S. Atlantic light-profiling system data from R/V Oceanus OC404-01, OC404-04, OC415-01, OC415-03 in the Sargasso Sea from 2004-2005 (EDDIES project)

Website: https://www.bco-dmo.org/dataset/3027
Data Type: Cruise Results
Version: 1
Version Date: 2007-11-17

Project
» Eddies Dynamics, Mixing, Export, and Species composition (EDDIES)

Program
» Ocean Carbon and Biogeochemistry (OCB)
ContributorsAffiliationRole
Siegel, DavidUniversity of California-Santa Barbara (UCSB-ICESS)Principal Investigator
Copley, NancyWoods Hole Oceanographic Institution (WHOI BCO-DMO)BCO-DMO Data Manager

Abstract
S. Atlantic light-profiling system data from R/V Oceanus OC404-01, OC404-04, OC415-01, OC415-03 in the Sargasso Sea from 2004-2005.


Coverage

Spatial Extent: N:37.1022 E:-58.752 S:28.7489 W:-69.41
Temporal Extent: 2004-06-13 - 2005-08-24

Dataset Description

Please refer to the separate document for the Methodology and PI notes. DMO note: appropriate wavelengths are listed with each parameter; 9.9E+35, -999, NA, and blank cells replaced with 'nd'; time_begin and time_end reformatted from hours and decimal minutes to hhmm

Change history: YYMMDD
    061212: original data downloaded from Eddies website
            (OCEANUS_SPMR_Profiles.xls)
    071004: prepared for OCB database by N. Copley, OCB DMO
    071117: added to OCB database by C.chandler (BCO-DMO, WHOI)

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Data Files

File
lightProbe_OC.csv
(Comma Separated Values (.csv), 6.70 MB)
MD5:fb75d7cd5b470b718dee4edb773a6121
Primary data file for dataset ID 3027

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Parameters

ParameterDescriptionUnits
Cruise_ID

cruise ID designation code

dimensionless
staProx

station number (nearest CTD)

dimensionless
date_begin

date sampling begins in the format YYYYMMDD

unitless
yrday

day of year sampling began (GMT)

