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Application of temperature, water stress, CO2 in rice growth models
Rice volume 5, Article number: 10 (2012)
In recent decades, numerous studies have attempted to project the impact of hypothesised anthropogenic climate change on rice production. In this study, we offer a comprehensive review of our current understanding related to temperature, CO2, and water-demand parameters in rice growth models. As to future rice yield, night time temperature should be focused in the models as well as day time temperature owing to the contribution of temperature on the night time respiration. Furthermore, although CO2-enhanced photosynthesis is critical for the accurate prediction of rice production in a higher CO2 atmosphere, we found that recent well-developed photosynthesis-stomatal model cannot realize the variation of CO2 stomatal sensitivity with humidity conditions. To estimate water stress under projected climate-change conditions, rice growth model should be required to link with water resource model, which includes natural processes and anthropogenic regulations. The understanding of abilities and limitations in the models is important not only to improve the schemes that models employ, but to also critically review the simulated results.
Rice is the most important staple food for a large part of the world’s population, especially in East and South Asia, the Middle East, Latin America, and the West Indies ([FAO, 2005]). As the population increases rapidly in these regions ([Coats, 2003]; [Bloom, 2011]), the demand for rice will grow to an estimated 2000 million metric tons by 2030 ([FAO, 2002]). To supply to this increasing demand, the methods of rice production will require significant improvement ([Ainsworth, 2008]). Achieving this goal, however, is sure to be a challenge with respect to future climatic changes ([Matthews et al., 1997]), which will basically be characterized by current global warming trends (Fischer et al., ). The rise in temperatures and levels of carbon dioxide and uncertain rainfall associated with climate change may have serious adverse effects either directly or indirectly on the growth, development, and yield of rice crops ([Lobell et al., 2011]).
In recent decades, numerous studies have attempted to project the impact of hypothesised anthropogenic climate change on rice production ([Long et al., 2005, 2006]; [Tubiello et al., 2007]; [Ziska and Bunce, 2007]). Rice growth models are routinely used for assessing the impact of diverse agro-environmental changes on rice growth and yield ([Spitters et al., 1989]). Statistical models (e.g., [Kandiannan et al., 2002]; [Lobell and Burke, 2008]; [Auffhammer et al., 2012]) based on multiple regression analysis of historical yields and weather data are useful tools to estimate the impacts of climate trends upon rice yields. However, it becomes difficult to use the statistical models to examine the direct or indirect impacts of climate change in the good management of a rice paddy field ([Wang et al., 1991]), because the data reflected in the model contains the human effort being made to mitigate environmental shocks (negative effects) in order to maintain a high level of production. In addition, statistical models do not fully account for the physiological responses of rice to the unexpected and not-yet-experienced agri-environments that will result from dramatic climate change ([Lobell and Burke, 2008]). The results obtained will, thus, not enable us to fully understand how climate change will affect future food availability.
Increasing concern about the sustainable management of environmental resources and the effects of climate change on rice production has triggered the development of a number of sophisticated models based on physical and physiological processes ([van Laar et al., 1992]; [de Vries FWT et al. 1989]; [Kropff et al. 1993]; [Matthews and Hunt, 1994]). Process-based rice growth models of varying degrees of complexity can benefit from a comprehensive assessment of the response to likely climate changes ([Lansigan et al., 1997]; Bouman and Tuong, ). As part of an effort to mimic a complex agrosystem, knowledge from experiments in both the field and laboratory will be incorporated into process-based models, using novel parameters and improved schemes. However, although these models are currently the best method available ([Bouman and Tuong, 2001]), they still rely on imperfect mechanistic processes and weak assumptions. Furthermore, these problems will not be solved even if a model includes all the parameters selected for an agricultural system, because the systems we are modelling are extremely complex. However, if we can demonstrate that certain parameters and schemes in a model are insignificant, then we can omit them to create a better and simpler model for good performance. Therefore, it is critically important to know which parameters will be the most significant for estimating rice productivity in the future environment.
With the current situation of global warming under the human-induced climate change, knowledge of the effects of (1) temperature, (2) CO2, and (3) water demand on the growth and development of rice crops has become essential over the past few years. In this study, we offer a comprehensive review of our current understanding related to temperature, CO2, and water-demand parameters. Our expectation is that this will be of significant use in understanding the development of the models for the prediction of future situations.
Effects of temperature on rice yield
The impact of air temperature on rice growth would be location-specific because of the different sensitivity of different locations with regard to temperature. In tropical regions, the temperature increase due to the climate change is probably near or above the optimum temperature range for the physiological activities of rice ([Hogan et al., 1991]; [Baker et al. 1992]). Such warming will thus reduce rice growth. In addition, higher temperatures will cause spikelet sterility owing to heat injury during panicle emergence ([Satake and Yoshida, 1978]). In temperate regions, increased air temperatures should hasten rice development, thereby shortening the time from transplanting (or direct seeding) to harvesting and reducing the total time for photosynthesis yield development ([Neue and Sass, 1994]). Similarly, in high latitude regions, atmospheric warming may also increase the duration of the rice growing season. Therefore, a location-specific-parameterized rice model is not appropriate for modelling future environments globally ([Shimono et al., 2008]).
