Rice yield estimation based on weather conditions and on technological level of production systems in Brazil

Estimativa da produtividade de arroz baseada em condições meteorológicas e no nível tecnológico dos sistemas de produção no Brasil

AGROMETEOROLOGY

Rice yield estimation based on weather conditions and on technological level of production systems in Brazil

Estimativa da produtividade de arroz baseada em condições meteorológicas e no nível tecnológico dos sistemas de produção no Brasil

José Eduardo Boffino de Almeida Monteiro^I; Letícia da Costa Azevedo^II; Eduardo Delgado Assad^II; Paulo Cesar Sentelhas^III

^IEmbrapa Uva e Vinho, Caixa Postal 130, CEP 95700‑000 Bento Gonçalves, RS, Brazil. E‑mail: [e-mail]

^IIEmbrapa Informática Agropecuária, Caixa Postal 6041, CEP 13083‑886 Campinas, SP, Brazil. E‑mail: [e-mail], [e-mail]

^IIIUniversidade de São Paulo, Escola Superior de Agronomia Luiz de Queiroz, Departamento de Engenharia de Biossistemas, Caixa Postal 9, CEP 13418‑900 Piracicaba, SP, Brazil. E‑mail: [e-mail]

ABSTRACT

The objective of this work was to evaluate an estimation system for rice yield in Brazil, based on simple agrometeorological models and on the technological level of production systems. This estimation system incorporates the conceptual basis proposed by Doorenbos & Kassam for potential and attainable yields with empirical adjusts for maximum yield and crop sensitivity to water deficit, considering five categories of rice yield. Rice yield was estimated from 2000/2001 to 2007/2008, and compared to IBGE yield data. Regression analyses between model estimates and data from IBGE surveys resulted in significant coefficients of determination, with less dispersion in the South than in the North and Northeast regions of the country. Index of model efficiency (E₁') ranged from 0.01 in the lower yield classes to 0.45 in higher ones, and mean absolute error ranged from 58 to 250 kg ha^‑1, respectively.

Index terms: crop simulation model, crop yield forecast, model efficiency, water deficit.

RESUMO

O objetivo deste trabalho foi avaliar um sistema de estimativa de produtividade da cultura do arroz no Brasil, com base em modelos agrometeorológicos simples e no nível tecnológico dos sistemas produtivos. Este sistema de estimativa incorpora as bases conceituais propostas por Doorenbos & Kassam para produtividades potenciais e alcançáveis com ajustes empíricos para produtividade máxima e sensibilidade da cultura à deficiência hídrica, considerando-se cinco classes de produtividade de arroz. A produtividade de arroz foi estimada de 2000/2001 a 2007/2008 e comparada aos dados do IBGE. Análises de regressão entre as estimativas do modelo e dados do IBGE resultaram em coeficientes de determinação significativos, com menor dispersão na região Sul do que nas regiões Norte e Nordeste do país. O índice de eficiência do modelo (E₁') variou de 0,01, nas classes de menor produtividade, a 0,45 nas classes de maior produtividade, e o erro médio absoluto variou de 58 a 250 kg ha^‑1, respectivamente.

Termos para indexação: modelo de simulação de cultura, previsão de safra, eficiência do modelo, deficiência hídrica.

Introduction

Crop yield forecasting and the knowledge of yield distribution are extremely important for governmental planning. This information is essential for public policy formulation, logistic distribution, food security, and for price formation at national and international markets (Figueiredo, 2005). Yield forecasting applications can be conducted either prior to crop planting or during the growing season. The main objective is to predict yield, since this information can be used at farm‑level for marketing decisions or at government level for policy issues and food security decisions (Hoogenboom, 2000).

