Deep-water renewal and biological production in Lake Baikal
作者： R. F. Weiss , E. C. Carmack Carmack , V. M. Koropalov
DOI: 10.1038/349665A0
关键词: Maximum density 、 Oceanography 、 Temperate climate 、 Deep water 、 Nutrient 、 Ecology 、 Renewal theory 、 Fresh water 、 Bottom water 、 Carbon
摘要: The physics of mixing in deep temperate lakes is strongly constrained by the existence a temperature maximum density for fresh water; and pressure dependence that temperature. world's deepest lake well suited to study such deep-water renewal processes, also determination rates using time-dependent chemical tracers. mean biological recycling oxygen, carbon nutrients entire can then be determined.
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