Zobrazeno 1 - 10
of 54
pro vyhledávání: '"ZBYNĚK ENGEL"'
Publikováno v:
Journal of Glaciology, Vol 69, Pp 27-39 (2023)
The retreat rates of Triangular Glacier since 1979 and its mass changes during the period 2014/15–2019/20 indicate the sensitive response of small ice masses on the eastern side of the Antarctic Peninsula to air temperature evolution. This cirque g
Externí odkaz:
https://doaj.org/article/017dd95470f34f02ae05a1067c1f444c
Autor:
Tereza Dlabáčková, Zbyněk Engel
Publikováno v:
Acta Universitatis Carolinae Geographica, Vol 57, Iss 1, Pp 3-15 (2022)
An extensive debris flow occurred, in the Smutná valley, Western Tatra Mts. in Slovakia on 15 May 2014. The aim of this study is to describe the morphology of the observed debris flow and to evaluate the conditions that preceded its formation as wel
Externí odkaz:
https://doaj.org/article/7d4c2637ed394ba494760bf2d2c73ff3
Autor:
Stephen J. A. Jennings, Bethan J. Davies, Daniel Nývlt, Neil F. Glasser, Zbyněk Engel, Filip Hrbáček, Jonathan L. Carrivick, Bedřich Mlčoch, Michael J. Hambrey
Publikováno v:
Journal of Maps, Vol 17, Iss 2, Pp 125-139 (2021)
This study presents a 1:25,000 geomorphological map of the northern sector of Ulu Peninsula, James Ross Island, Antarctic Peninsula. The map covers an area of c. 250 km2, and documents the landforms and surficial sediments of one of the largest ice-f
Externí odkaz:
https://doaj.org/article/d64bf174a8d140fb8a3c8bf4f273cd2d
Publikováno v:
Journal of Maps, Vol 15, Iss 2, Pp 563-569 (2019)
Patterned ground in mountainous areas has a high palaeogeographic significance as it is associated with cold environments and frequently with permafrost conditions. Most patterned ground (i.e. sorted polygons, sorted nets, sorted stripes) in the High
Externí odkaz:
https://doaj.org/article/1455e74b2ad14ac5b5dd80a45ce670d1
Publikováno v:
Journal of Glaciology, Vol 65, Pp 410-421 (2019)
The long-term warming on the Antarctic Peninsula in the second half of the 20th century prompted rapid retreat of glaciers on the peninsula and surrounding islands. Retreat accelerated until the beginning of the new millennium when the regional warmi
Externí odkaz:
https://doaj.org/article/891fb599e68f42a08d3a3c7af62dd764
Autor:
Vojtěch Ettler, Markéta Cihlová, Alice Jarošíková, Martin Mihaljevič, Petr Drahota, Bohdan Kříbek, Aleš Vaněk, Vít Penížek, Ondra Sracek, Mariana Klementová, Zbyněk Engel, Fred Kamona, Ben Mapani
Publikováno v:
Environment International, Vol 124, Iss , Pp 205-215 (2019)
Ore mining and processing in semi-arid areas is responsible for the generation of metal(loid)-containing dust, which is easily transported by wind to the surrounding environment. To assess the human exposure to dust-derived metal(loid)s (As, Cd, Cu,
Externí odkaz:
https://doaj.org/article/16886b65480d4bd8bf5cb769b1c35efc
Publikováno v:
Journal of Glaciology, Vol 64, Pp 349-361 (2018)
Two small glaciers on James Ross Island, the north-eastern Antarctic Peninsula, experienced surface mass gain between 2009 and 2015 as revealed by field measurements. A positive cumulative surface mass balance of 0.57 ± 0.67 and 0.11 ± 0.37 m w.e.
Externí odkaz:
https://doaj.org/article/60a839916398469897028939e98a6bf3
Publikováno v:
Journal of Glaciology, Pp 1-15
Glaciers cover 132 900 km2 around the Antarctic Ice Sheet, but few are subject to annual mass-balance measurements. Lookalike Glacier and Davies Dome on James Ross Island have been monitored since 2009, providing the third longest mass-balance record
Externí odkaz:
https://doaj.org/article/5075f5ae4a2e41ca956ca46593309128
Publikováno v:
Journal of Glaciology, Pp 1-1
Externí odkaz:
https://doaj.org/article/4750635fe2c348968c19c00f13f5f234
Publikováno v:
Journal of Glaciology. 69:27-39
The retreat rates of Triangular Glacier since 1979 and its mass changes during the period 2014/15–2019/20 indicate the sensitive response of small ice masses on the eastern side of the Antarctic Peninsula to air temperature evolution. This cirque g
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bcfd0c5424940dc4a650855c50aa4744
https://doi.org/10.1017/jog.2022.42
https://doi.org/10.1017/jog.2022.42