Oceanic response to the consecutive Hurricanes Dorian and Humberto (2019) in the Sargasso Sea

• Published in: Natural Hazards and Earth System Sciences
• Main Authors: Avila Alonso, Dailé, Baetens, Jan, Cardenas, Rolando, De Baets, Bernard
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2021
• Subjects: Earth and Environmental Sciences; DEEP CHLOROPHYLL MAXIMUM; EEL ANGUILLA-ANGUILLA; TROPICAL CYCLONES; SURFACE TEMPERATURE; HEAT-CONTENT; PHYTOPLANKTON BIOMASS; CLIMATE-CHANGE; TIME-SERIES; GULF-STREAM; IMPACT; Dorian; Anguilla anguilla
• Online Access: https://biblio.ugent.be/publication/8697336; http://hdl.handle.net/1854/LU-8697336; https://doi.org/10.5194/nhess-21-837-2021; https://biblio.ugent.be/publication/8697336/file/8697337

Understanding the oceanic response to tropical cyclones (TCs) is of importance for studies on climate change. Although the oceanic effects induced by individual TCs have been extensively investigated, studies on the oceanic response to the passage of consecutive TCs are rare. In this work, we assess the upper-oceanic response to the passage of Hurricanes Dorian and Humberto over the western Sargasso Sea in 2019 using satellite remote sensing and modelled data. We found that the combined effects of these slow-moving TCs led to an increased oceanic response during the third and fourth post-storm weeks of Dorian (accounting for both Dorian and Humberto effects) because of the induced mixing and upwelling at this time. Overall, anomalies of sea surface temperature, ocean heat content, and mean temperature from the sea surface to a depth of 100 m were 50 %, 63 %, and 57 % smaller (more negative) in the third-fourth post-storm weeks than in the first-second post-storm weeks of Dorian (accounting only for Dorian effects), respectively. For the biological response, we found that surface chlorophyll a (chl a) concentration anomalies, the mean chl a concentration in the euphotic zone, and the chl a concentration in the deep chlorophyll maximum were 16 %, 4 %, and 16 % higher in the third-fourth post-storm weeks than in the first-second post-storm weeks, respectively. The sea surface cooling and increased biological response induced by these TCs were significantly higher (Mann-Whitney test, p < 0.05) compared to climatological records. Our climatological analysis reveals that the strongest TC-induced oceanographic variability in the western Sargasso Sea can be associated with the occurrence of consecutive TCs and long-lasting TC forcing.