{"title":"评估气候变化对阿曼湾溶解氧的影响","authors":"Shirin Farkhani, Nasser Hadjizadeh Zaker","doi":"10.1016/j.dsr.2025.104487","DOIUrl":null,"url":null,"abstract":"<div><div>In this paper, we investigated the impacts of climate change on dissolved oxygen (DO) concentration in the Gulf of Oman using numerical modeling. We simulated and compared the DO concentration of the Gulf of Oman through the historical (1980–2000) and future (2080–2100) periods. Results demonstrated that in the future climate, the DO concentration levels in the upper 400 m of the Gulf of Oman will decrease. In the surface mixed layer, the mean DO concentration will decrease by 0.4, 0.5, and 0.7 mg/l in summer, and by 0.2, 0.3, and 0.4 mg/l in winter. Below the surface mixed layer, the mean DO concentration will decrease by 0.5, 0.6, and 0.8 mg/l in summer, and by 0.6, 0.7, and 1 mg/l in winter. The ventilation effect of the Persian Gulf outflow on the Gulf of Oman's water will also decrease in the future. The future climate deoxygenation will expand hypoxic waters upward. In summer, the mean thickness of the surface layer with DO > 2 mg/l will decrease from 40 m in the historical period to approximately 32, 26, and 23 m in the RCP 2.6, RCP 4.5, and RCP 8.5 scenarios, respectively. In winter, the hypoxic boundary will shift from 100 m depth in the historical period to about 91, 84, and 80 m in RCP 2.6, RCP 4.5, and RCP 8.5 scenarios, respectively.</div></div>","PeriodicalId":51009,"journal":{"name":"Deep-Sea Research Part I-Oceanographic Research Papers","volume":"219 ","pages":"Article 104487"},"PeriodicalIF":2.3000,"publicationDate":"2025-03-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Assessment of the effects of climate change on dissolved oxygen in the Gulf of Oman\",\"authors\":\"Shirin Farkhani, Nasser Hadjizadeh Zaker\",\"doi\":\"10.1016/j.dsr.2025.104487\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>In this paper, we investigated the impacts of climate change on dissolved oxygen (DO) concentration in the Gulf of Oman using numerical modeling. We simulated and compared the DO concentration of the Gulf of Oman through the historical (1980–2000) and future (2080–2100) periods. Results demonstrated that in the future climate, the DO concentration levels in the upper 400 m of the Gulf of Oman will decrease. In the surface mixed layer, the mean DO concentration will decrease by 0.4, 0.5, and 0.7 mg/l in summer, and by 0.2, 0.3, and 0.4 mg/l in winter. Below the surface mixed layer, the mean DO concentration will decrease by 0.5, 0.6, and 0.8 mg/l in summer, and by 0.6, 0.7, and 1 mg/l in winter. The ventilation effect of the Persian Gulf outflow on the Gulf of Oman's water will also decrease in the future. The future climate deoxygenation will expand hypoxic waters upward. In summer, the mean thickness of the surface layer with DO > 2 mg/l will decrease from 40 m in the historical period to approximately 32, 26, and 23 m in the RCP 2.6, RCP 4.5, and RCP 8.5 scenarios, respectively. In winter, the hypoxic boundary will shift from 100 m depth in the historical period to about 91, 84, and 80 m in RCP 2.6, RCP 4.5, and RCP 8.5 scenarios, respectively.</div></div>\",\"PeriodicalId\":51009,\"journal\":{\"name\":\"Deep-Sea Research Part I-Oceanographic Research Papers\",\"volume\":\"219 \",\"pages\":\"Article 104487\"},\"PeriodicalIF\":2.3000,\"publicationDate\":\"2025-03-14\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Deep-Sea Research Part I-Oceanographic Research Papers\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0967063725000469\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"OCEANOGRAPHY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Deep-Sea Research Part I-Oceanographic Research Papers","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0967063725000469","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"OCEANOGRAPHY","Score":null,"Total":0}
Assessment of the effects of climate change on dissolved oxygen in the Gulf of Oman
In this paper, we investigated the impacts of climate change on dissolved oxygen (DO) concentration in the Gulf of Oman using numerical modeling. We simulated and compared the DO concentration of the Gulf of Oman through the historical (1980–2000) and future (2080–2100) periods. Results demonstrated that in the future climate, the DO concentration levels in the upper 400 m of the Gulf of Oman will decrease. In the surface mixed layer, the mean DO concentration will decrease by 0.4, 0.5, and 0.7 mg/l in summer, and by 0.2, 0.3, and 0.4 mg/l in winter. Below the surface mixed layer, the mean DO concentration will decrease by 0.5, 0.6, and 0.8 mg/l in summer, and by 0.6, 0.7, and 1 mg/l in winter. The ventilation effect of the Persian Gulf outflow on the Gulf of Oman's water will also decrease in the future. The future climate deoxygenation will expand hypoxic waters upward. In summer, the mean thickness of the surface layer with DO > 2 mg/l will decrease from 40 m in the historical period to approximately 32, 26, and 23 m in the RCP 2.6, RCP 4.5, and RCP 8.5 scenarios, respectively. In winter, the hypoxic boundary will shift from 100 m depth in the historical period to about 91, 84, and 80 m in RCP 2.6, RCP 4.5, and RCP 8.5 scenarios, respectively.
期刊介绍:
Deep-Sea Research Part I: Oceanographic Research Papers is devoted to the publication of the results of original scientific research, including theoretical work of evident oceanographic applicability; and the solution of instrumental or methodological problems with evidence of successful use. The journal is distinguished by its interdisciplinary nature and its breadth, covering the geological, physical, chemical and biological aspects of the ocean and its boundaries with the sea floor and the atmosphere. In addition to regular "Research Papers" and "Instruments and Methods" papers, briefer communications may be published as "Notes". Supplemental matter, such as extensive data tables or graphs and multimedia content, may be published as electronic appendices.