Shifting westerlies and precipitation patterns during the Late Pleistocene in southern Africa determined using glacier reconstruction and mass balance modelling

Keyphrases

• Late Pleistocene 100%
• Glacier 100%
• Southern Africa 100%
• Glacier Reconstruction 100%
• Glacier Mass 100%
• Mass Balance Modelling 100%
• Precipitation Pattern 100%
• Snow 66%
• Small Glaciers 66%
• Last Glacial Maximum 66%
• Glaciation 66%
• Lesotho Highlands 66%
• Glacial Period 33%
• Subcontinent 33%
• Palaeoglacier 33%
• Radiation Index 33%
• Climatic Envelope 33%
• Equilibrium Line Altitude 33%
• Index Modelling 33%
• High-resolution Climate Model 33%
• Flow Dynamics 33%
• High Altitude 33%
• Temperature Variation 33%
• Seasonal Timing 33%
• Mass Balance 33%
• Climatic Regimes 33%
• Topographic Shading 33%
• Temperature Depression 33%
• Steady-state Mass-balance 33%
• Climate Change 33%
• Climatic Conditions 33%
• Environmental Change 33%
• Mass Flow 33%
• Drakensberg 33%
• Balanced Dynamics 33%
• Summer Months 33%
• Cold Fronts 33%
• Paleoclimate 33%
• Last Glacial Cycle 33%
• South Africa 33%
• Change in Precipitation 33%
• Palaeoprecipitation 33%
• Moisture Availability 33%
• Northward Shift 33%
• Modern Analogue 33%
• Temperature Radiation 33%
• Highly Sensitive 33%

Earth and Planetary Sciences

• Last Glacial Maximum 100%
• Lesotho 100%
• Southern Africa 100%
• Mountains 100%
• Late Pleistocene 100%
• Climate Change 50%
• Cold Front 50%
• Seasonality 50%
• Paleoclimate 50%
• Altitude 50%
• Republic of South Africa 50%
• Shading 50%
• Environmental Change 50%
• Continent 50%
• Last Glacial 50%
• Equilibrium Line 50%
• Climate Modeling 50%