Surface mass balance of small glaciers on James Ross Island, north-eastern Antarctic Peninsula, during 2009-2015
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F18%3A10380394" target="_blank" >RIV/00216208:11310/18:10380394 - isvavai.cz</a>
Alternative codes found
RIV/00216224:14310/18:00101230
Result on the web
<a href="https://doi.org/10.1017/jog.2018.17" target="_blank" >https://doi.org/10.1017/jog.2018.17</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1017/jog.2018.17" target="_blank" >10.1017/jog.2018.17</a>
Alternative languages
Result language
angličtina
Original language name
Surface mass balance of small glaciers on James Ross Island, north-eastern Antarctic Peninsula, during 2009-2015
Original language description
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. was observed during the 2009-2015 period on Whisky Glacier and Davies Dome, respectively. The results indicate a change from surface mass loss that prevailed in the region during the first decade of the 21st century to predominantly positive surface mass balance after 2009/10. The spatial pattern of annual surface mass-balance distribution implies snow redistribution by wind on both glaciers. The mean equilibrium line altitudes for Whisky Glacier (311 +/- 16 m a.s.l.) and Davies Dome (393 +/- 18m a.s.l.) are in accordance with the regional data indicating 200-300 m higher equilibrium line on James Ross and Vega Islands compared with the South Shetland Islands. The mean accumulation-area ratio of 0.68 +/- 0.09 and 0.44 +/- 0.09 determined for Whisky Glacier and Davies Dome, respectively, is similar to the value reported for Vega Island and within the range of typical values for high-latitude glaciers.
Czech name
—
Czech description
—
Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
—
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
2018
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
—
Volume of the periodical
64
Issue of the periodical within the volume
245
Country of publishing house
GB - UNITED KINGDOM
Number of pages
13
Pages from-to
349-361
UT code for WoS article
000434777300001
EID of the result in the Scopus database
2-s2.0-85045658570