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<article article-type="review-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">hydrophysics</journal-id><journal-title-group><journal-title xml:lang="ru">Фундаментальная и прикладная гидрофизика</journal-title><trans-title-group xml:lang="en"><trans-title>Fundamental and Applied Hydrophysics</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2073-6673</issn><issn pub-type="epub">2782-5221</issn><publisher><publisher-name>St. Petersburg Research Center of the Russian Academy of Sciences</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.59887/2073-6673.2023.16(3)-6</article-id><article-id custom-type="elpub" pub-id-type="custom">hydrophysics-1238</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>ФУНДАМЕНТАЛЬНЫЕ ВОПРОСЫ ГИДРОФИЗИКИ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>FUNDAMENTAL ISSUES OF HYDROPHYSICS</subject></subj-group></article-categories><title-group><article-title>Доплеровский эффект и волны Россби в океане: краткий экскурс в историю и новые подходы</article-title><trans-title-group xml:lang="en"><trans-title>Doppler effect and Rossby waves in the ocean: A brief history and new approaches</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-6654-5570</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Гневышев</surname><given-names>В. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Gnevyshev</surname><given-names>V. G.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Владимир Григорьевич Гневышев</p><p>117997</p><p>Нахимовский проспект, д. 36</p><p>Москва</p><p>РИНЦ Author ID: 298530</p><p>Scopus Author ID: AAZ-6352–2021</p><p>WoS ResearcherID: 6507346231</p></bio><bio xml:lang="en"><p>117997</p><p>36 Nakhimovsky Prosp.</p><p>Moscow</p></bio><email xlink:type="simple">avi9783608@gmail.com</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-4608-7781</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Белоненко</surname><given-names>Т. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Belonenko</surname><given-names>T. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Татьяна Васильевна Белоненко</p><p>199034</p><p>Университетская наб., д. 7–9</p><p>Санкт-Петербург</p><p>РИНЦ Author ID: 66026</p><p>Scopus Author ID: 6507005889</p><p>WoS ResearcherID: K-2162–2013</p></bio><bio xml:lang="en"><p>199034</p><p>7–9 Universitetskaya Emb.</p><p>St. Petersburg</p></bio><email xlink:type="simple">btvlisab@yandex.ru</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт океанологии им. П.П. Ширшова РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Shirshov Institute оf Oceanology, Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Санкт-Петербургский государственный университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>St. Petersburg State University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2023</year></pub-date><pub-date pub-type="epub"><day>19</day><month>10</month><year>2023</year></pub-date><volume>16</volume><issue>3</issue><fpage>72</fpage><lpage>92</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Гневышев В.Г., Белоненко Т.В., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Гневышев В.Г., Белоненко Т.В.</copyright-holder><copyright-holder xml:lang="en">Gnevyshev V.G., Belonenko T.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://hydrophysics.spbrc.ru/jour/article/view/1238">https://hydrophysics.spbrc.ru/jour/article/view/1238</self-uri><abstract><p>   Представленная обзорная статья посвящена волнам Россби в океане. Сегодня существует множество научных работ по этой теме, в которых авторы по-разному подходят к изложению материала. Для исследователей, которые не слишком подробно занимались представленными вопросами, анализ таких источников часто воспринимается как совокупность разрозненной и противоречивой информации, не позволяющей получить адекватное представление попредмету. В статье на основе анализа основных тематических публикаций систематизированы основные представления по различным аспектам, а также проведено сравнение различных подходов. Особое внимание уделяется обзору дисперсионных соотношений волн Россби при наличии фонового потока с акцентом на наличие либо отсутствие доплеровской добавки к частоте. Хотя рассматриваемые постановки задач и дисперсионные соотношения, как правило, являются общеизвестными, однако у многих авторов они изложены существенно по-разному, что часто приводит к непониманию и путанице. Мы обращаем внимание читателя на ключевые спорные моменты и приводим различные подходы в единую стройную систему. Если длинные волны Россби не «чувствуют» течения, то это справедливо для модели «мелкой воды» и является следствием галилеевской неинвариантности дисперсионного соотношения. Рассматривая различные подходы, мы показываем, что строгого дисперсионного соотношения для галилеево-неинвариантного дисперсионного соотношения нет. Всегда добавляются некие не совсем строгие предположения и допущения, такие как формальное существование вертикальных границ или зависимость баротропного радиуса от переменной поперечной координаты. Выводы дисперсионного соотношения с недоплеровским сдвигом содержат также некие асимптотические разложения, сопровождаемые анализом теории размерностей. Используя общую терминологию, мы соединяемосновные аналитические результаты по теме и излагаем их в единой логике.</p></abstract><trans-abstract xml:lang="en"><p>   The review is devoted to Rossby waves in the ocean. Currently, there are many monographs and scientific articles on this topic, in which the authors approach the presentation of the material in different ways. For researchers who have not delved too deeply into this topic, the analysis of these sources is often perceived as a collection of disparate and often contradictory information that does not allow an adequate understanding of the subject. The review is based on the analysis of the main publications on this topic, and it systematizes the main ideas in various aspects. We also give the readers a comparison of different approaches in this area. Particular attention is paid to the review of the dispersion relations of Rossby waves in the presence of a background flow with an emphasis on the presence or absence of a Doppler additive to the frequency. Although the problem statements and variance ratios under consideration are generally well-known, however, they are presented in significantly different ways by many authors, which often leads to misunderstanding and confusion. We draw the reader’s attention to the key controversial points and bring various approaches into a single coherent system. If long Rossby waves do not “feel” the flow, then this is true for the “shallow water” model and is a consequence of the Galilean non-invariance of the dispersion relation. Considering various approaches, we show that there is no strict dispersion relation for the Galilean-non-invariant dispersion relation. Some not quite strict assumptions and assumptions are always added, such as the formal existence of vertical boundaries or the dependence of the barotropic radius on the variable transverse coordinate. The derivation of the dispersion relation with the Doppler shift also contains some asymptotic expansions, accompanied by an analysis of the theory of dimensions. Using common terminology, we combine the main analytical results on the topic and present them in a single logic.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>волны Россби</kwd><kwd>дисперсионное соотношение</kwd><kwd>доплеровский сдвиг</kwd><kwd>галилеевская неинвариантность</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Rossby waves</kwd><kwd>dispersion relation</kwd><kwd>Doppler shift</kwd><kwd>Galilean noninvariance</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена по теме государственного задания 0128-2021-0003, а также при финансовой поддержке гранта СПбГУ № 94033410 и гранта РНФ 22-27-00004</funding-statement><funding-statement xml:lang="en">The publication was made with the financial support of State assignment theme No. 0128-2021-0003, the St Petersburg State University Grant No. 94033410, and RSF Grant No. 22-27-00004</funding-statement></funding-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Margules M. 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