Abstract
Abstract. Topographic heterogeneity and lateral subsurface flow at the
hillslope scale of ≤1 km may have outsized impacts on tropical forest
through their impacts on water available to plants under water-stressed conditions. However, vegetation dynamics and finer-scale hydrologic
processes are not concurrently represented in Earth system models. In this
study, we integrate the Energy Exascale Earth System Model (E3SM) land model (ELM) that includes the Functionally Assembled Terrestrial Ecosystem Simulator (FATES), with a three-dimensional hydrology model (ParFlow) to
explicitly resolve hillslope topography and subsurface flow and perform
numerical experiments to understand how hillslope-scale hydrologic processes modulate vegetation along water availability gradients at Barro Colorado
Island (BCI), Panama. Our simulations show that groundwater table depth
(WTD) can play a large role in governing aboveground biomass (AGB) when
drought-induced tree mortality is triggered by hydraulic failure. Analyzing
the simulations using random forest (RF) models, we find that the
domain-wide simulated AGB and WTD can be well predicted by static
topographic attributes, including surface elevation, slope, and convexity, and adding soil moisture or groundwater table depth as predictors further
improves the RF models. Different model representations of mortality due to
hydraulic failure can change the dominant topographic driver for the
simulated AGB. Contrary to the simulations, the observed AGB in the
well-drained 50 ha forest census plot within BCI cannot be well predicted by
the RF models using topographic attributes and observed soil moisture as
predictors, suggesting other factors such as nutrient status may have a larger influence on the observed AGB. The new coupled model may be useful for
understanding the diverse impact of local heterogeneity by isolating the
water availability and nutrient availability from the other external and
internal factors in ecosystem modeling.
Cited by
10 articles.
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