Fig. 4.7.

Wed, 2020-03-18 14:10 -- hwadmin
Summary: 
(A) Waters of the shelf slope of the GBR are generally stratified. Water temperatures at over 200 m are often ~10°C lower that that at the surface. The examples we present here show a well-mixed water column (i.e. similar temperature from the surface to typically 50–100 m depth). (B) Upwelling by low-frequency internal waves on the GBR continental slope. (C) Satellite view of near-surface chlorophyll a along the GBR (Map: NOAA).
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Figure
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F23
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