S. Atlantic profiling radiometer system (SPMR/SMSR) from R/V Weatherbird II WB0409, WB0413, WB0506, WB0508 in the Sargasso Sea from 2004-2005 (EDDIES project)

Website: https://www.bco-dmo.org/dataset/3028
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 profiling radiometer system (SPMR/SMSR) from R/V Weatherbird II WB0409, WB0413, WB0506, WB0508 in the Sargasso Sea from 2004-2005.


Coverage

Spatial Extent: N:31.9319 E:-64.08 S:29.7775 W:-69.391
Temporal Extent: 2004-06-24 - 2005-08-23

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 reformated from hours and decimal minutes to hhmm.

 Change history: YYMMDD
    061212: original data downloaded from Eddies website 
            (WEATHERBIRD_SPMR_Profiles.xls) 
    071008: prepared for OCB database by N. Copley, OCB DMO
    071117: added to OCB database by C.Chandler (BCO-DMO, WHOI)

[ table of contents | back to top ]

Data Files

File
lightProbe_WB.csv
(Comma Separated Values (.csv), 4.36 MB)
MD5:fe03df3668956017f596cb638c1b747a
Primary data file for dataset ID 3028

[ table of contents | back to top ]

Parameters

ParameterDescriptionUnits
Cruise_ID

cruise ID designation code

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

hhmm
time_end

time at end of profile

hhmm
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
temp_SPMR

in-situ temperature of sea water from SPMR

degrees Centigrade
fluor_chla_stim

stimulated fluorescence of chl-a

volts
lu324

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)
lu565

upwelling radiance at wavelength 565

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)
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)
ed565

downwelling irradiance at wavelength 565

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)
rrs325

remote sensing reflectances (lw/ed) at wavelength 325

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
rrs565

remote sensing reflectances (lw/ed) at wavelength 565

steradian^-1
rrs665

remote sensing reflectances (lw/ed) at wavelength 665

steradian^-1
rrs683

remote sensing reflectances (lw/ed) at wavelength 683

steradian^-1
kl324

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
kl565

up-welled (diffuse) attenuation coefficnent of lu at wavelenth 565

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
kd324

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
kd565

down-welled (diffuse) attenuation coefficient of ed at wavelength 565

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
es325

downwelling surface irradiance at wavelength 325

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

downwelling surface irradiance at wavelength 340

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

downwelling surface irradiance at wavelength 380

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

downwelling surface irradiance at wavelength 412

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

downwelling surface irradiance at wavelength 443

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

downwelling surface irradiance at wavelength 490

microWatts/centimeter^2/nanometer (uW/cm^2/nm)
es510

downwelling surface irradiance at wavelength 510

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

downwelling surface irradiance at wavelength 554

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

downwelling surface irradiance at wavelength 565

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)


[ table of contents | back to top ]

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
SeaWiFS Profiling Multi-Channel Radiometer
Generic Instrument Name
SeaWiFS Profiling Multi-Channel Radiometer
Generic Instrument Description
The SeaWiFS Profiling Multi-Channel Radiometer (SPMR) is a free-falling instrument that is equipped with two sensors, collecting the upwelling irradiance (Ed) and downwelling (Lu) radiance at the following 11 wavelengths: 324, 340, 380, 412, 443, 490, 510, 555, 565, 665, and 683nm. The unit is protected in a long case that contains the majority of the system's electronics, while the optical sensors are located at either end of the case and face in opposite directions (i.e., up and down). These sensors measure the irradiance in units of uW/cm2/nm and the radiance in units of uW/cm2/nm/sr. Tilt and pressure are recorded at the same frequency as the irradiance measurements (6Hz). The SPMR is accompanied by a deck reference sensor, called the SeaWiFS Multichannel Surface Reference (SMSR). This sensor is equipped with the same 11 wavelengths as the SPMR, and is based on the same electronics. Data acquisition is synchronized between the SPMR and the SMSR and is performed at the same (6Hz) frequency.


[ table of contents | back to top ]

Deployments

WB0409

Website
Platform
R/V Weatherbird II
Start Date
2004-06-23
End Date
2004-07-02
Description
EDT1 2004 Transect 1 cruise Funded by: NSF OCE-0241310

WB0413

Website
Platform
R/V Weatherbird II
Start Date
2004-08-02
End Date
2004-08-11
Description
EDT2 2004 Transect 2 cruise Funded by: NSF OCE-0241310

WB0506

Website
Platform
R/V Weatherbird II
Start Date
2005-07-06
End Date
2005-07-15
Description
EDT3 2005 Transect 1 cruise Funded by: NSF OCE-0241310

WB0508

Website
Platform
R/V Weatherbird II
Start Date
2005-08-17
End Date
2005-08-26
Description
EDT4 2005 Transect 2 Funded by: NSF OCE-0241310


[ table of contents | back to top ]

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.



[ table of contents | back to top ]

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.



[ table of contents | back to top ]