Although air temperature has conventionally been considered in the physiological processes of rice, the parameter of leaf temperature is more significant from the perspective of the energy balance on the leaf level, photosynthesis, and transpiration ([Morison and Gifford 1984]; [Lasseigne et al., 2007]). Therefore, the differences between leaf temperature and air temperature can create a significant uncertainty with regard to the season length and yield ([Baker et al., 1990]). For example, leaf temperatures could be warmer than the air owing to soil-surface influences, particularly in humid regions, which would result in a more rapid yield than that by air temperatures. The difference of 1°C will cause the change of leaf respiration by as much as approximately 1% of gross photosynthesis ([Mebrahtu et al., 1991]). However, only a few models calculate leaf temperature separately from air temperature, owing to the difficulty of parameterization of the related environmental factors. Basically, leaf temperature corresponds to air temperature ([Harley et al., 1985]). In addition, the temperature of an illuminated leaf is elevated by an amount proportional to the ratio of the incident radiation to a convention coefficient (e.g., humidity, wind speed, etc.) ([O’Toole and Tomar, 1982]). Therefore, a model requires the estimation of leaf temperature, using relevant mechanistic processes, in order to simulate the response of rice to changes in climatic variables.
Recent observation of climate variability shows an increase in the global mean surface air temperature, and a decrease in the diurnal temperature range ([Easterling et al., 1997]; [Braganza et al., 2004]; [Makowski et al., 2008]). This conclusion is derived from the fact that the daily minimum temperature is increasing at a faster rate than the daily maximum owing to the large specific heat of water, particularly in rice-growing areas ([Welcha et al. 2010]). Accordingly, in recent rice studies, attention has been directed to the effect of the daily minimum (night time) temperature. [Peng et al. (2004]), using field experiment data from 1979 to 2003, showed that yield might be more sensitive to the daily minimum temperature than to the daily maximum. The negative relationship between rice yield and daily minimum temperature is derived from the elevated specific dark respiration that takes place during the night time.
Indeed, the reported yields of maize, wheat, and soybeans cannot be fully understood by the relation of respiration to increased night time temperature ([Peng et al., 2004]). Nevertheless, the yield might be explained by their acclimation of crop dark respiration at higher temperatures, and the relationship between dark respiration and the previous daytime’s photosynthesis. The clear relationship between rice yield and daily minimum temperature implies that in a rice growth model, the physiological mechanisms of specific dark respiration are a priority in order to explain the effects of a warming atmosphere on the rice yield. Therefore, the simulation time-step should actually be on a less-than-daily scale, and the respiration scheme should be calculated separately from the estimation of the gross photosynthesis. However, models have mostly employed a daily time-step and have used a rather simple net calculation of the net photosynthesis, particularly for the estimation of future rice yield because the temperature projected by climate model still has sparse time scale. The possible overestimation of rice yield should thus be considered when discussing the simulated future yield.
Interactive responses to increased CO2
Atmospheric CO2 has been increasing at a rather steady rate, at least on the time scale of a decade. During the last 50 years it has increased exponentially at a rate of approximately 2.4% per year. For this reason, there is continued interest in how rice will respond to future increases in CO2, since rice uses CO2 in its photosynthesis and growth. Most agronomic models use the magnitude of CO2 fertilization factor, which is mostly based on data from three literature reviews from the 1980s ([Kimball 1983]; [Cure and Acock 1986]; Allen et al. ). According to laboratory experiments, rice grown at a higher CO2 level has more tillers than rice grown at an ambient level of CO2. Furthermore, the suppression of rice-specific dark respiration at high CO2 levels has been observed, despite the large variations in observed outputs ([Amthor 1991]; [Imai et al. 1992]; [Poorter et al. 1992]), and the physiological metabolism of nutrients in rice will become more critical under higher CO2 conditions.
According to previous enclosure experiments that have contributed to the physiological schemes used in rice growth models, the grain yield of rice will be promoted by higher CO2 levels. These studies, however, were probably conducted in the absence of other limiting factors. For example, [Long et al. (2006]) found that the photosynthesis stimulated in a rice free-air concentration enrichment (FACE) experiment is four times lower than the elevated CO2-enhanced value that is expected in enclosure studies. Given this circumstance, the most important scientific question is which physiological behaviours and environmental factors offset the direct fertilization effect of a rise in CO2 ([Harley et al., 1985]).
