Water Column Chemical and Biological Inventories from the Arctic Ocean from 2010-2012 (ArcticNITRO project)

Website: https://www.bco-dmo.org/dataset/535715
Version: 07 May 2015
Version Date: 2015-05-07

Project
» Does competition for nitrogen between autotrophs and heterotrophs control carbon fluxes in the western coastal Arctic? (ArcticNITRO)
ContributorsAffiliationRole
Yager, Patricia L.University of Georgia (UGA)Principal Investigator, Contact
Bronk, Deborah A.Virginia Institute of Marine Science (VIMS)Co-Principal Investigator
Frischer, Marc E.Skidaway Institute of Oceanography (SkIO)Co-Principal Investigator
Sipler, Rachel E.Virginia Institute of Marine Science (VIMS)Co-Principal Investigator
Sanderson, Marta P.Virginia Institute of Marine Science (VIMS)Data Manager
Gegg, Stephen R.Woods Hole Oceanographic Institution (WHOI BCO-DMO)BCO-DMO Data Manager


Dataset Description

Water Column Chemical and Biological Inventories

AMBIENT = Water column inventories


Methods & Sampling

(tbd)


Data Processing Description

BCO-DMO Processing Notes
- Generated from original file "ARCTICNITRO_MasterlDataReport.xlsx, sheet: "Ambient" contributed by Patricia Yager
- Date reformatted to YYYYMMDD
- Lat/Lon degs, mins, secs converted to decimal degrees
- Parameter names edited to conform to BCO-DMO naming convention found at Choosing Parameter Name
- "nd" (no data) inserted into blank cells


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Data Files

File
MasterData_Ambient.csv
(Comma Separated Values (.csv), 21.45 KB)
MD5:9d7dabb33541184bd0f3a6a2421d144b
Primary data file for dataset ID 535715

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Parameters

ParameterDescriptionUnits
Year

Collection Year

YYYY
Station_ID

Location of sample collection (name)

text
Date

Date of sample collection (local Alaska time)

