Impact of progressive global warming on the global-scale yield of maize and soybean
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Global surface temperature is projected to warm over the coming decades, with regional differences expected in temperature change, rainfall and the frequency of extreme events. Temperature is a major determinant of crop growth and development, affecting planting date, growing season length and yield. We investigated the effects of increments of mean global temperature warming from 0.5 °C to 4 °C on soybean and maize development and yield, both globally and for the main producing countries, and simulated adaptation through changing planting date and variety. Increasing temperature resulted in reduced growing season lengths and ultimately reduced yields for both crops. The global yield for maize decreased as temperature increased, although the severity of the decrease was dependent on geographic region. Small temperature increases of 0.5 °C had no effect on soybean yield, although yield decreased as temperature increased. These negative effects, however, were partly compensated for by the implementation of adaptation strategies including planting earlier in the season and changing variety. The degree of compensation was dependent on geographical area and crop, with maize adaptation delaying the negative effects of temperature on yield, compared to soybean adaptation which increased yield in China, India and Korea DPR as well as delaying the effects in the remaining countries. The results of this paper indicate the degree to which farmer-controlled adaptation strategies can alleviate the negative impacts of increasing temperature on two major crop species.
KeywordsAdaptation Strategy Maize Yield Sowing Date Crop Model Grow Season Length
There is now a high level of consensus that we live in a warming world. Recent studies have found compelling evidence that global temperatures are currently rising, with scientific consensus being unequivocal that the climate system is warming (Singh and Singh, 2015). The International Panel on Climate Change 5th Assessment Report (AR5) includes projected temperature increases for the year 2100 ranging from 0.9 °C to 5.4 °C depending on emissions scenario and climate model (Burkett et al., 2014). To inform climate mitigation policy decisions, evidence is needed of the possible impacts of various degrees of climate change.
Agriculture is one of the most climate-sensitive of human activities and global warming is predicted to have a large impact on yield, even when considering the uncertainty on rainfall projections. In particular, increases in average temperature alter physiological development stages. Warmer temperatures often result in a shortening of the growing season which reduces yield (Craufurd and Wheeler 2009), whilst brief periods of extreme temperatures can reduce the number of grains per spikelet which again reduces yield (Semenov et al., 2014). Historically, it has been challenging to investigate the impact of global climate on yield because the majority of crop simulation models have either required too much input data to be feasible at a global scale, or empirical models have been used whose output can not be extrapolated beyond their current environment (for example, they have not been able to take into account the effect of increased C02). Therefore, estimates of the likely impacts of climate change on crop production at a global scale were historically made by scaling-up the output of site studies (Rosenzweig and Parry 1994) or by aggregating individual studies on the basis of geography (IPCC 2007). However more recent studies including Osborne et al. (2013), Rosenzweig et al. (2013) and Arnell et al. (2014) have relied on smaller-scale studies. Such models have been used to investigate the impact of future temperatures on global or regional crop yield.
Maize is an established cereal crop that is extremely important for food security in developing countries, is the preferred staple for over 900 million poor consumers and is widely regarded as the most important staple food crop in Africa (CIMMYT, 2010). Soybean is one of the world’s major and fastest-expanding oilcrops, which contributes significantly to overall human nutrition in terms of both calorie and protein intake (Thoenes 2004). It is also extremely important in the processed food and animal feed industries.
Whilst the effects of climate change on maize and soybean have been studied previously, research has tended to focus on individual regions such as the North China Plain, Europe (Iglesias et al. 2012) and sub-Saharan Africa (Cairns et al. 2013). Whilst in some regions climate change positively affected yield of maize and soybean (Deryng et al. 2014), yield decreases are reported in others (Urban et al. 2011, Ray et al. 2012). Over larger geographical areas including China and the US, the overall yield has remained stable as a result of increases in yield in one area being balanced by decreases in yield in another area (Tao et al. 2012). Globally, therefore, it is important to understand the extent to which global yield will change and where these increases and decreases may occur.
