Date: Fri, 22 Jan 1999 19:09:03 GMT To: ALSUTHER@nsf.gov, KERB@nsf.gov, sanamowa@lmg.polar.org, asalmg@lmg.polar.org, mo-sciweekly@asa.org From: rossro@lmg.polar.org (Robin Ross) Subject: LMG Science Weekly Jan 11-17 Dear Colleagues, During the first 9 days of science operations for the Palmer LTER's annual summer cruise (Jan 9-17) we completed two of the five core transect lines, a total of 20 full stations. The two lines, the 500.* and 300.*, respectively 120 km and 320 km south of Anvers Island, run seaward from the inner shelf to about 200 km offshore (~ 3000 m deep). We also collected alongtrack data between each pair of stations and between the two lines for our analysis of determinants of spatial patterns, i.e. two complete on/offshore and one alongshore transect, each ~ 200 km long. The along track data include seabird distributions, bioacoustics (120 kHz), temperature, salinity, fluorescence, dissolved O2, CO2, pH and nitrate, with discrete samples taken at hourly intervals for nutrients and chlorophyll a. During the last 8 hr segment of the 200 km alongshore transect, which was in 3000 m deep water, we had to suspend collection of bioacoustic data due to the 18-25 ft swells. Our goal is to complete 3 stations a day when running the on/offshore transects. On two days during this time period we were only able to complete one station, once due to weather and 18-20 ft swells, and once due to a malfunction in the CTD that took most of the daylight hours to diagnose and fix. In addition, the spherical PAR collector on the CTD, the same sensor used in 98 January, is far less sensitive than anticipated, with a 36% error at the 1% light level for the most recent calibration. The relative insensitivity has been compounded by consistently overcast skies, and has complicated the timing of stations for optical measurements and primary productivity experiments. Some adjustments in the schedule have helped us avoid compromising these core data, but those adjustments create their own limitations on what we can accomplish. Complete results will not be available until the samples, frozen and preserved, are analyzed back at our respective home institutions. However, preliminary results suggest that bloom conditions are not present on the shelf at this time. Over most of the grid surveyed to date measurements of the bio-optical properties of the seawater have documented an optically clear water column. Chlorophyll a and primary productivity values have been low, close to baseline. The exceptions to this generality were the stations on the inner edge of the 500.* line in the Grandidier Channel where both chl a and primary productivity were elevated. However, surface waters have been undersaturated in CO2 relative to the atmosphere since leaving Palmer Station on Jan 8. Hydrogen peroxide concentrations are from 15-25 nM within the mixed layer and decrease with depth. Enzyme analysis shows glucosidase production rates to be low, while leucine aminopeptidase rates are much higher relatively at all stations sampled. =46or the higher trophic levels, salps and Antarctic krill have co-occurred at most stations on the shelf, with the exceptions of the stations in the Grandidier where only krill were found. Salps are abundant, with a maximum catch on these lines of 15 liters. However, the presence of salps is not limiting feeding and reproduction in krill. Spawning experiments have shown that female krill are spawning earlier at the outer stations of the 500.* line than in most of the previous 6 years. High seas and fog restricted observations of seabirds for the first few days of the cruise. While 20-30 knot winds made observations for penguins quite poor, sightings of wandering, gray headed, black browed, and light mantled sooty albatross were frequent. Ship followers have included southern fulmars, white chinned, cape, giant, antarctic, and snow petrels. On 19 January one of four giant petrels nesting near Palmer Station and fitted with a satellite transmitter was spotted from the bridge at 64=B0 27.375S and 65=B0 38.491W. This sighting is quite significant considering the low number of giant petrels fitted with transmitters this year, and will provide an accurate test of the Argos positions for this project. The level of support from both the ASA personnel and Captain Warren and his crew has been outstanding. The delays due to equipment malfunction and weather can be frustrating, but the quick and positive resolution to these problems has been appreciated. All field personnel are well, and work continues. Robin M. Ross (BP-028), Chief Scientist, and Field Team Leaders P. Duley (BP-013), W. Kozlowski (BP-016), K. Patterson (BP-032), L. Tupas (BP-046)