{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,2,28]],"date-time":"2026-02-28T07:03:05Z","timestamp":1772262185273,"version":"3.50.1"},"reference-count":40,"publisher":"Copernicus GmbH","issue":"5","license":[{"start":{"date-parts":[[2022,9,29]],"date-time":"2022-09-29T00:00:00Z","timestamp":1664409600000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"DOI":"10.13039\/501100001871","name":"Funda\u00e7\u00e3o para a Ci\u00eancia e a Tecnologia","doi-asserted-by":"publisher","award":["UIDB\/50019\/2020"],"award-info":[{"award-number":["UIDB\/50019\/2020"]}],"id":[{"id":"10.13039\/501100001871","id-type":"DOI","asserted-by":"publisher"}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Ocean Sci."],"abstract":"<jats:p>Abstract. Tropical cyclones (TCs) are extreme climate events that are known\nto strongly interact with the ocean through two mechanisms: dynamically\nthrough the associated intense wind stress and thermodynamically through\nmoist enthalpy exchanges at the ocean surface. These interactions contribute\nto relevant oceanic responses during and after the passage of a TC, namely\nthe induction of a cold wake and the production of chlorophyll (Chl\u00a0a)\nblooms. This study aimed to understand these interactions in the Azores\nregion, an area with relatively low cyclonic activity for the North Atlantic\nbasin, since the area experiences much less intense events than the rest of\nthe basin. Results for the 1998\u20132020 period showed that the averaged induced\nanomalies were on the order of +0.050\u2009mg\u2009m\u22123 for Chl\u00a0a and \u22121.615\u2009\u2218C for SST (sea surface temperature). Furthermore, looking at the role played by\nseveral TCs characteristics we found that the intensity of the TCs was the\nmost important condition for the development of upper-ocean responses.\nAdditionally, it was found that bigger TCs caused greater induced anomalies\nin both variables, while faster ones created greater Chl\u00a0a responses, and\nTCs that occurred later in the season had greater TC-related anomalies. Two\ncase studies (Ophelia in 2017 and Nadine in 2012) were conducted to\nbetter understand each upper-ocean response. Ophelia was shown to affect the\nSST at an earlier stage, while the biggest Chl\u00a0a induced anomalies were\nregistered at a later stage, allowing the conclusion that thermodynamic\nexchanges conditioned the SST more while dynamical mixing might have played\na more important role in the later stage. Nadine showed the importance of\nthe TC track geometry, revealing that the TC track observed in each event\ncan impact a specific region for longer and therefore result in greater induced\nanomalies.<\/jats:p>","DOI":"10.5194\/os-18-1419-2022","type":"journal-article","created":{"date-parts":[[2022,9,29]],"date-time":"2022-09-29T06:26:59Z","timestamp":1664432819000},"page":"1419-1430","source":"Crossref","is-referenced-by-count":4,"title":["Upper-ocean response to the passage of tropical cyclones  in the Azores region"],"prefix":"10.5194","volume":"18","author":[{"given":"Miguel M.","family":"Lima","sequence":"first","affiliation":[]},{"ORCID":"https:\/\/orcid.org\/0000-0002-3147-5696","authenticated-orcid":false,"given":"C\u00e9lia M.","family":"Gouveia","sequence":"additional","affiliation":[]},{"ORCID":"https:\/\/orcid.org\/0000-0002-4183-9852","authenticated-orcid":false,"given":"Ricardo M.","family":"Trigo","sequence":"additional","affiliation":[]}],"member":"3145","published-online":{"date-parts":[[2022,9,29]]},"reference":[{"key":"ref1","doi-asserted-by":"crossref","unstructured":"Amorim, P., Per\u00e1n, A. 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