortress, which this time met with the resistance of the military commissions. As a result of the conversion of disputed land in the late 30’s the post-fortress area was possible to invest. An example was enacted in 1939, pioneering in many respects, zoning plan Zamosc by Władyslaw Wieczorkiewicza and Jan Zachwatowicz in which the authors called for implementation of the downtown on the basis of a linear array of bifocal between the old town (Stare Miasto) and the Nowa Osada suburb.

Go to article

Authors and Affiliations

Jakub Żygawski
Download PDF Download RIS Download Bibtex

Abstract

The study analyses the notes written on the map of Bohemia and two Latin versions of the description of Bohemia in the first modern atlas Theatrum Orbis Terrarum by Abraham Ortelius. It examines the method of Ortelius’s work with cartographic material and his approach to the composition of the descriptive texts on the reverse sides, which he himself considered to be the main contribution of his atlas. The success of the atlas with its series of editions demonstrates the importance of the texts in their impact on the basic knowledge of regions and countries in early modern European society. The analysis of the two Latin versions of the description of Bohemia also proves Ortelius’s endeavor to update the information.
The map of Bohemia, published by Johann Criginger in 1568, was supplemented by Ortelius in his atlas with notes on some Czech towns and places, which he took from Sebastian Münster's Cosmographia. In the first Latin description of Bohemia, the author based his work primarily on Historia Bohemica by Annaeas Silvius Piccolomini (Pope Pius II), and in the second version, which appears in Theatrum Orbis Terrarum from the 1574 Latin edition, he takes the text from the recent Historiae Regni Boiemiae by Jan Dubravius. The annexes provide transcriptions of both of Ortelius’s versions of the characteristics of Bohemia.
Go to article

Authors and Affiliations

Jan Vojtíšek
1
ORCID: ORCID

  1. Department of Manuscripts and Early Printed Books, National Library of the Czech Republic, Klementinum 190, 110 00 Prague
Download PDF Download RIS Download Bibtex

Abstract

The South Sandwich Trench located eastward of the Drake Passage in the Scotia Sea between Antarctica and South America is one of the least studied deep-sea trenches. Its geomorphological formation and present shape formed under the strong influence of the tectonic plate movements and various aspects of the geological setting, i.e., sediment thickness, faults, fracture zones and geologic lineaments. The aim of this paper is to link the geological and geophysical setting of the Scotia Sea with individual geomorphological features of the South Sandwich Trench in the context of the phenomena of its formation and evolution. Linking several datasets (GEBCO, ETOPO1, EGM96, GlobSed and marine freeair gravity raster grids, geological vector layers) highlights correlations between various factors affecting deep-sea trench formation and development, using the Generic Mapping Tools (GMT) for cartographic mapping. The paper contributes to the regional studies of the submarine geomorphology in the Antarctic region with a technical application of the GMT cartographic scripting toolset.
Go to article

Authors and Affiliations

Polina Lemenkova
1
ORCID: ORCID

  1. Schmidt Institute of Physics of the Earth, Russian Academy of Sciences. Bolshaya Gruzinskaya St, 10, Bld. 1, Moscow, 123995, Russian Federation

This page uses 'cookies'. Learn more