{"title":"SEA SURFACE TEMPERATURE ANOMALIES FORMATION IN THE GULF OF MEXICO UNDER THE INFLUENCE OF HURRICANE SULLY ON SEPTEMBER11–17, 2020","authors":"Y. El Hadri, N. Berlinsky, M. Slizhe, O. V. Deryk","doi":"10.18524/2303-9914.2023.1(42).282234","DOIUrl":null,"url":null,"abstract":"Problem Statement and Purpose. Tropical cyclones are one of the most destructive natural phenomena on Earth, causing great social and economic losses. Given the destructive impact of tropical cyclones, the question of their study and the impact of climate change on their behavior is considerable scientific interest. Tropical cyclones \"draw\" energy from the surface of the ocean. Tropical cyclones arise and develop over the water surface, the temperature of which is not lower than 26 °C. In the case when a well-developed tropical cyclone hits the colder surface of the ocean, it begins to fill up quickly. Thus, a change in the SST on the path of the tropical cyclone may affect the further development and intensity of the storm, and as a result, its destructive power. The purpose of the work is to determine the deviations of the ocean surface temperature in the Gulf of Mexico under the influence of the passage of Hurricane Sally on September 11–17, 2020.\nData & Methods. The analysis of sea surface temperature anomalies was performed on the basis of data from the NOAA OI SST V2 High Resolution Dataset Optimum Daily Interpolation of Sea Surface Temperature product, which is long-term climate data (period 1971–2000) and allows determination of daily of sea surface temperature anomalies with a step of 1/4°.\nResults. Against the background of positive Sea Surface Temperature anomalies associated with the tendency to increase Sea Surface Temperature in the Gulf of Mexico, which has been observed in recent decades, in the places where the trajectory of Hurricane Sally passed during the next day, the appearance of negative Sea Surface Temperature anomalies was noted, which had a focal character and were comparable in area to horizontal dimensions of the hurricane. Over time, cells of negative Sea Surface Temperature anomalies increased in area and temperature deviation. The highest Sea Surface Temperature anomalies values were observed on September 15–16, 2020 and were –1 °C. Negative anomalies persisted after the passage of Sally for a month, after which a positive Sea Surface Temperature anomalies formed on the surface of the Gulf of Mexico, occupying the entire water area of the Gulf. This duration of preservation of anomalies may be related to the circulation of the waters.","PeriodicalId":398162,"journal":{"name":"Odesa National University Herald. Geography and Geology","volume":"27 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2023-08-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Odesa National University Herald. Geography and Geology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.18524/2303-9914.2023.1(42).282234","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Problem Statement and Purpose. Tropical cyclones are one of the most destructive natural phenomena on Earth, causing great social and economic losses. Given the destructive impact of tropical cyclones, the question of their study and the impact of climate change on their behavior is considerable scientific interest. Tropical cyclones "draw" energy from the surface of the ocean. Tropical cyclones arise and develop over the water surface, the temperature of which is not lower than 26 °C. In the case when a well-developed tropical cyclone hits the colder surface of the ocean, it begins to fill up quickly. Thus, a change in the SST on the path of the tropical cyclone may affect the further development and intensity of the storm, and as a result, its destructive power. The purpose of the work is to determine the deviations of the ocean surface temperature in the Gulf of Mexico under the influence of the passage of Hurricane Sally on September 11–17, 2020.
Data & Methods. The analysis of sea surface temperature anomalies was performed on the basis of data from the NOAA OI SST V2 High Resolution Dataset Optimum Daily Interpolation of Sea Surface Temperature product, which is long-term climate data (period 1971–2000) and allows determination of daily of sea surface temperature anomalies with a step of 1/4°.
Results. Against the background of positive Sea Surface Temperature anomalies associated with the tendency to increase Sea Surface Temperature in the Gulf of Mexico, which has been observed in recent decades, in the places where the trajectory of Hurricane Sally passed during the next day, the appearance of negative Sea Surface Temperature anomalies was noted, which had a focal character and were comparable in area to horizontal dimensions of the hurricane. Over time, cells of negative Sea Surface Temperature anomalies increased in area and temperature deviation. The highest Sea Surface Temperature anomalies values were observed on September 15–16, 2020 and were –1 °C. Negative anomalies persisted after the passage of Sally for a month, after which a positive Sea Surface Temperature anomalies formed on the surface of the Gulf of Mexico, occupying the entire water area of the Gulf. This duration of preservation of anomalies may be related to the circulation of the waters.
问题陈述和目的。热带气旋是地球上最具破坏性的自然现象之一,造成巨大的社会和经济损失。考虑到热带气旋的破坏性影响,对它们的研究以及气候变化对它们行为的影响的问题引起了相当大的科学兴趣。热带气旋从海洋表面“汲取”能量。热带气旋在水面上产生和发展,其温度不低于26℃。在这种情况下,当一个发展良好的热带气旋袭击较冷的海洋表面时,它开始迅速填满。因此,热带气旋路径上的海温变化可能会影响风暴的进一步发展和强度,从而影响其破坏力。本次工作的目的是确定2020年9月11日至17日飓风萨利通过墨西哥湾影响下的海洋表面温度偏差。数据与方法。海温异常分析是基于NOAA OI SST V2高分辨率数据集的数据进行的,该数据集是长期气候数据(1971-2000年),可以确定海温异常的日变化,步长为1/4°。在近几十年来观测到的墨西哥湾海温正异常与海温升高趋势相关的背景下,在第二天飓风萨莉轨迹经过的地方,注意到海温负异常的出现,这具有焦点特征,并且在面积上与飓风的水平尺度相当。随着时间的推移,海温负距平单元的面积和温度偏差均有所增加。2020年9月15-16日海面温度异常值最高,为-1°C。Sally通过后,负异常持续了一个月,此后墨西哥湾表面形成了正海温异常,占据了整个墨西哥湾水域。这种异常的保存时间可能与水的循环有关。