Information on Brazilian total production, cropped area and yield can be obtained from crop surveys conducted by Companhia Nacional de Abastecimento (the national supply company, Conab) and Instituto Brasileiro de Geografia e Estatística (Brazilian Institute of Geography and Statistics, IBGE). These surveys are done for each municipality through interviews with local farmers, agronomists and technicians of cooperatives, agricultural offices and technical assistance agencies. Therefore, the methodology requires a time consuming process for surveys and field data consolidation, which undermines the use of this information during the growing season, either for public policy measures or for crop management by farmers and cooperatives.

Agrometeorological monitoring systems (AMS) provide, in near real time, information on meteorological conditions in the production regions. This system, when associated to crop yield simulation models, allows to quantify the impacts of meteorological conditions on agricultural yield – also in near real time –, in different phases of crop development.

Rice is cultivated and consumed in all continents and has a strategic status (Heinemann et al., 2009) in Brazil and in many other countries. However, it is very sensitive to weather conditions, with high‑water requirement per unit of produced mass. Water deficit, even if moderate, can cause high‑yield losses, especially when occurring during flowering and early grain filling (Heinemann & Stone, 2009). Therefore, upland rice crops are considered under high climate risk (Silva & Assad, 2001)

Many models have been developed for crop yield estimation considering different parameters and complexity levels, most of them are based on agrometeorological variables (Doorenbos & Kassam, 1979; Assad et al., 2007; Heinemann & Stone, 2009). There is a group of simulation models for rice yield estimation and forecasting, among them is Infocrop (Aggarwal et al., 2006), Warm (Confalonieri et al., 2009) and Oryza (Bouman et al., 2006). In Brazil, some of these models have been parameterized, like Oryza/Apsim for upland (Lorençoni et al., 2010) and irrigated rice, which is based in temperature and solar radiation (Klering et al., 2008). However, despite all those advances in crop modeling, a challenge still needs to be addressed in Brazil. This challenge relies on integrating a reasonable yield model with the large amount of data provided annually by Conab and IBGE for the whole country. To accomplish this task, two major issues have to be overcome: the lack of information about crop, soil, and production systems for all the production regions; and the inaccuracy of crop surveys, which are done by sampling and not always produce exact results for all the municipalities. An additional constraint is the fact that the available statistics show only the total production per municipality, regardless of whether it comes from irrigated or rainfed rice. For this reason, to successfully estimate rice yield in all production areas of Brazil, it is crucial that the estimation system somehow consider the different types of crop systems and their sensitivity to water deficit.

The objective of this work was to evaluate an estimation system for rice yield in Brazil, based on simple agrometeorological models and on the technological level of production systems.

Materials and Methods

The crop yield simulation model developed in the present study follows the theoretical basis proposed by Doorenbos & Kassan (1979), which establishes relationships between relative yield losses and relative water deficiency along the crop phases. It was composed by two modules: one that estimates crop potential yield or maximum yield; and other that estimates the decrement of potential yield as a function of water deficit.

The proposed model was calibrated with basis on rice yield data derived from production and harvested area series surveyed by IBGE, for the growing seasons from 2000/2001 to 2007/2008. From the total of 5,561 municipalities, only 3,840 with data for at least four crop seasons during the evaluated period were considered. Municipalities were classified into five categories, according to the average yield in the last four seasons. Intervals of each yield class included areas of upland rice and irrigated rice, and were set as follows: class 1, from 0 to 2,000 kg ha^‑1; class 2, from 2,001 to 4,000 kg ha^‑1; class 3, from 4,001 to 6,000 kg ha^‑1; class 4, from 6,001 to 8,000 kg ha^‑1; and class 5, from 8,001 to 10,000 kg ha^‑1. Each yield class was analyzed independently, in order to produce specific parameterization for each of them in modules of both maximum and actual yields.

Normal sowing periods were identified for each state, according to Conab's annual surveys (Companhia Nacional de Abastecimento, 2009). In order to represent the distribution of planted areas of a state across time, a frequency distribution of planted area (FDPA) was adjusted to the sowing period, i.e. from mid‑October to mid‑December, in the state of Goiás, with higher concentration in November. FDPA was set to match start date, end date, and date of maximum planting of the whole sowing period. A proportion of planted area in each day was determined, within planting period, which was used to weight the final yield estimation.

