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Open Access 01-06-2025

Extreme weather events and crop diversification: climate change adaptation in Brazil

Authors: Elena Beatriz Piedra-Bonilla, Dênis Antônio Da Cunha, Marcelo José Braga, Laís Rosa Oliveira

Published in: Mitigation and Adaptation Strategies for Global Change | Issue 5/2025

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Abstract

This article delves into the critical relationship between extreme weather events and crop diversification in Brazil, emphasizing the need for adaptive strategies in the face of climate change. It examines how increased frequency and intensity of droughts, heavy rains, and heatwaves impact agricultural productivity and economic stability. The study reveals that crop diversification, including practices like intercropping, crop rotation, and agroforestry, can significantly enhance resilience and reduce the negative impacts of climatic shocks. By analyzing data from Brazilian municipalities, the article highlights regional variations in adaptation strategies and the potential future scenarios for agricultural diversification under different climate change projections. It underscores the importance of integrating socio-economic factors and public policies to support sustainable agricultural practices, providing a comprehensive overview of how Brazil can adapt to and mitigate the risks posed by extreme weather events.
Notes

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1 Introduction

Climate variability and the frequency and intensity of extreme events are expected to increase in some areas of the world (IPCC 2023). In Brazil, the frequency and intensity of drought have increased in the northern and northeast regions (Avila-Diaz et al. 2023). According to Ballarin et al. (2023), a reduction in the total amount of rain and the number of humid days is expected, and an increase in the number of consecutive dry days in different climate scenarios is proposed by the IPCC Sixth Assessment Report. In addition, an increase in heavy rain is expected in the Brazilian South and Southeast regions (Da Silva Tavares et al. 2023). There is also evidence of the increased frequency of heatwaves around Brazil, especially in the Semiarid region and the Amazon (Sanches et al. 2023; Avila-Diaz et al. 2023; Ballarin et al. 2023), as well as more severe and intense cold waves in most of the southern region (Marengo et al. 2023).
Furthermore, climate variability considerably impacts agriculture, especially in countries that depend on agricultural production. There is evidence that abiotic stress due to adverse climatic conditions reduces the productivity of crops in the main agricultural products in the world (Mittler 2006; Boyer 1982). According to Ray et al. (2015), the global variability in the productivity of important crops, such as corn, rice, wheat, and soy, depends, around 32% to 39%, on climate variation. Thus, studies that analyze how extreme weather affects agricultural production should be highlighted because this can impact the agricultural economies. A negative relationship exists between temperature and the Gross Domestic Product (GDP) levels in tropical countries, which depend economically on agriculture (Newell et al. 2021). Regarding Brazil, summer droughts have caused a decline in the GDP growth rate of the Northeast region, and summer floods have negatively affected the Northeast, Central-west, and Southeast, which are essential agricultural sectors (Tebaldi & Beaudin 2016). The economy could be vulnerable to climate variability in a country where the agribusiness sector had an average share of approximately 24% of the Brazilian GDP in 2023 (CEPEA 2023).
However, the negative impacts on agriculture due to extreme weather can be reduced if actions to adapt to climate change occur. In this way, crop diversification helps to reduce observed or projected climatic risks (Heal et al. 2014). Therefore, diversification will be considered an adaptive strategy that helps reduce negative impacts and takes advantage of positive effects to maximize the farmer's well-being. Crop diversification promotes economic benefits, such as reducing the variability of farmers' income (Chavas 2023) and reducing rural poverty (Renard and Tilman 2019). Additionally, diversification promotes agroecological services because the increased richness of crop species distributed in space and time decreases the susceptibility to diseases, pests, and weeds, reduces soil erosion, and improves soil fertility (Huss et al. 2022). These positive effects are related to different types of crop diversification, such as intercropping, double-cropping, crop rotation, crop-livestock integration or mixed farming systems, crop-livestock-forest integration or agroforestry (Piedra-Bonilla et al. 2020a, b). These are considered technologies that sustainably enhance resilience and reduce climate risks. For example, crop rotation can decrease crop yield losses caused by drought (Renwick et al. 2021) and yield gains in cereals with high temperatures and low precipitation levels (Marini et al. 2020). Similarly, agroforestry helps increase soil water storage even in drought conditions (Zhao et al. 2022) and mitigates floods (Baldwin et al. 2022). Moreover, intercropping cereals with legumes can enhance crop yield and resilience in situations such as deficit irrigation (Aslam et al. 2020; Amanullah et al. 2021). Simulation studies show that crop-livestock systems would present greater resilience under future climate change conditions (Peterson et al. 2020; Delandmeter et al. 2024).
