Related Experiment Video
Updated: Mar 27, 2026

In Situ Soil Moisture Sensors in Undisturbed Soils
Published on: November 18, 2022
Decadal-scale droughts disrupted the African Humid Period in the Sahara
Florence Sylvestre1, Martin Melles2, Volker Wennrich2
1Centre de Recherches et d'Enseignement en Géosciences de l'Environnement (CEREGE), Aix-Marseille Université, CNRS, IRD, INRAE, Aix-en-Provence, France. sylvestre@cerege.fr.
The African Humid Period experienced decadal droughts around 9.3 and 8.2 kyr BP. These African droughts were linked to North Atlantic freshwater pulses weakening the Atlantic Meridional Overturning Circulation.
Area of Science:
- Paleoclimatology
- Climate Dynamics
- African Climate History
Background:
- The early and mid-Holocene featured the African Humid Period (AHP), a wet phase in the Sahara and Sahel.
- The AHP, spanning from 14.8 kyr BP to 6.0 kyr BP, was marked by a significant humid interval but also experienced poorly dated short droughts.
- Understanding the precise timing and duration of these droughts is crucial for reconstructing past climate variability.
Purpose of the Study:
- To identify and precisely date decadal-scale droughts during the African Humid Period.
- To investigate the environmental impact of these droughts on the Lake Yoa region.
- To explore the teleconnections between African climate and North Atlantic circulation changes.
Main Methods:
- Analysis of a multiproxy time series from the annually layered sedimentary archive of Lake Yoa, Chad.
- Utilizing pollen, diatom, leaf-wax isotopes, and geochemical source area indicators.
- Employing climate simulations to link observed drought events with potential large-scale climate drivers.
Main Results:
- Identification of two decadal-scale droughts at approximately 9.3 kyr BP and 8.2 kyr BP, with a possible third at 6.3 kyr BP.
- Evidence of reduced local precipitation and fluvial supply during the 8.2 kyr BP drought, leading to lake-level drop and shoreline vegetation changes.
- Climate simulations suggest the 8.2 kyr BP drought was a rapid response to a weakened Atlantic Meridional Overturning Circulation (AMOC) due to North Atlantic freshwater input.
Conclusions:
- The African Humid Period was punctuated by significant decadal droughts, notably around 9.3 and 8.2 kyr BP.
- The 8.2 kyr BP drought event demonstrates a clear teleconnection between North Atlantic climate dynamics (AMOC weakening) and hydroclimate variability in the African Sahel.
- These findings highlight the sensitivity of African climate to abrupt climate shifts and underscore the need for improved decadal climate predictions.
More Related Videos
09:23JenaTron - An Experimental Approach to Study the Effects of Plant History and Soil History on Grassland Ecosystem Functioning
Published on: March 21, 2025
12:26Integrating Remote Sensing with Species Distribution Models; Mapping Tamarisk Invasions Using the Software for Assisted Habitat Modeling SAHM
Published on: October 11, 2016
Related Concept Videos
Global Climate Change
Responses to Drought and Flooding
What is Climate?
Ecological Disturbance
Threats to Biodiversity
Disorder of Water Balance
Dehydration
Dehydration occurs when the body loses fluids (particularly water).
Causes:
The major causes of dehydration include excessive sweating, fever, vomiting, diarrhea, and diuresis.
Signs and Symptoms:
Symptoms primarily include intense...