Options
Same soil, different climate: Crop model intercomparison on translocated lysimeters
ISSN
1539-1663
Date Issued
2022
Author(s)
Groh, Jannis
Diamantopoulos, Efstathios
Duan, Xiaohong
Ewert, Frank
Heinlein, Florian
Herbst, Michael
Holbak, Maja
Kamali, Bahareh
Kuhnert, Matthias
Gerke, Horst H.
Nendel, Claas
Priesack, Eckart
Steidl, Jörg
Pütz, Thomas
Vanderborght, Jan
Vereecken, Harry
Wallor, Evelyn
Weber, Tobias K. D.
Wegehenkel, Martin
Weihermüller, Lutz
DOI
10.1002/vzj2.20202
Abstract
Abstract
Crop model intercomparison studies have mostly focused on the assessment of predictive capabilities for crop development using weather and basic soil data from the same location. Still challenging is the model performance when considering complex interrelations between soil and crop dynamics under a changing climate. The objective of this study was to test the agronomic crop and environmental flux‐related performance of a set of crop models. The aim was to predict weighing lysimeter‐based crop (i.e., agronomic) and water‐related flux or state data (i.e., environmental) obtained for the same soil monoliths that were taken from their original environment and translocated to regions with different climatic conditions, after model calibration at the original site. Eleven models were deployed in the study. The lysimeter data (2014–2018) were from the Dedelow (Dd), Bad Lauchstädt (BL), and Selhausen (Se) sites of the TERENO (TERrestrial ENvironmental Observatories) SOILCan network. Soil monoliths from Dd were transferred to the drier and warmer BL site and the wetter and warmer Se site, which allowed a comparison of similar soil and crop under varying climatic conditions. The model parameters were calibrated using an identical set of crop‐ and soil‐related data from Dd. Environmental fluxes and crop growth of Dd soil were predicted for conditions at BL and Se sites using the calibrated models. The comparison of predicted and measured data of Dd lysimeters at BL and Se revealed differences among models. At site BL, the crop models predicted agronomic and environmental components similarly well. Model performance values indicate that the environmental components at site Se were better predicted than agronomic ones. The multi‐model mean was for most observations the better predictor compared with those of individual models. For Se site conditions, crop models failed to predict site‐specific crop development indicating that climatic conditions (i.e., heat stress) were outside the range of variation in the data sets considered for model calibration. For improving predictive ability of crop models (i.e., productivity and fluxes), more attention should be paid to soil‐related data (i.e., water fluxes and system states) when simulating soil–crop–climate interrelations in changing climatic conditions.
Crop model intercomparison studies have mostly focused on the assessment of predictive capabilities for crop development using weather and basic soil data from the same location. Still challenging is the model performance when considering complex interrelations between soil and crop dynamics under a changing climate. The objective of this study was to test the agronomic crop and environmental flux‐related performance of a set of crop models. The aim was to predict weighing lysimeter‐based crop (i.e., agronomic) and water‐related flux or state data (i.e., environmental) obtained for the same soil monoliths that were taken from their original environment and translocated to regions with different climatic conditions, after model calibration at the original site. Eleven models were deployed in the study. The lysimeter data (2014–2018) were from the Dedelow (Dd), Bad Lauchstädt (BL), and Selhausen (Se) sites of the TERENO (TERrestrial ENvironmental Observatories) SOILCan network. Soil monoliths from Dd were transferred to the drier and warmer BL site and the wetter and warmer Se site, which allowed a comparison of similar soil and crop under varying climatic conditions. The model parameters were calibrated using an identical set of crop‐ and soil‐related data from Dd. Environmental fluxes and crop growth of Dd soil were predicted for conditions at BL and Se sites using the calibrated models. The comparison of predicted and measured data of Dd lysimeters at BL and Se revealed differences among models. At site BL, the crop models predicted agronomic and environmental components similarly well. Model performance values indicate that the environmental components at site Se were better predicted than agronomic ones. The multi‐model mean was for most observations the better predictor compared with those of individual models. For Se site conditions, crop models failed to predict site‐specific crop development indicating that climatic conditions (i.e., heat stress) were outside the range of variation in the data sets considered for model calibration. For improving predictive ability of crop models (i.e., productivity and fluxes), more attention should be paid to soil‐related data (i.e., water fluxes and system states) when simulating soil–crop–climate interrelations in changing climatic conditions.
Core Ideas
We demonstrate the use of high precision weighable lysimeter for full model calibration and validation.
Lysimeter data from translocated soils represent effects of changing climatic conditions.
We compare calibration with blind forward simulations (fixed soil and calibrated crop parameter).
We compare individual crop model predictions with multi‐model mean.
We test the predictive ability of crop models and multi‐model mean.
We demonstrate the use of high precision weighable lysimeter for full model calibration and validation.
Lysimeter data from translocated soils represent effects of changing climatic conditions.
We compare calibration with blind forward simulations (fixed soil and calibrated crop parameter).
We compare individual crop model predictions with multi‐model mean.
We test the predictive ability of crop models and multi‐model mean.
File(s)
No Thumbnail Available
Name
VZJ2_VZJ220202.pdf
Size
4.54 MB
Checksum (MD5)
040505e936c23dc222fd820b84913ae4