Indeed, positive performance under elevated CO2 would be directly associated with four key parameters: a decreased stomatal aperture, enhanced photosynthetic activity, increased total biomass, and changed biomass partitioning. The reduced stomatal aperture would produce an increased rice canopy temperature as a result of suppressed transpiration. It can thus mediate negative feedback in a warmed atmosphere. Despite a small stomatal aperture, CO2-enhanced photosynthesis will be produced by a rise in the intercellular CO2 concentration under a higher level of atmospheric CO2 ([Mott 1988]). However, following long-term subjection to a higher CO2 level, the net leaf photosynthetic rate of rice often declines from the expected value ([Imai and Murata 1978]; [Peet 1986]). This process is called the acclimation of rice photosynthesis to higher CO2. Although this acclimation is difficult to realize in a rice growth model because its mechanism remains unclear, the acclimation scheme of an effect that is in contrast to elevated CO2-enhanced photosynthesis might be critical for the accurate prediction of rice production in a higher CO2 atmosphere ([Makino et al., 1997]). In addition, considering the increased rice biomass that is produced in a higher CO2 atmosphere, which takes place through the increased photosynthesis and the decreased respiration, it is important for the process of biomass allocation to be accounted for in order to investigate these factors’ possible significance in a rice growth model. Previous measurement studies showed that specific leaf weight often increases in a higher CO2 atmosphere as a result of the thicker leaves and the increased number and length of the crown roots that are produced. However, the contribution of the changed leaf area or root biomass to the rice yield remains unclear.
Although the response of rice growth to elevated CO2 is critically associated with other environmental factors, the interactive effects of simultaneous change have not been well investigated either in modelling studies or in experimental measurements. For example, few studies have mentioned the different sensitivity of stomatal behaviour to vapour pressure deficit (VPD) in terms of elevated atmospheric CO2 concentrations (Bunce 1998, 2001); [Katul et al. 2009]). Indeed, stomata, which are the strategic juncture for CO2 and water exchange between plant and atmosphere, are strongly linked not only to CO2 concentration, but also to the humidity as an atmospheric demand for moisture. The measurement data in [Bunce (1998, 2001]) shows that the ratio (gs_700/gs_350) of stomatal conductance at 700 μmol mol-1 to that at a concentration of 350 μmol mol-1 CO2 is negatively correlated with VPD to a significant degree (see Figure 1). However, according to our sensitivity test, one current well-developed model, which was proposed by [Collatz et al. (1991)] and which uses the biochemical photosynthesis model of [Farquhar et al. (19800] as well as the stomatal conductance model of ([Ball et al. 1987)], could not realize this actual behaviour (see Table 1 for formula). Basically, their coupled photosynthesis-stomatal conductance model can represent accurate stomata behaviours in response to CO2 and VPD under controlled conditions. Therefore, it is possible that failure of the model with regards to the interactive performance of CO2 and humidity can cause uncertainties as to the future rice yield and water demand, given the close linkage between the two processes in the two photosynthetic and stomatal schemes.
Consideration of water stress and demand in models
Rice cultivation is suited to regions with high rainfall because it requires ample water. However, it is expected that the hydrological cycle accelerated by a warmed atmosphere will change the pattern of rainfall in these regions. Basically, rice is very sensitive to a reduction in soil moisture, and rice production consumes much more water than the production of other crops. Approximately 500 L of water is required to produce 1 kg of biomass ([Jodo et al. 1995]). This high degree of water consumption is related to diverse physiological processes in rice. The transpiration that is reduced under stressful water conditions will result in the suppression of nutrient uptake by the rice root system. The reductions in leaf expansion and in the photosynthetic rate that result from moderate water deficits are responsible for a reduction in dry matter production and grain yield ([Gifford 1979]). Furthermore, drought during the flowering stage causes spikelet sterility and yield losses, particularly in upland areas ([Ekanayake et al., 1993]). These direct effects of water stress on numerous metabolic and physiological processes in rice are relatively well established in models, mostly using optimal trends obtained from field or laboratory experiments.
The difference between leaf and air temperatures is commonly used as an indicator of rice water stress ([Long et al., 2006]), because leaf temperature is more strongly correlated with transpiration than with photosynthesis. This implies that a shortage of water produces two important physiological responses: in leaf temperature and in transpiration. Water stress in combination with a warmed atmosphere will increasingly limit rice production owing to a much higher leaf temperature ([Garrity and O’Toole, 1994]). In addition, although water stress will simply result in stomatal closure, as in the case of elevated CO2 levels, the effects and possible interaction of elevated CO2 and water stress on rice stomatal behaviour are a critical issue to be considered in the current context of climate change ([Turner et al., 1986]). For example, a complementary acclimatization of photosynthesis in water stressed rice growth under elevated CO2 conditions has been reported, despite an increased rate of net leaf photosynthesis under these same conditions ([Imai and Murata 1978]; [Makino et al., 1997]). Therefore, the calculated water stress parameter is linked to diverse other schemes in a rice growth model because the physiological processes under water stress are complex and may vary according to the presence or absence of other stresses. This means that model developers have to validate and evaluate their models’ performance with regards to the effect of water stress on rice growth under a variety of environmental changes. It is critically important for us to predict rice yield for unexpected climate events.
