4.2 Article

Soil Carbon Losses Reduce Soil Moisture in Global Climate Model Simulations

Journal

EARTH INTERACTIONS
Volume 26, Issue 1, Pages 195-208

Publisher

AMER METEOROLOGICAL SOC
DOI: 10.1175/EI-D-22-0003.1

Keywords

Atmosphere-land interaction; Anthropogenic effects/forcing; Biosphere-atmosphere interaction; Climatology; Soil moisture; Water budget/balance

Funding

  1. NASA Modeling, Analysis, and Prediction program [80NSSC21K1497]

Ask authors/readers for more resources

The losses of soil organic carbon in agricultural soils have significant impacts on regional hydroclimate, including reductions in soil moisture, water holding capacity, and infiltration. Therefore, restoring soil organic carbon is important for improving hydrology and climate change mitigation.
Most agricultural soils have experienced substantial soil organic carbon losses in time. These losses motivate recent calls to restore organic carbon in agricultural lands to improve biogeochemical cycling and for climate change mitigation. Declines in organic carbon also reduce soil infiltration and water holding capacity, which may have important effects on regional hydrology and climate. To explore the regional hydroclimate impacts of soil organic carbon changes, we conduct new global climate model experiments with NASA Goddard Institute for Space Studies ModelE that include spatially explicit soil organic carbon concentrations associated with different human land management scenarios. Compared to a no land use case, a year 2010 soil degradation scenario, in which organic carbon content (OCC; weight%) is reduced by a factor of similar to 0.12 on average across agricultural soils, resulted in soil moisture losses between 0.5 and 1 temporal standard deviations over eastern Asia, northern Europe, and the eastern United States. In a more extreme idealized scenario where OCC is reduced uniformly by 0.66 across agricultural soils, soil moisture losses exceed one standard deviation in both hemispheres. Within the model, these soil moisture declines occur primarily due to reductions in porosity (and to a lesser extent infiltration) that overall soil water holding capacity. These results demonstrate that changes in soil organic carbon can have meaningful, large-scale effects on regional hydroclimate and should be considered in climate model evaluations and developments. Further, this also suggests that soil restoration efforts targeting the carbon cycle are likely to have additional benefits for improving drought resilience.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.2
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available