Coastlines:
29 to 36degN, -125 to -115deg W | 28.5 to 38.5degN, -125 to -115W |
CalCOFI CTD HISTORY | ||||
YYYYMM | CruiseSC | Date | Author | Description |
201008 | 1008NH | JRW | 3500m deep CTD casts performed on stas 90.90 & 80.90 | |
201004 | 1004MF | JRW | 12 Niskin bottles only; 2 CTD casts performed on prodo stations to target prodo depths; not enough wire for deep casts | |
201001 | 1001NH | 17-Jan-2010, 29-Jan-2013 | JRW | 3500m deep CTD casts changed to stas 90.90 & 80.90 |
200911 | 0911NH | 6-Nov-2009 | J.Wilkinson | New SBE9plus CTD (09P53161-0936; 6800m) deployed; new sensor pairs T,C,& Ox + Seabird pH sensor, transmissometer, altimeter. New Seapoint fluorometer NOT deployed. |
200911 | 0911NH | 10-Nov-2009, 20-Nov-2009 | JRW | 3500m deep CTD casts performed on stas 90.100 & 80.100; Note for 3500m casts the following sensors are removed: ISUS & battery, PAR & pH. |
200907 | 0907MH | 14-Jul-2009 | J.Wilkinson | New version 2 Deck Unit purchased (27-Mar-2009); offsets secondary conductivity automatically; plus complete new set of sensors: SBE14 Remote depth readout; SBE18 pH sensor; QSP-2300 PAR; Wetlabs C-Star transmissometer; Teledyne Altimeter (on older 'fish') |
200411 | 0411RR | 2-Nov-2004 | J.Wilkinson | Satlantic ISUS nitrate sensor with battery pack added to CTD-rosette sensor array. |
199808 | 31-Aug-1998 | J.Wilkinson | CTD SN 93235-0203 (Arnold) upgraded to 9plus; 2058 rated | |
199807 | 9807NH | 08-Jul-1998 | J.Wilkinson | Added a second pair of temperature & conductivity; prompted by failure on previous cruise of the primary conductivity sensor - returned from calibration cracked. |
199807 | 01-Jul-1998 | J.Wilkinson | SBE32 Carousel Water Sampler replaces General Oceanics Pylon (Model 1015 purchased 8/1989) | |
199805 | 26-May-1998 | J.Wilkinson | CTD Sn 91338-1 (Homer) upgrade to 9plus; 3400m rating | |
199308 | 9308NH | 11-Aug-1993 | J.Wilkinson | Seabird CTD officially used for all 66 stations; 66 casts; 20 bottles |
199210 | 9210NH | 26-Sep1992 | J.Wilkinson | Seabird CTD used for prodo casts; 13 casts; 12 bottles; Ed Renger Prodo Cast operator |
199207 | 9207NH | 02-Jul-1992 | J.Wilkinson | Seabird CTD tested during prodo casts; 14 casts; 10 bottles |
199204 | 9204JD | 26-Apr-1992 | J.Wilkinson | One cast; conductive wire winch failure; hanging prodo cast on hydrowire |
199202 | 9202JD | 29-Jan-1992 | J.Wilkinson | Seabird CTD tested during prodo casts; 14 casts; 10 bottles |
199110 | 9110NH | 28-Sep-1991 | J.Wilkinson | New and improved Seabird CTD tested; 13 casts; 12 bottles. |
199011 | 9011NH | 8-Nov-1990 | J.Wilkinson | Second test of Seabird CTD on CalCOFI; 12 casts; 9 bottles. |
199003 | 9003JD | 4 Mar 1990 | J.Wilkinson | Seabird CTD first tested on CalCOFI; 13 casts; 10 bottles |
The California Cooperative Oceanic Fisheries Investigations (CalCOFI) are a unique partnership of the California Department of Fish and Wildlife, the NOAA Fisheries Service and the Scripps Institution of Oceanography. The organization was formed in 1949 to study the ecological aspects of the collapse of the sardine populations off California. Today its focus has shifted to the study of the marine environment off the coast of California and the management of its living resources. The organization hosts an annual conference, publishes data reports and a scientific journal and maintains a publicly accessible data server (www.calcofi.com).
The Field Program
Since 1949, CalCOFI has organized cruises to measure the physical and chemical properties of the California Current System and census populations of organisms from phytoplankton to avifauna. This is the foremost observational oceanography program in the United States.
