CRUISE REPORT HUDSON 99022 LABRADOR SEA WOCE LINE AR7W 27 June - 13 July, 1999 CRUISE NARRATIVE Highlights WOCE Designation: WOCE Line AR7W Atlantic Circulation Experiment Expedition Designation: Hudson 99022 Chief Scientist: R. Allyn Clarke Ocean Sciences Division Department of Fisheries and Oceans Bedford Institute of Oceanography PO Box 1006 Dartmouth, NS, Canada B2Y 2A4 Internet clarkea@mar.dfo-mpo.gc.ca Ship: CCGS Hudson Ports of Call: June 27 BIO, Dartmouth, NS, Canada July 13 BIO, Dartmouth, NS, Canada Cruise Dates: June 27 to July 13, 1998 2. Cruise Summary Information a. Cruise Track A cruise track is shown in Figure 1*. Ship position at 0000Z on each day of the cruise is indicated with a date label. The WOCE cruise station summary file outlines the science operations conducted during the cruise. Note that additional cast types have been defined as: NET - Biological net tow; AGT - alongtrack temperature-salinity measurements; SAP - alongtrack shipboard ADCP measurements; GOF - GO Flow bottle cast; PMP - pump cast; MNT - Biological multinet cast; CLG - Challenger pump cast. As well, additional time codes have been defined as: BD - Begin Descent; EA - End Ascent. These codes are used during Lowered ADCP casts. Finally, in the Comment section of the SUM file there is frequent mention of operation notes indicated by "Op Note". These notes will be included in the final cruise report. Figure 1*. Cruise track for 18HU99022/1. The date labels indicate the ships position at 0000Z. Additional parameter codes have also been defined and appear in the parameter column of the WOCE SUM file. These codes are: 510 - extracted chlorophyll; 511 - phytoplankton count; 512 - High Pressure Liquid Chromatography (HPLC); 513 - Absorption Spectra; 515 - Thorium (234-Th); 516 - Protactinium (231-Pa); 517 - Iodine (129-I) ; 518 - Technetium (99 -Tc). Sections that follow in the cruise report describe these measurements. b. Total Number of Stations Occupied The CTD and ROS station positions are shown in Figure 2*. The WHP stations are all contained in the box defined by 50-62°N and 43-60°W. Table 1 lists the science operations for 99022. Cast Number of Detailed Division Operation Numbers Type Operations Rosette 56 27 regular AR7W Sites plus Site 8.5 see Table 2 & CTD 7 Halifax Line Sites see Table 3 2 Seacat Calibrations 61 (also in Table 2), 147 19 Biology Casts 32,35,56,70,71,84,87,90, 99,109,111,112,124,126, 134,137,145,152,154 1 Basin test 1 Moorings 5 2 recoveries 58, 144 2 deployments 59, 146 1 release test 136 Biology 72 64 shallow net tows 4-6,8-10,12-14,16- 18,20,21,22,24,28,31, 34,36,37,39,41,43,45,47,49, 51,55,60,67,72,74,78,79,85,89, 95,98,102, 103,105,106,110,119,121,123, 125,128,130,131,135,139,140, 148,150,151,153,155-160 8 multinet tows 26,30,69,100,108,133, 142,143 Chemistry 25 8 Challenger Pump deployments at 57,64,76,83,92,96,113, 4 locations 118 10 Go-Flo casts at 5 locations 33 (test), 53,54,63,66, 82,91,94,97,115 7 surface pump casts at 4 locations 27 (test), 62,65,77,81, 114,117 I, Tc sampling at CTD locations 38,42,46,50,52,56,70,73, 75,80,86,87,88,141,138, 137,93,99,132,134,104, 129,107,109,126,112,124, 120 Th, Pa sampling at CTD locations 38,42,46,50,52,68,70,86, 87,129,134,107,109,112, 116,124,120 Table 1. Science operations conducted on 18HU99022/1. Cast Number of Detailed Division Operation Numbers Type Operations Other 2 Ship Board ADCP 2 Along track t, s, and fluorescence 3 Table 1. Science operations conducted on 18HU99022/1. AR7W Site Number 99022 Deep Cast Operation Number 1 38 2 40 3 42 4 44 5 46 6 48 7 50 8 52 8.5 149 9 61 10 68 11 73 12 75 13 80 14 86 15 88 16 141 17 138 18 93 19 101 20 132 21 104 22 129 23 107 24 127 25 116 26 122 27 120 28 not occupied Table 2. AR7W sites and rosette operation numbers for 18HU99022/1. Figure 2*. CTD, rosette and LADCP station positions on for Hudson 18HU99022/1. Halifax Line Number 99022 Deep Cast Operation Number 1 7 2 