Abstract

Advances in climate science have rendered obsolete the gridded observation data widely used in downstream applications. Novel climate reanalysis products outperform legacy data products in accuracy, temporal resolution, and provision of uncertainty metrics. Consequently, there is an urgent need to develop a workflow through which to integrate these improved data into biological analyses. The ERA5 product family (ERA5 and ERA5-Land) are the latest and most advanced global reanalysis products created by the European Center for Medium-range Weather Forecasting. These data products offer up to 83 essential climate variables at hourly intervals for the time-period of 1981 to today with preliminary back-extensions being available for 1950–1981. Spatial resolutions range from 30 × 30 km (ERA5) to 11 × 11 km (ERA5-Land) and can be statistically downscaled to study-requirements at finer spatial resolutions. Kriging is one such method to interpolate data to finer resolutions and has the advantages that one can leverage additional covariate information and obtain the uncertainty associated with the downscaling. The KrigR R-package enables users to (a) download ERA5(-Land) climate reanalysis data for a user-specified region, and time-period, (b) aggregate these climate products to desired temporal resolutions and metrics, (c) acquire topographical co-variates, and (d) statistically downscale spatial data to a user-specified resolution using co-variate data via kriging. KrigR can execute all these tasks in a single function call, thus enabling the user to obtain any of 83 (ERA5)/50 (ERA5-Land) climate variables at high spatial and temporal resolution with a single R-command. Additionally, KrigR contains functionality for computation of bioclimatic variables and aggregate metrics from the variables offered by ERA5(-Land). This R-package provides an easy-to-implement workflow for implementation of state-of-the-art climate data while avoiding issues of storage limitations at high temporal and spatial resolutions by providing data according to user-needs rather than in global data sets. Consequently, KrigR provides a toolbox to obtain a wide range of tailored climate data at unprecedented combinations of high temporal and spatial resolutions thus enabling the use of world-leading climate data through the R-interface and beyond.

Highlights

  • CLIMATE DATA NEEDS IN THE 21ST CENTURY With the onset of the Anthropocene, the numerous fields of study that investigate the effects of climate change require spatially and temporally consistent climate data at high spatial and temporal resolutions (Hewitt, Stone, & Tait, 2017; Bjorkman et al, 2018; Trisos, Merow, & Pigot, 2020)

  • CLIMATE REANALYSES MEET DEMANDS Climate reanalysis products represent a major achievement of climate science (Buizza et al, 2018). They meet the demand for high temporal resolutions and abundance of self-consistent climatic information criteria. These products optimally combine a wide range of surface and satellite observations with a dynamical model in order to produce a self-consistent dataset which includes all essential climate variables (ECVs) (Sabater, 2017; Hersbach et al, 2020) effectively eliminating the need for retrieval of data from a multitude of climate products for a full picture of environmental conditions

  • Third-party data can be introduced to the workflow to use the functionality of KrigR on any spatial product with any co-variate as supplied by the user. This is important for two reasons: (1) applicability of kriging has been demonstrated for non-climate spatial products (Bruelheide et al, 2018) and users might want to downscale other climatic data sets than ERA5(-Land), (2) flexibility in choice of co-variates allows for accurate downscaling of a variety of climate variables and other spatial products

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Summary

INTRODUCTION

CLIMATE DATA NEEDS IN THE 21ST CENTURY With the onset of the Anthropocene, the numerous fields of study that investigate the effects of climate change require spatially and temporally consistent climate data at high spatial and temporal resolutions (Hewitt, Stone, & Tait, 2017; Bjorkman et al, 2018; Trisos, Merow, & Pigot, 2020). They meet the demand for high temporal resolutions and abundance of self-consistent climatic information criteria (see Table 1) These products optimally combine a wide range of surface and satellite observations with a dynamical model in order to produce a self-consistent dataset which includes all essential climate variables (ECVs) (Sabater, 2017; Hersbach et al, 2020) effectively eliminating the need for retrieval of data from a multitude of climate products for a full picture of environmental conditions. Due to increased data accuracy, temporal resolution, provision of data uncertainty metrics, and number of climate variables provided, ERA5-products are arguably the most appropriate climate data products for macroecological studies

LIMITATIONS
STATISTICAL DOWNSCALING
USING THE KRIGR TOOLBOX
FUTURE DIRECTIONS
CONCLUSIONS
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