|
Hawaii Ocean Time-series (HOT)
in the School of Ocean and Earth Science and Technology at the University of Hawai'i at Manoa |
| » Home » Cruise Schedules, Reports & Cast Sheets » HOT-40 CS Report | |
HOT-40: Chief Scientist ReportChief Scientist: D. HEBELHOT 40 Cruise Report R/V Moana Wave 20-25 Sept. 1992 Personnel List: Dale Hebel Chief Scientist UH WOCE group: Fred Bingham Scientist UH Sean Kennan Graduate Student UH Rich Muller Technician UH JGOFS group: Ricardo Letelier Graduate Student UH John Dore Graduate Student UH Terry Houlihan Technician UH Chris Carrillo Technician UH Dan Sadler Graduate Student UH Ancillary projects Emerson's O2 project: Chuck Stump Technician UW Campbell's Picoplankton project: Hector Nolla Technician UH STAG: Ken Shultis Elect. Tech. Bradley Tolivar Deck Tech. Itinerary (approximate local time): ----------------------------------- Sunday, 20 Sept. 0900 Departed Snug Harbor 1130 Arrived Kahe Pt. (Sta. 1) 1600 Departed Kahe 1230 Arrived Aloha (Sta. 2) trap deployment site Monday, 21 Sept. 0200 Completed sediment trap array deployment 0400 Arrived Aloha (center of circle), began CTD time series Wednesday, 23 Sept. 0500 Completed Sta. 2 CTD operations 0900 Arrived Sta. 3 (23 25' N 158 W), conducted deep cast 1430 Departed Sta. 3, began Sean's CTD transect Thursday, 24 Sept. 0330 Began tow-yos 1100 Completed sediment trap retrieval and resumed CTD transect profiling 2100 Completed CTD transect profile Friday, 25 Sept. 0700 Arrived Snug Harbor Narrative: ---------- All aspects of the cruise went well with the exception of intermittent albeit persistent pylon problems. All samples were collected and we were able to maintain the cruise schedule. Just outside the harbor, during the abandon ship drill, we happened upon what appeared to be a surface accumulation of tricodesmium. The extent was not large and no obvious surface accumulation was present at Kahe. At Kahe we experienced problems with the transmissometer and fluorometer which necessitated aborting the first cast. The problem was found to be in the new transmissometer therefore we switched to the old one. We used this throughout the cruise however we need to determine what the problem is with new unit. We deployed the sediment traps in the usual location and headed for the center of the circle. Initial problems with the pinger temporarily delayed deployment of the deep cast. After retrieval it was noted that bottle S7 was missing both end caps and spring and that only 20 of the 23 bottles fired. We took a series of split samples for silica (refrigerated), spiked some other samples and took a large number of replicates from ~1400 m. These samples will be used to help resolve the nutrient problems observed periodically since HOT 33. All sampling has been going according to scheduling except for the interruption of the 3 hr CTD intervals due to the necessity to pump the ship's holding tanks. This caused a six hour hiatus since we needed to deploy the primary productivity array before daylight once we were back on station. I am unaware of a similar problem on other Wave cruises, therefore, we should ask the Captain if this type of operation can be completed before we arrive on station (center of circle), where the CTD time series takes place. I am assuming that if the tanks are empty they should have enough capacity for the 40-48 hrs we are on station. We continue to experience sporadic multiple bottle trips and general pylon problems. This resulted in a number of casts being repeated. Fortunately, water demand was not high on this cruise and there were enough casts to supply our needs. We have also ran a time course taking samples for low level phosphorus (llp), low level nitrate and nitrite (NOx), dissolved organic carbon (DOC) and pH from the 5 m niskin on all casts (at least those where we were reasonably confident that the bottle tripped at 5 m). In addition we took NOx samples at Kahe, ALOHA and station 3. It will be interesting to see if we observe any inshore-offshore gradient with the low level technique. The remainder of the cruise was occupied by Sean Kennan's CTD profiling and trap retrieval. We had been monitoring the drift track of the traps and uncharacteristically they traveled in a southwesterly direction. We had to curtail Sean's tow-yoing when we learned that the traps were nearing the middle of the Kaui channel. Fortunately, the tow-yoing was less interesting than anticipated so that activity was not resumed after the trap retrieval. However, Sean continued his profiling to just off Kahuku followed by a leisurely steam back to Snug Harbor. Weather: -------- The weather was good throughout the cruise with light winds, mostly sunny skies and calm seas during the first few days of the cruise. Toward the end the winds picked up to normal trades (10-20 kts) with concomitant seas. Skies remained relatively clear. Equipment and methods: ---------------------- All equipment used on HOT 40 was standard for past HOT cruises. All equipment function properly with the exception of the rosette pylon and new transmissometer. The only equipment lost was 2 end caps and teflon coated spring from one 12 l niskin on s2c1. Ancillary programs: ------------------- Investigator: Project: ------------- -------- Steve Emerson (UW) O2, respiration, and DO intercalibratin Charles Keeling (SIO) CO2 dynamics and intercalibration Paul Quay (UW) DIC13 dynamics (new production estimates) Lisa Campbell (UH) Picoplankton studies Students: --------- Ricardo Letelier Tricodesmium studies John Dore NH4, NO2 and NO3 dynamics Sean Kennan Intrusive salinity features Dan Sadler Time series pH measurements Others: ------- Amy Baylor (student) Seawater collection for Loihi plume comparison studies Ted Walsh (Prj Mgr Anly Svc) Seawater diluent collection Taro Takahashi pCO2 intercalibration (C. Winn P.I.) | |