There are many methods by which farmers might adapt their practices to a changing climate. Thus it is important to also examine the impact of adaptation strategies, particularly given that it has been found that in the short term, and with little financial input, autonomous adaptation may overcome the negative effects of climate change on yield (e.g. Lobell et al. 2008). Two of the suggested adaptation strategies include altering the sowing date and changing variety (Matthews et al. 1997), and there are several studies which suggest that either of these strategies might help to mitigate the impact of climate at a local or regional scale (Calvino et al. 2003; de Bruin and Pederson, 2008; Andrade, 1995; Fakorede 1985; Challinor et al. 2005; Miglietta et al. 2000 and Makadho 1996).
This paper introduces a methodology for estimating global maize and soybean yield for different levels of global temperature increases. The General Large Area Model for annual crops (GLAM) is a process-based crop model, developed for large-scale global studies (Challinor et al. 2004) and has previously been used to simulate soybean (Osborne et al., 2013, Arnell et al. 2014) and maize (Greatrex 2012, Watson et al. 2014). A pattern-scaling approach is described which provides climate scenarios consistent with prescribed increases in global temperature. The impacts of climate change under a range of global temperature increases from 0.5 °C to 4 °C, compared to 1961–1990, on regional and global maize and soybean yields are examined, along with the effects of autonomous adaptation strategies (changing variety and planting date).
There are a range of crop models for maize and soybean; however, in order to establish model effectiveness at predicting yield, it is important to determine how the responses of the models differ (Bassu et al., 2014). For example, the degree to which climate change may affect yield may differ between models, with some models predicting increases in yield whilst others predict decreases. By assessing the effect of climate change on crops using a range of crop models it may be possible to gain a consensus on the direction of change (positive or negative), if not the degree of change. This study is unique in assessing the impact of climate change on not only two crops, both at the global level, but also for the major production regions representing 75 % of the world’s maize production and 92 % of global soybean production.
2.1 Crop modelling
Crop yield was simulated using the General Large Area Model (GLAM) for annual crops (Challinor et al. 2004). This intermediate complexity process-based crop simulation model captures the non-linear interactions between climate and crop yield, but has few enough inputs that it can be run at spatial scales similar to global and regional climate models. Different crops are represented by changes to parameter values and by minor changes in parameterization. GLAM has been developed for a number of crops and will be used here for soybean (Osborne et al. 2013) and maize (Greatrex 2012, Watson et al. 2014). Reductions in yield are presented at % compared to the baseline data.
2.1.1 Crop parameters
GLAM was run using three varieties of maize and soybean, representing the two extremes of the photothermal time response and an intermediate variety. Geographic areas suitable for growing each variety were identified by a crop-suitability algorithm integrated as described by Osborne et al. (2013) with baseline and all future climate scenarios. Accumulated thermal time and precipitation values were calculated and compared against minimum thresholds related to each variety. The crop-suitability algorithm also determined the sowing date for the crop. Because the algorithm was integrated through the calendar year the derived sowing dates represent the earliest possible date - based on base temperature-for germination which might not be optimum for yield. For each crop variety, two GLAM simulations were performed: one run for a rain-fed crop and one for a fully-irrigated crop in which it was assumed that no soil water stress occurred.
2.1.2 Geographic scale
The spatial scale at which GLAM is run is dependent on the spatial scale of the input data (Challinor et al. 2004). In this study, as in Osborne et al. 2013, GLAM was applied over a global domain with input data at 0.5° spatial resolution. Soil-type information was derived from the ISRIC WISE database (Batjes 2005). The 0.5° resolution end-of-season yield output of GLAM was aggregated to national level using the observed area of each crop in the MIRCA2000 dataset (Portmann et al. 2010). Results are presented for the 10 major maize/soybean producing countries which represent 84 % and 94 % of the world’s maize and soybean production respectively (FAOSTAT 2015). For each country, total production was calculated by multiplying the 30-year mean yield at each grid point by the cultivated area, and national yield was calculated by dividing this national production by the total cultivated area over all grid cells in each country at which GLAM was run.
