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<article article-type="research-article" dtd-version="1.3" 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" xml:lang="ru"><front><journal-meta><journal-id journal-id-type="publisher-id">geomorf</journal-id><journal-title-group><journal-title xml:lang="ru">Геоморфология и палеогеография</journal-title><trans-title-group xml:lang="en"><trans-title>Geomorfologiya i Paleogeografiya</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2949-1789</issn><issn pub-type="epub">2949-1797</issn><publisher><publisher-name></publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">geomorf-2788</article-id><article-categories><subj-group subj-group-type="heading"><subject>Research Article</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>Научные сообщения</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Short communications</subject></subj-group></article-categories><title-group><article-title>Интенсивность современной денудации северного склона Алайского хребта</article-title><trans-title-group xml:lang="en"><trans-title>Present-day erosion rate at the northern slope of the Altai Ridge</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Курбатова</surname><given-names>Л. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Kurbatova</surname><given-names>L. S.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Переслегина</surname><given-names>Р. Е.</given-names></name><name name-style="western" xml:lang="en"><surname>Pereslegina</surname><given-names>R. E.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт географии АН СССР</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1988</year></pub-date><pub-date pub-type="epub"><day>21</day><month>11</month><year>2022</year></pub-date><volume>0</volume><issue>4</issue><issue-title>Геоморфология</issue-title><fpage>49</fpage><lpage>54</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Курбатова Л.С., Переслегина Р.Е., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Курбатова Л.С., Переслегина Р.Е.</copyright-holder><copyright-holder xml:lang="en">Kurbatova L.S., Pereslegina R.E.</copyright-holder><license xml:lang="ru" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>Данная работа распространяется под лицензией Creative Commons Attribution 4.0.</license-p></license><license xml:lang="en" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>This work is licensed under a Creative Commons Attribution 4.0 License.</license-p></license></permissions><self-uri xlink:href="https://geomorphology.igras.ru/jour/article/view/2788">https://geomorphology.igras.ru/jour/article/view/2788</self-uri><abstract><p>The present-day erosion rate has been estimated within mountain area of the northern slope of the Alai Ridge using two methods: 1) based on solid runoff data, and 2) based on sediments volume in the Abshirsai Lake. Total rate of erosion on the Alai Ridge slope amounts to 0.22 mm per year. The value calculated from the volume of the lake deposits is in reasonable agreement with data obtained by solid runoff measurements in the rivers near the lake.</p></abstract><trans-abstract xml:lang="en"><p>The present-day erosion rate has been estimated within mountain area of the northern slope of the Alai Ridge using two methods: 1) based on solid runoff data, and 2) based on sediments volume in the Abshirsai Lake. Total rate of erosion on the Alai Ridge slope amounts to 0.22 mm per year. The value calculated from the volume of the lake deposits is in reasonable agreement with data obtained by solid runoff measurements in the rivers near the lake.</p></trans-abstract></article-meta></front><back><ref-list><title>References</title></ref-list><fn-group><fn fn-type="conflict"><p>The authors declare that there are no conflicts of interest present.</p></fn></fn-group></back></article>