dimensionless
time_begin

time at start of profile in the format hhmm

unitless
time_end

time at end of profile in the format hhmm

unitless
lon

longitude, negative denotes West

decimal degrees
lat

latitude, negative denotes South

decimal degrees
lon_eddy

longitude of eddy negative denotes West

decimal degrees
lat_eddy

latitude of eddy negative denotes South

decimal degrees
dist_EC

radial distance from eddy center

kilometers
comments

comments

dimensionless
depth

depth, sample, best estimate, usually calculated from pressure

meters
ed305

downwelling irradiance at wavelength 305

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
ed324

downwelling irradiance at wavelength 324

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
ed340

downwelling irradiance at wavelength 340

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
ed380

downwelling irradiance at wavelength 380

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
ed412

downwelling irradiance at wavelength 412

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
ed443

downwelling irradiance at wavelength 443

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
ed490

downwelling irradiance at wavelength 490

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
ed510

downwelling irradiance at wavelength 510

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
ed555

downwelling irradiance at wavelength 555

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
ed665

downwelling irradiance at wavelength 665

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
ed683

downwelling irradiance at wavelength 683

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
lu305

upwelling radiance at wavelength 305

microWatts/meter^2/nanometer/steradian (uW/cm^2/nm/sr)
lu325

upwelling radiance at wavelength 324

microWatts/meter^2/nanometer/steradian (uW/cm^2/nm/sr)
lu340

upwelling radiance at wavelength 340

microWatts/meter^2/nanometer/steradian (uW/cm^2/nm/sr)
lu380

upwelling radiance at wavelength 380

microWatts/meter^2/nanometer/steradian (uW/cm^2/nm/sr)
lu412

upwelling radiance at wavelength 412

microWatts/meter^2/nanometer/steradian (uW/cm^2/nm/sr)
lu443

upwelling radiance at wavelength 443

microWatts/meter^2/nanometer/steradian (uW/cm^2/nm/sr)
lu490

upwelling radiance at wavelength 490

microWatts/meter^2/nanometer/steradian (uW/cm^2/nm/sr)
lu510

upwelling radiance at wavelength 510

microWatts/meter^2/nanometer/steradian (uW/cm^2/nm/sr)
lu555

upwelling radiance at wavelength 555

microWatts/meter^2/nanometer/steradian (uW/cm^2/nm/sr)
lu665

upwelling radiance at wavelength 665

microWatts/meter^2/nanometer/steradian (uW/cm^2/nm/sr)
lu683

upwelling radiance at wavelength 683

microWatts/meter^2/nanometer/steradian (uW/cm^2/nm/sr)
es325

downwelling surface irradiance at wavelength 305

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
es340

downwelling surface irradiance at wavelength 324

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
es380

downwelling surface irradiance at wavelength 340

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
es412

downwelling surface irradiance at wavelength 380

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
es443

downwelling surface irradiance at wavelength 412

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
es490

downwelling surface irradiance at wavelength 443

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
es509

downwelling surface irradiance at wavelength 490

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
es554

downwelling surface irradiance at wavelength 510

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
es565

downwelling surface irradiance at wavelength 555

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
es665

downwelling surface irradiance at wavelength 665

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
es683

downwelling surface irradiance at wavelength 683

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
kl305

up-welled (diffuse) attenuation coefficnent of lu at wavelenth 305

meter^-1
kl325

up-welled (diffuse) attenuation coefficnent of lu at wavelenth 324

meter^-1
kl340

up-welled (diffuse) attenuation coefficnent of lu at wavelenth 340

meter^-1
kl380

up-welled (diffuse) attenuation coefficnent of lu at wavelenth 380

meter^-1
kl412

up-welled (diffuse) attenuation coefficnent of lu at wavelenth 412

meter^-1
kl443

up-welled (diffuse) attenuation coefficnent of lu at wavelenth 443

meter^-1
kl490

up-welled (diffuse) attenuation coefficnent of lu at wavelenth 490

meter^-1
kl510

up-welled (diffuse) attenuation coefficnent of lu at wavelenth 510

meter^-1
kl555

up-welled (diffuse) attenuation coefficnent of lu at wavelenth 555

meter^-1
kl665

up-welled (diffuse) attenuation coefficnent of lu at wavelenth 665

meter^-1
kl683

up-welled (diffuse) attenuation coefficnent of lu at wavelenth 683

meter^-1
kd305

down-welled (diffuse) attenuation coefficient of ed at wavelength 305

meter^-1
kd325

down-welled (diffuse) attenuation coefficient of ed at wavelength 324

meter^-1
kd340

down-welled (diffuse) attenuation coefficient of ed at wavelength 340

meter^-1
kd380

down-welled (diffuse) attenuation coefficient of ed at wavelength 380

meter^-1
kd412

down-welled (diffuse) attenuation coefficient of ed at wavelength 412

meter^-1
kd443

down-welled (diffuse) attenuation coefficient of ed at wavelength 443

meter^-1
kd490

down-welled (diffuse) attenuation coefficient of ed at wavelength 490

meter^-1
kd510

down-welled (diffuse) attenuation coefficient of ed at wavelength 510

meter^-1
kd555

down-welled (diffuse) attenuation coefficient of ed at wavelength 555

meter^-1
kd665

down-welled (diffuse) attenuation coefficient of ed at wavelength 665

meter^-1
kd683

down-welled (diffuse) attenuation coefficient of ed at wavelength 683

meter^-1
rrs305

remote sensing reflectances (lw/ed) at wavelength 305

steradian^-1
rrs325

remote sensing reflectances (lw/ed) at wavelength 324

steradian^-1
rrs340

remote sensing reflectances (lw/ed) at wavelength 340

steradian^-1
rrs380

remote sensing reflectances (lw/ed) at wavelength 380

steradian^-1
rrs412

remote sensing reflectances (lw/ed) at wavelength 412

steradian^-1
rrs443

remote sensing reflectances (lw/ed) at wavelength 443

steradian^-1
rrs490

remote sensing reflectances (lw/ed) at wavelength 490

steradian^-1
rrs510

remote sensing reflectances (lw/ed) at wavelength 510

steradian^-1
rrs555

remote sensing reflectances (lw/ed) at wavelength 555

steradian^-1
rrs665

remote sensing reflectances (lw/ed) at wavelength 665

steradian^-1
rrs683

remote sensing reflectances (lw/ed) at wavelength 683

steradian^-1


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Instruments

Dataset-specific Instrument Name
Fluorometer
Generic Instrument Name
Fluorometer
Generic Instrument Description
A fluorometer or fluorimeter is a device used to measure parameters of fluorescence: its intensity and wavelength distribution of emission spectrum after excitation by a certain spectrum of light. The instrument is designed to measure the amount of stimulated electromagnetic radiation produced by pulses of electromagnetic radiation emitted into a water sample or in situ.