Currently, 18 to 28 day cruises are conducted quarterly - summer & fall cruises are typically 18 days, winter & spring cruises are longer. Scripps and NOAA provide equally in terms of ship time, personnel, and other cruise-related costs. On each cruise a grid of 75 stations off Southern California is occupied. Winter & spring cruise may occupy stations just north of Pt Conception up to Monterey or San Francisco. At each station a suite of physical and chemical measurements are made to characterize the environment and map the distribution and abundance of phytoplankton, zooplankton, fish eggs and larvae.
Core measurements
CalCOFI hydrographic CTD data, particularly the thermodynamic properties, are computed by Seasoft based on EOS-80. Temperatures, typically from the primary temperature sensor, are merged with bottle sample data into station files which produce the hydrographic database and other data products, Hydrographic Reports, figures, IEHs. CTD sensor salinities, and oxygen values may also replace bottle measurements on mistrip or missing samples.
Currently (May 2014) no TEOS-10 calculation for absolute salinities are calculated.
Algorithms used for calculation of derived parameters in Data Conversion, Derive, Sea Plot, SeaCalc III [EOS-80 (Practical Salinity) tab], and Seasave are identical, except as noted in Derived Parameter Formulas (EOS-80; Practical Salinity), and are based on EOS-80 equations.
For formulas for the calculation of conductivity, temperature, and pressure, see the calibration sheets for your instrument.
Formulas for the computation of salinity, density, potential temperature, specific volume anomaly, and sound velocity were obtained from "Algorithms for computation of fundamental properties of seawater", by N.P. Fofonoff and R.C Millard Jr.; Unesco technical papers in marine science #44, 1983.
The SIO-CalCOFI method of termination is one of many techniques used to interface a CTD on a conductive wire. Over the years, our method has evolved - this document describes our current technique.
Since many ships have a 3-conductor wire (3 internal wires plus shield), each wire is terminated separately, isolating it from the other wires. If any single conductor fails over the course of the cruise, it can be disconnected from the CTD pigtail without having to re-terminate. Although each of the 3 wires & shield has its own connector, the CTD pigtail can combines the two 'best' conductive wires for the signal, reducing resistance. The remaining conductor is a spare or can be paired with the shield as ground. CalCOFI typically uses only the shield for ground.
On vessels with a single-wire conductive sea-cable, the standard termination (signal=conductive wire; ground=shield) method is used with a Seabird two-pin CTD pigtail. The wire stripping, soldering, and sealing of the termination is done the same way but with only one wire and shield. A standard two-pin Seabird termination pigtail is interfaced with the ship's single conductor wire. Wire shield is used for ground.
Part 1: The termination | (click photos for larger image) |
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Part II: The Sea-cable Connection | |
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Part III: The Rigging | |
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Tips & Reminders | |
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CalCOFI Data Management: Setting Community Standards
(presented as a poster at the 2007 CalCOFI Conference by James Wilkinson, Karen Baker & Richard Charter)
Introduction
CalCOFI represents a partnership of multiple agencies conducting quarterly joint oceanographic cruises. CalCOFI cruise participants work as a cohesive cross-agency unit to accomplish cruise objectives. Ancillary researchers frequently integrate their field measurements and sampling with the long-term core CalCOFI measurements and samples. Once a cruise concludes, however, this cohesive unit disperses; individuals return to their respective agencies and labs to process samples and analyze data. Each group uses legacy lab or agency specific methods and software to generate data products in local formats. These diverse data processing methods, products, and storage formats create challenges for merging final datasets. Development and incorporation of shared data management practices and joint community standards enable data integration.
Establishing Shared Practices
Identifying and establishing common, queriable columns, such as order occupied and event number, and including them in final data products allows heterogeneous datasets to be related. In addition, standardizing data elements such as column headers, date-time specifications, spatial designations such as GPS decimal format are easy to implement with minimal impact on existing data production. Standard, linkable data elements allow ingestion into relational databases, applications, and other analytical tools such as Data Zoo using import templates.
CalCOFI Standardization Strategies:
Shared Practices Begin in the Field
With quarterly cruises generating a persistent influx of data, the CalCOFI technical team must maintain an established routine to keep pace. Changes in procedure or protocol impact the expediency of the ongoing process. To minimize the impact of new data integration practices, the change process best begins at sea. Careful attention to sta activities & event logs create both a shared index and initiates a dialogue about organizational design.
