| Title | Using geological history of the Laurentian Great Lakes to better understand their future |
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| Author | Lewis, C F M ;
Rea, D K; Hubeny, J B; Thompson, T A; Blasco, S M; King, J W; Reddin, M; Moore, T C, Jr. |
| Source | Aquatic Ecosystem Health and Management vol. 13, no. 2, 2010 p. 118-126, https://doi.org/10.1080/14634981003799950 |
| Image |  |
| Year | 2010 |
| Alt Series | Earth Sciences Sector, Contribution Series 20070274 |
| Publisher | Informa UK Limited |
| Document | serial |
| Lang. | English |
| Media | paper; on-line; digital |
| File format | pdf |
| Province | Ontario |
| Area | Great Lakes; Lake Ontario; Lake Huron; Lake Erie; Lake Michigan; Lake Superior; Canada; United States of America |
| Lat/Long WENS | -92.0000 -76.0000 49.5000 41.0000 |
| Subjects | hydrogeology; surficial geology/geomorphology; glacial history; deglaciation; limnology; lake sediments; lake water depths; lakes; lake water; hydrologic environment; Huron Basin; Quaternary |
| Illustrations | location maps; photographs; graphs; plots |
| Program | Enhancing resilience in a changing climate |
| Abstract | With growing use of numerical models to forecast lake conditions under future climates and other stressors, paleo-events in the history of the Great Lakes have greater potential for relevance. Past
events and history may extend records of observations, provide estimates of the sensitivity of the lake system to stressing conditions, and contribute scenarios for model validation. Here we describe four examples that hold promise for improving
understanding of the present and future Great Lakes: 1) using an event of lake closure to derive climate-hydrology sensitivity, 2) extending the record of lake-level history by examining beach ridge sequences, 3) investigating sedimentary black bands
to indicate past anoxia at the lakebed in deep basins, and 4) deriving evidence of lake process teleconnections with atmospheric circulation. |
| GEOSCAN ID | 224294 |
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