Maximum yield, named as technological maximum yield (TYm), was estimated from a statistical adjustment based on data series of observed actual yield. Observed yields were assumed as those which actually occurred in each municipality, which are surveyed and published by IBGE every year (Instituto Brasileiro de Geografia e Estatística, 2010). The first step consisted in adjusting a first degree linear equation (Y = ax + b) to the observed yield data (Ya) against time (year). The straight line generated by the equation indicates the observed yield trend over years (Ya'). Yield deviations that may happen over and under the line are caused by variation in productivity factors, including weather conditions, water availability and crop management. The second step consisted in determining a correction factor that, when multiplied by the observed yield trend (Ya'), would elevate values to the yield level without water restriction. This correction factor was named coefficient of technological maximum yield (Δp). Thus, technological maximum yield (TYm) was calculated for each year "n" as a function of the adjusted actual yield multiplied by Δp: TYm = Ya' × Δp.

In this sense, Δp was adjusted through a detrended regression, and consisted in one of the parameters calibrated in this model, according to the method shown ahead.

Values of crop coefficient (kc) and yield response factor (ky) – presented by Heinemann et al. (2009) for initial vegetative development, late vegetative development, flowering, and maturation phases of rice – were adapted to the daily scale. Crop coefficient (kc) values, in the present work, were 0.4, 0.9, 1.3, and 1.0, respectively, whereas yield response factor (ky) were 0.2, 0.6, 1.25, and 0.4. Daily weather data were used from 1,053 weather stations, spread throughout the Brazilian states, to estimate potential evapotranspiration. These stations are owned by governmental and private institutions and integrate the Embrapa's Agrometeorological Monitoring System (Agritempo). Actual crop evapotranspiration (ETa) was determined by sequential water balance, computing daily changes in soil water content, according to Thornthwaite´s method. Due to the impossibility of precisely inferring the water holding capacity most suited for soils of different municipalities, an effective depth of the root system of 35 cm was considered for upland rice, as well as the water holding capacity of 1 mm cm^‑1 (Araújo & Assad, 2001).

Actual yield (Ya) was estimated from the relationship between relative water deficit [1 ‑ (ETa/ETc)] and relative crop yield loss, weighted by the yield response factor to water deficit (ky), for each phenological phase, resulting in the following model, presented in Doorenbos & Kassam (1979), Ya/Ym = 1 ‑ ky[1 ‑ (ETa/ETc)], in which: Ym is the maximum yield, ETa is the actual crop evapotranspiration, and ETc is the maximum crop evapotranspiration. One of the changes in this model, if compared to the one cited above, is that yield calculation is updated daily, whenever the system receives new weather data, at the end of each day, similarly to the system developed for soybean by Assad et al. (2007) in Brazil. Another difference is the introduced empirical parameter, called adjusted yield response factor (ky*), bellow explained, which results in higher or lower response to water deficit, according to technological specificities related to different production systems, in each yield class. The third and last difference is the use of the technological maximum yield (TYm). With all these changes, the final model results in: Ya/TYm = 1 - ky* × ky[1 ‑ (ETa/ETc)]. In this equation, TYm is used as the initial reference to begin the calculation process in each season. Once Ya of the first day is calculated, it will be used as the new reference in replacement to TYm in the second day, and so on.

