Abstract
This paper analyzes the impact of climate, crop production technology, and atmospheric carbon dioxide (CO2) on current and future crop yields. The analysis of crop yields endeavors to advance the literature by estimating the effect of atmospheric CO2 on observed crop yields. This is done using an econometric model estimated over pooled historical data for 1950–2009 and data from the free air CO2 enrichment experiments. The main econometric findings are: 1) Yields of C3 crops (soybeans, cotton, and wheat) directly respond to the elevated CO2, while yields of C4 crops (corn and sorghum) do not, but they are found to indirectly benefit from elevated CO2 in times and places of drought stress; 2) The effect of technological progress on mean yields is non-linear; 3) Ignoring atmospheric CO2 in an econometric model of crop yield likely leads to overestimates of the pure effects of technological progress on crop yields of about 51, 15, 17, 9, and 1 % of observed yield gain for cotton, soybeans, wheat, corn and sorghum, respectively; 4) Average climate conditions and climate variability contribute in a statistically significant way to average crop yields and their variability; and 5) The effect of CO2 fertilization generally outweighs the effect of climate change on mean crop yields in many regions resulting in an increase of 7–22, 4–47, 5–26, 65–96, and 3–35 % for yields of corn, sorghum, soybeans, cotton, and wheat, respectively.
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Notes
In the FACE experiments, air enriched with CO2 is blown into the rings where crops are grown in the real field (not in the chamber). Then, a computer-control system uses the wind speed and CO2 concentration information to adjust the CO2 flow rates to maintain the desired CO2 concentration. Finally, crop yield in the elevated CO2 rings are compared to that in the control rings with non-elevated CO2 (ambient) environment. Details of the FACE experiments are provided in Long et al. (2006).
The ENSO events, which are associated with differing sea-surface temperatures (SSTs) patterns between the eastern equatorial Pacific and the southern Pacific (Southern Oscillation Index, SOI), is an important controlling factors in global interannual climate variability (Hastenrath 1995; Phillips et al. 1999) and in crop yields (e.g., Hansen et al. 1998).
For robustness, the observational data were tested for unit roots, although after we pooled the observational and FACE data, our data does not fully have a panel data structure. Using a Fisher-type test (Choi 2001) and a Levin-Lin-Chu test (Levin et al. 2002) test, all series except CO2, which is I(1), are stationary in the level, I(0). However, after we apply the panel unit root tests to the residuals we find it is stationary in the level, I(0), implying that our model might not have the problem of spurious regression (Granger 1981). We thank Dr. David Bessler, Texas A&M University, for his useful suggestion on how to approach this testing.
The log-likelihood function of equation (1) is:
\( l\mathrm{nL}=-\frac{1}{2}\left[\mathrm{n}* \ln \left(2\uppi \right)+{\displaystyle \sum_{\mathrm{i}=1}^{\mathrm{n}} \ln \left(\mathrm{h}{\left({\mathrm{X}}_{\mathrm{i}},\upalpha \right)}^2\right)+{\displaystyle \sum_{\mathrm{i}=1}^{\mathrm{n}}\frac{{\left({\mathrm{y}}_{\mathrm{i}}-\mathrm{f}\left({\mathrm{X}}_{\mathrm{i}},\upbeta \right)\right)}^2}{\mathrm{h}{\left({\mathrm{X}}_{\mathrm{i}},\upalpha \right)}^2}}}\right] \) under the assumption that yi ~ N(f(Xi, β), h(Xi, α)2) and εi ~ N(0, 1).
The PDSI is a standardized measure of surface moisture conditions, ranging from about -10 to +10 with negative values denoting dry conditions and positive values indicating wet conditions (Palmer 1965).
We thank Dr. Chi-Chung Chen, National Chung-Hsing University, Taiwan for his useful suggestion regarding the selection of ENSO phases.
We thank Dr. Bruce A. Kimball from USDA-ARS, Arid-Land Agricultural Research Center, Arizona; Dr. Donald R. Ort; Dr. Lisa Ainsworth; and Dr. Andrew Leakey from University of Illinois at Urbana Champaign in providing us the FACE experimental datasets.
To derive these estimates we fix all other independent variables at their 2008 levels and vary time and the CO2 concentration variable from the 1950 to 2100 levels.
The A1B scenario reflects a move away from fossil fuel reliance with lower emissions than today’s levels but less reduction than in the more optimistic B1 and B2 scenarios. For our time frame (2050) the choice of SRES scenarios does not make much difference as emissions and climate change implications of different SRES scenarios do not diverge significantly as noted in The citation “IPCC (2007a)” (original) has been changed to “IPCC (2007a)”. Please check if appropriate.IPCC (2007a).
Timmermann et al. (1999) produce estimates that the El Nino phase will shift from occurring 23.8 % of the time to 33.9 % of the time, while La Niña phase will shift from 25 to 31 %, and Neutral from 51.5 to 35.1 %.
In Long et al. (2006) and Leakey (2009), as atmospheric CO2 increases from about 367 to 550 ppm, yields of wheat, soybeans, and C-4 crop are projected to increase 13, 14, and 0%, respectively, while chamber studies find that yields of wheat, soybeans, and C-4 crop are forecasted to increase 31, 32, and 18%, respectively.
For a definition of the regions see note 1 on Table 5.
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Attavanich, W., McCarl, B.A. How is CO2 affecting yields and technological progress? A statistical analysis. Climatic Change 124, 747–762 (2014). https://doi.org/10.1007/s10584-014-1128-x
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DOI: https://doi.org/10.1007/s10584-014-1128-x