Surface chlorophyll distributions in the upper Gulf of Thailand investigated using satellite imagery and ecosystem model
| dc.contributor.author | Buranapratheprat, Anukul | |
| dc.contributor.supervisor | Niemann, K. Olaf | |
| dc.date.accessioned | 2007-11-30T00:35:41Z | |
| dc.date.available | 2007-11-30T00:35:41Z | |
| dc.date.copyright | 2007 | en_US |
| dc.date.issued | 2007-11-30T00:35:41Z | |
| dc.degree.department | Department of Geography | |
| dc.degree.level | Doctor of Philosophy Ph.D. | en_US |
| dc.description.abstract | MERIS data and Nutrient-Phytoplankton-Zooplankton-Detritus (NPZD) ecosystem model coupled with the Princeton Ocean Model (POM), were used to investigate seasonal variations in surface chlorophyll distributions and their controlling factors to clarify phytoplankton dynamics in the upper Gulf of Thailand. Chlorophyll maps were produced by application on MERIS Level 2 data an empirical algorithm derived from the regression analysis of the relationship between chlorophyll-a concentration and remote sensing reflectance ratio. The results indicated that the patterns of seasonal chlorophyll distributions corresponded to local wind and water circulations. The model simulation highlighted the importance of river water as a significant nutrient source, and its movement after discharge into the sea is controlled by seasonal circulations. High chlorophyll concentration located along the western coast following the direction of counter-clockwise circulation, forced by the northeast winds, while chlorophyll accumulation was observed in the northeastern corner of the gulf due to clockwise circulation, driven by the southwest winds. These key simulated results are consistent with those of field observations and satellite images captured in the same periods of time, and also described seasonal shifting of blooming areas previously reported. Sensitivity analysis of simulated chlorophyll distributions suggested that not only nutrients but also wind-induced vertical movement plays a significant role in controlling phytoplankton growth. Plankton blooms occur in zones of upwelling or where vertical diffusivities are low. Increasing nutrients in the water column due to river loads leads to increasing potential for severe plankton blooms when other photosynthetic factors, such as water stability and light, are optimized. The knowledge of seasonal patterns of blooming can be used to construct environmental risk maps which are very useful for planning to mitigate the eutrophic problems. Effective measures need to be applied to control amount of nutrients released into natural water in order to minimize severity of red tides. | en_US |
| dc.identifier.uri | http://hdl.handle.net/1828/259 | |
| dc.language | English | eng |
| dc.language.iso | en | en_US |
| dc.rights | Available to the World Wide Web | en_US |
| dc.subject | Remote Sensing | en_US |
| dc.subject | POM | en_US |
| dc.subject | Circulation | en_US |
| dc.subject | Ecosystem model | en_US |
| dc.subject | Gulf of Thailand | en_US |
| dc.subject.lcsh | UVic Subject Index::Sciences and Engineering::Earth and Ocean Sciences::Physical geography | en_US |
| dc.title | Surface chlorophyll distributions in the upper Gulf of Thailand investigated using satellite imagery and ecosystem model | en_US |
| dc.type | Thesis | en_US |