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Water Mass Characteristic in the Eastern Inflow Region of the Indonesian Throughflow during Leg-3 of Nusa Manggala Expedition (December 2018)
Putri M.R.a, Anwar I.P.a, Avrionestib, Surinati D.c
a Research Group of Oceanography, Faculty of Earth Sciences and Technology, Institut Teknologi Bandung, Indonesia
b Marine Technology Cooperation Research Center (MTCRC), Indonesia
c Research Center for Oceanography, Indonesian Institutes of Sciences (LIPI), 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]© Published under licence by IOP Publishing Ltd.The Nusa Manggala (ENM) leg-3 expedition in 2018 was held on December 6-16 2018. The survey achieved eighteen Conductivity Temperature Depth measurement points and centered at North of West Papua and Halmahera Sea as the inflow area of eastern part of Indonesian Throughflow (ITF). The results of this study prove that Pacific Surface Water is present on the surface up to 70 m with a temperature of 26 °C – 30°C and salinity of 24 psu – 24.5 psu. Then, South Pacific Subtropical Water and South Pacific Intermediate Water are simultaneously 70 m – 250 m and 250 m – 1000 m at the northern of Halmahera Sea. They not exceed till the southern part of Halmahera Sea.[/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]Conductivity temperature depths,Indonesian throughflow,Measurement points,Pacific intermediate water,Subtropical water,Water mass[/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]eastern part of ITF,Nusa Manggala Expedition 2018,Water mass[/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][/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/10.1088/1755-1315/618/1/012013[/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]