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BNL
INL
Lateral Transport of Dissolved and Particulate TEIs at Ocean Margins
K2-NW Pacific
% TransmissionAlong Line W
228Ra
Attributes of Line W as a GEOTRACES section
• Detailed hydrographic template within which to interpret geochemical profiles (proposed PO program to run until 2013).
• Frequency of cruises between Woods Hole and Bermuda facilitate re-occupation of stations along transect (Process studies? GEOTRACES Intercalibration Station?).
• Intersects with planned ORION/IOOS PIONEER program designed to characterize shelf-slope processes on NW Atlantic margin.
• Intersects major components of MOC (DWBC and Gulf Stream).
• Sharp, well-defined contrasts in water mass source/age/history.
• High productivity margin.
• Significant and distinct lateral particle fluxes in intermediate and bottom nepheloid layers.
• Prior and on-going sediment trap studies.
• Ideal for studies of elemental boundary scavenging.
• Potential western limb of an east-west transatlantic GEOTRACES section that interests major particle flux time-series stations.
http://www.whoi.edu/science/PO/linew/index.htm
PIONEER Array, Line W, and the Northeast Regional Coastal Ocean Observing System
Line WPioneer
Array
Deep
WesternBoundary
Curre
nt
On-going and planned physical oceanographicmeasurements along Line W (J. Toole et al.)
Moorings:
Fixed instruments (moorings 2,4,6)-T/C sensors- Vector averaging current meters (VACMs)
Moored Profilers (MMPs, moorings 1,3,5)- CTD- ADCP- Optical backscatter- Transmissometry (proposed)
1 2 3 4 5 6
Hydrographic survey cruises:
- CTD- Nutrients- Dissolved O2- I-129- CFCs/SF6
- Optical backscatter + transmissometry
(Joyce et al., 2005)
Composite mean property sections (1995 and 2006) along Line W. Average, net southward DWBC transport across Line W is estimated to be 16 Sv.
Recent and proposed biogeochemical flux studies on Line W
Sediment traps
0
50
100
150
200
250
300
W-Pacific Site-12-2304
Weddell_Sea_VIII_upper-2453
E-Pacific HOTS-1500m
Nordic Atlantic PARFLUX-Fram_Strait-FS-2400m
Atlantic Southern Ocean South_Georgia_Island-SGI-2000m
JGOFS-Equatorial_Pacific-EQPAC-9N-2150m
atlantic Southern Ocean Bouvet_Island-BO5-lower-2251m
Sargasso_Sea-OFP-1500m
N-AtlanticL1-94-2000m
E-Pacific MANOP-Site-S-1600m
N-Atlantic L1-93-2020m
JGOFS-Equatorial_Pacific-EQPAC-5S-avg of 2099, 2209,
2316m
N-Atlantic JGOFS-NABE-34N-2067m
JGOFS-Arabian_Sea-M5-2363m
Nordic Atlantic PARFLUX-Bear_Island-BI-1700m
JGOFS-Equatorial_Pacific-EQPAC-2N-2203mJGOFS-Equatorial_Pacific-EQPAC-5N-2100m
N-Atlantic L2-94-2000m
S-Atlantic Walvis_Ridge-WR3/4-LOWER-average of 1640 and
1648
Indo-German_Bay_of_Bengal-NBBTs-1717m avg of 2 years
W-Pacific Site_2-1769m
JGOFS-Equatorial_Pacific-EQPAC-Eq-2284m
E-Pacific MANOP-TP-C-1883m
W-Pacific JAST01-Okinawa_Trough-1547m
Indo-German_Bay_of_Bengal-NBBTn-1727m avg of 2 years
N-Atlantic Cape_Blanc-CB1/2-deep-2195m
Indo-German_Bay_of_Bengal-CBBT-2282m avg of 3 years
N-Atlantic Cape_Blanc-CB1-deep-2195m
W-Pacific Site_1_shallow-1590mE-Pacific Off_Chile-CH4-2300mJGOFS-Arabian_Sea-M3-1857mJGOFS-Arabian_Sea-M2-1974m
StW average three depths, 2 years
Average daily mass flux (mg/m2/d)
Line W(mooring @ 3000 m isobath)
The Northwest Atlantic Margin is characterized by high mass fluxes!
Global variations in mass fluxes for particles intercepted by sediment traps deployed within or below the mesopelagic zone
Line W Mooring deployment timelines (past and proposed)
Spring2004
Spring2005
Spring2006
Spring2007
Spring2008
3000 mTrap mooring
POmoorings
Proposed
WHOI funded
WHOI funded NSF-CO funded NSF-CO funded
NSF-PO funded NSF-PO funded NSF-PO funded NSF-PO funded
WHOI funded
Toole proposal
2000 mTrap mooring
4700 mTrap mooring
Spring2009
Spring2010
ProposedProposed
Toole proposal Toole proposal
Spring2012
PossiblePossible
Toole proposal Toole proposal
Spring2011
Proposed
Spring2013
Proposed
An E-W transatlantic GEOTRACES section?
LineW
BermudaOFP
ESTOC
PO measurement program consists of a moored array spanning the continental slope plus annual/semi-annual (spring and fall)
hydrographic survey cruises
http://www.whoi.edu/science/PO/linew/index.htm
Line W
Rasmussen (2003)
The NW Atlantic Margin: A Productive, dynamic and spatially heterogenous system
Three-day composite satellite SST (left) and chlorophyll concentration (right) for 18-20 June 2001.
Turbidity sensor measurements from MMP deployed at 3000 m (Station W)
Jan 30, 2005