Marine Heatwave Characteristics in the Makassar Strait and Its Surrounding Waters

This study aimed to investigate the characteristics of marine heatwaves (MHWs) in the Makassar Strait and adjacent waters (MSAW) using the Optimum Interpolation Sea Surface Temperature (OISSTv2) dataset from 1982 to 2021. The analysis revealed a significant positive trend in the frequency and durati...

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Main Authors: Nining Sari Ningsih, Sekar Ramdanira Gunawan, Erlin Beliyana, Ayi Tarya
Format: Article
Language:English
Published: MDPI AG 2023-07-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/15/14/2645
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author Nining Sari Ningsih
Sekar Ramdanira Gunawan
Erlin Beliyana
Ayi Tarya
author_facet Nining Sari Ningsih
Sekar Ramdanira Gunawan
Erlin Beliyana
Ayi Tarya
author_sort Nining Sari Ningsih
collection DOAJ
description This study aimed to investigate the characteristics of marine heatwaves (MHWs) in the Makassar Strait and adjacent waters (MSAW) using the Optimum Interpolation Sea Surface Temperature (OISSTv2) dataset from 1982 to 2021. The analysis revealed a significant positive trend in the frequency and duration of MHWs, while the mean and maximum intensities displayed a negative trend over the 40-year period. By examining two different phases of the Pacific Decadal Oscillation (PDO), it was observed that the cold phase (more frequent La Niña events than El Niño) had higher MHW frequency and duration, whereas the warm phase (more frequent El Niño events than La Niña) exhibited higher mean and maximum intensities. Moreover, the occurrence of high-intensity MHWs was associated with weakened winds, the decaying phase of El Niño and positive Indian Ocean Dipole (IOD), and high net surface heat flux (NSHF). An intriguing finding emerged, indicating a notable lag of 7–9 months (10 months) between El Niño (positive IOD) events and the emergence of high-intensity MHWs. This lag suggests that MHWs are more likely to manifest during the transition towards La Niña and negative IOD conditions. Additionally, the study highlighted a stronger correlation between the El Niño–Southern Oscillation and MHW intensity in the MSAW compared to the IOD. Furthermore, the different intensities of MHWs were found to be linked to NSHF, which exhibited higher values during the warm phase of the PDO compared to the cold phase.
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spelling doaj.art-ef570799629345929cf8b0583f40da632023-11-18T21:48:15ZengMDPI AGWater2073-44412023-07-011514264510.3390/w15142645Marine Heatwave Characteristics in the Makassar Strait and Its Surrounding WatersNining Sari Ningsih0Sekar Ramdanira Gunawan1Erlin Beliyana2Ayi Tarya3Research Group of Oceanography, Faculty of Earth Sciences and Technology, Bandung Institute of Technology (ITB), Bandung 40132, IndonesiaDepartment of Oceanography, Faculty of Earth Sciences and Technology, Bandung Institute of Technology (ITB), Bandung 40132, IndonesiaDoctoral Program in Earth Sciences, Faculty of Earth Sciences and Technology, Bandung Institute of Technology (ITB), Bandung 40132, IndonesiaResearch Group of Oceanography, Faculty of Earth Sciences and Technology, Bandung Institute of Technology (ITB), Bandung 40132, IndonesiaThis study aimed to investigate the characteristics of marine heatwaves (MHWs) in the Makassar Strait and adjacent waters (MSAW) using the Optimum Interpolation Sea Surface Temperature (OISSTv2) dataset from 1982 to 2021. The analysis revealed a significant positive trend in the frequency and duration of MHWs, while the mean and maximum intensities displayed a negative trend over the 40-year period. By examining two different phases of the Pacific Decadal Oscillation (PDO), it was observed that the cold phase (more frequent La Niña events than El Niño) had higher MHW frequency and duration, whereas the warm phase (more frequent El Niño events than La Niña) exhibited higher mean and maximum intensities. Moreover, the occurrence of high-intensity MHWs was associated with weakened winds, the decaying phase of El Niño and positive Indian Ocean Dipole (IOD), and high net surface heat flux (NSHF). An intriguing finding emerged, indicating a notable lag of 7–9 months (10 months) between El Niño (positive IOD) events and the emergence of high-intensity MHWs. This lag suggests that MHWs are more likely to manifest during the transition towards La Niña and negative IOD conditions. Additionally, the study highlighted a stronger correlation between the El Niño–Southern Oscillation and MHW intensity in the MSAW compared to the IOD. Furthermore, the different intensities of MHWs were found to be linked to NSHF, which exhibited higher values during the warm phase of the PDO compared to the cold phase.https://www.mdpi.com/2073-4441/15/14/2645marine heatwavesMakassar Straitsea surface temperaturePDOIODENSO
spellingShingle Nining Sari Ningsih
Sekar Ramdanira Gunawan
Erlin Beliyana
Ayi Tarya
Marine Heatwave Characteristics in the Makassar Strait and Its Surrounding Waters
Water
marine heatwaves
Makassar Strait
sea surface temperature
PDO
IOD
ENSO
title Marine Heatwave Characteristics in the Makassar Strait and Its Surrounding Waters
title_full Marine Heatwave Characteristics in the Makassar Strait and Its Surrounding Waters
title_fullStr Marine Heatwave Characteristics in the Makassar Strait and Its Surrounding Waters
title_full_unstemmed Marine Heatwave Characteristics in the Makassar Strait and Its Surrounding Waters
title_short Marine Heatwave Characteristics in the Makassar Strait and Its Surrounding Waters
title_sort marine heatwave characteristics in the makassar strait and its surrounding waters
topic marine heatwaves
Makassar Strait
sea surface temperature
PDO
IOD
ENSO
url https://www.mdpi.com/2073-4441/15/14/2645
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AT erlinbeliyana marineheatwavecharacteristicsinthemakassarstraitanditssurroundingwaters
AT ayitarya marineheatwavecharacteristicsinthemakassarstraitanditssurroundingwaters