Identification of thermal front dynamics in the northern Malacca Strait using ROMS 3D-model

Ku Nor Afiza Asnida Ku MANSOR; Nur Hidayah ROSELI; Poh Heng KOK; Fariz Syafiq Mohamad ALI; Mohd Fadzil Mohd AKHIR

doi:10.1007/s00343-023-2263-x

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Identification of thermal front dynamics in the northern Malacca Strait using ROMS 3D-model

Physics | Updated：2024-10-15

- Identification of thermal front dynamics in the northern Malacca Strait using ROMS 3D-model
- Journal of Oceanology and Limnology Vol. 42, Issue 1, Pages: 41-57(2024)
- Affiliations：
  
  1.Institute of Oceanography and Environment, Universiti Malaysia Terengganu, Kuala Nerus 21030, Malaysia
  2.Faculty of Science and Marine Environment, Universiti Malaysia Terengganu, Kuala Nerus 21030, Malaysia
- Author bio：
  
  nurhidayahroseli@umt.edu.my
- Funds：
- DOI：10.1007/s00343-023-2263-x
  CLC：
- Received：27 June 2022，
  
  Accepted：15 October 2022，
  
  Online First：07 February 2023，
  
  Published：03 January 2024
- Accepted：
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MANSOR Ku Nor Afiza Asnida Ku,ROSELI Nur Hidayah,KOK Poh Heng,et al.Research Paper Identification of thermal front dynamics in the northern Malacca Strait using ROMS 3D-model[J].Journal of Oceanology and Limnology,2024,42(01):41-57.
DOI：

MANSOR Ku Nor Afiza Asnida Ku,ROSELI Nur Hidayah,KOK Poh Heng,et al.Research Paper Identification of thermal front dynamics in the northern Malacca Strait using ROMS 3D-model[J].Journal of Oceanology and Limnology,2024,42(01):41-57. DOI： 10.1007/s00343-023-2263-x.

摘要

Abstract

The thermal front in the oceanic system is believed to have a significant effect on biological activity. During an era of climate change

changes in heat regulation between the atmosphere and oceanic interior can alter the characteristics of this important feature. Using the simulation results of the 3D Regional Ocean Modelling System (ROMS)

we identified the location of thermal fronts and determined their dynamic variability in the area between the southern Andaman Sea and northern Malacca Strait. The Single Image Edge Detection (SIED) algorithm was used to detect the thermal front from model-derived temperature. Results show that a thermal front occurred every year from 2002 to 2012 with the temperature gradient at the location of the front was 0.3 °‍‍C/km. Compared to the years affected by El Niño and negative Indian Ocean Dipole (IOD)

the normal years (e.g.

May 2003) show the presence of the thermal front at every selected depth (10

and 75 m)

whereas El Niño and negative IOD during 2010 show the presence of the thermal front only at depth of 75 m due to greater warming

leading to the thermocline deepening and enhanced stratification. During May 2003

the thermal front was separated by cooler SST in the southern Andaman Sea and warmer SST in the northern Malacca Strait. The higher SST in the northern Malacca Strait was believed due to the besieged Malacca Strait

which trapped the heat and make it difficult to release while higher chlorophyll

in Malacca Strait is due to the freshwater conduit from nearby rivers (Klang

Langat

Perak

and Selangor). Furthermore

compared to the southern Andaman Sea

the chlorophyll

in the northern Malacca Strait is easier to reach the surface area due to the shallower thermocline

which allows nutrients in the area to reach the surface faster.

关键词

Keywords

references

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