Abstract

Abstract. Land surface models are important for improving our understanding of the Earth system. They are continuously improving and becoming better in representing the different land surface processes, e.g., the Community Land Model version 5 (CLM5). Similarly, observational networks and remote sensing operations are increasingly providing more data, e.g., from new satellite products and new in situ measurement sites, with increasingly higher quality for a range of important variables of the Earth system. For the optimal combination of land surface models and observation data, data assimilation techniques have been developed in recent decades that incorporate observations to update modeled states and parameters. The Parallel Data Assimilation Framework (PDAF) is a software environment that enables ensemble data assimilation and simplifies the implementation of data assimilation systems in numerical models. In this study, we present the development of the new interface between PDAF and CLM5. This newly implemented coupling integrates the PDAF functionality into CLM5 by modifying the CLM5 ensemble mode to keep changes to the pre-existing parallel communication infrastructure to a minimum. Soil water content observations from an extensive in situ measurement network in the Wüstebach catchment in Germany are used to illustrate the application of the coupled CLM5-PDAF system. The results show overall reductions in root mean square error of soil water content from 7 % up to 35 % compared to simulations without data assimilation. We expect the coupled CLM5-PDAF system to provide a basis for improved regional to global land surface modeling by enabling the assimilation of globally available observational data.

Highlights

  • The land surface forms the interface between the atmosphere and the lithosphere and plays a crucial role in the global climate system

  • We presented the newly coupled data assimilation framework Community Land Model version 5 (CLM5)-Parallel Data Assimilation Framework (PDAF)

  • The presented implementation can be summarized by the following three main aspects, which are discussed : the online variant of PDAF, re-use of CLM5 ensemble mode, and the Terrestrial System Modelling Platform (TSMP) framework

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Summary

Introduction

The land surface forms the interface between the atmosphere and the lithosphere and plays a crucial role in the global climate system. A growing number of soil moisture products from remote sensing has become available e.g., Soil Moisture and Ocean Salinity (SMOS) (Kerr et al, 2010), Soil Moisture Active Passive (SMAP) (Entekhabi et al, 2010), European Space Agency Climate Change Initiative (ESA-CCI) (Dorigo et al, 2017), which are used to improve the accuracy of land surface model predictions, e.g., of soil moisture, energy, and carbon fluxes, through data assimilation. Ling et al (2019) assimilated the Global Land Surface Satellite (GLASS) leaf area index (LAI) product into CLM4.0 using DART They showed that updating both model LAI and leaf C/N can reduce the largest bias from 5 m2/m2 by 1 m2/m2 and significantly improve LAI predictions especially in forested regions. We end with a discussion, conclusions, and an outlook on further planned improvements, for example concerning parameter updating

Model description
Ensemble Kalman filter
Parameter updating
Coupling CLM5 with PDAF
Study site
Soil water content – in situ measurements
Atmospheric forcings
Surface parameters
Simulation experiments
Comparison of the four different simulation setups
Findings
Discussion and conclusions
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