In fact, the change in yield caused by water shortage is difficult to validate because of limited observation data for water stress. The critical parameters for water stress, such as leaf water potential and leaf temperature, are rarely investigated by in-situ measurement. However, we could indirectly predict the effect of a water deficit on field yields through the relationship between evaporation (or transpiration) and yield. Such information could be available from numerous previous studies ([Simpson et al., 1992]; [Bouman and Tuong, 2001]; [Tuong et al., 2005]). This relationship may or may not be linear, in part because the fraction of evaporation that does not contribute to rice growth varies throughout the rice life cycle. In addition, water-use efficiency (yield or biomass divided by evaporation) is another relevant parameter in evaluating the water demand for rice growth. This factor could be affected by climate change through changes in the irrigation water demand for rice growth. For example, increased evapotranspiration (from the water body of the paddy field and rice stomata) in a warmer atmosphere will require a greater amount of water. On the contrary, a higher temperature will result in a reduced number of irrigation days, on account of the decreased rice growth period ([Simpson et al., 1992]; [Bouman and Tuong, 2001]). Furthermore, water-use efficiency will increase at higher CO2 concentration levels owing to the expected decrease in transpiration and increase in photosynthesis (if the leaf temperature is constant). Therefore, in a rice growth model, the water stress scheme should not be designed in isolation from other environmental changes, such as air temperature, and CO2 level.
These likely interactive phenomena will affect water resource planning and management of irrigation water demand. In addition, the availability of water for rice production is dependent not only on the precipitation and environmental factors related to evapotranspiration, but also on irrigation management ([Tuong et al., 2005]). Indeed, the efficiency of water use for grain production is higher in a saturated soil culture than in an unsaturated soil moisture condition. In most cases, rice production is associated with flood irrigation. Although this method is simple, it also requires sound planning and servicing of the water damming and channelling. Therefore, in a rice growth model, this has to be emphasized to account for the variations of water resources, not only in terms of climate variability but also in terms of anthropogenic effects. However, the realization of terrestrial water resources is not an easy task in the design of a model because of the complex interactions among urban, industrial, agricultural, and natural water requirements. Recently, [Pokhrel et al. (2012]) introduced an integrated model to estimate terrestrial global water resources. The model contains four different anthropogenic water regulation modules (a crop growth module, reservoir operation module, water withdrawal module, and environmental flow requirement module; see also [Hanasaki et al. 2008] for more details) that operate on the basis of a surface and sub-surface runoff process module ([Stieglitz et al. 1997]) a hydrological and biophysical exchange module ([Takata et al. 2003]), and a river routing module ([Oki and Sud 1998]). Although their model is not directly coordinated with a rice growth model, such modules related to water resource assessment are needed in order for us to better investigate the growth stage of a water-sensitive crops such as rice.
Rice growth models are subject to many uncertainties. The conventional way of addressing this uncertainty has been to obtain comprehensive information about the physiological and phenological responses of rice to environmental factors. Even though a given model cannot take into account all the relevant processes, we need to critically understand which parameters will make a definite contribution to obtaining the desired result, and which will not. It is important not only to improve the schemes that models employ, but to also critically review the simulated results (see Figure 2). In this review, we have examined the existing or required processes related to temperature, CO2, and water stress in rice growth models because these are the three factors that are most vulnerable to climate change. It is thus obvious that we must understand the actual roles they play in the physiological processes of rice, as well as the ways these roles may be altered in order to predict rice yields in the future.
In addition, the interactive effects that result from both positive and negative factors are necessary if we are to consider uncertain climate changes. In this review, we have emphasized the importance of accounting for the interactive effects of temperature, CO2, and water demand in a model. However, although our knowledge of the effects that these three factors have on the growth and development of the rice has increased in the past few years, it has remained difficult to realize these interactive effects in a model because of unclear mechanisms involved and the limited experimental data. Therefore, theoretical considerations and experiments that are designed to increase our understanding of this issue are recommended, along with validation studies. ‘Semi-empirical schemes’ and ‘clear assumptions’ based on decades of agronomic knowledge might be the best approach, particularly in light of our limited understanding. Semi-empirical schemes derived from both mechanical approaches and observed characteristics will be suitable to reasonably reflect the latest validation results, particularly under projected climate-change conditions. Showing a clear assumption in a model will improve our understanding of a model’s results, and will also suggest further tasks to pursue in model development.
