Abstract

Abstract. Land use and land cover change (LULCC) alter the biophysical properties of the Earth's surface. The associated changes in vegetation cover can perturb the local surface energy balance, which in turn can affect the local climate. The sign and magnitude of this change in climate depends on the specific vegetation transition, its timing and its location, as well as on the background climate. Land surface models (LSMs) can be used to simulate such land–climate interactions and study their impact in past and future climates, but their capacity to model biophysical effects accurately across the globe remain unclear due to the complexity of the phenomena. Here we present a framework to evaluate the performance of such models with respect to a dedicated dataset derived from satellite remote sensing observations. Idealized simulations from four LSMs (JULES, ORCHIDEE, JSBACH and CLM) are combined with satellite observations to analyse the changes in radiative and turbulent fluxes caused by 15 specific vegetation cover transitions across geographic, seasonal and climatic gradients. The seasonal variation in net radiation associated with land cover change is the process that models capture best, whereas LSMs perform poorly when simulating spatial and climatic gradients of variation in latent, sensible and ground heat fluxes induced by land cover transitions. We expect that this analysis will help identify model limitations and prioritize efforts in model development as well as inform where consensus between model and observations is already met, ultimately helping to improve the robustness and consistency of model simulations to better inform land-based mitigation and adaptation policies. The dataset consisting of both harmonized model simulation and remote sensing estimations is available at https://doi.org/10.5281/zenodo.1182145.

Highlights

  • Terrestrial vegetation regulates land–climate interactions through both biogeochemical and biogeophysical mechanisms

  • Land use and land cover change (LULCC) alters these biophysical properties and in turn affects the local climate through changes in the surface energy balance (Anderson et al, 2011; Bonan, 2008; Davin and de Noblet-Ducoudré, 2010; Lee et al, 2011; Mahmood et al, 2014; Pielke et al, 2011)

  • This study presents a framework for process-oriented model evaluation tailored towards analysing how local biophysical effects of vegetation cover change are represented in Land surface models (LSMs)

Read more

Summary

Introduction

Terrestrial vegetation regulates land–climate interactions through both biogeochemical and biogeophysical mechanisms. Changes in land cover, which are dominated by forest area loss, have a pronounced effect on climate by reducing the terrestrial carbon stocks (Canadell and Raupach, 2008). Land cover controls both radiative and non-radiative biophysical surface properties of vegetation that influence the water, momentum and energy budgets (Bonan, 2008). Land use and land cover change (LULCC) alters these biophysical properties and in turn affects the local climate through changes in the surface energy balance (Anderson et al, 2011; Bonan, 2008; Davin and de Noblet-Ducoudré, 2010; Lee et al, 2011; Mahmood et al, 2014; Pielke et al, 2011). The associated changes in biophysical properties may offset the intended biogeochemical effects of land-based mitigation (Betts, 2000). Policies tackling climate mitigation through land management focus only on biogeochemical mechanisms and neglect their biophysical consequences

Objectives
Methods
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call