Abstract
The temporal sequence of hydrological fluctuations during the last 30 000 14C yr BP was reconstructed using published data from 198 lake basins between 41oS and 51oN. These data were coded at 1000-yr intervals in terms of lake status (an index of relative depth) and lake-level trend. The broad pattern of glacial/interglacial variations was established by aggregating the status/trend information from particular regions. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 118-129 |
| Number of pages | 12 |
| Journal | American Society of Mechanical Engineers (Paper) |
| Publication status | Published - 1984 |
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