IDENTIFICATION OF EXTREME SEA LEVELS AND CONCURRENT MARINE HEATWAVES-EXTREME SEA LEVELS IN SETIO WATERS 1993-2022

The continuously increasing global warming triggers an increase in sea surface temperatures. The rise in sea surface temperatures affects various parameters, particularly sea levels. When extreme sea level (ESLs) events coincide with MHWs events, a phenomenon known as CHESLs (Concurrent Marine He...

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Main Author: Claudia Boedihardjo, Denise
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/82399
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:82399
spelling id-itb.:823992024-07-08T10:40:10ZIDENTIFICATION OF EXTREME SEA LEVELS AND CONCURRENT MARINE HEATWAVES-EXTREME SEA LEVELS IN SETIO WATERS 1993-2022 Claudia Boedihardjo, Denise Indonesia Final Project Extreme Sea Levels (ESLs), Concurrent Marine Heatwaves-Extreme Sea Levels (CHESLs), SETIO waters, monsoon, ENSO, IOD, statistics INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/82399 The continuously increasing global warming triggers an increase in sea surface temperatures. The rise in sea surface temperatures affects various parameters, particularly sea levels. When extreme sea level (ESLs) events coincide with MHWs events, a phenomenon known as CHESLs (Concurrent Marine Heatwaves-Extreme Sea Levels/CHESLs) emerges with greater impact. This study aims to identify ESLs and CHESLs events in the Southeastern Tropical Indian Ocean (SETIO), which includes the waters off the western coast of Sumatra, southern Java, and Nusa Tenggara, over the period of 1993–2022 (30 years). The research focuses on four station locations: Padang (location A), Cilacap (location B), Prigi (location C), and Benoa (location D). The primary data used are sea level anomaly (SLA) and sea surface temperature anomaly (SSTA) obtained from satellite altimetry. The analysis method employed is statistical. The analysis results indicate a positive linear trend of SLA and SSTA with varying values at each location. Over the 30 years, 22 ESL events and 4 CHESL events were identified in Padang, 16 ESL events and 4 CHESL events in Cilacap, 18 ESL events and 4 CHESL events in Prigi, and 23 ESL events and 4 CHESL events in Benoa. ESLs predominantly occur when the Australian monsoon is active during the DJF period (45%), the La Niña phase (76%), and N-IOD (40%). CHESLs predominantly occur when the Indian monsoon is active during the MAM period (53%), the La Niña phase (76%), and N-IOD (82%). The influence of N-IOD is more dominant at the Padang station. Conversely, the influence of La Niña is more dominant at the Cilacap, Prigi, and Benoa stations. ESLs events are more frequently found in onshore areas, while CHESLs are more frequently found in offshore areas. The total frequency of ESLs and CHESLs events has increased by 66.7% over the last decade. text
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description The continuously increasing global warming triggers an increase in sea surface temperatures. The rise in sea surface temperatures affects various parameters, particularly sea levels. When extreme sea level (ESLs) events coincide with MHWs events, a phenomenon known as CHESLs (Concurrent Marine Heatwaves-Extreme Sea Levels/CHESLs) emerges with greater impact. This study aims to identify ESLs and CHESLs events in the Southeastern Tropical Indian Ocean (SETIO), which includes the waters off the western coast of Sumatra, southern Java, and Nusa Tenggara, over the period of 1993–2022 (30 years). The research focuses on four station locations: Padang (location A), Cilacap (location B), Prigi (location C), and Benoa (location D). The primary data used are sea level anomaly (SLA) and sea surface temperature anomaly (SSTA) obtained from satellite altimetry. The analysis method employed is statistical. The analysis results indicate a positive linear trend of SLA and SSTA with varying values at each location. Over the 30 years, 22 ESL events and 4 CHESL events were identified in Padang, 16 ESL events and 4 CHESL events in Cilacap, 18 ESL events and 4 CHESL events in Prigi, and 23 ESL events and 4 CHESL events in Benoa. ESLs predominantly occur when the Australian monsoon is active during the DJF period (45%), the La Niña phase (76%), and N-IOD (40%). CHESLs predominantly occur when the Indian monsoon is active during the MAM period (53%), the La Niña phase (76%), and N-IOD (82%). The influence of N-IOD is more dominant at the Padang station. Conversely, the influence of La Niña is more dominant at the Cilacap, Prigi, and Benoa stations. ESLs events are more frequently found in onshore areas, while CHESLs are more frequently found in offshore areas. The total frequency of ESLs and CHESLs events has increased by 66.7% over the last decade.
format Final Project
author Claudia Boedihardjo, Denise
spellingShingle Claudia Boedihardjo, Denise
IDENTIFICATION OF EXTREME SEA LEVELS AND CONCURRENT MARINE HEATWAVES-EXTREME SEA LEVELS IN SETIO WATERS 1993-2022
author_facet Claudia Boedihardjo, Denise
author_sort Claudia Boedihardjo, Denise
title IDENTIFICATION OF EXTREME SEA LEVELS AND CONCURRENT MARINE HEATWAVES-EXTREME SEA LEVELS IN SETIO WATERS 1993-2022
title_short IDENTIFICATION OF EXTREME SEA LEVELS AND CONCURRENT MARINE HEATWAVES-EXTREME SEA LEVELS IN SETIO WATERS 1993-2022
title_full IDENTIFICATION OF EXTREME SEA LEVELS AND CONCURRENT MARINE HEATWAVES-EXTREME SEA LEVELS IN SETIO WATERS 1993-2022
title_fullStr IDENTIFICATION OF EXTREME SEA LEVELS AND CONCURRENT MARINE HEATWAVES-EXTREME SEA LEVELS IN SETIO WATERS 1993-2022
title_full_unstemmed IDENTIFICATION OF EXTREME SEA LEVELS AND CONCURRENT MARINE HEATWAVES-EXTREME SEA LEVELS IN SETIO WATERS 1993-2022
title_sort identification of extreme sea levels and concurrent marine heatwaves-extreme sea levels in setio waters 1993-2022
url https://digilib.itb.ac.id/gdl/view/82399
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