11 April, 2000
LTER Phytoplankton Group; Part 3
Question 52: Does Antarctica have any mountains?
Continued from 4/10...
The LTER group is looking at phytoplankton because it is the base of the food web here. Phytoplankton doesn't eat; it produces its own food. Krill and other zooplankton eat phytoplankton. In turn, they support the large animals of the area. Based on the amount of time each water sample takes to filter, there are many fewer phytoplankton lower in the water column. The bloom has ended now. The last two days the group went out on Bruiser there was nothing in the water. The field season is set up to encompass the bloom, from early November to the end of March.
Besides the photosynthetic rate experiments, the LTER group also looks at the chemistry of the water and some of its bio-optic properties. The CTD instrument pack they deployed from Bruiser has instruments that measure water temperature, conductivity, density and depth. Data is collected from satellite observations and automatic weather stations to assist in prediction of sea-ice formation: sea ice extent, sea surface temperatures, ozone concentration, ocean color, cloud coverage and basic weather statistics. The LTER has automatic weather stations on three islands on the Antarctic Peninsula.
Part of the work the group was doing during March was a comparison of two light-intensity measuring buoys. Natacha Bernier was involved with this; she came down from Dalhousie University in Halifax, Nova Scotia. She is currently working towards her masters in oceanography, and their degree program requires a certain amount of field research time. Natacha says she likes the equality of Palmer, for example, staff and science clean the kitchen and station together. Also, Antarctica is a place she has always wanted to go. Both buoys record light intensity in the water column compared to light intensity at the surface. Visible light wave lengths are in the range of 400-770 nm (nanometers). In the metric scale micro is 1000 times smaller than milli, and nano is 1000 times smaller than micro. The buoys record the light intensity at each wave length band or channel. The buoy Natacha was sent down to test measures 256 channels. Kirk's buoy, that the LTER has been using, measures only 13 channels but does have a profiler that shows how light changes with depth. In water with phytoplankton, light is lost more quickly. Natacha's buoy was modified to work off several 12-volt batteries, but would need still more power to profile (the downside of her buoy is that it is a power hog). Water absorbs red light and phytoplankton absorb blue light; so, the more phytoplankton, the greener the ocean. By measuring the light intensities along the visible light spectrum both at the surface and in the water column, the buoys tell the group how much energy is available for phytoplankton and how much phytoplankton is present.
We had to abort our dive today. At lunch there was a brief window when the wind went down. We rushed into our gear and took the boat out towards DeLaca Island. Part way out, the wind started to pick up again, no treat with large waves blowing into your face! By the time we got to the site and started donning our gear, it was hard to stand in the boat because of the swells. Several of our group (including the tender from the station) are prone to seasickness, and we were all feeling miserable. We didn't call off the dive until we were fully in our gear and it had started to sleet on us. Katrin and I lay on the floor of the boat with tanks, masks, fins and BCs on all the way back to the station. The winds had picked up to 35 knots while we were out.
Answer 51: The coldest temperature recorded in Antarctica (and in the world!) was -89.2 degrees C (-128.6 degrees F) at Vostok, one of the Russian bases, in July 1983.
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