Contributors | Affiliation | Role |
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Lam, Phoebe J. | Woods Hole Oceanographic Institution (WHOI) | Principal Investigator, Contact |
Gegg, Stephen R. | Woods Hole Oceanographic Institution (WHOI BCO-DMO) | BCO-DMO Data Manager |
Seabird data processed on board R/V Islandia by Mr. Pericles Silva
File |
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CTD_ISL0109.csv (Comma Separated Values (.csv), 8.44 MB) MD5:3d4dc504a0a59cee01c1b445734bcb9b Primary data file for dataset ID 3482 |
Parameter | Description | Units |
CTD_DataSet_Id | CTD Dataset Id | text |
station | station number | integer |
cast | cast number | integer |
date | Station date | YYYYMMDD |
time | Station time | HHMMSS |
lat | Station latitude (South is negative) | decimal degrees |
lon | Station longitude (West is negative) | decimal degrees |
tv290C | Temperature ITS-90 | degrees celsius |
c0S_m | Conductivity | S/m |
prdM | Pressure Strain Gauge | decibars |
sbeox0Mm_Kg | Oxygen SBE 43 | umol/Kg |
sal00 | Salinity | PSU |
sigma_e00 | Density sigma-theta | Kg/m^3 |
depSM | Depth salt water | meters |
ptempC | Pressure Temperature | degrees celsius |
oxsatML_L | Oxygen Saturation | ml/l |
timeM | Time Elapsed | minutes |
flag | flag | nd |
Dataset-specific Instrument Name | CTD Sea-Bird SEACAT 19 |
Generic Instrument Name | CTD Sea-Bird SEACAT 19 |
Generic Instrument Description | The Sea-Bird SBE 19 SEACAT Recorder measures conductivity, temperature, and pressure (depth). The SEACAT is self-powered and self-contained and can be deployed in profiling or moored mode. The SBE 19 SEACAT was replaced in 2001 by the 19plus. more information from Sea-Bird Electronics |
Website | |
Platform | R/V Islandia |
Start Date | 2009-03-10 |
End Date | 2009-03-11 |
Description | */
TENATSO (Tropical Eastern North Atlantic Time-Series Observatory) time series station
16°N, 24°W, North-east of Mindelo, Sao Vicente, Cape Verde
TENATSO Home
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Science party:
Phoebe J. Lam, WHOI
Daniel C. Ohnemus, WHOI
Kanchan Maiti, WHOI
Pericles Silva, Instituto Nacional de Desenvolvimento das Pescas (INDP)
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We will test the hypothesis that the continental margin of northwest Africa provides a significant subsurface supply of iron to the open eastern tropical Atlantic that supplements dust.
We will test our continental margin hypothesis with a wintertime visit to the new Tropical Eastern North Atlantic Time-Series Observatory (TENATSO) near Cape Verde, located in the eastern tropical Atlantic about 850 km downstream of Mauritanian coastal upwelling, and a summertime cross-shelf transect from the Mauritanian coast to TENATSO with Ed Boyle, who is already funded to study iron in the tropical Atlantic. Our cross-shelf transect will closely examine the potential lateral source of Fe, and evaluate it against an atmospheric source of Fe. Our proposal takes advantage of a novel combination of measurements to uniquely determine the importance of lateral transport vs. dust inputs and subsurface remineralization as Fe sources to the surface ocean. These measurements include:
1) synchrotron x-ray analysis of particulate iron "hotspots": micron-size particles of iron detected with a synchrotron x-ray fluorescence microprobe have been previously shown to exhibit maxima at depths of continental margin input in two ocean basins. Further, the Ti:Fe ratios and the mineralogy of these particles of iron can distinguish dust-derived vs. continental margin iron. This is a qualitative tracer for a dust vs continental margin source of Fe.
2) radium isotopes: the major source of 228Ra into the study area is by diffusion from 232Th-bearing near shore and continental shelf sediments. An open-ocean to coastal transect of 228Ra activities will allow us to determine horizontal mass transfer. 228Ra will be used to quantify the lateral flux of iron from the shelf.
3) 234Th profiles: high vertical resolution 234Th profiles can be used to determine the depth of particle remineralization. This will be used to determine whether or not putative subsurface Fe maxima are from remineralization of Fe-bearing particles.
TENATSO (Tropical Eastern North Atlantic Time-Series Observatory) time series station
16°N, 24°W, North-east of Mindelo, Sao Vicente, Cape Verde
The Ocean Carbon and Biogeochemistry (OCB) program focuses on the ocean's role as a component of the global Earth system, bringing together research in geochemistry, ocean physics, and ecology that inform on and advance our understanding of ocean biogeochemistry. The overall program goals are to promote, plan, and coordinate collaborative, multidisciplinary research opportunities within the U.S. research community and with international partners. Important OCB-related activities currently include: the Ocean Carbon and Climate Change (OCCC) and the North American Carbon Program (NACP); U.S. contributions to IMBER, SOLAS, CARBOOCEAN; and numerous U.S. single-investigator and medium-size research projects funded by U.S. federal agencies including NASA, NOAA, and NSF.
The scientific mission of OCB is to study the evolving role of the ocean in the global carbon cycle, in the face of environmental variability and change through studies of marine biogeochemical cycles and associated ecosystems.
The overarching OCB science themes include improved understanding and prediction of: 1) oceanic uptake and release of atmospheric CO2 and other greenhouse gases and 2) environmental sensitivities of biogeochemical cycles, marine ecosystems, and interactions between the two.
The OCB Research Priorities (updated January 2012) include: ocean acidification; terrestrial/coastal carbon fluxes and exchanges; climate sensitivities of and change in ecosystem structure and associated impacts on biogeochemical cycles; mesopelagic ecological and biogeochemical interactions; benthic-pelagic feedbacks on biogeochemical cycles; ocean carbon uptake and storage; and expanding low-oxygen conditions in the coastal and open oceans.
Funding Source | Award |
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NSF Division of Ocean Sciences (NSF OCE) |