Abstract

Abstract. Soil is an important regulator of Earth system processes, but remains one of the least well-described data layers in Earth system models (ESMs). We reviewed global soil property maps from the perspective of ESMs, including soil physical and chemical and biological properties, which can also offer insights to soil data developers and users. These soil datasets provide model inputs, initial variables, and benchmark datasets. For modelling use, the dataset should be geographically continuous and scalable and have uncertainty estimates. The popular soil datasets used in ESMs are often based on limited soil profiles and coarse-resolution soil-type maps with various uncertainty sources. Updated and comprehensive soil information needs to be incorporated into ESMs. New generation soil datasets derived through digital soil mapping with abundant, harmonized, and quality-controlled soil observations and environmental covariates are preferred to those derived through the linkage method (i.e. taxotransfer rule-based method) for ESMs. SoilGrids has the highest accuracy and resolution among the global soil datasets, while other recently developed datasets offer useful compensation. Because there is no universal pedotransfer function, an ensemble of them may be more suitable for providing derived soil properties to ESMs. Aggregation and upscaling of soil data are needed for model use, but can be avoided by using a subgrid method in ESMs at the expense of increases in model complexity. Producing soil property maps in a time series still remains challenging. The uncertainties in soil data need to be estimated and incorporated into ESMs.

Highlights

  • Soil or the pedosphere is a key component of the Earth system, and plays an important role in water, energy, and carbon balances and other biogeochemical processes

  • Soil information is required by land surface models (LSMs), which are a component of Earth system models (ESMs)

  • The soil datasets derived by digital soil mapping provide grid-based spatially continuous estimation, while the soil datasets derived by the linkage method provide estimations with abrupt changes at the boundaries of soil polygons

Read more

Summary

Introduction

Soil or the pedosphere is a key component of the Earth system, and plays an important role in water, energy, and carbon balances and other biogeochemical processes. An accurate description of soil properties is essential in modelling the capability of Earth system models (ESMs) to predict land surface processes at the global and regional scales (Luo et al, 2016). Y. Dai et al.: A review of the global soil property maps incorporated the depth-to-bedrock data into a land surface model using variable soil layers instead of the previous constant depth. ESMs usually incorporate soil property maps (i.e. horizontal spatial distribution) for multiple layers rather than a global constant or a single layer. Can be incorporated into ESMs. The prediction of changing soil properties can be performed by digital soil mapping using the changing climate and land use as covariates.

Global and national soil datasets
Soil dataset incorporated into ESMs
Estimating secondary parameters using PTFs
Comparison of available global soil datasets
Model use of soil data derived by the linkage method
Upscaling detailed soil data for model use
The changing soil properties
Incorporating the uncertainty of soil data into ESMs
Layer schemes and lack of deep layer soil data
Findings
Summary and outlook
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