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<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:ali="http://www.niso.org/schemas/ali/1.0/" article-type="other" dtd-version="1.2" xml:lang="en"><front><journal-meta><journal-id journal-id-type="publisher-id">Ice and Snow</journal-id><journal-title-group><journal-title xml:lang="en">Ice and Snow</journal-title><trans-title-group xml:lang="ru"><trans-title>Лед и снег</trans-title></trans-title-group></journal-title-group><issn publication-format="print">2076-6734</issn><issn publication-format="electronic">2412-3765</issn><publisher><publisher-name xml:lang="en">The Russian Academy of Sciences</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="publisher-id">659380</article-id><article-id pub-id-type="doi">10.31857/S2076673423020138</article-id><article-id pub-id-type="edn">RVESBM</article-id><article-categories><subj-group subj-group-type="toc-heading" xml:lang="en"><subject>Glaciers and ice sheets</subject></subj-group><subj-group subj-group-type="toc-heading" xml:lang="ru"><subject>Ледники и ледниковые покровы</subject></subj-group><subj-group subj-group-type="article-type"><subject></subject></subj-group></article-categories><title-group><article-title xml:lang="en">Intra-Annual Variability of the Surface Ablation of the Aldegondabreen Glacier (Spitsbergen)</article-title><trans-title-group xml:lang="ru"><trans-title>Внутрисезонная изменчивость абляции ледника Альдегонда (Шпицберген)</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Prokhorova</surname><given-names>U. V.</given-names></name><name xml:lang="ru"><surname>Прохорова</surname><given-names>У. В.</given-names></name></name-alternatives><email>uvprokhorova@aari.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Terekhov</surname><given-names>A. V.</given-names></name><name xml:lang="ru"><surname>Терехов</surname><given-names>А. В.</given-names></name></name-alternatives><email>uvprokhorova@aari.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Demidov</surname><given-names>V. E.</given-names></name><name xml:lang="ru"><surname>Демидов</surname><given-names>В. Э.</given-names></name></name-alternatives><email>uvprokhorova@aari.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Ivanov</surname><given-names>B. V.</given-names></name><name xml:lang="ru"><surname>Веркулич</surname><given-names>С. Р.</given-names></name></name-alternatives><email>uvprokhorova@aari.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Verkulich</surname><given-names>S. R.</given-names></name><name xml:lang="ru"><surname>Иванов</surname><given-names>Б. В.</given-names></name></name-alternatives><email>uvprokhorova@aari.ru</email><xref ref-type="aff" rid="aff3"/></contrib></contrib-group><aff-alternatives id="aff1"><aff><institution xml:lang="en">Arctic and Antarctic Research Institute</institution></aff><aff><institution xml:lang="ru">Арктический и Антарктический научно-исследовательский институт</institution></aff></aff-alternatives><aff-alternatives id="aff2"><aff><institution xml:lang="en">Saint Petersburg State University</institution></aff><aff><institution xml:lang="ru">Арктический и Антарктический научно-исследовательский институт</institution></aff></aff-alternatives><aff-alternatives id="aff3"><aff><institution xml:lang="en">Arctic and Antarctic Research Institute</institution></aff><aff><institution xml:lang="ru">Санкт-Петербургский государственный университет</institution></aff></aff-alternatives><pub-date date-type="pub" iso-8601-date="2023-04-01" publication-format="electronic"><day>01</day><month>04</month><year>2023</year></pub-date><volume>63</volume><issue>2</issue><fpage>214</fpage><lpage>224</lpage><history><date date-type="received" iso-8601-date="2025-02-20"><day>20</day><month>02</month><year>2025</year></date></history><permissions><copyright-statement xml:lang="en">Copyright ©; 2023, У.В. Прохорова, А.В. Терехов, В.Э. Демидов, С.Р. Веркулич, Б.В. Иванов</copyright-statement><copyright-statement xml:lang="ru">Copyright ©; 2023, У.В. Прохорова, А.В. Терехов, В.Э. Демидов, С.Р. Веркулич, Б.В. Иванов</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="en">У.В. Прохорова, А.В. Терехов, В.Э. Демидов, С.Р. Веркулич, Б.В. Иванов</copyright-holder><copyright-holder xml:lang="ru">У.В. Прохорова, А.В. Терехов, В.Э. Демидов, С.Р. Веркулич, Б.В. Иванов</copyright-holder><license><ali:license_ref xmlns:ali="http://www.niso.org/schemas/ali/1.0/">http://creativecommons.org/licenses/by/4.0</ali:license_ref></license></permissions><self-uri xlink:href="https://journals.eco-vector.com/2076-6734/article/view/659380">https://journals.eco-vector.com/2076-6734/article/view/659380</self-uri><abstract xml:lang="en"><p id="idm45181323422096">The intra-annual variability of the surface ice ablation on the 5.5 km<sup>2</sup> Aldegondabreen glacier (Spitsbergen Island, Barentsburg area) is presented. The ice ablation was measured during five seasons (2018–2022) at the two stakes, installed in the lower part of the glacier and at the index site, where the amount of ablation numerically coincides with the glacier-averaged value with the <italic>r</italic> = 0.99 agreement. The temporal resolution of the ice ablation data is uneven and varies from 3 to 45 days. To carry out the correlation analysis, meteorological data from the automated weather station located near the glacier terminus are used. The ice ablation rates, obtained after normalization for the number of days between stake readings, have a tight correlation with both the air temperature and the downwelling shortwave radiation flux for most of the seasons, in 2018–2021 (<italic>r</italic> = 0.71–0.99). Surface air temperature and short-wave radiation are closely related; the above estimates indicate the leading role of short-wave radiation in the summer ablation of the glacier in the period 2018–2021. The year 2022 became anomalous, as the correlation with the shortwave radiation significantly decreased (<italic>r =</italic> 0.21–0.34). The European heat wave of 2022, which also affected the Svalbard archipelago, interrupted the ordinary intra-annual variability of the air temperature, causing the unprecedented ice melt on Aldegondabreen in September. The predicted increase in frequency and intensity of the future heat waves will result in an increased role of turbulent fluxes in the surface energy balance of the low-elevated Svalbard glaciers. The article demonstrates how the empirically identified dependencies can change from season to season in a non-stationary climate.</p></abstract><trans-abstract xml:lang="ru"><p id="idm45181323425024">Рассмотрена зависимость внутрисезонной изменчивости абляции льда на леднике Альдегонда (Шпицберген) от приземной температуры воздуха и потока коротковолновой радиации. В 2018–2021 гг. абляция льда хорошо согласуется с обоими факторами (<italic>r</italic> = 0.80–0.98 и 0.71–0.99 соответственно). 2022 год – аномальный с точки зрения нарушения связей абляции и радиации, что объясняется продолжительной волной тепла в Европе.</p></trans-abstract><kwd-group xml:lang="en"><kwd>Arctic</kwd><kwd>Svalbard</kwd><kwd>glacier mass balance</kwd><kwd>short-wave radiation</kwd><kwd>heat wave</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>Арктика</kwd><kwd>Шпицберген</kwd><kwd>баланс массы ледника</kwd><kwd>коротковолновая радиация</kwd><kwd>волна тепла</kwd></kwd-group></article-meta></front><body></body><back><ref-list><ref id="B1"><label>1.</label><citation-alternatives><mixed-citation xml:lang="en">Borisik A.L., Novikov A.L., Glazovsky A.F., Lavrentiev I.I., Verkulich S.R. Structure and dynamics of Aldegondabreen, Spitsbergen, according to repeated GPR surveys in 1999, 2018 and 2019. Led i Sneg. 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