Dataset-specific Instrument Name
Satlantic Micro-profiler II
Generic Instrument Name
Satlantic Micro-profiler II
Generic Instrument Description
The Satlantic Micro-Profiler II is a type of profiling radiometer system. The primary optical measurements are downwelling irradiance (Ed) and upwelling radiance (Lu).The Micro-Pro collects measurements in the following wavelengths: 305, 325, 340, 380, 412, 443, 490, 510, 555, 665, and 683. (Note the additional UV channel).


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Deployments

OC404-01

Website
Platform
R/V Oceanus
Report
Start Date
2004-06-11
End Date
2004-07-03
Description
EDDIES 2004 Survey 1 cruise Funded by: NSF OCE-0241310 Original cruise data are available from the NSF R2R data catalog (Cruise DOI: 10.7284/900337)

OC404-04

Website
Platform
R/V Oceanus
Report
Start Date
2004-07-25
End Date
2004-08-12
Description
EDDIES project 2004 Survey 2 cruise Funded by: NSF OCE-0241310 Original cruise data are available from the NSF R2R data catalog

OC415-01

Website
Platform
R/V Oceanus
Report
Start Date
2005-06-20
End Date
2005-07-15
Description
EDDIES project 2005 Survey 1 cruise Funded by: NSF OCE-0241310 Original cruise data are available from the NSF R2R data catalog

OC415-03

Website
Platform
R/V Oceanus
Report
Start Date
2005-08-07
End Date
2005-08-26
Description
EDDIES project 2005 Survey 2 cruise Funded by: NSF OCE-0241310 Original cruise data are available from the NSF R2R data catalog


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Project Information

Eddies Dynamics, Mixing, Export, and Species composition (EDDIES)


Coverage: Sargasso Sea


The original title of this project from the NSF award is: Collaborative Research: Impacts of Eddies and Mixing on Plankton Community Structure and Biogeochemical Cycling in the Sargasso Sea".

Prior results have documented eddy-driven transport of nutrients into the euphotic zone and the associated accumulation of chlorophyll. However, several key aspects of mesoscale upwelling events remain unresolved by the extant database, including: (1) phytoplankton physiological response, (2) changes in community structure, (3) impact on export out of the euphotic zone, (4) rates of mixing between the surface mixed layer and the base of the euphotic zone, and (5) implications for biogeochemistry and differential cycling of carbon and associated bioactive elements. This leads to the following hypotheses concerning the complex, non-linear biological regulation of elemental cycling in the ocean:

H1: Eddy-induced upwelling, in combination with diapycnal mixing in the upper ocean, introduces new nutrients into the euphotic zone.

H2: The increase in inorganic nutrients stimulates a physiological response within the phytoplankton community.

H3: Differing physiological responses of the various species bring about a shift in community structure.

H4: Changes in community structure lead to increases in export from, and changes in biogeochemical cycling within, the upper ocean.

Publications

Andrews, J.E., Hartin, C., and Buesseler, K.O.. "7Be Analyses in Seawater by Low Background Gamma-Spectroscopy.," Journal of Radioanalytical and Nuclear Chemistry, v.277, 2008, p. 253.

Andrews, J.E., Hartin, C., Buesseler, K.O.. "7Be Analyses in Seawater by Low Background Gamma-Spectroscopy," Journal of Radioanalytical and Nuclear Chemistry, v.277, 2008, p. 253.

Benitez-Nelson, C.R. and McGillicuddy, D.J.. "Mesoscale Physical-Biological-Biogeochemical Linkages in the Open Ocean: An Introduction to the Results of the E-Flux and EDDIES Programs.," Deep Sea Research II, v.55, 2008, p. 1133.

Benitez-Nelson, C.R. and McGillicuddy, D.J.. "Mesoscale Physical-Biological-Biogeochemical Linkages in the Open Ocean: An Introduction to the Results of the E-Flux and EDDIES Programs," Deep-Sea Research II, v.55, 2008, p. 1133.

Bibby, T.S., Gorbunov, M.Y., Wyman, K.W., Falkowski, P.G.. "Photosynthetic community responses to upwelling in mesoscale eddies in the subtropical North Atlantic and Pacific Oceans," Deep-Sea Research Part II: Topical Studies in Oceanography, v.55, 2008, p. 1310.

Buesseler, K.O., Lamborg, C., Cai, P., Escoube, R., Johnson, R., Pike, S., Masque, P., McGillicuddy, D.J., Verdeny, E.. "Particle Fluxes Associated with Mesoscale Eddies in the Sargasso Sea," Deep Sea Research II, v.55, 2008, p. 1426.

