Persistent mass loss of Triangular Glacier, James Ross Island, northeastern Antarctic Peninsula
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F23%3A10447342" target="_blank" >RIV/00216208:11310/23:10447342 - isvavai.cz</a>
Alternative codes found
RIV/00216224:14310/23:00129985
Result on the web
<a href="https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=XqYEZi~-~r" target="_blank" >https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=XqYEZi~-~r</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1017/jog.2022.42" target="_blank" >10.1017/jog.2022.42</a>
Alternative languages
Result language
angličtina
Original language name
Persistent mass loss of Triangular Glacier, James Ross Island, northeastern Antarctic Peninsula
Original language description
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 glacier in the northern part of James Ross Island receded rapidly during the period of regional warming in the late 20th century, losing 30.8% of its surface area between 1979 and 2006 (-1.7% a(-1)). The retreat rate then dropped to -0.3% a(-1) following the regional cooling trend, but started to accelerate again (-0.8 to -2.3% a(-1)) with increasing air temperature since the summer 2014/15. Since the glaciological year 2015/16, Triangular Glacier has experienced enhanced snow melt, wind scour and permanent mass loss with annual mass balance ranging from -0.08 +- 0.35 to -0.56 +- 0.25 m w.e. The largest mass loss was observed in the glaciological year 2019/20, which included the warmest summer of the observation period. The cumulative mass balance of -1.66 +- 0.83 m w.e. over the years 2014/15-2019/20 is consistent with the termination of the positive mass-balance period that occurred in the north-eastern Antarctic Peninsula from 2009/10 to 2014/15.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10508 - Physical geography
Result continuities
Project
Result was created during the realization of more than one project. More information in the Projects tab.
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2023
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Journal of Glaciology
ISSN
0022-1430
e-ISSN
1727-5652
Volume of the periodical
69
Issue of the periodical within the volume
273
Country of publishing house
GB - UNITED KINGDOM
Number of pages
13
Pages from-to
27-39
UT code for WoS article
000808370600001
EID of the result in the Scopus database
2-s2.0-85148709899