Parameterization process consisted in adjusting the maximum yield coefficient (Δp) and the adjusted yield response factor (ky*), in order to maximize correlation between estimated and observed actual yields, and also to minimize mean absolute error (MAE) between them. In this process, ky* starts with value 1.0 and is subsequently increased or decreased according to the gain or loss in the correlation and in the MAE between estimated and observed yields. References used for evaluating model estimations were the independent yield values, surveyed and published by IBGE (Instituto Brasileiro de Geografia e Estatística, 2010). These data came from 143 municipalities with complete yield data series from 2001 to 2008, distributed in four yield classes, with weather stations located in the same municipality. The fifth yield class, 8,000 to 10,000 kg ha^‑1, could not be tested, due to the absence of weather data series for municipalities of that class. Weather data were managed for allowing only series without missing data, to avoid errors in the water balance. When data were missing, the crop season was disregarded. From the total of municipalities, 71 were used for model parameterization and 72 for model performance evaluation.

Estimated Ya values (P) were compared to those from IBGE (O) by regression analysis and also by evaluating absolute and relative errors. The significance of the coefficient of determination (R²) was determined by T test at 5% and 1% of probability. Model accuracy was evaluated according to the Legates' modified index of model efficiency (E₁') (Legates & McCabe Junior, 1999), as given in the following equation:

in which: E₁' is the ratio of the mean error to the variance in the observed data, subtracted from the unity; and O and P stands for observed and predicted Ya values, respectively. Thus, a zero value for the coefficient of efficiency indicates that the observed mean is as good a predictor as the model, negative values indicate that the observed mean is a better predictor than the model, and positive values indicate better predictions than the observed mean.

Results and Discussion

About 63% of the Brazilian rice production was concentrated in 403 high‑yielding municipalities, where flood irrigated systems are typical (Table 1). Although the remaining 37% came from upland rainfed rice, with lower yield, its fields were spread over 3,746 municipalities, which gives an idea of the widespread cultivation of this crop in the country. The average yield of upland rice in Brazil is around 1,800 kg ha^‑1, much lower than those observed for flooded rice, which is about 6,110 kg ha^‑1 (Instituto Rio Grandense do Arroz, 2008). Therefore, the production in municipalities of yield classes 1 and 2 is likely to be from upland rice, while production in municipalities of classes 3 and 4 is likely to be predominantly from lowland irrigated crops. Upland rice naturally shows lower maximum yield than flood–irrigated rice, which shows lower yields even without water deficits. Thus, it is expected that lower the yield of a municipality, the higher is the proportion of rainfed crops. At this point, it is convenient to emphasize that this model is suited to estimate yield variability of rainfed crops. For irrigated rice, it is limited to the determination of yield trends, besides being a manner to distinguish irrigated from rainfed rice. This large distinction between yields of irrigated and rainfed rice allowed to minimize the effect of it in the estimations. Classifying municipalities by yield classes, with independent calibration of ky* for each one, allowed to identify the degree of susceptibility to water deficits for each of them (Table 2).

The ky* and Δp calibration process was performed in order to obtain the higher correlation and the smaller absolute error possible. After calibration, ky* tended to zero with higher rice yields. A small ky* value indicates lower crop susceptibility to local water deficit. The Δp values reflected the average loss for each class during the studied period, i.e. 30% in class 1 and 5% in class 4.

Coefficients of determination between estimated and observed yields were high, even when the effect of water deficiency was lower, and the inter‑annual variations were smaller, as in class 3 and 4. However, E₁' was very low in classes of low productivity. In class 1, despite estimated yields represented well the variations in IBGE series (R² = 0.76), E₁' was very sensible to systematical error. For yield class 1, an error of 250 kg ha^‑1 represents a high error of 25% relatively to the average yield, while the same absolute error represents a relative error of 3.8% in yield class 4.

In general, yield model estimations were comparable to IBGE data trend over the years (Figure 1). Some differences were observed in the yield class 2 in 2004, and in the class 3, in 2004 and 2005. Classes 2 and 3 also showed the highest mean relative errors, possibly for being located in regions where both systems (rainfed and irrigated) are used. Different proportions of each crop system in a same municipality may result in over‑ or underestimation of yield. Moreover, differences in water availability and in crop management can also result in missing estimations of yield. This occurs because models are parameterized per yield class considering the data set of the country as a whole, as there are no specific parameterization per region.

