TY - JOUR
T1 - Uncertainty of wheat water use
T2 - Simulated patterns and sensitivity to temperature and CO2
AU - Cammarano, Davide
AU - Rötter, Reimund P.
AU - Asseng, Senthold
AU - Ewert, Frank
AU - Wallach, Daniel
AU - Martre, Pierre
AU - Hatfield, Jerry L.
AU - Jones, James W.
AU - Rosenzweig, Cynthia
AU - Ruane, Alex C.
AU - Boote, Kenneth J.
AU - Thorburn, Peter J.
AU - Kersebaum, Kurt Christian
AU - Aggarwal, Pramod K.
AU - Angulo, Carlos
AU - Basso, Bruno
AU - Bertuzzi, Patrick
AU - Biernath, Christian
AU - Brisson, Nadine
AU - Challinor, Andrew J.
AU - Doltra, Jordi
AU - Gayler, Sebastian
AU - Goldberg, Richie
AU - Heng, Lee
AU - Hooker, Josh E.
AU - Hunt, Leslie A.
AU - Ingwersen, Joachim
AU - Izaurralde, Roberto C.
AU - Müller, Christoph
AU - Kumar, Soora Naresh
AU - Nendel, Claas
AU - O'Leary, Garry
AU - Olesen, Jørgen E.
AU - Osborne, Tom M.
AU - Priesack, Eckart
AU - Ripoche, Dominique
AU - Steduto, Pasquale
AU - Stöckle, Claudio O.
AU - Stratonovitch, Pierre
AU - Streck, Thilo
AU - Supit, Iwan
AU - Tao, Fulu
AU - Travasso, Maria
AU - Waha, Katharina
AU - White, Jeffrey W.
AU - Wolf, Joost
N1 - Publisher Copyright:
© 2016 Elsevier B.V.
PY - 2016/11/1
Y1 - 2016/11/1
N2 - Projected global warming and population growth will reduce future water availability for agriculture. Thus, it is essential to increase the efficiency in using water to ensure crop productivity. Quantifying crop water use (WU; i.e. actual evapotranspiration) is a critical step towards this goal. Here, sixteen wheat simulation models were used to quantify sources of model uncertainty and to estimate the relative changes and variability between models for simulated WU, water use efficiency (WUE, WU per unit of grain dry mass produced), transpiration efficiency (Teff, transpiration per kg of unit of grain yield dry mass produced), grain yield, crop transpiration and soil evaporation at increased temperatures and elevated atmospheric carbon dioxide concentrations ([CO2]). The greatest uncertainty in simulating water use, potential evapotranspiration, crop transpiration and soil evaporation was due to differences in how crop transpiration was modelled and accounted for 50% of the total variability among models. The simulation results for the sensitivity to temperature indicated that crop WU will decline with increasing temperature due to reduced growing seasons. The uncertainties in simulated crop WU, and in particularly due to uncertainties in simulating crop transpiration, were greater under conditions of increased temperatures and with high temperatures in combination with elevated atmospheric [CO2] concentrations. Hence the simulation of crop WU, and in particularly crop transpiration under higher temperature, needs to be improved and evaluated with field measurements before models can be used to simulate climate change impacts on future crop water demand.
AB - Projected global warming and population growth will reduce future water availability for agriculture. Thus, it is essential to increase the efficiency in using water to ensure crop productivity. Quantifying crop water use (WU; i.e. actual evapotranspiration) is a critical step towards this goal. Here, sixteen wheat simulation models were used to quantify sources of model uncertainty and to estimate the relative changes and variability between models for simulated WU, water use efficiency (WUE, WU per unit of grain dry mass produced), transpiration efficiency (Teff, transpiration per kg of unit of grain yield dry mass produced), grain yield, crop transpiration and soil evaporation at increased temperatures and elevated atmospheric carbon dioxide concentrations ([CO2]). The greatest uncertainty in simulating water use, potential evapotranspiration, crop transpiration and soil evaporation was due to differences in how crop transpiration was modelled and accounted for 50% of the total variability among models. The simulation results for the sensitivity to temperature indicated that crop WU will decline with increasing temperature due to reduced growing seasons. The uncertainties in simulated crop WU, and in particularly due to uncertainties in simulating crop transpiration, were greater under conditions of increased temperatures and with high temperatures in combination with elevated atmospheric [CO2] concentrations. Hence the simulation of crop WU, and in particularly crop transpiration under higher temperature, needs to be improved and evaluated with field measurements before models can be used to simulate climate change impacts on future crop water demand.
KW - Multi-model simulation
KW - Sensitivity
KW - Transpiration efficiency
KW - Uncertainty
KW - Water use
UR - http://www.scopus.com/inward/record.url?scp=84984823835&partnerID=8YFLogxK
U2 - 10.1016/j.fcr.2016.08.015
DO - 10.1016/j.fcr.2016.08.015
M3 - Article
AN - SCOPUS:84984823835
SN - 0378-4290
VL - 198
SP - 80
EP - 92
JO - Field Crops Research
JF - Field Crops Research
ER -