Influence of the 2015–2016 El Niño on the record-breaking mangrove dieback along northern Australia coast

Abstract This study investigates the underlying climate processes behind the largest recorded mangrove dieback event along the Gulf of Carpentaria coast in northern Australia in late 2015. Using satellite-derived fractional canopy cover (FCC), variation of the mangrove canopies during recent decades...

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Main Authors: S. Abhik, Pandora Hope, Harry H. Hendon, Lindsay B. Hutley, Stephanie Johnson, Wasyl Drosdowsky, Josephine R. Brown, Norman C. Duke
Format: Article
Language:English
Published: Nature Portfolio 2021-10-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-021-99313-w
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author S. Abhik
Pandora Hope
Harry H. Hendon
Lindsay B. Hutley
Stephanie Johnson
Wasyl Drosdowsky
Josephine R. Brown
Norman C. Duke
author_facet S. Abhik
Pandora Hope
Harry H. Hendon
Lindsay B. Hutley
Stephanie Johnson
Wasyl Drosdowsky
Josephine R. Brown
Norman C. Duke
author_sort S. Abhik
collection DOAJ
description Abstract This study investigates the underlying climate processes behind the largest recorded mangrove dieback event along the Gulf of Carpentaria coast in northern Australia in late 2015. Using satellite-derived fractional canopy cover (FCC), variation of the mangrove canopies during recent decades are studied, including a severe dieback during 2015–2016. The relationship between mangrove FCC and climate conditions is examined with a focus on the possible role of the 2015–2016 El Niño in altering favorable conditions sustaining the mangroves. The mangrove FCC is shown to be coherent with the low-frequency component of sea level height (SLH) variation related to the El Niño Southern Oscillation (ENSO) cycle in the equatorial Pacific. The SLH drop associated with the 2015–2016 El Niño is identified to be the crucial factor leading to the dieback event. A stronger SLH drop occurred during austral autumn and winter, when the SLH anomalies were about 12% stronger than the previous very strong El Niño events. The persistent SLH drop occurred in the dry season of the year when SLH was seasonally at its lowest, so potentially exposed the mangroves to unprecedented hostile conditions. The influence of other key climate factors is also discussed, and a multiple linear regression model is developed to understand the combined role of the important climate variables on the mangrove FCC variation.
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spelling doaj.art-d21a2d04af7649a19118fdf130ea2ed02022-12-21T21:31:53ZengNature PortfolioScientific Reports2045-23222021-10-0111111210.1038/s41598-021-99313-wInfluence of the 2015–2016 El Niño on the record-breaking mangrove dieback along northern Australia coastS. Abhik0Pandora Hope1Harry H. Hendon2Lindsay B. Hutley3Stephanie Johnson4Wasyl Drosdowsky5Josephine R. Brown6Norman C. Duke7Bureau of MeteorologyBureau of MeteorologyBureau of MeteorologyResearch Institute for the Environment and Livelihoods, Charles Darwin UniversityDepartment of Ecology, Environment and Evolution, La Trobe UniversityBureau of MeteorologySchool of Geography, Earth and Atmospheric Sciences, University of MelbourneCentre for Tropical Water and Aquatic Ecosystem Research, James Cook UniversityAbstract This study investigates the underlying climate processes behind the largest recorded mangrove dieback event along the Gulf of Carpentaria coast in northern Australia in late 2015. Using satellite-derived fractional canopy cover (FCC), variation of the mangrove canopies during recent decades are studied, including a severe dieback during 2015–2016. The relationship between mangrove FCC and climate conditions is examined with a focus on the possible role of the 2015–2016 El Niño in altering favorable conditions sustaining the mangroves. The mangrove FCC is shown to be coherent with the low-frequency component of sea level height (SLH) variation related to the El Niño Southern Oscillation (ENSO) cycle in the equatorial Pacific. The SLH drop associated with the 2015–2016 El Niño is identified to be the crucial factor leading to the dieback event. A stronger SLH drop occurred during austral autumn and winter, when the SLH anomalies were about 12% stronger than the previous very strong El Niño events. The persistent SLH drop occurred in the dry season of the year when SLH was seasonally at its lowest, so potentially exposed the mangroves to unprecedented hostile conditions. The influence of other key climate factors is also discussed, and a multiple linear regression model is developed to understand the combined role of the important climate variables on the mangrove FCC variation.https://doi.org/10.1038/s41598-021-99313-w
spellingShingle S. Abhik
Pandora Hope
Harry H. Hendon
Lindsay B. Hutley
Stephanie Johnson
Wasyl Drosdowsky
Josephine R. Brown
Norman C. Duke
Influence of the 2015–2016 El Niño on the record-breaking mangrove dieback along northern Australia coast
Scientific Reports
title Influence of the 2015–2016 El Niño on the record-breaking mangrove dieback along northern Australia coast
title_full Influence of the 2015–2016 El Niño on the record-breaking mangrove dieback along northern Australia coast
title_fullStr Influence of the 2015–2016 El Niño on the record-breaking mangrove dieback along northern Australia coast
title_full_unstemmed Influence of the 2015–2016 El Niño on the record-breaking mangrove dieback along northern Australia coast
title_short Influence of the 2015–2016 El Niño on the record-breaking mangrove dieback along northern Australia coast
title_sort influence of the 2015 2016 el nino on the record breaking mangrove dieback along northern australia coast
url https://doi.org/10.1038/s41598-021-99313-w
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