11 3 15 4 19 5 23 6 25 7 29 Table 3. Halifax Line sites and rosette operation numbers for 18HU99022/1. Along AR7W, the stations were full depth WHP small volume rosette casts with up to 24 rosette bottles. Depending on the station, water samples were analyzed for CFC's, carbon tetrachloride, methyl chloroform, total carbonate, alkalinity, oxygen, salinity, nutrients, oxygen isotopes, helium and tritium. On some casts, chemistry isotope sampling was also conducted for iodine, technetium, protactinium and thorium. c. Floats and Drifters deployed No floats or drifters were deployed. d. Moorings deployed or recovered A total of 5 mooring related operations, consisting of 2 deployments, 2 recoveries and 1 release test were conducted at various sites. The following summarizes the mooring operations. Deployments: 1 M1326 standard mooring consisting of one current meter positioned 20m off bottom along AR7W on the Labrador Slope (12-month deployment) along the 1000m isobath. 1 M1325 multi-instrument mooring near OWS Bravo on AR7W. This mooring consisted of 4 microcats, 3 Seacat temperature/conductivity recorders, and 6 Aanderaa current meters Recoveries: 1 M1276 standard mooring consisting of one current meter positioned 20m off bottom along AR7W on the Labrador Slope (12 month deployment) along the 1000m isobath. This mooring was deployed on 18HU98023. M1275 multi-instrument mooring near OWS Bravo on AR7W. This mooring consisted of 7 Seacat temperature/conductivity recorders, 6 Aanderaa current meters, and 3 SBE39 (two with temperature and one with temperature and pressure). This mooring was deployed on 18HU98023. 3. List of Principal Investigators Name Affiliation Responsibility Allyn Clarke BIO Senior scientist clarkea@mar.dfo-mpo.gc.ca Overall co-ordination Bob Gershey BDR Research Alkalinity, carbonate, CFC's rgershey@fox.nstn.ns.ca Glen Harrison BIO Coordinator biological program harrisong@mar.dfo-mpo.gc.ca nitrate and ammonium utilization by phytoplankton Erica Head BIO Macrozooplankton distribution, heade@mar.dfo-mpo.gc.ca abundance and metabolism Robert Houghton LDEO Oxygen isotopes houghton@ldeo.columbia.edu Paul Kepkay BIO Dissolved organic carbon, kepkayp@mar.dfo-mpo.gc.ca colloid chemistry and plankton respiration Peter Jones BIO Alkalinity, carbonate, CFC's jonesp@mar.dfo-mpo.gc.ca John Lazier BIO CTD data, moored instrument lazierj@mar.dfo-mpo.gc.ca data Bill Li BIO Pico-plankton distribution and lib@mar.dfo-mpo.gc.ca abundance, bacteria Robert Pickart WHOI Lowered ADCP pickart@rsp.whoi.edu Peter Rhines UW Moored instrument data rhines@killer.ocean.washington.edu John Smith BIO Chemistry isotopes smithjn@mar.dfo-mpo.gc.ca Table 4. List of Principal Investigators. See Section 7 for addresses. 4. Scientific Program and Methods 4.1 Physical - Chemical Program a. Narrative This expedition was conducting operations in support of three ongoing scientific initiatives. The first initiative is in support of the North Atlantic Oscillation and the Atlantic Thermohaline Circulation Principal Research Areas of the Climate Variability and Predictability (CLIVAR) project of the World Climate Research Programme (WCRP). The occupation of the Labrador Sea section and the recovery and replacement of the two Labrador Sea moorings provide a measure of the winter cooling and water mass transformations over the winters of 1998/99 and 1999/2000. The second initiative is the Labrador Sea project of the Canadian Joint Global Ocean Flux Study (JGOFS). The biological program is designed to characterize the late spring biological processes in the Labrador Sea and its shelf regions. The purposes of the program are to determine the role of the biological pump to sequester carbon and to develop the regional algorithms that will allow primary productivity estimates to be made using data from Ocean Colour satellite sensors such as Sea Wifs. The physical oceanographic program is observing total carbonate, alkalinity and CFC's over the entire water column in support of these JGOFS objectives. The third objective is to occupy the Halifax Section in support of DFO Atlantic Zone's monitoring strategy. During this cruise, an ADCP was added to the CTD/rosette package to provide an estimate of the full depth velocity profile at each CTD station. This data will be useful for the detection and definition of various subsurface currents such as the deep western boundary undercurrents. 