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).
Type: 
Figure
Sub Component: 
Normal
Slug: 
F23
Highwire: Type: 
fragment
Highwire: Parent: 
Oceanography
HighWire: Journal/Corpus Code: 
csirobk
Highwire: pisa_id: 
csirobk;9781486308200/1/BK07763_ch04/F23
Highwire: pisa_master: 
csirobk;9781486308200/1/BK07763_ch04/F23
HighWire: Atom Path: 
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Highwire: cpath: 
/content/9781486308200/9781486308200/SEC6/SEC9/F23
Image - Large: 
Large
Highwire: cpathalias: 
/content/csirobk/9781486308200/9781486308200/SEC6/SEC9/F23
Image - Medium: 
Medium
Highwire: Variants: 
expansion
Image - Small: 
Small
Highwire: State: 
Released
Contributors: 
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