Abstract

Land surface/ecosystem models (LSEMs) play a key role in understanding the Earth’s climate. They represent ecosystem dynamics by simulating fluxes occurring between the biosphere and atmosphere. However, for a correct flux simulation, it is critical to calibrate the model using robust and state-of-the-art calibration techniques. In this work, we optimize parameters of the Integrated Model of Land Surface Processes (INLAND) using the hierarchical multi-objective calibration method (AMALGAM) to improve the representation of surface processes in a natural ecosystem over the Pampa biome in South America. The calibration was performed using experimental data of energy and CO2 flux collected in a native field located in southern Brazil. We compared simulations using the default and calibrated parameter set. The results show that the calibration of the model significantly improved all fluxes analyzed. The mean errors and bias values were significantly reduced, and the seasonality of fluxes was better represented. This work is one of the first to apply a multi-objective calibration in an LSEM to represent surface fluxes in the Pampa biome, presenting a consistent set of parameters for future applications used in studies of biome land use and land cover.

Highlights

  • Studies on interactions between the land surface and atmosphere are fundamental to understanding the Earth’s climate

  • We used AMALGAM to estimate parameters that will improve the performance of the Integrated Model of Land Surface Processes (INLAND) model to represent land surface processes of the natural vegetation in the Pampa biome of southern Brazil

  • We improve the representation of surface processes that occur in the Pampa biome through the use of a hierarchical and multi-objective calibration applied to the INLAND model

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Summary

Introduction

Studies on interactions between the land surface and atmosphere are fundamental to understanding the Earth’s climate In this context, the land surface and ecosystem models (LSEMs) play an important role to simulate fluxes and complex processes occur between the land surface and atmosphere [1,2]. To simplify the spatiotemporal representation of these processes, values of parameters are obtained for a single site that is characterized by a particular vegetation class or plant functional type (PFT) and extrapolated to an entire region with the same PFT [6,7]. This set of parameters is called default parameters. The LSEM models must be carefully calibrated to minimizing errors in different regions regarding the local complexity of the soil, vegetation, and climatology

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