4.2 Biological Program a. Narrative The biological program conducted as part of cruise 99022, with some modifications, was a continuation of studies began in 1994 to describe the large scale (spatial and temporal) variability in plankton biomass and productivity in the Labrador Sea. The program has consisted of essentially four elements: (1) a phytoplankton biomass/primary productivity program - conducted most years by Jeff Anning (this year included Brian Irwin), (2) a microbial program conducted by Bill Li or Paul Dickie, (3) a mesozooplankton program conducted by Erica Head or Les Harris (this year including Tim Perry) and (4) a dissolved organic carbon/community respiration program conducted by Paul Kepkay or Jay Bugden. The ultimate aim of these studies is twofold: (1) to provide a description of the inventories of biogenic carbon in the Labrador Sea, their turnover rates and variability in space and time as part of OSD's continuing climate-studies and (2) to provide a description of plankton life-cycles and productivity in the Labrador Sea and its influence or contribution to ecosystems downstream in support of OSD's fisheries-related research. New studies during this cruise included a more detailed investigation of microbial plankton (pico-phytoplankton, bacteria and viruses), measurements of phytoplankton utilization of nitrate and ammonium and more detailed studies of deep meso/macrozooplankton populations using the Multinet system. In addition to the Labrador Sea study, phytoplankton, mesozooplankton and nutrient samples were collected at the seven stations along the Halifax line and three zooplankton tows were taken on the Cabot Strait line in support of OSD's obligations to the Atlantic Zone Monitoring Program. b. Stable Isotope Studies of Carbon and Nitrogen (nitrate and ammonium) Utilization by Phytoplankton Glen Harrison This work represents a continuation of research begun in 1994 to determine the primary productivity (in terms of carbon and nitrogen) of phytoplankton in the Labrador Sea. Carbon (CO2), nitrate and ammonium utilization rates from eight depths in the photic zone (i.e. the 1% light level ranged from 35-60 m) were determined using stable isotope tracer (13-C and 15-N) methods. Incubations experiments were carried out in on-deck 'simulated in-situ' incubators. At a few stations, 14-C incubations were done for comparison. A total of 14 experiments were conducted (see Table 5); 10 stations were occupied along the AR7/W line and four in transit to and from the line. Four of the stations occupied were those where the chemistry in-situ pumps were deployed. Carbon- based primary productivity rates at these locations will be compared with vertical fluxes of particulate biogenic carbon derived from the thorium/carbon analyses to estimate fraction biogenic carbon export in the region. Date Site Operation LAT (N) LON (W) Photic Depth 15N/13C 14C Number (m) 29-Jun-99 LL3 32 45.48 -59.51 50 x 30-Jun-99 NE-GSL#1 35 49.74 -59.39 50 x 1-Jul-99 L3_1 38 53.68 -55.54 45 x 2-Jul-99 L3_9 56 55.26 -53.97 35 x 3-Jul-99 L3_10 70 55.42 -53.82 45 x 4-Jul-99 L3_13 84 56.12 -53.05 40 x 5-Jul-99 L3_18 90 58.20 -50.88 50 x x 6-Jul-99 L3_19 99 58.63 -50.42 45 x x 7-Jul-99 L3_25 111 60.29 -48.56 60 x x 8-Jul-99 L3_24 126 60.17 -48.68 60 x x 9-Jul-99 L3_17 137 57.82 -51.34 50 x x 10-Jul-99 Mooring 145 56.72 -52.48 40 x x 1275 11-Jul-99 Hamilton 152 54.08 -54.51 55 x Bank 12-Jul-99 NE-GSL#2 154 49.71 -58.41 