PRIMARY PRODUCTIVITY DISTRIBUTION IN BALI STRAIT
Waters fertility level can be determined from primary productivity which can be used to determine the potential area of fishing ground. In this Final Project, primary productivity in Bali Strait has been calculated by using Marra Algorithm and Gauss Model where its five paramater coefficients are ca...
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id-itb.:703612023-01-09T10:26:08ZPRIMARY PRODUCTIVITY DISTRIBUTION IN BALI STRAIT Lany Putri Yuliananingrum, Trie Indonesia Final Project Marra Algorithm, vertical Chlorophyll-a, primary productivity, Bali Strait, upwelling INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/70361 Waters fertility level can be determined from primary productivity which can be used to determine the potential area of fishing ground. In this Final Project, primary productivity in Bali Strait has been calculated by using Marra Algorithm and Gauss Model where its five paramater coefficients are calculated from observation data in June and September 2012. The sea surface temperature data and both surface chlorophyll and surface Photosynthetically Active Radiation data are taken from HAMburg Shelf Ocean Model (HAMSOM) simulation result and Moderate Resolution Imaging Spectroradiometer (MODIS) satelitte respectively for East Season and Second Transition Season. The result shows that the highest surface primary productivity is occured in August at the southwest area with value around 0,35gC/m²/day which is related to upwelling phenomenone. Primary productivity vertically also varies with the season where the depth of maximum primary productivity in East Season (0-10 meter) is shallower than in Second Transition Season (0-20 meter). text |
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Waters fertility level can be determined from primary productivity which can be used to determine the potential area of fishing ground. In this Final Project, primary productivity in Bali Strait has been calculated by using Marra Algorithm and Gauss Model where its five paramater coefficients are calculated from observation data in June and September 2012. The sea surface temperature data and both surface chlorophyll and surface Photosynthetically Active Radiation data are taken from HAMburg Shelf Ocean Model (HAMSOM) simulation result and Moderate Resolution Imaging Spectroradiometer (MODIS) satelitte respectively for East Season and Second Transition Season. The result shows that the highest surface primary productivity is occured in August at the southwest area with value around 0,35gC/m²/day which is related to upwelling phenomenone. Primary productivity vertically also varies with the season where the depth of maximum primary productivity in East Season (0-10 meter) is shallower than in Second Transition Season (0-20 meter). |
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Final Project |
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Lany Putri Yuliananingrum, Trie |
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Lany Putri Yuliananingrum, Trie PRIMARY PRODUCTIVITY DISTRIBUTION IN BALI STRAIT |
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Lany Putri Yuliananingrum, Trie |
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Lany Putri Yuliananingrum, Trie |
title |
PRIMARY PRODUCTIVITY DISTRIBUTION IN BALI STRAIT |
title_short |
PRIMARY PRODUCTIVITY DISTRIBUTION IN BALI STRAIT |
title_full |
PRIMARY PRODUCTIVITY DISTRIBUTION IN BALI STRAIT |
title_fullStr |
PRIMARY PRODUCTIVITY DISTRIBUTION IN BALI STRAIT |
title_full_unstemmed |
PRIMARY PRODUCTIVITY DISTRIBUTION IN BALI STRAIT |
title_sort |
primary productivity distribution in bali strait |
url |
https://digilib.itb.ac.id/gdl/view/70361 |
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1822991502548140032 |