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Agricultural and Forest Meteorology
journal homepage: www.elsevier.com/locate/agrformet
Climate change impact on Mexico wheat production
Ixchel M. Hernandez-Ochoa
a
, Senthold Asseng
a,
⁎
, Belay T. Kassie
a,b
, Wei Xiong
a,d
,
Ricky Robertson
c
, Diego Notelo Luz Pequeno
d
, Kai Sonder
d
, Matthew Reynolds
d
, Md Ali Babar
e
,
Anabel Molero Milan
d
, Gerrit Hoogenboom
f
a
Department of Agricultural and Biological Sciences, University of Florida, FL 32611, USA
b
DuPont Pioneer, 8650 NW 62nd Avenue, Johnston, IA, 50131, USA
c
International Food Policy Research Institute, Washington, DC, 20006-1002, USA
d
International Maize and Wheat Improvement Center, Apdo. Postal 6-641, 06600, D.F, Mexico
e
Department of Agronomy, University of Florida, FL, 110965, USA
f
Institute for Sustainable Food Systems, Frazier Rogers Hall, University of Florida, Gainesville, FL, 32611, USA
ARTICLE INFO
Keywords:
Triticum
Model ensemble
Crop simulation model
Uncertainty
ABSTRACT
Wheat is one of the most important cereal crops in Mexico, but the impact of future climate change on pro-
duction is not known. To quantify the impact of future climate change together with its uncertainty, two wheat
crop models were executed in parallel, using two scaling methods, five Global Climate Models (GCMs) and two
main Representative Concentration Pathways (RCPs) for the 2050s. Simulated outputs varied among crop
models, scaling methods, GCMs, and RCPs; however, they all projected a general decline in wheat yields by the
2050s. Despite the growth-stimulating effect of elevated CO
2
concentrations, consistent yield declines were
simulated across most of the main wheat growing regions of Mexico due to the projected increase in tempera-
ture. Exceptions occurred in some cooler areas, where temperature improved sub-optimal conditions, and in a
few areas where rainfall increased, but these increases only provided negligible contributions to national pro-
duction. Larger and more variable yield declines were projected for rainfed wheat due to current and projected
spatial variability of temperature and rainfall patterns. Rainfed wheat, however, only contributes about 6% of
Mexico’s wheat production. When aggregating the simulated climate change impacts, considering temperature
increase, rainfall change, and elevated atmospheric CO
2
concentrations for irrigated and rainfed wheat cropping
systems, national wheat production for Mexico is projected to decline between 6.9% for RCP 4.5 and 7.9% for
RCP 8.5. Model uncertainty (combined for crop and climate models) in simulated yield changes, and across two
scaling methods, was smaller than temporal and spatial variability in both RCPs. Spatial variability tends to be
the largest in both future scenarios. To maintain or increase future wheat production in Mexico, adaptation
strategies, particularly to increasing temperatures affecting irrigated wheat, or expanding the cropping area, will
be necessary.
1. Introduction
Wheat is one of the major cereal crops in the world because of its
importance as a main source of energy and protein in human diets
(Curtis et al., 2002). In Mexico, wheat is among the top five produced
crops: national production during the 2015–2016 season was 3.8 mil-
lion tons (around $750 million value), cultivated on 720,000 ha
(SAGARPA, 2016b). Production is concentrated in Sonora, Baja Cali-
fornia, Sinaloa, Guanajuato, and Michoacán states, which together re-
present about 86% of the total national production (SAGARPA, 2016a).
More than 90% of the produced wheat is irrigated due to the arid and
semi-arid climate in most of the wheat production area. Rainfed wheat
production is typical of the high elevation areas in the central and
southern states and Mediterranean-type climate in Baja California,
where winter and spring temperature and rainfall are more suitable for
the cropping system (Escobar, 2014).
Past global temperature trends already show the effects of warming
temperatures on wheat production. Historical wheat yield analysis
showed a 5.5% global decline in aggregated wheat production since
1980, as a result of increased global mean temperature (Lobell et al.,
2011). In Mexico, Asseng et al. (2014) reported warming decadal trends
in Obregon (Sonora) and Toluca (Mexico State) of 0.46 and 0.27 °C,
https://doi.org/10.1016/j.agrformet.2018.09.008
Received 16 March 2018; Received in revised form 7 September 2018; Accepted 10 September 2018
⁎
Corresponding author. Current address: Department of Agricultural and Biological Sciences, University of Florida, FL 32611, USA.
E-mail address: sasseng@ufl.edu (S. Asseng).
Agricultural and Forest Meteorology 263 (2018) 373–387
0168-1923/ © 2018 Elsevier B.V. All rights reserved.
T