40 x Table 5. Sampling for stable isotopes. c. Zooplankton Sampling L. Harris The zooplankton sampling is part of an ongoing program, the aim of which is to investigate the distribution, abundance and life history of the major zooplankton groups found in the Labrador Sea and its associated shelf systems. Particular emphasis is placed on the copepod species of the Calanus genus, which dominate the zooplankton in this region. Vertical net tows were taken at 42 stations (11 on or near the Scotian Shelf, 2 in the Gulf and 29 from the Labrador Shelf/Labrador Sea) using a 3/4 meter 200 um mesh ring net. At all stations, tows were made from 100 meters to the surface. Additional stratified deep tows (2500 meters to the surface) were taken at 7 of the stations (1 off the Scotian Shelf and 6 in the Labrador Sea) using a multinet. Samples will be analysed for species composition, copepod stage structure and biomass. Vertical net tow and multinet tow locations are shown in Figure 3*. d. Measurements Of Copepod Metabolic Rates L. Harris Respiration rates (CO2 production) of the copepod communities were determined at 7 stations in the Labrador Sea. Egg production rates of Calanus finmarchicus, the dominant copepod species, were measured at 6 stations in the Labrador Sea. Figure 3*. Net tow and multinet tow locations for 18HU99022/1. e. Dissolved Organic Carbon (DOC) and Jay Bugden / Microbial Community Respiration Paul Kepkay Samples for DOC profiles, size fractionation of DOC (ultrafiltration) and microbial community respiration were collected at 27 sites on the AR7W line (see Table 6). Ultrafiltration and rates of respiration of seawater samples were carried out at the time of collection (the ultrafiltration samples were frozen for later laboratory analysis), while samples for the DOC profiles were collected and frozen for later analysis. Station Respiration Ultrafiltration DOC Profile Site 1 (AR7W Line) X X X Site 2 X Site 3 X Site 4 X X X Site 5 X Site 6 X Site 7 X Site 8 X Site 9 X X X Site 10 X X X Site 11 X Site 12 X Site 13 X X X Site 14 X Site 15 X Site 16 X Site 17 X X X Site 18 X X X Site 19 X X X Site 20 X Site 21 X Site 22 X Site 23 X Site 24 X X X Site 25 X X X Site 26 X Site 27 X Table 6. Ultrafiltration, respiration and DOC sample collection. f. Primary Production Measurements Brian Irwin / Jeff Anning Photosynthesis Irradiance (PI) measurements were done at fourteen (14) stations - one at Louisbourg Line 3, two in the Gulf of St Lawrence, one on Hamilton Bank and ten on AR7W (Table 7). Water samples were collected from three depths in the upper 40 meters of the water column. Depth selection depended on the depth of the chlorophyll maximum and the shape of the chlorophyll profile. High Pressure Liquid Chromatography (HPLC) and Absorption Spectra samples were also collected at these depths. At seven of the PI stations on AR7W water column primary production was measured with C-14 at eight depths using deck incubators. These results will be compared with estimates of primary production measured with C-13 at the same depths. At all fourteen stations chlorophyll and CO2 samples were collected at 10 metre interval from 100m to surface where depth permitted. Station Operation ID Depth Latitude Longitude Date Label Number (N) (W) LL3 32 213544 10 45 29.06 59 30.50 29-Jun-99 LL3 32 213542 20 45 29.06 59 30.50 29-Jun-99 LL3 32 213538 50 45 29.06 59 30.50 29-Jun-99 Gulf 35 213563 10 49 44.99 59 23.65 30-Jun-99 Gulf 35 213561 20 49 44.99 59 23.65 30-Jun-99 Gulf 35 213558 40 49 44.99 59 23.65 30-Jun-99 AR7W 01 38 213585 10 53 40.76 55 32.95 01-Jul-99 AR7W 01 38 213582 20 53 40.76 55 32.95 01-Jul-99 AR7W 01 38 213579 40 53 40.76 55 32.95 01-Jul-99 AR7W 09 56 213723 10 55 16.06 53 58.60 02-Jul-99 AR7W 09 56 213721 20 55 16.06 53 58.60 02-Jul-99 AR7W 09 56 213718 30 55 16.06 53 58.60 02-Jul-99 AR7W 10 70 213788 10 55 25.07 53 49.82 03-Jul-99 AR7W 10 70 213786 20 55 25.07 53 49.82 03-Jul-99 