日本地球惑星科学連合2019年大会

講演情報

[J] ポスター発表

セッション記号 A (大気水圏科学) » A-CG 大気海洋・環境科学複合領域・一般

[A-CG45] 水圏科学における可視域リモートセンシングとその応用

2019年5月28日(火) 17:15 〜 18:30 ポスター会場 (幕張メッセ国際展示場 8ホール)

コンビーナ:石坂 丞二(名古屋大学宇宙地球環境研究所)、虎谷 充浩(東海大学工学部)、作野 裕司(広島大学大学院工学研究科)、平譯 享(北海道大学大学院水産科学研究院)

[ACG45-P09] Monthly variability of Chlorophyll-a distribution in the Gulf of Thailand

*Dudsadee Leenawarat1Anukul Buranapratheprat2Joji Ishizaka3 (1.Graduate School of Environmental Studies, Nagoya University, Japan、2.Department of Aquatic Science, Faculty of Science, Burapha University, Thailand、3.Institute for Space-Earth Environmental Research, Nagoya University, Japan)

キーワード:Gulf of Thailand, Chlorophyll-a, Variability

The Gulf of Thailand (GoT) is semi-enclosed sea located in the western part of the South China Sea. This area is important to fisheries production in this region. The satellite data can reveal the primary production through chlorophyll-a (Chl-a) which is basic for the food chain. The objectives of this study are to investigate the variation and spatial distribution patterns of Chl-a in the GoT by using long-term satellite data from SeaWiFS (1997-2010), MERIS (2002-2012), MODIS AQUA (2002-2018), and VIIRS (2012-2018) level 3 compared with oceanographic conditions from previous study and circulation model name Princeton Ocean Model (POM). Tide and climatological data of wind, salinity, temperature and river discharge are forcing in the model. The results from averaged monthly Chl-a concentration in the central GoT illustrate low Chl-a concentration occurred in transition periods (April-May, and October) by lowest in May when the water column was stratified. High Chl-a concentration occurred during the northeast monsoon (November to February) with the highest in December when the water column was well mixed, and a small peak was found during June to August. Hight Chl-a was found along the coast, especially near the northern coast in the southwest monsoon (June to October). During the northeast monsoon Chl-a near cape CaMau spread offshore, due to strong surface currents flew into GoT from the southern part of cape CaMau to the middle of GoT mouth.