Abstract

Crop simulation models can be used to estimate impact of current and future climates on crop yields and food security, but require long-term historical daily weather data to obtain robust simulations. In many regions where crops are grown, daily weather data are not available. Alternatively, gridded weather databases (GWD) with complete terrestrial coverage are available, typically derived from: (i) global circulation computer models; (ii) interpolated weather station data; or (iii) remotely sensed surface data from satellites. The present study's objective is to evaluate capacity of GWDs to simulate crop yield potential (Yp) or water-limited yield potential (Yw), which can serve as benchmarks to assess impact of climate change scenarios on crop productivity and land use change. Three GWDs (CRU, NCEP/DOE, and NASA POWER data) were evaluated for their ability to simulate Yp and Yw of rice in China, USA maize, and wheat in Germany. Simulations of Yp and Yw based on recorded daily data from well-maintained weather stations were taken as the control weather data (CWD). Agreement between simulations of Yp or Yw based on CWD and those based on GWD was poor with the latter having strong bias and large root mean square errors (RMSEs) that were 26–72% of absolute mean yield across locations and years. In contrast, simulated Yp or Yw using observed daily weather data from stations in the NOAA database combined with solar radiation from the NASA-POWER database were in much better agreement with Yp and Yw simulated with CWD (i.e. little bias and an RMSE of 12–19% of the absolute mean). We conclude that results from studies that rely on GWD to simulate agricultural productivity in current and future climates are highly uncertain. An alternative approach would impose a climate scenario on location-specific observed daily weather databases combined with an appropriate upscaling method.

Highlights

  • Anthropogenic greenhouse gas emissions are likely to modify climate in coming decades (Allen et al, 2000; Oreskes, 2004), and there is increasing concern about impact of climate change on food security (IPCC, 2007; Schmidhuber & Tubiello, 2007)

  • No previous studies have compared how these baselines may vary depending on source of the global weather data used in the analysis. To fill this knowledge gap, we evaluated how well currently available global gridded weather databases (GWD) perform when used as input for crop model estimates of yield potential (Yp) or Yw compared with similar simulations made with observed, high quality site-based weather data

  • Of particular note was the average upward bias of about 4.0 t haÀ1 for Yw of US maize estimated by CRU and National Aeronautics and Space Administration’s POWER database (NASA), and for Yp of rice in China by NCEP

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Summary

Introduction

Anthropogenic greenhouse gas emissions are likely to modify climate in coming decades (Allen et al, 2000; Oreskes, 2004), and there is increasing concern about impact of climate change on food security (IPCC, 2007; Schmidhuber & Tubiello, 2007). Most studies examining global impacts of climate change on crop yields have been based on derived, gridded weather databases (GWDs) that provide complete coverage of earth’s terrestrial surface Establishing research plots in every geographic area of interest to analyze effects of climate on crop production is difficult and cost prohibitive. For this reason agronomists turn to crop simulation models, which capture major interactions among crop genotype, Yield potential can be simulated using site-specific, observed weather data or gridded weather data. Values within a cell are typically derived by interpolating site-specific weather data based on coordinates of the sites within the grid and in nearest-neighbor grids, their distance from each other, elevation, and other variables (Hutchinson, 1995; Boer et al, 2001). Studies that have used gridded weather data to simulate Yp or Yw for a grid are rarely validated against Yp or Yw estimated using actual weather station data from a location within the same grid (Fischer et al, 2002; Foley et al, 2005; Lobell et al, 2008)

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