Meridional Oceanic Heat Transport Influences Marine Heatwaves in the Tasman Sea on Interannual to Decadal Timescales

Marine heatwaves (MHWs) pose an increasing threat to the ocean’s wellbeing as global warming progresses. Forecasting MHWs is challenging due to the various factors that affect their occurrence, including large variability in the atmospheric state. In this study we demonstrate a causal link between o...

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Main Authors: Erik Behrens, Denise Fernandez, Phil Sutton
Format: Article
Language:English
Published: Frontiers Media S.A. 2019-05-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/article/10.3389/fmars.2019.00228/full
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spelling doaj-9f803fdca33846b194daad0fd029cbd22020-11-24T22:20:51ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452019-05-01610.3389/fmars.2019.00228436714Meridional Oceanic Heat Transport Influences Marine Heatwaves in the Tasman Sea on Interannual to Decadal TimescalesErik Behrens0Denise Fernandez1Phil Sutton2Phil Sutton3National Institute of Water and Atmospheric Research, Auckland, New ZealandNational Institute of Water and Atmospheric Research, Auckland, New ZealandNational Institute of Water and Atmospheric Research, Auckland, New ZealandSchool of Environment, The University of Auckland, Auckland, New ZealandMarine heatwaves (MHWs) pose an increasing threat to the ocean’s wellbeing as global warming progresses. Forecasting MHWs is challenging due to the various factors that affect their occurrence, including large variability in the atmospheric state. In this study we demonstrate a causal link between ocean heat content and the area and intensity of MHWs in the Tasman Sea on interannual to decadal time scales. Ocean heat content variations are more persistent than ‘weather-related’ atmospheric drivers (e.g., blocking high pressure systems) for MHWs and thus provide better predictive skill on timescales longer than weeks. Using data from a forced global ocean sea-ice model, we show that ocean heat content fluctuations in the Tasman Sea are predominantly controlled by oceanic meridional heat transport from the subtropics, which in turn is mainly characterized by the interplay of the East Australian Current and the Tasman Front. Variability in these currents is impacted by wind stress curl anomalies north of this region, following Sverdrup’s and Godfrey’s ‘Island Rule’ theories. Data from models and observations show that periods with positive upper (2000 m) ocean heat content anomalies or rapid increases in ocean heat content are characterized by more frequent, larger, longer and more intense MHWs on interannual to decadal timescales. Thus, the oceanic heat content in the Tasman Sea acts as a preconditioner and has a prolonged predictive skill compared to the atmospheric state (e.g., surface heat fluxes), making ocean heat content a useful indicator and measure of the likelihood of MHWs.https://www.frontiersin.org/article/10.3389/fmars.2019.00228/fullTasman Seamarine heatwavesclimate variabilityEast Australian CurrentTasman Frontclimate extremes
collection DOAJ
language English
format Article
sources DOAJ
author Erik Behrens
Denise Fernandez
Phil Sutton
Phil Sutton
spellingShingle Erik Behrens
Denise Fernandez
Phil Sutton
Phil Sutton
Meridional Oceanic Heat Transport Influences Marine Heatwaves in the Tasman Sea on Interannual to Decadal Timescales
Frontiers in Marine Science
Tasman Sea
marine heatwaves
climate variability
East Australian Current
Tasman Front
climate extremes
author_facet Erik Behrens
Denise Fernandez
Phil Sutton
Phil Sutton
author_sort Erik Behrens
title Meridional Oceanic Heat Transport Influences Marine Heatwaves in the Tasman Sea on Interannual to Decadal Timescales
title_short Meridional Oceanic Heat Transport Influences Marine Heatwaves in the Tasman Sea on Interannual to Decadal Timescales
title_full Meridional Oceanic Heat Transport Influences Marine Heatwaves in the Tasman Sea on Interannual to Decadal Timescales
title_fullStr Meridional Oceanic Heat Transport Influences Marine Heatwaves in the Tasman Sea on Interannual to Decadal Timescales
title_full_unstemmed Meridional Oceanic Heat Transport Influences Marine Heatwaves in the Tasman Sea on Interannual to Decadal Timescales
title_sort meridional oceanic heat transport influences marine heatwaves in the tasman sea on interannual to decadal timescales
publisher Frontiers Media S.A.
series Frontiers in Marine Science
issn 2296-7745
publishDate 2019-05-01
description Marine heatwaves (MHWs) pose an increasing threat to the ocean’s wellbeing as global warming progresses. Forecasting MHWs is challenging due to the various factors that affect their occurrence, including large variability in the atmospheric state. In this study we demonstrate a causal link between ocean heat content and the area and intensity of MHWs in the Tasman Sea on interannual to decadal time scales. Ocean heat content variations are more persistent than ‘weather-related’ atmospheric drivers (e.g., blocking high pressure systems) for MHWs and thus provide better predictive skill on timescales longer than weeks. Using data from a forced global ocean sea-ice model, we show that ocean heat content fluctuations in the Tasman Sea are predominantly controlled by oceanic meridional heat transport from the subtropics, which in turn is mainly characterized by the interplay of the East Australian Current and the Tasman Front. Variability in these currents is impacted by wind stress curl anomalies north of this region, following Sverdrup’s and Godfrey’s ‘Island Rule’ theories. Data from models and observations show that periods with positive upper (2000 m) ocean heat content anomalies or rapid increases in ocean heat content are characterized by more frequent, larger, longer and more intense MHWs on interannual to decadal timescales. Thus, the oceanic heat content in the Tasman Sea acts as a preconditioner and has a prolonged predictive skill compared to the atmospheric state (e.g., surface heat fluxes), making ocean heat content a useful indicator and measure of the likelihood of MHWs.
topic Tasman Sea
marine heatwaves
climate variability
East Australian Current
Tasman Front
climate extremes
url https://www.frontiersin.org/article/10.3389/fmars.2019.00228/full
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