Fortunately, current rice growth models have been improving as a result of the kind of continuous validation and development mentioned in this review. These recent results for the projection of future rice yields will produce meaningful information that is of great use to society. However, the impact assessment related to global future food security could have a considerable bias owing to not only limitations of a model’s performance, but also to the uncertainties of future weather inputs ([Aggarwal, 1994]). For example, general circulation models (GCMs) still produce uncertain predictions as to how climate variability will vary as a consequence of an increase in greenhouse gases. Nevertheless, there is continued interest in how rice will respond to future changes in temperature, CO2, and water demand because climate change has been a consistent feature of the global climate. It is worth incorporating as the likely impacts of GCM-derived climate change scenarios into the results simulated in rice growth models’. Therefore, an accurate understanding of model behaviour and details is needed in order to produce accurate and well-organized information for our society.
Aggarwal PK: Uncertainties in Plant, Soil and Weather Inputs in Crop Growth Models: Implications for Simulated Outputs and their Applications. Agric Systems 1994, 48: 361–384.
Ainsworth EA: Rice production in a changing climate: a meta-analysis of responses to elevated carbon dioxide and elevated ozone concentration. Global Change Biol 2008, 14: 1642–1650. 10.1111/j.1365-2486.2008.01594.x
Allen LH Jr, Boote KJ, Jones JW, Jones PH, Valle RR, Acock B, Rogers HH, Dahlman RC: Response of vegetation to rising carbon dioxide: photosynthesis, biomass, and seed yield of soybean. Global Biogeochem Cy 1987, 1: 1–14. 10.1029/GB001i001p00001
Amthor JS: Respiration in a future, high-CO2 world. Plant Cell Environ 1991, 14: 13–20. 10.1111/j.1365-3040.1991.tb01367.x
Auffhammer M, Ramanathan V, Vincent VR: Climate change, the monsoon, and rice yield in India. Clim Chang 2012, 111: 411–424. 10.1007/s10584-011-0208-4
Avissar R, Pielke RA: The impact of plant stomatal control on mesoscale atmospheric circulations. Agric For Meteorol 1991, 54: 353–372. 10.1016/0168-1923(91)90013-G
Baker JT, Allen LH Jr, Boote KJ, Jones JW, Jones P: Developmental responses of rice to photoperiod and carbon dioxide concentration. Agric For Meteorol 1990, 50: 201–210. 10.1016/0168-1923(90)90054-A
Baker JT, Allen LH Jr, Boote KJ: Temperature effects on rice at elevated CO2 concentration. J Exp Bot 1992, 43: 959–964. 10.1093/jxb/43.7.959
Ball JT, Woodrow IE, Berry JA: A model predicting stomatal conductance and its contribution to the control of photosynthesis under different environmental conditions. In Progress in photosynthesis research. Edited by: Biggens I. Martinus Nijhoff Publishers, The Netherlands; 1987:221–224.
Bloom DE: 7 Billion and counting. Science 2011, 333: 562–569. 10.1126/science.1209290
Bouman BAM, Tuong TP: Field water management to save water and increase its productivity in irrigated lowland rice. Agric Water Manage 2001, 49: 11–30. 10.1016/S0378-3774(00)00128-1
Braganza K, Karoly DJ, Arblaster JM: Diurnal temperature range as an index of global climate change during the twentieth century. Geophys Res Lett 2004, 31: L13217. 10.1029/2004GL019998
Bunce JA: Effects of humidity on short-term responses of stomatal conduce to an increase in carbon dioxide concentration. Plant Cell Environ 1998, 21: 115–120. 10.1046/j.1365-3040.1998.00253.x
Bunce J: Direct and acclamatory responses of stomatal conductance to elevated carbon dioxide in four herbaceous crop species in the field. Global Change Biol 2001, 7: 323–331. 10.1046/j.1365-2486.2001.00406.x
Coats B: Global rice production. In Rice origin, history, technology and production. Edited by: Smith CW, Dilday RH. Wiley, Hoboken; 2003:247–470.
Collatz GT, Ball JT, Grivet C, Berry JA: Physiological and environmental regulation of stomatal conductance, photosynthesis and transpiration: a model that includes a laminar boundary layer. Agric For Meteorol 1991, 54: 107–136. 10.1016/0168-1923(91)90002-8
Cure JD, Acock B: Crop responses to carbon dioxide doubling: a literature survey. Agric For Meteorol 1986, 38: 127–145. 10.1016/0168-1923(86)90054-7
Easterling DR, Horton B, Jones PD, Peterson TC, Karl TR, Parker DE, Salinger MJ, Razuvayev V, Plummer N, Jamason P, Folland CK: Maximum and minimum temperature trends for the globe. Science 1997, 277: 364–367. 10.1126/science.277.5324.364
Ekanayake IJ, de Datta SK, Steponkus PL: Effect of water deficit stress on diffusive resistance, transpiration, and spikelet desiccation of rice (Oryza sativa L.). Annuals of Botany 1993, 72: 73–80. 10.1006/anbo.1993.1082
FAO. World Agriculture: Towards 2015/2030 Summary Report. Food and Agriculture Organization of the United Nations, Rome; 2002.