YYYYMMDD
Latitude

Latitude of sample collection

decimal degrees
Longitude

Longitude of sample collection

decimal degrees
Water_Depth

Station Water Depth

meters
Ice_Thickness

Ice Thickness

meters
Snow_Thickness

Snow Thickness

centimeters
Surface_Water_Temp

Surface Water Temp

degrees Celsius
Sample_ID

Sample Unique Identifier

text
Sample_Depth

Sample Depth

meters
CTD_Water_Temperature

CTD Water Temperature

degrees Celsius
CTD_Salinity

CTD Salinity

PSU
CTD_Dissolved_Oxygen

Water column dissolved oxygen from CTD depth profile

mg/l
CTD_Dissolved_Oxygen_Saturation

Water column % oxygen saturation from CTD depth profile

percentage
CTD_pH

Water column pH from CTD depth profile

pH Units
CTD_Relative_Turbidity

Water column turbidity from CTD depth profile

NTU
CTD_Chla_Fluorescense

Fluorometer from CTD depth profile

umol C/L
Ambient_Total_Dissolved_Nitrogen

Water column total dissolved nitrogen

umol N/L
Ambient_Total_Dissolved_Nitrogen_SD

Water column total dissolved nitrogen SD

dimensionless
Ambient_Ammonium

Water column NH4 concentration

umol N/L
Ambient_Ammonium_SD

Water column NH4 concentration SD

dimensionless
Ambient_Nitrite

Water column NO2 concentration

umol N/L
Ambient_Nitrite_SD

Water column NO2 concentration SD

dimensionless
Ambient_Nitrate

Water column NO3 concentration

umol N/L
Ambient_Nitrate_SD

Water column NO3 concentration SD

dimensionless
Ambient_Dissolved_Organic_Nitrogen

Water column total dissolved organic nitrogen

umol N/L
Ambient_Dissolved_Organic_Nitrogen_SD

Water column total dissolved organic nitrogen SD

dimensionless
Ambient_Urea

Water column urea concentration

umol N/L
Ambient_Urea_SD

Water column urea concentration SD

dimensionless
Ambient_Dissolved_Primary_Amines

Water column dissolved primary amine

umol N/L
Ambient_Dissolved_Primary_Amines_SD

Water column dissolved primary amine SD

dimensionless
Ambient_Dissolved_Organic_Carbon

Water column dissolved organic carbon

umol C/L
Ambient_Dissolved_Organic_Carbon_SD

Water column dissolved organic carbon SD

dimensionless
Ambient_Phosphate

Water column PO4 concentration

umol P/L
Ambient_Phosphate_SD

Water column PO4 concentration SD

dimensionless
Ambient_Silicate

Water column Si concentration

umol Si/L
Ambient_Silicate_SD

Water column Si concentration SD

dimensionless
Total_Dissolved_Phosphate

Water column dissolved phosphorous

umol P/L
Total_Dissolved_Phosphate_SD

Water column dissolved phosphorous SD

dimensionless
Dissolved_Organic_Phosphate

Water column dissolved organic phosphorous

umol P/L
Chlorophyll_a

Chl a concentration

ug/L
Chlorophyll_a_SD

Chl a concentration SD

dimensionless
Bacterial_Abundance

Flow cytometer counts using CYBR gold

cells/mL
Bacterial_Abundance_SE

Flow cytometer counts using CYBR gold SE

dimensionless
AVE_Bacterial_Production

Leucine incorporation rates per liter per hour

pmol Leu / L / h
AVE_Bacterial_Production_SD

Leucine incorporation rates per liter per hour SD

dimensionless
Whole_Community_Respiration

Whole community respiration from time series increases in DIC

umol O L-1 hr-1
nasA_gene_abundance

Gene abundance of bacterial nitrate reducase genes

gene copy L-1
nasA_gene_abundance_SD

Gene abundance of bacterial nitrate reducase genes SD

dimensionless
nasA_transcript_abundance

Normalized gene expression rates of bacterial nitrate reductase

transcript copy/ng total RNA L-1

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Deployments

ArcticNitro_Barrow

Website
Platform
ArcticNitro
Start Date
2010-08-30
End Date
2012-01-19
Description
Extracted from the NSF proposal Study sites: Because of its unique combination of year-round access to the coastal Arctic Ocean and strong scientific support system (Barrow Arctic Science Consortium we propose to make our primary winter and summer measurements from Barrow, Alaska. At 71°N, Barrow receives 24- hour sunlight between May 10 and August 2, and is in 24-h darkness between November 18 and January 24.  Less than 1 km from shore, shelf depths exceed 10m, and significantly deeper waters (>100 m) are not far away. Twice each year (January and July) for two years, working from Barrow, we will use either small boat or skidoo to travel offshore to sample seawater. We anticipate having access to surface waters of 10-20 m depth within a mile of the town of Barrow. We plan to sample biological and biogeochemical inventories along three offshore transects, with 3-5 depths that sample through the surface mixed layer and into the subsurface layer, accessing both the eastward coastal and the offshore westward currents (Weingartner 2006). More extensive rate measurements and incubation studies will be made at selected sites and depths The rationale for the transects is to sample the microbial community response to the cross-shelf and depth gradients DIN availability. Nearshore stations will be N-limited throughout the water column in the summer. Offshore stations may have significant NO3 below summer stratification. As part of SNACS (Study of the Northern Alaska Coastal) C. Ashjian and colleagues have recently completed summer research near Barrow, using small (43’) boats to investigate environmental controls on zooplankton populations. They will have nutrient profiles offshore, which will help guide our study. During the summer, we will coordinate with native Inupiat subsistence whalers (Barrow Whaling Captain Association. In the winter, safe travel over the ice by foot or snow machine, as far out as the nearshore lead, will offer access to the ocean using an ice auger. We will not be able to sample far offshore during winter, but gradients will be weaker due to mixing.


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Project Information

Does competition for nitrogen between autotrophs and heterotrophs control carbon fluxes in the western coastal Arctic? (ArcticNITRO)


Coverage: Nearshore Arctic Ocean; Barrow, Alaska; 71.25-71.50N, 156-157W


The Arctic is changing. Warm air is melting the sea ice at an accelerating pace, impacting the marine ecosystem. Further changes on land mean higher river discharge, rising seas, thawing of permafrost, and coastal erosion.

For the Arctic continental shelf, these physical changes impact the creatures that live there in major ways, ultimately altering the pathways and magnitude of energy transfer to fish, sea birds and marine mammals, and impacting the people dependant on those resources.  Our challenge today is to understand what is happening in specific Arctic ecosystems to assess future change.  

Understanding the microorganisms in Arctic coastal ecosystems is important because microbes dominate the biological biomass, production, and remineralization in marine systems. They are the "composters." Microbes are also the major producers and consumers of carbon dioxide and other greenhouse gases.

This study is focused on the climate-sensitive relationship between these microbes -- particularly the competition for nitrogen between phytoplankton/algae and bacteria -- and the productivity of the food web that depends on these organisms.



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Funding

Funding SourceAward
NSF Arctic Sciences (NSF ARC)
NSF Arctic Sciences (NSF ARC)
NSF Arctic Sciences (NSF ARC)

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