Since systematic errors can be corrected through recalibration, the most important is quantifying the inter‑annual variability. Therefore, the coefficient of determination (R²) is a useful indicator. More attention should be given to cases where estimated yield shows one trend, and observed yield shows an opposite one. In these cases, the sources of error can be related to eventual changes in agricultural practices and management, which include used genotypes, soil management, fertilization, diseases and pests outbreaks etc. These are factors not computed by this model, due the impossibility of systematically survey them in the wide areas to be considered. Therefore, unpredictable variations may occur and degrade the model performance estimated by R², MAE, MRE, and E₁'.

Lower R² and E₁' were observed for regional‑scale evaluations in most cases (Table 3). The lower model performance in these evaluations shows that the parameterization with national data sets is not readily available to be extrapolated to more specific areas. A potential limitation in this case might be the uneven distribution of municipalities in each region, since yield class frequencies vary for each region. However, South region had a better model performance than that of national data. In that region, the model simulated the occurrence of yield losses in 2005, in classes 1 and 2 (Figure 2), due to an abnormally intense drought in that year, mainly in the state of Rio Grande do Sul. Observed and estimated yields in class 4, however, were not reduced in 2005, due to the evident predominance of irrigated rice crops in that class. But, even in these classes, extreme droughts may affect water reservoirs and limit water availability for irrigation, which is a situation that could not be estimated. With these extreme events, observed yields should be reduced, while estimated yields would remain in the main trend. Data from the municipality of Pelotas in 2005 is a possible example (Figure 3). Similar results were reported in Assad et al. (2007), when soybean showed high‑yield losses in 2005 in this region.

Yield estimations were made individually for each year and municipality, and for each year and yield class (Figure 4). A clear difference was observed between the lower yield (0 to 2,000 and 2,000 to 4,000 kg ha^‑1), and the higher yield classes (4,000 to 6,000 and 6,000 to 8,000 kg ha^‑1). Municipalities grouped into the classes 1 and 2 had average yields of 1,440 kg ha^‑1 and 2,200 kg ha^‑1, respectively. In contrast, municipalities of class 3 and 4 had average yields of nearly 5,000 kg ha^‑1 and 6,300 kg ha^‑1.

An important aspect to be addressed is the water availability in each phenological stage of the crop. The detailed approach, which weights the areas according to each sowing date, throughout the entire sowing period, is an attempt to reduce the main source of error regarding water availability. As the planting season may extend for up to 3.5 months, this may result in very different water conditions in areas planted at the beginning of the season or at the end of it. Due to the shallow root system of rice, even the nonirrigated crops explore small water reservoir in the soil, being hard to determine precisely the water holding capacity for each site or yield class. Therefore, small inaccuracies in estimating actual daily evapotranspiration, accumulated in a given period (e.g. 10 days), should not exceed the water deficit accumulated in 2 or 3 days of water restriction, in order to not compromise yield estimations. Moreover, within a sowing period of more than three months, crops may reach critical stages (e.g. flowering) under water conditions very different from those observed in areas planted sooner or later. Given the gradual depletion of water in soil, the number of days of water stress becomes a more important factor in estimating yield than minor inaccuracies in the water balance calculation.

Despite the water factor, the use of technological maximum yield concept, with correction of yield trends over time, is important to improve accuracy and precision of estimates in both low and high yield classes. This reference yield represents the actual portion of the theoretical potential yield that can be achieved, depending on the available technology for inputs and crop management techniques. Similarly, adjusted yield series were used by Fernandes et al. (2010) in order to minimize the effects of technological advances in rice yields while comparing them to drought indices.

