Mechanisms of Interannual Variability of Ocean Bottom Pressure in the Southern Indian Ocean

The study of ocean bottom pressure (OBP) helps to understand the changes in the sea level budget and ocean deep circulation. In this study, the characteristics and mechanisms of interannual OBP variability in the Southern Indian Ocean are examined using Gravity Recovery and Climate Experiment (GRACE...

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Main Authors: Yuting Niu, Xuhua Cheng, Jianhuang Qin, Niansen Ou, Chengcheng Yang, Duotian Huang
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-06-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2022.916592/full
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author Yuting Niu
Yuting Niu
Xuhua Cheng
Xuhua Cheng
Jianhuang Qin
Jianhuang Qin
Niansen Ou
Chengcheng Yang
Chengcheng Yang
Duotian Huang
Duotian Huang
author_facet Yuting Niu
Yuting Niu
Xuhua Cheng
Xuhua Cheng
Jianhuang Qin
Jianhuang Qin
Niansen Ou
Chengcheng Yang
Chengcheng Yang
Duotian Huang
Duotian Huang
author_sort Yuting Niu
collection DOAJ
description The study of ocean bottom pressure (OBP) helps to understand the changes in the sea level budget and ocean deep circulation. In this study, the characteristics and mechanisms of interannual OBP variability in the Southern Indian Ocean are examined using Gravity Recovery and Climate Experiment (GRACE) satellite data from 2003 to 2016. Results show that there are two energetic OBP centers in the Southern Indian Ocean (50°–60°S, 40°–60°E and 45°–60°S, 80°–120°E). The OBP magnitudes at two centers have strong variability on interannual time scales, and their values are larger during austral summer (NDJF) and winter (JJAS). Atmospheric forcing plays an important role in local OBP variability. The high (low) sea level pressure (SLP) over the Southern Indian Ocean benefits positive (negative) OBP anomalies via the convergence (divergence) of Ekman transport driven by local wind. Such SLP anomalies are related to the Southern Annular Mode (SAM), Southern Oscillation (SO) and Indian Ocean dipole (IOD). SAM can influence the OBP changes in both austral summer and winter, while SO and IOD have positive correlations with OBP variability during austral summer and austral winter, respectively. These results are validated by a mass-conservation ocean model, which further confirms the importance of atmospheric forcing on the interannual OBP variations.
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spelling doaj.art-b40805a206dd49afa352d0c1ac7b792c2022-12-22T00:39:54ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452022-06-01910.3389/fmars.2022.916592916592Mechanisms of Interannual Variability of Ocean Bottom Pressure in the Southern Indian OceanYuting Niu0Yuting Niu1Xuhua Cheng2Xuhua Cheng3Jianhuang Qin4Jianhuang Qin5Niansen Ou6Chengcheng Yang7Chengcheng Yang8Duotian Huang9Duotian Huang10Key Laboratory of Marine Hazards Forecasting, Ministry of Natural Resources, Hohai University, Nanjing, ChinaCollege of Oceanography, Hohai University, Nanjing, ChinaKey Laboratory of Marine Hazards Forecasting, Ministry of Natural Resources, Hohai University, Nanjing, ChinaCollege of Oceanography, Hohai University, Nanjing, ChinaKey Laboratory of Marine Hazards Forecasting, Ministry of Natural Resources, Hohai University, Nanjing, ChinaCollege of Oceanography, Hohai University, Nanjing, ChinaCollege of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang, ChinaKey Laboratory of Marine Hazards Forecasting, Ministry of Natural Resources, Hohai University, Nanjing, ChinaCollege of Oceanography, Hohai University, Nanjing, ChinaKey Laboratory of Marine Hazards Forecasting, Ministry of Natural Resources, Hohai University, Nanjing, ChinaCollege of Oceanography, Hohai University, Nanjing, ChinaThe study of ocean bottom pressure (OBP) helps to understand the changes in the sea level budget and ocean deep circulation. In this study, the characteristics and mechanisms of interannual OBP variability in the Southern Indian Ocean are examined using Gravity Recovery and Climate Experiment (GRACE) satellite data from 2003 to 2016. Results show that there are two energetic OBP centers in the Southern Indian Ocean (50°–60°S, 40°–60°E and 45°–60°S, 80°–120°E). The OBP magnitudes at two centers have strong variability on interannual time scales, and their values are larger during austral summer (NDJF) and winter (JJAS). Atmospheric forcing plays an important role in local OBP variability. The high (low) sea level pressure (SLP) over the Southern Indian Ocean benefits positive (negative) OBP anomalies via the convergence (divergence) of Ekman transport driven by local wind. Such SLP anomalies are related to the Southern Annular Mode (SAM), Southern Oscillation (SO) and Indian Ocean dipole (IOD). SAM can influence the OBP changes in both austral summer and winter, while SO and IOD have positive correlations with OBP variability during austral summer and austral winter, respectively. These results are validated by a mass-conservation ocean model, which further confirms the importance of atmospheric forcing on the interannual OBP variations.https://www.frontiersin.org/articles/10.3389/fmars.2022.916592/fullocean bottom pressureSouthern Indian Oceanwind forcingsea level pressure anomalyEkman transport
spellingShingle Yuting Niu
Yuting Niu
Xuhua Cheng
Xuhua Cheng
Jianhuang Qin
Jianhuang Qin
Niansen Ou
Chengcheng Yang
Chengcheng Yang
Duotian Huang
Duotian Huang
Mechanisms of Interannual Variability of Ocean Bottom Pressure in the Southern Indian Ocean
Frontiers in Marine Science
ocean bottom pressure
Southern Indian Ocean
wind forcing
sea level pressure anomaly
Ekman transport
title Mechanisms of Interannual Variability of Ocean Bottom Pressure in the Southern Indian Ocean
title_full Mechanisms of Interannual Variability of Ocean Bottom Pressure in the Southern Indian Ocean
title_fullStr Mechanisms of Interannual Variability of Ocean Bottom Pressure in the Southern Indian Ocean
title_full_unstemmed Mechanisms of Interannual Variability of Ocean Bottom Pressure in the Southern Indian Ocean
title_short Mechanisms of Interannual Variability of Ocean Bottom Pressure in the Southern Indian Ocean
title_sort mechanisms of interannual variability of ocean bottom pressure in the southern indian ocean
topic ocean bottom pressure
Southern Indian Ocean
wind forcing
sea level pressure anomaly
Ekman transport
url https://www.frontiersin.org/articles/10.3389/fmars.2022.916592/full
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