AR7W 10 70 213784 30 55 25.07 53 49.82 03-Jul-99 AR7W 13 84 213884 10 56 05.00 53 03.87 04-Jul-99 AR7W 13 84 213882 20 56 05.00 53 03.87 04-Jul-99 AR7W 13 84 213879 30 56 05.00 53 03.87 04-Jul-99 Flo Thru 191944 4 57 53.75 51 13.23 05-Jul-99 AR7W 18 90 213975 10 58 12.80 50 53.76 05-Jul-99 AR7W 18 90 213973 20 58 12.80 50 53.76 05-Jul-99 AR7W 18 90 213969 40 58 12.80 50 53.76 05-Jul-99 AR7W 19 99 214023 10 58 38.05 50 25.84 06-Jul-99 AR7W 19 99 214021 20 58 38.05 50 25.84 06-Jul-99 AR7W 19 99 214018 40 58 38.05 50 25.84 06-Jul-99 AR7W 25 111 214135 10 60 18.14 48 34.45 07-Jul-99 AR7W 25 111 214133 20 60 18.14 48 34.45 07-Jul-99 AR7W 25 111 214129 40 60 18.14 48 34.45 07-Jul-99 AR7W 24 126 214244 5 60 10.76 48 34.45 08-Jul-99 AR7W 24 126 214239 10 60 10.76 48 34.45 08-Jul-99 AR7W 24 126 214236 20 60 10.76 48 34.45 08-Jul-99 AR7W 22 129 210502 0 59 45.06 49 10.01 08-Jul-99 AR7W 17 137 214359 10 57 49.81 51 21.18 09-Jul-99 AR7W 17 137 214355 30 57 49.81 51 21.18 09-Jul-99 AR7W 17 137 214353 40 57 49.81 51 21.18 09-Jul-99 Mooring 145 214428 10 56 43.47 52 28.83 10-Jul-99 Mooring 145 214426 20 56 43.47 52 28.83 10-Jul-99 Mooring 145 214424 30 56 43.47 52 28.83 10-Jul-99 Ham Bank 152 214449 10 54 04.98 54 30.91 11-Jul-99 Ham Bank 152 214447 20 54 04.98 54 30.91 11-Jul-99 Ham Bank 152 214445 25 54 04.98 54 30.91 11-Jul-99 Gulf 154 214463 5 49 24.75 58 24.49 12-Jul-99 Gulf 154 214461 10 49 24.75 58 24.49 12-Jul-99 Gulf 154 214459 20 49 24.75 58 24.49 12-Jul-99 Table 7. Sampling for primary production. g. Distribution of Microbial Plankton William Li Samples were collected from the CTD rosette for cryogenic preservation and for onboard shipboard flow cytometric enumeration of microbial plankton (Table 8). Plankton were fixed using 1% paraformaldehyde and then cryogenically stored in liquid nitrogen. These samples will be analyzed on shore for abundance of picophytoplankton, heterotrophic bacteria, and viruses. Picophytoplankton are detected on the basis of autofluorescence from chlorophyll a and from phycoerythrin. Heterotrophic bacteria and viruses are detected after staining with the nucleic acid binding fluorochrome SYBR Green 1. Preliminary examination using shipboard flow cytometry has revealed high abundances of heterotrophic bacteria (up to 3 million cells per millilitre) in the upper mixed layer of the central Labrador Sea. Event Station Cast Samples Cyro-storage Picophytoplankton Bacteria 7 Hfx-1 Shallow 9 X X 11 Hfx-2 Shallow 9 X X 15 Hfx-3 Shallow 13 X 19 Hfx-4 Shallow 8 X X 23 Hfx-5 Shallow 9 X X 25 Hfx-6 Shallow 8 X X 29 Hfx-7 Deep 23 X X 32 Louisburg-3 Shallow 14 X X 35 Shallow 10 X X X 38 L3-01 Shallow 14 X X X 40 L3-02 Shallow 12 X X 42 L3-03 Shallow 13 X X 44 L3-04 Shallow 11 X X 46 L3-05 Shallow 15 X 48 L3-06 Shallow 14 X 50 L3-07 Deep 18 X 52 L3-08 Deep 23 X 56 L3-09 Shallow 17 X X X 61 L3-09 Deep 18 X 68 L3-10 Deep 24 X X 70 L3-10 Shallow 16 X X X 73 L3-11 Deep 18 X 75 L3-12 Deep 22 X 80 L3-13 Deep 23 X X 84 L3-13 Shallow 17 X X X 88 L3-15 Deep 24 X 90 L3-18 Shallow 16 X X X 93 L3-18 Deep 24 X X 99 L3-19 Shallow 16 X X X 101 L3-19 Deep 24 X 104 L3-21 Deep 24 X 107 L3-23 Deep 15 X X 109 L3-23 Shallow 19 X X 111 L3-25 Shallow 12 X X X 119 L3-28 Shallow 6 X X 121 L3-27 Shallow 6 X X 123 L3-26 Deep 17 X X 126 L3-24 Shallow 11 X X X 127 L3-24 Deep 24 X X 132 L3-20 Deep 19 X X 133 L3-20 Shallow 15 X X 137 L3-17 Shallow 13 X X X 138 L3-17 Deep 24 X 140 L3-16 Deep 24 X X 145 M-1275 Shallow 15 X X X 152 HamiltonBank Shallow 14 X X X 154 GukfStLawr Shallow 10 X X X Table 8. Sampling for microbial plankton. h. Metals and Radioisotopes Sampling Program H. Edmonds, J. Dalziel, R. Nelson Samples for dissolved and particulate metals, isotopes and particulate organic carbon were collected at several stations during this expedition. The data will be used to determine the flux of particulate metals and particulate organic carbon (POC) in the Labrador Sea. The samples were