In the regional evaluation, greater systematic errors were found, especially on yield class 1 (Table 3). Therefore, better results should be possible using a narrower yield range interval for classes of lower averages. Probably, a better approach to parameterize this yield model is to consider the data source in the smallest, possible spatial scale, which means municipality data. This could result in better correlations between model and observed data, smaller MRE, and better E₁'. By applying this idea to the examples of the municipalities Janaúba, MG, Picos, PI, and Pelotas, RS (Figure 3), the municipal parameterization reduced the mean relative error respectively from 45 to 13%, 13 to 7%, and 11 to 8%, increasing E₁' accordingly.

Regarding the yield that will initiate calculations, another reference of maximum yield is clearly necessary for better representing the diversity of conditions of rice production in Brazil. The concept of technological maximum yield suggested here (TYm) is adequate for Ya ranging from 500 to 8,000 kg ha^‑1. More detailed methods that use crop specific factors, such as Oryza models (Bouman et al., 2006), would hardly find enough information to perform estimations for large regions, with different genotypes, soil, and production systems. In this sense, the concept of technological level summarizes all productivity factors besides water in a given production system. These factors are more related to technological resources used for crop production than to the agroecological potential of the region.

IBGE data also allowed to detect other production factors which may have higher or lesser importance at municipality context, depending on the year. Those factors could not be accounted by this model without including new sub‑models and more detailed information about production systems. An example of year to year variations is seen for the municipality Janaúba, MG (Figure 3 B), in which a 500 kg ha^‑1 error was determined between model estimation and observed data, in 2006. However, mean absolute error was 53 kg ha^‑1 in the average of the other six analyzed years. In the case of upland rice yield, for example, IBGE data shows Brazilian municipalities with average rice yield higher than 3,000 kg ha^‑1, while showing others with less than 500 kg ha^‑1 (Instituto Brasileiro de Geografia e Estatística, 2010). Startlingly, this variation may occur within the same agroecological zone, with similar soil, climate, and theoretical maximum yield. This fact reveals the diversity of technological levels and crop management practices used across the country.

Conclusions

1. The proposed model consistently represents the relationships between rainfed rice yield and water deficit, throughout the crop cycle, in all Brazilian regions.

2. Model parameterization according to rice yield classes is essential to differentiate the technological level effect, both to calibrate the sensitivity to water deficit and to define the technological maximum yield.

3. Combined calibration of the technological maximum yield coefficient (Δp) and of the corrected yield response factor to water deficit (ky*) allows to isolate the effect of water deficit on the potential yield, for each yield class.

