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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-3364</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>Роль экстремальных метеорологических явлений в развитии эрозионных процессов в Прибайкалье</article-title><trans-title-group xml:lang="en"><trans-title>Importance of extreme meteorological events in the erosional processes in the Baikal region</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>Рыжов</surname><given-names>Ю. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Ryzhov</surname><given-names>Yu. V.</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 СО РАН, Иркутск</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1996</year></pub-date><pub-date pub-type="epub"><day>26</day><month>10</month><year>2023</year></pub-date><volume>0</volume><issue>3</issue><fpage>96</fpage><lpage>99</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Рыжов Ю.В., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Рыжов Ю.В.</copyright-holder><copyright-holder xml:lang="en">Ryzhov Y.V.</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/3364">https://geomorphology.igras.ru/jour/article/view/3364</self-uri><abstract><p>A relief-forming role of extreme meteorological events is discussed with reference to the Barguzin Basin, erosional landform development (rills and gullies) being analysed. lt is found that the most favorable conditions for erosion exist on the inclined piedmont plains.</p></abstract><trans-abstract xml:lang="en"><p>A relief-forming role of extreme meteorological events is discussed with reference to the Barguzin Basin, erosional landform development (rills and gullies) being analysed. lt is found that the most favorable conditions for erosion exist on the inclined piedmont plains.</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>