FAO. FAOSTATS Food and Agriculture Organization of the United Nations, Rome; 2005.http://faostat.fao.org
Farquhar GD, von Caemmerer S, Berry JA: A biochemical model of photosynthesis CO2 assimilation in leaves of C3 species. Planat 1980, 149: 78–90. 10.1007/BF00386231
Fischer G, Shah M, Tubiello FN, van Velhuizen H: Socio-economic and climate change impacts on agriculture: an integrated assessment, 1990–2080. Philos Trans R Soc B 2005, 360: 2067–2083. 10.1098/rstb.2005.1744
Garrity DP, O’Toole JC: Screening rice for drought resistance at the reproductive phase. Field Crop Res 1994, 39: 99–110. 10.1016/0378-4290(94)90012-4
Gifford RM: Growth and yield of carbon dioxide-enriched wheat under water-limited conditions. Aust J Plant Physiol 1979, 6: 367–378. 10.1071/PP9790367
Granier A, Biron P, Kӧstner B, Gay LW, Najjar G: Comparisons of xylem sap flow and water vapour flux at the stand level and derivation of canopy conductance for Scots Pine. Theor Appl Climatol 1996, 53: 115–122. 10.1007/BF00866416
Hanasaki N, Kanae S, Oki T, Masuda K, Motoya K, Shirakawa N, Shen Y, Tanaka K: An integrated model for the assessment of global water resour. – part 1: Model description and input meteorological forcing. Hydrol Earth. Syst Sci 2008, 12: 1007–1025.
Harley PC, Weber JA, Gates DM: Interactive effects of light, leaf temperature, CO2, and O2 on photosynthesis in soybean. Planta 1985, 165: 249–263. 10.1007/BF00395048
Hogan KP, Smith AP, Ziska LH: Potential effects of elevated CO2 and changes in temperature on tropical plants. Plant Cell Environ 1991, 14: 763–778. 10.1111/j.1365-3040.1991.tb01441.x
Imai K, Murata Y: Effect of carbon dioxide concentration on growth and dry matter production of crop plants. V. Analysis of after-effect of carbon dioxide- treatment on apparent photosynthesis. Jpn J Crop Sci 1978, 47: 587–595. 10.1626/jcs.47.587
Imai K, Nomura M Proc Int Symp on Global Change (IGBP). In Effects of phosphorus nutrition on gas exchanges of rice leaves at elevated atmospheric partial pressure of carbon dioxide. Waseda University, Tokyo; 1992:573–578.
Jarvis PG, James GB, Landsberg JJ: Coniferous forest. In Vegetation and Atmosphere. Edited by: Monteith JL. Academic, San Diego, CA; 1976.
Jodo S: Water use efficiency. In Science of the Rice Plant. 2. Physiology. Edited by: Matsuo T, Kumazawa K, Ishii R, Ishihara K, Hirate H. Food and Agriculture Policy Research Center, Tokyo; 1995:447–461.
Jones HG: Plant and Microclimate. 2nd edition. Cambridge University Press, Cambridge, UK; 1992.
Kandiannan K, Karthikeyan R, Krishnan R, Kailasam C, Balasubramanian TN: A Crop-Weather Model for Prediction of Rice (Oryza sativa L.) Yield Using an Empirical-Statistical Technique. J Agron Crop Sci 2002, 188: 59–62. 10.1046/j.1439-037x.2002.00533.x
Katul GG, Palmroth S, Oren R: Leaf stomatal responses to vapour pressure deficit under current and CO2-enriched atmosphere explained by the economics of gas exchanges. Plant Cell Environ 2009, 32: 968–979. 10.1111/j.1365-3040.2009.01977.x
Kim J, Verma S: Modelling canopy stomatal conductance in a temperate grassland ecosystem. Agric For Meteorol 1991, 55: 149–166. 10.1016/0168-1923(91)90028-O
Kimball BA: Carbon dioxide and agricultural yield: an assemblage and analysis of 430 prior observations. Agron J 1983, 75: 779–788. 10.2134/agronj1983.00021962007500050014x
Knorr W: Annual and interannual CO2 exchanges of the terrestrial biosphere: process-based simulations and uncertainties. Glob Ecol Biogeogr 2000, 9: 225–252. 10.1046/j.1365-2699.2000.00159.x
Kropff MJ, van Laar HH: Modelling Crop-Weed Interactions. CAB International, and International Rice Research Institute, Wallingford, UK, Manila, The Philippines; 1993:274.
Lansigan FP, Pandey S, Bouman BAM: Combining crop modeling with economic risk-analysis for the evaluation of crop management strategies. Field Crops Res 1997, 51: 133–145. 10.1016/S0378-4290(96)01037-4
Lasseigne FT, Warren SL, Blazich FA, Ranney TG: Day/Night Temperature Affects Growth and Photosynthesis of Cultivated Salvia Taxa. J Amer Soc Hort Sci 2007, 132: 492–500.