Received on May 8, 2012 and accepted on January 28, 2013

• AGGARWAL, P.K.; KALRA, N.; CHANDER, S.; PATHAK, H. InfoCrop: a dynamic simulation model for the assessment of crop yields, losses due to pests, and environmental impact of agro‑ecosystems in tropical environments. I. Model description. Agricultural Systems, v.89, p.1‑25, 2006. DOI: 10.1016/j.agsy.2005.08.001.
• ARAÚJO, A.G.; ASSAD, M.L. Zoneamento de risco climático por cultura a partir de levantamento de solos de baixa intensidade. Revista Brasileira de Ciência do Solo, v.25, p.103‑111, 2001.
• ASSAD, E.D.; MARIN, F.R.; EVANGELISTA, S.R.; PILAU, F.G.; FARIAS, J.R.B.; PINTO, H.S.; JULLO JÚNIOR, J. Sistema de previsão da safra de soja para o Brasil. Pesquisa Agropecuária Brasileira, v.42, p.615‑625, 2007. DOI: 10.1590/S0100‑204X2007000500002.
• BOUMAN, B.A.M.; VAN LAAR, H.H. Description and evaluation of the rice growth model ORYZA2000 under nitrogen‑limited conditions. Agricultural Systems, v.87, p.249‑273, 2006. DOI: 10.1016/j.agsy.2004.09.011.
• COMPANHIA NACIONAL DE ABASTECIMENTO. Acompanhamento da safra brasileira de grãos 2008/2009 ‑ décimo segundo levantamento ‑ setembro 2009 Brasília: Conab, 2009. 41p.
• CONFALONIERI, R.; ACUTIS M.; BELLOCCHI G.; DONATELLI M. Multi‑metric evaluation of the models WARM, CropSyst, and WOFOST for rice. Ecological Modelling, v.220, p.1395‑1410, 2009. DOI: 10.1016/j.ecolmodel.2009.02.017.
• DOORENBOS J.; KASSAM A.H. Yield response to water Rome: FAO, 1979. 201p. (FAO. Irrigation and drainage paper, 33).
• FERNANDES, D.S.; HEINEMANN, A.B.; PAZ, R.L.F.; AMORIM, A.O. Desempenho de índices quantitativos de seca na estimativa da produtividade de arroz de terras altas. Pesquisa Agropecuária Brasileira, v.45, p.771-779, 2010. DOI: 10.1590/S0100-204X2010000800001.
• FIGUEIREDO, D.C. Projeto GeoSafras ‑ aperfeiçoamento do sistema de previsão de safras da Conab. Revista de Política Agrícola, v.14, p.110‑120, 2005.
• HEINEMANN, A.B.; STONE, L.F. Efeito da deficiência hídrica no desenvolvimento e rendimento de quatro cultivares de arroz de terras altas. Pesquisa Agropecuária Tropical, v.39, p.134‑139, 2009.
• HEINEMANN, A.B.; STONE, L.F.; SILVA, S.C. da. Arroz. In: MONTEIRO, J.E.B.A. (Ed.). Agrometeorologia dos cultivos: o fator meteorológico na produção agrícola. Brasília: Instituto Nacional de Meteorologia, 2009. p.63‑79.
• HOOGENBOOM, G. Contribution of agrometeorology to the simulation of crop production and its applications. Agricultural and Forest Meteorology, v.103, p.137‑157, 2000. DOI: 10.1016/S0168‑1923(00)00108‑8.
• INSTITUTO BRASILEIRO DE GEOGRAFIA E ESTATÍSTICA. Banco de dados agregados: Sistema IBGE de Recuperação Automática – SIDRA. 2010. Available at: <http://www.sidra.ibge.gov.br>. Accessed on: 26 June 2010.
• INSTITUTO RIO GRANDENSE DO ARROZ. IRGA [home page] 2008. Available at: <http://www.irga.rs.gov.br>. Accessed on: 20 Dec. 2008.
• KLERING, E.V.; FONTANA, D.C.; BERLATO, M.A.; CARGNELUTTI FILHO, A. Modelagem agrometeorológica do rendimento de arroz irrigado no Rio Grande do Sul. Pesquisa Agropecuária Brasileira, v.43, p.549‑558, 2008. DOI: 10.1590/S0100‑204X2008000500001.
• LEGATES, D.R.; MCCABE JUNIOR, G.J. Evaluating the use of "goodness‑of‑fit" measures in hydrologic and hydroclimatic model validation. Water Resources Research, v.35, p.233‑241, 1999. DOI: 10.1029/1998WR900018.
• LORENÇONI, R.; DOURADO NETO, D.; HEINEMANN, A.B. Calibração e avaliação do modelo ORYZA‑APSIM para o arroz de terras altas no Brasil. Revista Ciência Agronômica, v.41, p.605‑613, 2010. DOI: 10.1590/S1806‑66902010000400013.
• SILVA, S.C. da; ASSAD, E.D. Zoneamento de riscos climáticos para o arroz de sequeiro nos estados de Goiás, Mato Grosso, Mato Grosso do Sul, Minas Gerais, Tocantins e Bahia. Revista Brasileira de Agrometeorologia, v.9, p.536‑543, 2001.

Publication Dates

• Publication in this collection
  14 June 2013
• Date of issue
  Feb 2013

History

• Received
  08 May 2012
• Accepted
  28 Jan 2013