2.2 Climate scenarios
Daily weather data was derived from the University of East Anglia Climate Research Unit (CRU) TS3 dataset of Mitchell and Jones (2005). Under baseline (1961–1990) conditions the monthly data of maximum and minimum temperature, rainfall and cloud cover were interpolated to daily time-series using the method of Gosling and Arnell (2011). Future climates were derived using a pattern-scaling approach as described in Todd et al. (2011). In essence, pattern-scaling is based upon the assumption that changes in local (i.e. grid box) climate are linearly proportional to global mean temperature. Therefore, spatially-explicit future climates can be created by scaling patterns of local change by the global mean temperature rise. This method has been used in previous studies to derive future climates associated with a particular future time period under a particular greenhouse gas emission scenario (e.g. 2050 A1B in Osborne et al. 2013). In this study, the method was applied to generate future climates associated with prescribed levels of global warming, specifically increases of 0.5, 1.0, 1.5, 2.0, 2.5, 3.0 and 4.0 °C from the 1961–1990 average. Daily weather data to drive the crop model was interpolated from the monthly values. Because this approach essentially decouples the climate change scenarios from the emissions scenarios there are no specific associated concentrations of CO2 for each level of warming. Instead, a range is possible given the range of climate sensitivity observed for global climate models. Because CO2 concentration is a required input for GLAM a fixed value of 532 ppm (the level associated with the 2050s under the A1B greenhouse gas emissions scenario) was used for all future simulations. The climate model, including all relevant climate variables, used to determine the patterns of local climate change was HadCM3, a commonly-used climate model for impact assessments.
Limited autonomous adaptation was represented by altering variety and/or sowing date. Under each climate scenario as many of the three varieties of each crop as deemed suitable by the crop-suitability algorithm were simulated by GLAM. Therefore, one possible adaptation under changed climatic conditions would be to switch to a different variety from that which was highest-yielding under baseline climate conditions. The future climate simulations were performed both with the crop being sown on the date determined by the crop suitability algorithm under baseline conditions, and on the date determined when the algorithm was run for the future climate scenarios. Therefore, another possible adaptation could be to alter the sowing date of the crop. However, it is important to emphasise that the sowing date was never chosen to optimise yield. The yield simulation results are presented for two adaptation scenarios: No Adaptation, where sowing date and variety choice is fixed to that suitable in the baseline climate, and Adaptation, where sowing date and/or variety choice was allowed to vary from that suitable in the baseline climate.
4 Discussion and conclusions
Previous impact studies have shown that in mid- to high latitudes, temperature increases of 1–2 °C positively affect yield of maize, whilst temperature increases up to 5 °C had negative impacts (Parry et al., 2007). Although there was no clear correlation between latitude and temperature response in this study, yield response to climate change was dependent on country and crop. At the global level, Deryng et al. (2011) found that the yield of soybean and maize decreased in response to climate change, with decreases ranging from 15 to 30 % and 19 % - 34 % respectively. This is in line with the decreases found in this study, and the severity of the decrease confirms that soybean is less affected by temperature increases at the lower end of the scale compared to maize. Lobell and Gourdji (2012) predicted a yield reduction of 3–8 % for every 1 °C increase in temperature; however, our results suggest a more severe global reaction to increasing temperature for maize with temperature increases of 0.5 °C and 1 °C decreasing global maize yield by 10 % and 20 % respectively. With the addition of adaptation strategies the decrease in maize yield is in line with Lobell and Gourdji’s (2012) values. At country-level there are clear differences in maize yield with temperature increases of only 0.5 °C negatively affecting yield in USA, China, France and Italy. However, some countries are less affected, with a 2 °C increase reducing maize yield by 20 % compared to a 50 % reduction in France, South Africa and Ukraine. Contrary to Parry et al. (2007), no increase in global yield for maize was predicted regardless of the temperature increase. Similarly, for the top 10 producing countries no increase in yield was predicted. With the inclusion of adaptation strategies the yield of maize remained unchanged in response to a 0.5 °C temperature increase within 6 of the top 10 producing countries; however, greater temperature increases resulted in reduced yield. Contrary to previous research, there was no relationship between effect of temperature and the country being classified as either tropical or temperate. Our results are however consistent with the accepted view that adaptation strategies were much more effective for maize grown in temperate regions (Porter et al., 2014).