Leuning R: A critical appraisal of a combined stomatal-photosynthesis model for C3 plants. Plant Cell Environ 1995, 18: 339–355. 10.1111/j.1365-3040.1995.tb00370.x
Lobell DB, Burke MB: Why are agricultural impacts of climate change so uncertain? The importance of temperature relative to precipitation. Environ Res Lett 2008, 3: 034007. 10.1088/1748-9326/3/3/034007
Lobell DB, Schlenker W, Costa-Roberts J: Climate trends and global crop production since 1980. Science 2011, 333: 616–620. 10.1126/science.1204531
Long SP, Ainsworth EA, Leakey ADB, Morgan PB: Global food insecurity. Treatment of major food crops with elevated carbon dioxide or ozone under large-scale fully open-air conditions suggests recent models may have overestimated future yields. Phil Trans Royal Soc Lond B 2005, 360: 2011–2020. 10.1098/rstb.2005.1749
Long SP, Ainsworth EA, Leakey ADB, Nosberger J, Ort DR: Food for thought: lower than expected crop yield stimulation with rising CO2 concentrations. Science 2006, 312: 1918–1921. 10.1126/science.1114722
Lu P, Yunusa IAM, Walker RR, Muller WJ: Regulation of canopy conductance and transpiration and their modelling in irrigated grapevines. Funct Plant Biol 2003, 30: 689–698. 10.1071/FP02181
Makino A, Harada M, Sato T, Nakano H, Mae T: Growth and N Allocation in Rice Plants under CO2 Enrichment. Plant Physiol 1997, 115: 199–203.
Makowski K, Wild M, Ohmura A: Diurnal temperature range over Europe between 1950 and 2005. Atmos Chem Phys 2008, 8: 6483–6498. 10.5194/acp-8-6483-2008
Massman WJ, Kaufmann MR: Stomatal response to certain environmental factors: a comparison of models for subalpine trees in the Rocky Mountains. Agric For Meteorol 1991, 54: 155–167. 10.1016/0168-1923(91)90004-A
Matthews RB, Hunt LA: A model describing the growth of cassava (Manihot esculenta L. Crantz). Field Crops Res 1994, 36: 69–84. 10.1016/0378-4290(94)90054-X
Matthews RB, Kropff MJ, Horie T, Bachelet D: Simulating the impact of climate change on rice production in Asia and evaluating options for adaptation. Agric Syst 1997, 54: 399–425. 10.1016/S0308-521X(95)00060-I
Mebrahtu T, Hanover JW, Layne DR, Flore JA: Leaf temperature effects on net photosynthesis, dark respiration, and photorespiration of seedlings of black locust families with contrasting growth rates. Can J For Res 1991, 21: 1616–1621. 10.1139/x91-224
Noilhan J, Planton S: A simple parameterization of land surface processes for meteorological models. Mon Weather Rev 1989, 117: 536–549. 10.1175/1520-0493(1989)117<0536:ASPOLS>2.0.CO;2
Norman JM: Simulation of Microclimates. In Biometeorology and Integrated Pest Management. Edited by: Hatfield JL, Thompson I. Academic, New York; 1982:65–99.
Morison JIL, Gifford RM: Stomatal Sensitivity to Carbon Dioxide and Humidity. Plant Physiol 1983, 71: 789–796. 10.1104/pp.71.4.789
Morison JIL, Gifford RM: Plant growth and water use with limited water supply in high CO2 concentrations. I. Leaf area. water use and transpiration. Aust J Plant Physiol 1984, 11: 361–374. 10.1071/PP9840361
Mott KA: Do stomata respond to CO2 concentrations other than intercellular? Plant Physiol 1988, 86: 200–203. 10.1104/pp.86.1.200
Neue H-U, Sass R: Trace gas emissions from rice fields. In Global atmospheric-biospheric chemistry. Edited by: Prinn RG. Plenum Press, New York; 1994:119–148.
O’Toole JC, Tomar VS: Transpiration, leaf temperature and water potential of rice and barnyard grass in flooded fields. Agric Meteorol 1982, 26: 285–296. 10.1016/0002-1571(82)90046-2
Oki T, Sud Y: Design of Total Runoff Integrating Pathways (TRIP)–A global river channel network. Earth Interact 1998, 2: 1–37.
Oren R, Phillips N, Ewers BE, Pataki DE, Megonigal JO: Sap-flux-scaled transpiration responses to light, vapour pressure deficit, and leaf area reduction in a flooded Taxodium distichum forest. Tree Physiol 1999, 19: 337–347. 10.1093/treephys/19.6.337
Peet MM: Acclimation to high CO2 in monoecious cucumbers: 1 Vegetative and reproductive growth. Plant Physiol 1986, 80: 59–62. 10.1104/pp.80.1.59
Peng S, Huang J, Sheehy JE, Laza RC, Visperas RM, Zhong X, Centeno GS, Khush GS, Cassman KG: Rice yields decline with higher night temperature from global warming. P Natl Acad Sci USA 2004, 101: 9971–9975. 10.1073/pnas.0403720101
de Vries FWT Penning, Jansen DM, ten Berge HFM, Bakema A: Simulation of Ecophysiological Processes of Growth in Several Annual Crops. Los Baños: Pudoc. Wageningen and IRRI; 1989:271.
