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Temporal and spatial variation of surface heat flux in Makassar Strait
Radjawane I.M.a, Hatmaja R.B.a, Manullang J.F.a, Trilaksono N.J.a
a Oceanography Department, Faculty of Earth Sciences and Technology, Bandung Institute of Technology, Bandung – West Java, 40132, Indonesia
[vc_row][vc_column][vc_row_inner][vc_column_inner][vc_separator css=”.vc_custom_1624529070653{padding-top: 30px !important;padding-bottom: 30px !important;}”][/vc_column_inner][/vc_row_inner][vc_row_inner layout=”boxed”][vc_column_inner width=”3/4″ css=”.vc_custom_1624695412187{border-right-width: 1px !important;border-right-color: #dddddd !important;border-right-style: solid !important;border-radius: 1px !important;}”][vc_empty_space][megatron_heading title=”Abstract” size=”size-sm” text_align=”text-left”][vc_column_text]© 2019 IOP Publishing Ltd. All rights reserved.Indonesian Seas have an important role on the sea-air interaction in Indo-Pacific region. Makassar Strait is located in the center of Indonesian Seas and part of Indonesian Throughflow (ITF), which has been influenced due to the coupled ocean-atmosphere phenomenon in Pacific and Indian Oceans, such as monsoon, El-Ni?o Southern Oscillation (ENSO), and Indian Ocean Dipole (IOD). The temporal and spatial variation of surface heat flux in Makassar Strait has been evaluated using the multi satellite dataset from 1984-2009. The remote sensing data with resolution of 1° × 1° obtained from Objectively Analyzed air-sea Fluxes (OAFlux) produced by Woods Hole Oceanographic Institution (WHOI). The results show that there is a seasonal fluctuation of surface heat flux related to the wind monsoon. The variation of the shortwave radiation and latent heat flux give a large contribution to the net surface heat flux that associated with ENSO and IOD events. In Makassar Strait, the variation of shortwave radiation and sea surface temperature (SST) is in a good agreement with the El-Ni?o/La-Ni?a events. There is a time lag between surface heat fluxes with the ENSO events.[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Author keywords” size=”size-sm” text_align=”text-left”][vc_column_text]Indonesian throughflow,Interannual variability,Makassar Strait,monsoon,Sea surface temperature (SST),Surface heat fluxes,Temporal and spatial variation,Woods hole oceanographic institutions[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Indexed keywords” size=”size-sm” text_align=”text-left”][vc_column_text]Interannual variability,Makassar Strait,monsoon,surface heat flux.[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Funding details” size=”size-sm” text_align=”text-left”][vc_column_text][{‘$’: ‘This research was supported by the ITB Research Grant. The ocean heat flux products were provided by the WHOI OAFlux Project funded by the NOAA Climate Observations and Monitoring (COM) Program http://oaflux.whoi.edu/. The shortwave and longwave radiation (ISCCP-FD) data were obtained from the International Satellite Cloud Climatology Project (ISCCP) data archives at http://oaflux.whoi.edu/heatflux.html. Advances in understanding the radiative flux from ISCCP J. Geophys. Res., 109, (27pp). We would like to thank to Mr. Giovanni Gunawan who helps editing the figures.’}, {‘$’: ‘This research was supported by the ITB Research Grant. The ocean heat flux products were provided by the WHOI OAFlux Project funded by the NOAA Climate Observations and Monitoring (COM) Program http://oaflux.whoi.edu/. The shortwave and longwave radiation (ISCCP-FD) data were obtained from the International Satellite Cloud Climatology Project (ISCCP) data archives at http://oaflux.whoi.edu/heatflux.html. Advances in understanding the radiative flux from ISCCP J.’}][/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”DOI” size=”size-sm” text_align=”text-left”][vc_column_text]https://doi.org/10.1088/1755-1315/303/1/012028[/vc_column_text][/vc_column_inner][vc_column_inner width=”1/4″][vc_column_text]Widget Plumx[/vc_column_text][/vc_column_inner][/vc_row_inner][/vc_column][/vc_row][vc_row][vc_column][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][/vc_column][/vc_row]