collected from three sources: Challenger pumps, 12 litre Go-Flo bottles and CTD rosette bottles. The following is a description of the samples processed from each of the sampling sources. Figure 4 indicates the location of chemical sampling. Challenger Pump Sampling: The pumps were used at four stations (9, 13, 18 and 25) on the AR7W line to sample for dissolved/particulate metals, Thorium (234-Th) and POC. At each station, the pumps were deployed twice, to four depths (25, 50, 100, 250 m). One cast was deployed to sample for particulate and dissolved 234-Th and POC. The pumps were deployed again to the same depths to collect a particulate sample for metals, 230-Th and Protactinium (231-Pa). At all stations, the pumps were programmed to sample for 2 to 2.5 hours. While the Challenger pumps were deployed, a surface pumping system was deployed to 1-2 m to collect a corresponding sample from the surface. At station 18, sea and weather conditions prohibited the deployment of the surface pump. Go-Flo Sampling: At each of the four pumping stations, water samples were collected at matching depths i.e. surface, 25, 50, 100, 250 m for total mercury, dissolved - metals, 230-Th, and 231-Pa and particulate - metals, 230-Th, 231-Pa. The 12 litre Go- Flos were deployed on stainless steel hydrowire from the foredeck and subsampled in a clean area of the forward lab. All materials used to handle the water samples have been acid cleaned and all filter manipulations required on board were conducted in a positive air laminar flow "clean bench". Salinity and nutrient samples were collected from each Go-Flo as a check of the sampling depth. At stations 9 and 18, in addition to the sampling at the Challenger pump depths, the water column was also sampled at depths >250 m coincident with depths chosen for CTD samples. A total of 24 samples were collected for total Hg, 36 for dissolved/particulate metals and 32 samples each for 230-Th and 231-Pa. CTD Sampling: Water samples were collected from the CTD at 25 stations on the AR7W line. A total of 118 samples were collected for Iodine (129-I) from 25 stations and 8 samples for Technetium (99- Tc) at 4 stations. These samples were collected to measure the extent of the "Sellafield" reprocessing signal flowing in and out of the Labrador Sea. Samples for 230-Th and 231-Pa were also collected at 12 stations with a total of 80 samples collected for each of these isotopes. Figure 4*. Chemical sampling for 18HU99022/1. Red circles indicate I, Tc, Th, or Pa sampling from the rosette, while green triangles indicate Go-Flo, Challenger pump or surface pump sampling. 5. Major Problems and Goals Not Achieved none 6. Other Incidents of Note This was the first deep ocean cruise to use the recently acquired HP NT NetServers (Model LH3 PII 400). These servers have replaced the MicroVAX systems first used in 1986. The HP servers provide Science staff with 12 gigabytes of disk space, are mirrored internally and operate in parallel. Science backups on the servers were easy and rapid using the HP DAT tapes. This was also the first cruise to use the OSD Ocean Data and Information system (ODIN). ODIN is a shipboard database application for tracking and collecting the metadata and water sample data associated with an oceanographic cruise. ODIN was beta tested last year, during 18HU98023/1 in the Labrador Sea. The system was implemented on 99022 as an operational system. Our standard paper based system was maintained in parallel to ODIN. 7. List of Cruise Participants Name Responsibility Affiliation Jeff Anning Underway Sampling, photosynthesis BIO Jay Bugden DOC Levels, respiration rates BIO Allyn Clarke Senior Scientist BIO Pierre Clement Nutrients BIO John Dalziel Tracers BIO Jennifer Dixon CO2, CFC's, Alkalinity BDR Henrietta Edmonds Tracers URI Bob Gershey Scientist, CO2, CFC's, Alkalinity BDR Jean Hanley Helium, Tritium LDEO Les Harris Zooplankton, Net Tows BIO Glen Harrison