Abstract
A comprehensive process-based numerical model of catchment hydrology and alluvial channel dynamics is applied to the evolution of the river Maas during the Last Glacial-Interglacial Transition. Palaeo-climatological reconstructions based on a number of climatic and environmental proxies are combined with atmospheric circulation model predictions to yield continuous time series for temperature, precipitation and vegetation cover for the period of 14-9
| Original language | English |
|---|---|
| Pages (from-to) | 2097-2110 |
| Number of pages | 14 |
| Journal | Quaternary Science Reviews |
| Volume | 22 |
| DOIs | |
| Publication status | Published - 2003 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 13 Climate Action
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