Pokhrel Y, Hanasaki N, Koirala S, Cho J, Yeh PJ-F, Kim H, Kanae S, Oki T: Incorporating anthropogenic water regulation modules into a land surface model. J Hydrometeor 2012, 13: 255–267. 10.1175/JHM-D-11-013.1
Poorter H, Gifford RM, Kridemann PE, Wong SC: A quantitative analysis of dark respiration and carbon content as factors in the growth response of plants to elevated CO2. Aust J Bot 1992, 40: 501–513. 10.1071/BT9920501
Satake T, Yoshida S: High temperature-induced sterility in indica rice at flowering. Jpn J Crop Sci 1978, 47: 6–17. 10.1626/jcs.47.6
Shimono H, Okada M, Yamakawa Y, Nakamura H, Kobayashi K, Hasegawa T: Rice yield enhancement by elevated CO2 is reduced in cool weather. Global Change Biol 2008, 14: 276–284. 10.1111/j.1365-2486.2007.01498.x
Simpson HJ, Herczeg AL, Meyer WS: Stable isotope ratios in irrigation water an estimate rice crop evaporation. Geophy Res Lett 1992, 19: 377–380. 10.1029/91GL02952
Spitters CJT, van Keulen H, van Kraalingen DWG, et al.: A simple and universal crop growth simulator: SUCROS8 7. In Simulation and Systems Management in Crop Protection. Pudoc. Edited by: Rabbinge R. Wageningen; 1989:147–181.
Stieglitz M, Rind D, Famiglietti J, Rosenzweig C: An efficient approach to modeling the topographic control of surface hydrology for regional and global climate modeling. J Climate 1997, 10: 118–137. 10.1175/1520-0442(1997)010<0118:AEATMT>2.0.CO;2
Takata K, Emori S, Watanabe T: Development of the minimal advanced treat- ments of surface interaction and runoff. Global Planet Change 2003, 38: 209–222. 10.1016/S0921-8181(03)00030-4
Tubiello FN, Amthor JS, Boote KJ, Donatelli M, Easterling W, Fischer G, Gifford RM, Howden M, Reilly J, Rosenzweig C: Crop response to elevated CO2 and world food supply. A comment on “Food for Thought”. by Long et al., Science 312:1918–1921, 2006. Eur J Agron 2007, 26: 215–223. 10.1016/j.eja.2006.10.002
Tuong TP, Bouman BAM, Mortimer M: More rice, less water: integrated approaches for increasing water productivity in irrigated rice-based systems in Asia. Plant Prod Sci 2005, 8: 231–241. 10.1626/pps.8.231
Turner NC, O’Toole JC, Cruz RZ, Yambao EB, Ahmad S, Namuco OS, Dingkuhn M: Responses of seven diverse rice cultivars to water deficits. II. Osmotic adjustment, leaf elasticity, leaf extension, leaf death, stomatal conductance and photosynthesis. Field Crop Res 1986, 13: 273–286.
van Laar HH, Goudriaan J, van Keulen H: Simulation of Crop Growth for Potential and Water-limited Production Situations (us Applied to Spring Wheat). CABO-TT Simulation Reports 27. Centre for Agrobiological Research, Wageningen; 1992:72.
Wang F, Wang S, Li Y, Zhong M: A preliminary modeling of the effects of climatic changes on food production in China. In Climate Variations and Change: Implications for Agriculture in the Pacific Rim. Edited by: Geng S, Cady CW. University of California, California; 1991:115–126.
Welcha JR, Vincentb JR, Auffhammerc M, Moyae PF, Dobermannf A, Daweg D: Rice yields in tropical/subtropical Asia exhibit large but opposing sensitivities to minimum and maximum temperatures. P Natl Acad Sci USA 2010, 33: 14562–14567.
Ziska LH, Bunce JA: Predicting the impact of changing CO2 on crop yields: some thoughts on food. New Phytol 2007, 175: 607–618. 10.1111/j.1469-8137.2007.02180.x
This work was supported by JSPS KAKENHI, Grants-in-Aid for Scientific Research on Innovative Areas (22119009) and (S)(23226012), and Innovative program of climate change projection for the 21st Century from The Ministry of Education, Culture, Sports, Science and Technology (MEXT).
The authors declare that they have no competing interests.
All of the authors contributed equally to the drafting and revising of this paper and have read and approved the final manuscript.
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Cho, J., Oki, T. Application of temperature, water stress, CO2 in rice growth models. Rice 5, 10 (2012). https://doi.org/10.1186/1939-8433-5-10
- Carbon dioxide
- Water stress
- Rice growth model