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Published by means of the yankee Geophysical Union as a part of the Antarctic study Series.
The four million to twenty million sq. kilometers of sea ice that surrounds the Antarctic continent represents one of many greatest and so much dynamic ecosystems in the world. This sea ice matrix presents a habitat for a large choice of organisms, a few of which dwell their complete lives in the ice whereas others are just occasional viewers. huge grazers, reminiscent of copepods and krill which come to the ocean ice to feed, characterize vital hyperlinks among sea ice biota and the pelagic surroundings. regrettably, a result of inherent hassle of sampling such an atmosphere, many points of this exact habitat are nonetheless poorly understood. the aim of this quantity is to give new information regarding this environment in order that its function in the Antarctic food-web (and as a sink for carbon dioxide) and its susceptibility to environmental alterations could be greater understood.
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Extra resources for Antarctic Sea Ice: Biological Processes, Interactions and Variability
Results of the model show that the infiltration community in the Weddell Sea benefited greatly from this thicker snow cover since the resulting surface flooding ensured a greater nutrient supply and higher growth rates. Althoughsnowalsoreducedlight availability,the average snowdepthin the Weddell Sea was insufficientto seriouslyinhibit the algal growth,exceptin somemulti-year ice areas. nutrient limitation. 7. 75øS) are plotted together(Figure 7). When algal biomass was somewhat less than in the Ross Sea.
53 meters. 53 meters. 75 meters. Both multi-yearand first-yearice were initialized on et al. . The solid line refers to the estimates made after subdividingeachpixel into the nine grid pointsas describedin the text. The snow depth for each grid point was includedin the frequencydistribution. Over 1400 in situ measurements of snow thicknesswere made in the Weddell Sea during 1986, 1989, and 1992. October 1 with a uniform Chl a concentrationof 1 mg m-3,consistent with ice-coreobservations. 75 metersandaninitialChla concentration of 1 mgm'3.
Levitus, and T. P.
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