Satellite-Derived Photic Depth on the Great Barrier Reef: Spatio-Temporal Patterns of Water Clarity

被引:36
|
作者
Weeks, Scarla [1 ]
Werdell, P. Jeremy [2 ]
Schaffelke, Britta [3 ]
Canto, Marites [1 ]
Lee, Zhongping [4 ]
Wilding, John G. [2 ]
Feldman, Gene C. [2 ]
机构
[1] Univ Queensland, Sch Geog Planning & Environm Management, Biophys Oceanog Grp, Brisbane, Qld 4072, Australia
[2] NASA, Goddard Space Flight Ctr, Ocean Biol Proc Grp, Greenbelt, MD 20771 USA
[3] Australian Inst Marine Sci, Townsville, Qld 4810, Australia
[4] Univ Massachusetts, Dept Environm Earth & Ocean Sci, Boston, MA 02125 USA
来源
REMOTE SENSING | 2012年 / 4卷 / 12期
基金
澳大利亚研究理事会;
关键词
water clarity; photic depth; Secchi depth; satellite; Great Barrier Reef; spatio-temporal patterns; biophysical processes; OCEAN COLOR OBSERVATIONS; MULTISENSOR APPROACH; CORAL SEA; LAGOON; PRODUCTS; ECOLOGY; MONSOON; RUNOFF; REGION; DRIVER;
D O I
10.3390/rs4123781
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Detecting changes to the transparency of the water column is critical for understanding the responses of marine organisms, such as corals, to light availability. Long-term patterns in water transparency determine geographical and depth distributions, while acute reductions cause short-term stress, potentially mortality and may increase the organisms' vulnerability to other environmental stressors. Here, we investigated the optimal, operational algorithm for light attenuation through the water column across the scale of the Great Barrier Reef (GBR), Australia. We implemented and tested a quasi-analytical algorithm to determine the photic depth in GBR waters and matched regional Secchi depth (ZSD) data to MODIS-Aqua (2002-2010) and SeaWiFS (1997-2010) satellite data. The results of the in situ ZSD/satellite data matchup showed a simple bias offset between the in situ and satellite retrievals. Using a Type II linear regression of log-transformed satellite and in situ data, we estimated ZSD and implemented the validated ZSD algorithm to generate a decadal satellite time series (2002-2012) for the GBR. Water clarity varied significantly in space and time. Seasonal effects were distinct, with lower values during the austral summer, most likely due to river runoff and increased vertical mixing, and a decline in water clarity between 2008-2012, reflecting a prevailing La Nina weather pattern. The decline in water clarity was most pronounced in the inshore area, where a significant decrease in mean inner shelf ZSD of 2.1 m (from 8.3 m to 6.2 m) occurred over the decade. Empirical Orthogonal Function Analysis determined the dominance of Mode 1 (51.3%), with the greatest variation in water clarity along the mid-shelf, reflecting the strong influence of oceanic intrusions on the spatio-temporal patterns of water clarity. The newly developed photic depth product has many potential applications for the GBR from water quality monitoring to analyses of ecosystem responses to changes in water clarity.
引用
收藏
页码:3781 / 3795
页数:15
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