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Combining in-situ water quality and remotely sensed data across spatial and temporal scales to measure variability in wet season chlorophyll-a: Great Barrier Reef lagoon (Queensland, Australia)
被引:0
|作者:
Devlin M.J.
[1
]
da Silva E.T.
[1
]
Petus C.
[1
]
Wenger A.
[1
,2
,3
]
Zeh D.
[1
]
Tracey D.
[1
]
Álvarez-Romero J.G.
[2
]
Brodie J.
[1
]
机构:
[1] Catchment to Reef Research Group, TropWater, James Cook University, Townsville
[2] Australian Research Council Centre of Excellence for Coral Reef Studies, James Cook University, Townsville, QLD
[3] School of Marine and Tropical Biology, James Cook University, Townsville, QLD
关键词:
Chlorophyll-a;
Great barrier reef;
MODIS;
Monitoring;
Phytoplankton;
Remote sensing;
D O I:
10.1186/2192-1709-2-31
中图分类号:
学科分类号:
摘要:
Introduction Combining in-situ data from single-point time series with remotely sensed spatial data allowed a greater elucidation of changes in chlorophyll-a concentrations through wet season conditions in the Great Barrier Reef coastal waters. Methods Single-point time-series data were collected from 2006 to 2012 during high river flow conditions to assess changes in phytoplankton biomass (measured as chlorophyll-a). Additionally, three flood plume water types, derived from classified true-colour Aqua moderate resolution imaging spectroradiometer (MODIS) images, were used to group single-point time-series data for the phytoplankton biomass assessment. Results Survey data illustrate the heterogeneity of chlorophyll-a distribution over seasonal and inter-annual cycles and the difficulty in describing community responses through the wet season. The spatial data demonstrate distinct regional differences throughout the Great Barrier Reef. The high chlorophyll-a concentrations measured in flood plume waters immediately adjacent to the inshore, highly turbid 'inner' flood plume are a product of sufficient light, given most of the suspended solids have settled from the plume, and the availability of sufficient nutrients, which drive higher phytoplankton production and characterise the formation of secondary stage flood plumes. The formation and extent of these secondary flood plumes were mapped using MODIS true-colour satellite imagery. The distance and the location of the secondary plume water are reliant on flow, coastal hydrodynamics, and biological activity. Conclusions The combination of in-situ data and remotely sensed data provides information on the complexity of these coastal processes during the wet season and offers managers a more comprehensive understanding of the extent of nutrient enrichment in the Great Barrier Reef coastal area and the potential influence of flood plumes on coastal marine ecosystems. © 2013 Devlin et al.
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