| ||
|
| ||
|
doi:10.24411/2687-1092-2019-10608 1 V. S. Sobolev Institute of Geology and Mineralogy SB RAS, Novosibirsk, Russia 2 A. A. Trofimuk Institute of Petroleum Geology and Geophysics SB RAS, Novosibirsk, Russia 3 Novosibirsk State University, Novosibirsk, Russia
|
|
Abstract. We repeated UAV-based imaging of Samoylov Island (south part of the Lena river Delta). Early, we got remote sensing data of this island during the 2016 summer. These data allowed carrying out detail geomorphological mapping. Results of 2019 UAV-based imaging, e.g. orthophoto maps and a digital elevation model could be used for estimation of topography changes and reveling of relief dynamic main trends. Keywords: UAV, photogrammetry, geomorphological mapping, ice-wedge polygons, Arctic Centre – Scientific Research station “Samoylovsky Island”.
REFERENCES: Kartoziia A. Assessment of the Ice Wedge Polygon Current State by Means of UAV Imagery Analysis (Samoylov Island, the Lena Delta) // Remote Sensing. 2019. Vol. 11, 1627. doi:10.3390/rs11131627 Schwamborn G., Rachold V., Grigoriev M.N. Late Quaternary Sedimentation History of the Lena Delta // Quaternary International. 2002. Vol. 89. Is. 1. P. 119–134. doi:10.1016/S1040-6182(01)00084-2 Bolshiyanov D.Yu., Makarov A.S., Schneider V., Shtof G. Origin and development of the Lena River delta. St. Petersburg: AARI publishing house, 2013. 268 p. Grigoriev M.N. Cryomorphogenesis of the mouth area of the Lena River. Yakutsk: Institute of Permafrost Science SB RAS, 1993. 176 p. Olenchenko V.V., Kartoziya A.A., Tsibizov L.V., Osipova P.S., Esin E.I. Geoelectrical characteristics of Samoylov Island coastline (Lena river delta) // Russian Journal of Geophysical Technologies. 2018. Is. 4. P. 39-49. doi:10.18303/2619-1563-2018-4-5 |
|
Cite this article:
Kartoziia А.А., Mishina A. Detail geomorphological mapping of periglacial landforms by using GIS-analyze of UAV remote sensing data // Relief and Quaternary deposits of the Arctic, Subarctic and North-West Russia. 2019. Issue 6. P. 47-52. doi:10.24411/2687-1092-2019-10608 |
