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- W4313153569 abstract "Information of the characteristics of upwelling in the Indonesian sea has a very important role to estimate the potential fishing areas. The purpose of this study is to identify upwelling based on the Ekman pumping value that occurs in northeastern and southwestern Indonesia. The data used in this study are surface wind, sea surface temperature, chlorophyll-a and geostrophic current. Where the last three data are used as supporting analysis data for the calculation results of Ekman pumping. The method used in this study is to calculate Ekman pumping based on surface wind data for a period of 25 years (1995–2019). From the results, it can be seen that the Sea Surface Temperature (SST) at the time of the December January February (DJF) in the southern sea of Java is warmer than its surroundings around 30 °C, and vice versa during the June July August (JJA) about 27 °C. Chlorophyll-a (0.9 mg/m3), geostrophic currents (1.1 m/s), and Ekman pumping (4.8 × 10–5 m/s) have a fairly high intensity in the northern region of Java during DJF, while during JJA it occurs in southern Java. From the temporal analysis, it can be seen that the minimum intensity of chlorophyll a, geostrophic currents and Ekman pumping occurs during DJF and maximum occurs during JJA and vice versa for SST. This study supports previous studies, where the maximum Ekman pumping was followed by the minimum SST that occurred in both observation areas. However, chlorophyll-a and geostrophic currents in the southwest of Indonesia follow seasonal characteristics but not for the northeastern region." @default.
- W4313153569 created "2023-01-06" @default.
- W4313153569 creator A5040583250 @default.
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- W4313153569 date "2022-01-01" @default.
- W4313153569 modified "2023-09-25" @default.
- W4313153569 title "Comparative Analysis of Upwelling Characteristics in Northeast and Southwest of Indonesian Seas Area" @default.
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- W4313153569 doi "https://doi.org/10.1007/978-981-19-0308-3_47" @default.
- W4313153569 hasPublicationYear "2022" @default.
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