CTD data from California Current System (CCS) Process/Mesoscale Cruises on the R/Vs New Horizon, Revelle, Thompson, and Wecoma in the Northeast Pacific from 2000-2002 as part of the U.S. GLOBEC program (NEP project)

Website: https://www.bco-dmo.org/dataset/2462
Data Type: Cruise Results
Version: 1
Version Date: 2007-04-10

Project
» U.S. GLOBEC Northeast Pacific (NEP)

Program
» U.S. GLOBal ocean ECosystems dynamics (U.S. GLOBEC)
ContributorsAffiliationRole
Batchelder, HalOregon State University (OSU-CEOAS)Principal Investigator
Allison, DickyWoods Hole Oceanographic Institution (WHOI BCO-DMO)BCO-DMO Data Manager

Abstract
CTD data from California Current System (CCS) Process/Mesoscale Cruises on the R/Vs New Horizon, Revelle, Thompson, and Wecoma in the Northeast Pacific from 2000-2002 as part of the U.S. GLOBEC program.


Coverage

Spatial Extent: N:44.675 E:-123.692 S:38.7977 W:-126.1972
Temporal Extent: 2000-05-30 - 2002-08-19

Dataset Description

California Current System Process Cruises - CTD data


Methods & Sampling

Physical Influences on Populations in the California Current (Botsford, L. [Univ. Calif. Davis (UCD)], Hastings, A. M. [UCD], Largier, J. [Scripps Institute of Oceanography]) We propose to formulate models spanning the individual level to the metapopulation level for two genera of interest to GLOBEC in the CCS: ( 1) the two CCS salmon species identified by GLOBEC, coho salmon (Oncorhynchus kisutch) and chinook salmon (O. tshawytscha) and (2) Dungeness crab (Cancer magister), a species which covaries with salmon, is a significant prey of both species, and is subject to similar mesoscale circulation patterns. The ultimate purpose of these models will be to link the different scales of variability and levels of ecological organization in the various retrospective, monitoring and process studies so that the effects of changes in the physical environment on populations can be projected. Also, we will answer a number of questions through modeling and analysis of existing data, that will allow better focus of field studies on critical issues.

While upwelling and the regime shift in the mid-1970s are believed to have affected survival through this period, results of field studies of the cause are equivocal. We will develop a model to evaluate the interaction of time of ocean entry, size at entry, varying growth rate, and size dependent mortality rate on the fraction surviving this phase, and use it to compare the various field results in a common context. The results will help to focus field studies, and the model will provide a framework for evaluation of those studies. Even though Core Hypothesis III focuses on the juvenile stage, ENSO events are known to have a dramatic effect on survival of pre-spawning adults. Because the behavior of random populations of semelparous, anadromous species is poorly understood, the relative effects of environmental variability on their persistence and productivity is unknown. We will formulate a population model to determine which variable life history stage has the greater effect so that the GLOBEC process studies can focus on the appropriate one. We will formulate a metapopulation model to evaluate whether covariability between the environmental influences on different subpopulations affect persistence, and if it does, whether more productive populations can "rescue" extinct less productive populations?

We will also model and analyze the Dungeness crab population because the dramatic fluctuations in their abundance along the coast may be caused by the same environmental factor(s) that cause the salmon populations to vary, and may also be a cause of that variability through predation. We will apply a new approach to population analysis that answers the question: which environmental forcing function can combine with known density-dependent recruitment mechanisms to produce the observed variability in crab catch? (abstract)

This page was last updated on March 15, 2007.

Hal Batchelder
College of Oceanic and Atmospheric Sciences
Oregon State University
Corvallis, OR 97331-5503
phone: 541-737-4500; FAX 541-737-2064


Data Processing Description

Salinity was computed using standard algorithms from Fofonoff and Millard, 1983 (Algorithms for computation of fundamental properties of sea water. UNESCO Technical Papers in Marine Science, 44, 53 pp.)

Progress Report: April 1999: http://nepglobec.bco-dmo.org/projs/99.botsford.html


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Data Files

File
ccs_proc_ctd.csv
(Comma Separated Values (.csv), 11.47 MB)
MD5:5f1c5e1558c8e6d2dcf71e0214ea7598
Primary data file for dataset ID 2462

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Parameters

ParameterDescriptionUnits
cruiseidCruise identifier, e.g. W0005 R/V Wecoma cruise 0005. unitless
yearYear, e.g. 2002. unitless
stationConsecutive station number. unitless
station_nameStation code. unitless
dayDay of month (local time). unitless
monthMonth of measurement (0 to 12); local time. unitless
timeTime of day, local time, using 2400 clock format. unitless
depth_wWater depth, in meters. meters
latLatitude; north is positive. decimal degrees
lonLongitude, in decimal degrees, east is positive. decimal degrees
pressPressure. decibars
tempWater temperature. degrees Celsius
salsalinity, calculated from the CTD 'primary sensors' of conductivity and temperature. See 'Processing Description'. Practical Salinity Scale, dimensionless
potempPotential temperature. International Practical Temperature Scale - 68 ,or 90
sigma_0Sigma-theta density. not supplied
sp_vol_anSpecific volume anomaly. CL/T
DYN_HTDynamic height. J/KG
flvoltFluoresence volts
translight transmission, as percent %
trans_vlight transmission, as volts volts
O2_vOxygen current volts
O2SO2 saturation (guessing from O2S and units) ml per liter
O2dissolved oxygen milliliter/liter
PARdownwell Photosynthetically Available Radiation uE/cm2/sec
O2_tempoxygen temperature degrees C