Assistant Scientist BIO Albert Hartling Winch Room, moorings BIO Brian Irwin Primary Production BIO Anthony Isenor Data Manager BIO Jeffrey Jackson Computer Room BIO John Lazier Oxygens BIO Bill Li Bacterial abundance and activity BIO Richard Nelson Tracers BIO Tim Perry Zooplankton, Net Tows BIO Bob Ryan CTD Technician, Moorings BIO Murray Scotney Moorings, instrumentation BIO Igor Yashayaev Scientist BDR Frank Zemlyak Technician, CO2, CFC's, Alkalinity BIO BIO Bedford Institute of Oceanography PO Box 1006 Dartmouth, NS, B2Y 2A4 Canada BDR BDR Research Ltd. Box 652, Station 'M' Halifax, NS, B3J 2T3 Canada LDEO Lamont-Doherty Geological Observatory Columbia University Palisades, NY 10964 USA URI University of Rhode Island Graduate School of Oceanography South Ferry Road Narragansett, RI 02882 USA UW University of Washington Seattle, WA 98195 USA WHOI Woods Hole Oceanographic Institution Woods Hole, MA 02543 USA -------------------------------------------------------------------------------- B. UNDERWAY MEASUREMENTS 1. Navigation and Bathymetry Anthony W. Isenor The navigation system onboard CCGS Hudson consists of a differential GPS receiver and AGCNAV. The receiver also broadcasts navigation NMEA strings throughout the ship's network at about 1 Hz. The navigation data are then logged at one minute intervals on a PC. This PC was running the AGCNAV software package, a PC based display and waypoint setting software package, developed at the Atlantic Geoscience Centre at BIO. This software graphically displays ship position, waypoints, course, speed, etc. to the various science working areas. The echo sounder system used for collecting bathymetric data consisted of a Raytheon Line Scan Recorder, Model LSR 1811-2 (serial number A117) connected to a hull mounted 12kHz transducer. The transducer beam width is 15 degrees. The sweep rate of the record was adjusted throughout the course of data collection to aid in identifying the bottom signal. One transducer is positioned on a Ram that can be lowered or raised depending on conditions. When the ram is up, the waterline to transducer offset is 6 m. When the ram is down, the offset is 8 m. 2. Vessel Mounted Acoustic Doppler Current Profiler Murray Scotney The Hudson was equipped with a hull mounted RDI Acoustic Doppler Current Profiler (ADCP). The transducer (serial number 177) had VM ADCP electronics (serial number 607). Logging, using Transect software on a 486 PC, was started on June 27 at 1535 Z in Halifax Harbour. Two different configurations were used for logging. On the Halifax Line, 30 second averages were logged. From the Louisbourg Site (on July 29, 1999 at 1522 Z), 5 minute averages were logged. The configuration of the equipment results in a bin length of 4 metros and a total of 128 bins. The averaged data are stored to disk and backed up every few days. ADCP logging was stopped on July 13 at 2247 Z in Halifax Harbour. 3. Continuous Flow Multisensor Package (CFMP) Jeff Anning Water from approximately 4m was continuously pumped to the forward lab. The temperature, conductivity and fluorescence was measured and logged every 30 sec. Temperature and conductivity were measured with Seabird sensors and the fluorescence by a Wetlabs follow-through fluorometer. Incident Photosynthetically Active Radiation was measured with a Li-Cor Spherical Quantum Sensor and this data was merged with the sea water parameters. Exact time and positions were provided by a Northstar GPS and logged with the other data. In addition discrete water samples were collected every 15 minutes by an auto sampler for later analysis for nitrate and silicate. The computer also logged the time and position of these samples. 4. XBT and XCTD No probes were used. 5. Meteorological observations The ship's crew logged routine reporting of meteorological variables. 6. Atmospheric Chemistry There was no atmospheric chemistry program. * All figures shown in PDF file.