A temperature increase of 0.5 °C had no effect on soybean yield for the vast majority of the 10 top producing countries, although the only positive effect was predicted in India for temperature increases in excess of 3 °C. This is in contrast to Deryng et al. (2014), where an overall increase in yield was predicted globally. However, variation in response was found depending on climate model. Utilisation of adaptation strategies increased yield of soybean in China, India and Korea DPR and in a further 5 countries reduced the impact of increasing temperature. This is supported by Rosenzweig et al. (2013) who also reported an increase in soybean yield in response to increasing temperature through the use of adaptation strategies. However adaptation had no effect on soybean yield in Paraguay or Bolivia. Effectiveness of adaptation strategy was found to be increased in temperature rises less than 2 °C and where water was not limited (Howden et al., 2007). Our soybean results suggest adaptation can be effective at temperatures up to 4 °C but that response is country-dependent.
Adaptation strategies investigated included planting earlier in the season or changing crop variety, and results suggest these strategies resulted in a lower growing season temperature as the growing season started earlier in the year. For maize and soybean adaptation strategies yield decreases are at the lower end of the temperature scale and for soybean in specific geographical regions they resulted in yield increases. Crop development is directly related to temperature, therefore by sowing earlier in the season when temperatures are cooler, the rate of crop development will decrease, which allows more time for grain/pod filling and would therefore be expected to increase yield (Craufurd and Wheeler 2009).
Crop models are generally run on relatively small scales, with input data reflecting local agricultural practices, such as planting date, and meteorological inputs. In this and other recent studies, crop models have been applied over global domains to determine the impact of climate change on crop productivity at national, regional and global levels. Such application necessitates the making of simplifying assumptions regarding crop characteristics (such as variations in thermal time requirement) and management (such as planting date). Therefore, the results of this study should not be viewed as providing the evidence for local adaptation decisions but rather the potential impacts at aggregate scale of a range of global-warming scenarios. Adaptation strategies were included as some level of autonomous adaptation should be expected under changing environmental conditions.
The ability to examine the impacts of prescribed levels of global warming was permitted by the utilisation of a pattern-scaling technique for creating the climate scenarios. Pattern-scaling is reliant upon the linear response of local climate to global warming. The existence of such relationships has since been disputed (Cabre et al., 2010) but Mitchell (2003) argues that the errors are relatively small – globally 0.1 °C or 0.02 mm/day and not exceeding 0.3 °C or 0.3 mm/day for an individual grid box. A more specific caveat of the approach for crop impact studies is the de-coupling of atmospheric concentration of CO2 from the global warming response.
The results of this modelling study suggest that even small (0.5 °C) increases in temperature will have negative impacts on maize yield, the severity of which will increase with increasing temperature. Use of farmer-instigated adaptation strategies may alleviate the effects of a 0.5 °C warming; however, temperatures greater than 1 °C will negatively affect yield. Negative impacts of temperature are not demonstrated globally in soybean until warming increases to 1 °C, although this effect is country-specific, with 5 of the top 10 producing countries having reduced yield in response to 0.5 °C increases in temperature. Adaptation can promote yield at small temperature increases, and can off-set the negative impact until the temperature increases globally to 2 °C, however this response is also country-specific, with France demonstrating no decrease in yield under a 4 °C increase in temperature, whilst Brazil may demonstrate a decrease after a 1 °C temperature increase.
We would like to acknowledge the support of the Natural Environment Research Council for funding for the QUEST-GSI project.
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