Carlson, C.A., del Giorgio, P., Herdl, G.. "Microbes and the dissipation of energy and respiration: From cells to ecosystems," Oceanography, v.20, 2007, p. 89.

Davis, C.S., and McGillicuddy, D.J.. "Transatlantic Abundance of the N2-Fixing Colonial Cyanobacterium Trichodesmium," Science, v.312, 2006, p. 1517.

Ewart, C.S., Meyers, M.K., Wallner, E., McGillicuddy, D.J., Carlson, C.A.. "Microbial Dynamics in Cyclonic and Anticyclonic Mode-Water Eddies in the Northwestern Sargasso Sea," Deep Sea Research II, v.55, 2008, p. 1334.

Ewart, C.S., Meyers, M.K., Wallner, E., McGillicuddy, D.J., Carlson, C.A.. "Microbial Dynamics in Cyclonic and Anticyclonic Mode-Water Eddies in the Northwestern Sargasso Sea," Deep-Sea Research II, v.55, 2008, p. 1334.

Goldthwait, S.A. and Steinberg, D.K.. "Elevated biomass of mesozooplankton and enhanced fecal pellet flux in cyclonic and mode-water eddies in the Sargasso Sea," Deep-Sea Research Part II: Topical Studies in Oceanography, v.55, 2008, p. 1360.

Greenan, B.J.W.. "Shear and Richardson number in a mode-water eddy," Deep-Sea Research Part II: Topical Studies in Oceanography, v.55, 2008, p. 1161.

Jenkins, W.J., McGillicuddy, D.J., and Lott III, D.E.. "The Distributions of, and Relationship Between 3 He and Nitrate in Eddies," Deep Sea Research II, v.55, 2008, p. 1389.

Jenkins, W.J., McGillicuddy, D.J., Lott III, D.E.. "The Distributions of, and Relationship Between 3 He and Nitrate in Eddies," Deep-Sea Research II, v.55, 2008, p. 1389.

Ledwell, J.R., McGillicuddy, D.J., and Anderson, L.A.. "Nutrient Flux into an Intense Deep Chlorophyll Layer in a Mode-water Eddy.," Deep Sea Research II, v.55, 2008, p. 1139.

Ledwell, J.R., McGillicuddy, D.J., Anderson, L.A.. "Nutrient Flux into an Intense Deep Chlorophyll Layer in a Mode-water Eddy," Deep-Sea Research II, v.55, 2008, p. 1139.

Li, Q.P. and Hansell, D.A.. "Intercomparison and coupling of MAGIC and LWCC techniques for trace analysis of phosphate in seawater," Analytical Chemica Acta, v.611, 2008, p. 68.

Li, Q.P., Hansell, D.A., McGillicuddy, D.J., Bates, N.R., Johnson, R.J.. "Tracer-based assessment of the origin and biogeochemical transformation of a cyclonic eddy in the Sargasso Sea," Journal of Geophysical Research, v.113, 2008, p. 10006.

Li, Q.P., Hansell, D.A., Zhang, J.-Z.. "Underway monitoring of nanomolar nitrate plus nitrite and phosphate in oligotrophic seawater," Limnology and Oceanography: Methods, v.6, 2008, p. 319.

Li, Q.P., Zhang, J.-Z., Millero, F.J., Hansell, D.A.. "Continuous colorimetric determination of trace ammonium in seawater with a long-path liquid waveguide capillary cell," Marine Chemistry, v.96, 2005, p. 73.

McGillicuddy, D.J., et. al.. "Eddy/Wind Interactions Stimulate Extraordinary Mid-Ocean Plankton Blooms," Science, v.316, 2007, p. 1021.

McGillicuddy, D.J., Ledwell, J.R., and Anderson, L.A.. "Response to Comment on "Eddy/Wind Interactions Stimulate Extraordinary Mid-Ocean Plankton Bloom".," Science, v.320, 2008.

McGillicuddy, D.J., Ledwell, J.R., Anderson, L.A.. "Response to Comment on "Eddy/Wind Interactions Stimulate Extraordinary Mid-Ocean Plankton Bloom"," Science, v.320, 2008.

McGillicuddy, et. al.. "Eddy/Wind Interactions Stimulate Extraordinary Mid-Ocean Plankton Blooms.," Science, v.316, 2007, p. 1021.

Mourino B., and McGillicuddy, D.J.. "Mesoscale Variability in the Metabolic Balance of the Sargasso Sea," Limnology & Oceanography, v.51, 2006, p. 2675.



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Program Information

Ocean Carbon and Biogeochemistry (OCB)


Coverage: Global


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.



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