Near Surface Gradients During
the SAGE Cruise
Introduction  Cruise Log  SkinDeEP M-AERI SAGE Homepage   SOLAS Homepage
Cruise Log:  Friday, April 2, 2004

March
Sun
Mon
Tue
Wed
Thu
Fri
Sat
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
April
2
16
17
18
19
20
21
22
23
24
25
26
27
28
29
30
 
Associate Professor Graham Jones with the automatic underway dissolved DMS analyzer used onboard Tangaroa.
Location of the R/V Tangaroa on April 2, 2004.
Position: 46 34. 12S 172 01. 12E
Contributor: Graham Jones
Southern Cross University, Australia

Dissolved dimethylsulphide (DMS) is determined onboard by Associate Professor Graham Jones (Southern Cross University, Australia), Mike Harvey and John McGregor (NIWA), and Hilton Swan (Australian Government Analytical Laboratories, Sydney). A measurement is made every 14 minutes and this data with sea surface temperature and wind speed measurements will be used to calculate the flux of DMS as Tangaroa samples in and out of the patch. Wind speed has varied markedly during this voyage and seems to have affected not only the biological response and supply of DMS to the surface ocean, but has also stripped the surface ocean of DMS. Comparison of DMS flux measurements using the equations derived by Liss and Merlivat with flux measurements using the relaxed eddy accumulation (REA) technique developed at NIWA by Mike Harvey and Murray Smith will also be made on this voyage.
In addition, CTD samples of "in patch" and "out of patch" seawater have been processed for phytoplankton pigment measurements by Dr. Simon Wright of the Australian Antarctic Division. Next Day >>


          
AOPE Home