Figure 1: Typical CalCOFI-SIO Data Flow from Field Collection to Publication
Figure 2: Typical CalCOFI-SWFSC Data Flow from Field Collection to Publication
Developing Data Integration Standards
At sea:
Cross-Project Data Interfacing
CalCOFI cruises generate multiple data formats such as station data; continuous meteorological, ADCP, & SCIMS (universal format SCS or MET continuous data + event numbers) data; avifauna & marine mammal visual observations and acoustic recordings. Each research group has their own data publishing goals. It must be the goal of all data-producing participants to generate a standard product with common indices for use by the data community. CalCOFI-SIO & CalCOFI-SWFSC are establishing a common vocabulary and standardizing final data formats & practices so hydrographic, zooplankton, and ichthyologic data can be integrated.
Data Interfacing Strategies:
Acknowledgements
We would like to recognize the added work done by field participants - ship and scientific staff - in helping to plan forward for data integration and by the cross-project community of participants working to create a common information environment. This work is supported by NOAA CalCOFI SIO and SWFSC together with the NSF LTER California Current Ecosystem and the Ocean Informatics team.
This information was presented as a poster at CalCOFI Conference 2007 (image).
Authors: James Wilkinson, Karen Baker from Scripps Institution of Oceanography and Richard Charter from NOAA Southwest Fisheries Science Center
Sample Drawing:
1. Chl samples are drawn on all rosette bottles tripped from ~200m to surface; sampling on a standard 20-bottle cast usually starts at #7 but refer to electronic sample log. For shallow stations, all the bottles may be sampled; noontime prodo casts may have extra bottles to sample; duplicate depths are usually skipped. Refer to the electronic sample log to verify which bottles to sample or ask the watchleader.
2. Drawing from the middle valve, add ~20mls, cap loosely, rinse-shake then dump; three rinses. Double-check the sample bottle number matches the rosette bottle number (often).
3. Chl samples are volumetric so after rinsing, fill it completely, cap loosely, tap the bottle gently against the rosette frame to dislodge any small bubbles then top-off, cap tightly, invert the bottle – if you see a large bubble, top-off and check again. Squeezing the sides of the bottle can change the sample volume so cup the bottle in your palm during the final fill to minimize this problem.
The graphic below is a reproduction from an article in which researchers at SIO are corroborating these predictions with observations.
El Niño is an abnormal warming phase in the Pacific Ocean Sea Surface Temperature (SST), while the abnormal cooling is known as La Niña - these shifts are part of the El Niño Southern Oscillation or ENSO. The current ENSO phase is often quantized by a deviation from normally observed SST using the Oceanic Niño Index or ONI. While El Niño and its counterpart cooling phase La Niña are still being researched, the seasonal effects are becoming well understood with long term data sets.
Using the table below from NOAA's Climate Prediction Center in conjunction with the CalCOFI database - can offer information on how the environment has reacted in response to the different phases and intensities of the ENSO.
Common mistakes are empty tubes that shouldn’t be; contaminated samples; and duplicate draws – two sample tubes filled from the same bottle
Seasoft computes PAR using the following equation:
PAR = [multiplier * (109 * 10(V-B) / M) / calibration constant] + offset
Enter the following coefficients in the CTD configuration file:
M = 1.0 (Notes 2 and 3)
B = 0.0 (Notes 2 and 3)
calibration constant = 105 / Cw (Notes 2 and 4)
multiplier = 1.0 for output units of μEinsteins/m2•sec (Note 5)
offset = - (104 * Cw * 10V) (Note 6)
Notes:
Instead of using the dark voltage to calculate the offset, you can also directly obtain the offset using the following method: Enter M, B, and Calibration constant, and set offset = 0.0 in the configuration (.con or .xmlcon) file. In Seasave V7, display the calculated PAR output with the sensor dark; then enter the negative of this reading as the offset in the configuration file.
104 (cm2/m2) * Cw * (10Light Signal Voltage - 10Dark Voltage) = (109 * 10V) / Calibration constant + offset
Since offset = - (104 * Cw * 10Dark Voltage), and V = Light Signal Voltage:
Calibration constant = 109 / (104 * Cw) = 105 / Cw
Example: If Wet calibration factor = 4.00 * 10-5 μEinsteins/cm2•sec, then C = 2,500,000,000 (for entry into configuration file).
Notes:
The CalCOFI Handbook is a compilation of information for cruise participants. It explains many aspects of the science performed at sea, particularly the sample drawing methods for each sample type.
CalCOFI Data File Formats
CalCOFI standard practices for sample analysis, data processing, metadata & general methodology.
SIO-CalCOFI software used at-sea and ashore, developed by the SIO CalCOFI Technical Group. Plus other software: auto-titrator oxygen analysis software developed by SIO's Ocean Data Facility; Seabird Seasoft & Data Processing software; Microsoft Office, Ultraedit, Ztree, hxD hex editor, Matlab, Surfer, Ocean Data View.