Soil Moisture Influence on Seasonality and Large-Scale Circulation in Simulations of the West African Monsoon
Open Access
- 1 April 2017
- journal article
- research article
- Published by American Meteorological Society in Journal of Climate
- Vol. 30 (7) , 2295-2317
Abstract
Prior studies have highlighted West Africa as a regional hotspot of land–atmosphere coupling. This study focuses on the large-scale influence of soil moisture variability on the mean circulation and precipitation in the West African monsoon. A suite of six models from the Global Land–Atmosphere Coupling Experiment (GLACE)-CMIP5 is analyzed. In this experiment, model integrations were performed with soil moisture prescribed to a specified climatological seasonal cycle throughout the simulation, which severs the two-way coupling between soil moisture and the atmosphere. Comparison with the control (interactive soil moisture) simulations indicates that mean June–September monsoon precipitation is enhanced when soil moisture is prescribed. However, contrasting behavior is evident over the seasonal cycle of the monsoon, with core monsoon precipitation enhanced with prescribed soil moisture but early-season precipitation reduced, at least in some models. These impacts stem from the enhancement of evapotranspiration at the dry poleward edge of the monsoon throughout the monsoon season, when soil moisture interactivity is suppressed. The early-season decrease in rainfall with prescribed soil moisture is associated with a delayed poleward advancement of the monsoon, which reflects the relative cooling of the continent from enhanced evapotranspiration, and thus a reduced land–ocean thermal contrast, prior to monsoon onset. On the other hand, during the core/late monsoon season, surface evaporative cooling modifies meridional temperature gradients and, through these gradients, alters the large-scale circulation: the midlevel African easterly jet is displaced poleward while the low-level westerlies are enhanced; this enhances precipitation. These results highlight the remote impacts of soil moisture variability on atmospheric circulation and precipitation in West Africa.Keywords
Funding Information
- National Science Foundation (AGS-1331375)
- National Science Foundation (AGS-1505198)
This publication has 70 references indexed in Scilit:
- Role of inertial instability in the West African monsoon jumpJournal of Geophysical Research: Atmospheres, 2015
- Interannual Coupling between Summertime Surface Temperature and Precipitation over Land: Processes and Implications for Climate Change*Journal of Climate, 2015
- Impact of Soil Moisture–Atmosphere Interactions on Surface Temperature DistributionJournal of Climate, 2014
- Forced Sahel rainfall trends in the CMIP5 archiveJournal of Geophysical Research: Atmospheres, 2013
- Irrigation induced surface cooling in the context of modern and increased greenhouse gas forcingClimate Dynamics, 2010
- Delayed Sahel rainfall and global seasonal cycle in a warmer climateGeophysical Research Letters, 2009
- Soil Moisture Feedbacks to Precipitation in Southern AfricaJournal of Climate, 2006
- The impact of decadal‐scale Indian Ocean sea surface temperature anomalies on Sahelian rainfall and the North Atlantic OscillationGeophysical Research Letters, 2003
- Generation of the African Easterly Jet and Its Role in Determining West African PrecipitationJournal of Climate, 1999
- Dynamics of Wet and Dry Years in West AfricaJournal of Climate, 1996