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Instruments

Dataset-specific Instrument Name
Conductivity, Temperature, Depth
Generic Instrument Name
CTD - profiler
Dataset-specific Description
CTD measurements taken, CTD unit unidentified.
Generic Instrument Description
The Conductivity, Temperature, Depth (CTD) unit is an integrated instrument package designed to measure the conductivity, temperature, and pressure (depth) of the water column. The instrument is lowered via cable through the water column. It permits scientists to observe the physical properties in real-time via a conducting cable, which is typically connected to a CTD to a deck unit and computer on a ship. The CTD is often configured with additional optional sensors including fluorometers, transmissometers and/or radiometers. It is often combined with a Rosette of water sampling bottles (e.g. Niskin, GO-FLO) for collecting discrete water samples during the cast. This term applies to profiling CTDs. For fixed CTDs, see https://www.bco-dmo.org/instrument/869934.

Dataset-specific Instrument Name
Conductivity, Temperature, Depth
Generic Instrument Name
CTD - profiler
Generic Instrument Description
The Conductivity, Temperature, Depth (CTD) unit is an integrated instrument package designed to measure the conductivity, temperature, and pressure (depth) of the water column. The instrument is lowered via cable through the water column. It permits scientists to observe the physical properties in real-time via a conducting cable, which is typically connected to a CTD to a deck unit and computer on a ship. The CTD is often configured with additional optional sensors including fluorometers, transmissometers and/or radiometers. It is often combined with a Rosette of water sampling bottles (e.g. Niskin, GO-FLO) for collecting discrete water samples during the cast. This term applies to profiling CTDs. For fixed CTDs, see https://www.bco-dmo.org/instrument/869934.


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Deployments

NH0005

Website
Platform
R/V New Horizon
Report
Start Date
2000-05-28
End Date
2000-06-13

NH0007

Website
Platform
R/V New Horizon
Report
Start Date
2000-07-27
End Date
2000-08-12

NH0207

Website
Platform
R/V New Horizon
Report
Start Date
2002-07-31
End Date
2002-08-19

R0208

Website
Platform
R/V Roger Revelle
Report
Start Date
2002-07-31
End Date
2002-08-19

T0205

Website
Platform
R/V Thomas G. Thompson
Report
Start Date
2002-06-01
End Date
2002-06-17

W0005A

Website
Platform
R/V Wecoma
Report
Start Date
2000-05-29
End Date
2000-06-17

W0008

Website
Platform
R/V Wecoma
Report
Start Date
2000-07-29
End Date
2000-08-17

W0205A

Website
Platform
R/V Wecoma
Report
Start Date
2002-05-29
End Date
2002-06-18


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Project Information

U.S. GLOBEC Northeast Pacific (NEP)


Coverage: Northeast Pacific Ocean, Gulf of Alaska


Program in a Nutshell

Goal: To understand the effects of climate variability and climate change on the distribution, abundance and production of marine animals (including commercially important living marine resources) in the eastern North Pacific. To embody this understanding in diagnostic and prognostic ecosystem models, capable of capturing the ecosystem response to major climatic fluctuations.

Approach: To study the effects of past and present climate variability on the population ecology and population dynamics of marine biota and living marine resources, and to use this information as a proxy for how the ecosystems of the eastern North Pacific may respond to future global climate change. The strong temporal variability in the physical and biological signals of the NEP will be used to examine the biophysical mechanisms through which zooplankton and salmon populations respond to physical forcing and biological interactions in the coastal regions of the two gyres. Annual and interannual variability will be studied directly through long-term observations and detailed process studies; variability at longer time scales will be examined through retrospective analysis of directly measured and proxy data. Coupled biophysical models of the ecosystems of these regions will be developed and tested using the process studies and data collected from the long-term observation programs, then further tested and improved by hindcasting selected retrospective data series.



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Program Information

U.S. GLOBal ocean ECosystems dynamics (U.S. GLOBEC)


Coverage: Global


U.S. GLOBEC (GLOBal ocean ECosystems dynamics) is a research program organized by oceanographers and fisheries scientists to address the question of how global climate change may affect the abundance and production of animals in the sea.

The U.S. GLOBEC Program currently had major research efforts underway in the Georges Bank / Northwest Atlantic Region, and the Northeast Pacific (with components in the California Current and in the Coastal Gulf of Alaska). U.S. GLOBEC was a major contributor to International GLOBEC efforts in the Southern Ocean and Western Antarctic Peninsula (WAP).



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Funding

Funding SourceAward
NSF Division of Ocean Sciences (NSF OCE)
National Oceanic and Atmospheric Administration (NOAA)

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