{"title":"Volume Budget of Antarctic Intermediate Water in the Southern Ocean from an Eddy-Resolving Ocean Simulation","authors":"Jinjuan Zhang, Yiyong Luo, Wang Jing, Dexing Wu","doi":"10.1080/07055900.2022.2118568","DOIUrl":null,"url":null,"abstract":"ABSTRACT The volume budget of Antarctic Intermediate Water (AAIW) in the Southern Ocean was examined using a 0.1° ocean model output, from 1955 to 2017. Results show that AAIW volume has significant seasonal variation, with the maximum volume occurring in September and the minimum volume occurring in March, as a result of air-sea buoyancy fluxes. Comparing the AAIW on an interannual time scale, the volume appears to be driven by interior diapycnal mixing and air-sea buoyancy fluxes. While the diapycnal mixing dominates the interannual variation of AAIW in the Indian Ocean, the air-sea formation dominates the interannual variation of AAIW in the Pacific Ocean. The AAIW volume in the Southern Ocean decreased by from 1955 to 2017, due to a consistent increase of oceanic buoyancy gain over the outcropping area around 27.1 and, thus, more AAIW being transformed into lighter water.","PeriodicalId":55434,"journal":{"name":"Atmosphere-Ocean","volume":"61 1","pages":"94 - 104"},"PeriodicalIF":1.6000,"publicationDate":"2022-09-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Atmosphere-Ocean","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1080/07055900.2022.2118568","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"METEOROLOGY & ATMOSPHERIC SCIENCES","Score":null,"Total":0}
引用次数: 0
Abstract
ABSTRACT The volume budget of Antarctic Intermediate Water (AAIW) in the Southern Ocean was examined using a 0.1° ocean model output, from 1955 to 2017. Results show that AAIW volume has significant seasonal variation, with the maximum volume occurring in September and the minimum volume occurring in March, as a result of air-sea buoyancy fluxes. Comparing the AAIW on an interannual time scale, the volume appears to be driven by interior diapycnal mixing and air-sea buoyancy fluxes. While the diapycnal mixing dominates the interannual variation of AAIW in the Indian Ocean, the air-sea formation dominates the interannual variation of AAIW in the Pacific Ocean. The AAIW volume in the Southern Ocean decreased by from 1955 to 2017, due to a consistent increase of oceanic buoyancy gain over the outcropping area around 27.1 and, thus, more AAIW being transformed into lighter water.
期刊介绍:
Atmosphere-Ocean is the principal scientific journal of the Canadian Meteorological and Oceanographic Society (CMOS). It contains results of original research, survey articles, notes and comments on published papers in all fields of the atmospheric, oceanographic and hydrological sciences. Arctic, coastal and mid- to high-latitude regions are areas of particular interest. Applied or fundamental research contributions in English or French on the following topics are welcomed:
climate and climatology;
observation technology, remote sensing;
forecasting, modelling, numerical methods;
physics, dynamics, chemistry, biogeochemistry;
boundary layers, pollution, aerosols;
circulation, cloud physics, hydrology, air-sea interactions;
waves, ice, energy exchange and related environmental topics.