<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD JATS (Z39.96) Journal Publishing DTD v1.3 20210610//EN" "JATS-journalpublishing1-3.dtd">
<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-2165</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>Статьи</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Article</subject></subj-group></article-categories><title-group><article-title>О механизме деятельности речного бассейна (результаты стационарных наблюдений)</article-title><trans-title-group xml:lang="en"><trans-title>The mechanism of river basin action (on the basis of the experimental site data)</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>Хмелева</surname><given-names>Н. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Khmeleva</surname><given-names>N. V.</given-names></name></name-alternatives></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Виноградова</surname><given-names>Н. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Vinogradova</surname><given-names>N. N.</given-names></name></name-alternatives></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Шевченко</surname><given-names>Б. Ф.</given-names></name><name name-style="western" xml:lang="en"><surname>Shevchenko</surname><given-names>B. F.</given-names></name></name-alternatives></contrib></contrib-group><pub-date pub-type="collection"><year>2003</year></pub-date><pub-date pub-type="epub"><day>16</day><month>07</month><year>2022</year></pub-date><volume>0</volume><issue>4</issue><issue-title>Геоморфология</issue-title><fpage>23</fpage><lpage>32</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Хмелева Н.В., Виноградова Н.Н., Шевченко Б.Ф., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Хмелева Н.В., Виноградова Н.Н., Шевченко Б.Ф.</copyright-holder><copyright-holder xml:lang="en">Khmeleva N.V., Vinogradova N.N., Shevchenko B.F.</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/2165">https://geomorphology.igras.ru/jour/article/view/2165</self-uri><abstract><p>The erosion and accumulation phases of river basin action were distinguished as a result of nearly 30-year stationary field study. The phase changes are affected by 11-year cycle of solar activity, which causes the changes in humidity and hence in the exogenous processes activity. The 20th cycle corresponds to the phase of accumulation, the 21st - to the phase of erosion.</p></abstract><trans-abstract xml:lang="en"><p>The erosion and accumulation phases of river basin action were distinguished as a result of nearly 30-year stationary field study. The phase changes are affected by 11-year cycle of solar activity, which causes the changes in humidity and hence in the exogenous processes activity. The 20th cycle corresponds to the phase of accumulation, the 21st - to the phase of erosion.</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>