Regarding climate variables, most research indicates statistically significant effects on crop concentration. Research converges on the positive impacts of temperature variables on diversification, including their different units of measurement. However, precipitation shocks show ambiguous results (Seo and Mendelsohn 2008; Dillon et al. 2015; Asfaw et al. 2018; Arslan et al. 2018). These results depend on the geographical conditions of the regions. However, scant empirical evidence exists on how farmers respond to extreme weather, especially using the climate extreme indices. Thus, the present work intends to focus on the effect of extreme weather in the recent past and the future climate change scenarios on crop diversification.
Dealing with this topic in Brazil is especially important since the country is one of the world's main food producers and exporters (FAO 2018). Furthermore, Brazilian agriculture is heterogeneous around its regions. According to Piedra-Bonilla et al. (2020a, b), small farms (0 to 10 ha) in regions such as the South, Mid-West, and North are conducive to crop diversification. However, the Mid-West region, the area of grain production, tends to crop specialization. In this context, research that makes it possible to understand land-use changes due to the concentration of agricultural activities is essential. In addition, we can examine adaptive responses to the adverse effects of extreme weather on Brazilian agriculture. Understanding these responses in agricultural adaptation is crucial for prioritizing crop diversification investments and designing risk-mitigating strategies depending on the type of extreme event. The results may support the development of public policies to reduce climate vulnerability through rural extension services or credits.
In this sense, this paper has two main objectives: first, to identify the impact of extreme weather on crop diversification in Brazilian municipalities in the recent past. Events of climate variability include, specifically, frosts in the south region, droughts, heavy rains, and hot days. It uses a fixed-effects panel model for 3818 Brazilian municipalities. The results indicate that increasing consecutive dry days (CDD), dry days, and hot days positively affect crop diversification. This study also understands the effect of future climate change scenarios on the diversification of municipal agricultural production. The results show that the increase in the percentage of hot days in 2045–2065 would increase crop diversification in both scenarios RCP4.5 and RCP8.5 of climate change. The analysis of the impact of extreme climate events on agricultural diversification could help to understand when this practice becomes relevant to be promoted through technical assistance, credit, or research.
The paper is divided into five sections, including this Introduction. The second section presents the empirical strategy, the econometric model, the future simulation specifications, and the data source. The third section presents the empirical results, while Sect. 4 presents a discussion and explores policy implications. Finally, Sect. 5 presents the conclusions.

2 Empirical Strategy

In this study, we used a panel data model. Data at the Minimum Comparable Area1 (MCA) level (cross-section) were combined with the years of agricultural censuses 95/96, 2006, and 2017 (time series). In this way, greater precision is obtained in the estimates, the possibility of consistent estimation of models that allow unobserved effects potentially correlated with the regressors, and the possibility of learning more about the dynamics of individual behavior (Cameron and Trivedi 2005). Thus, using panel data made it possible to study the dynamics of crop diversification over the period considered in the study, as well as the effects of climate on these dynamics.
Agricultural diversification at the regional level is an aggregate response to individual farmers' crop choice decisions. This immediate allocation of crops responds to several factors, such as climate variables (Asravor 2018; Rahman 2016). To determine the causal relationship between climate variability and crop diversification, it would be necessary to carry out a natural experiment that would make the farmer's choice of crops a random decision. So, extreme weather can be considered an ideal experiment since climate anomalies cannot be predicted precisely. This can also cause exogenous and random variations in the farmers' decision to allocate crops, affecting crop diversification at the municipal level. Then, it was possible to compare the diversification of the municipalities and to know the effect of extreme events without having problems of selection bias (Piedra-Bonilla et al. 2020a, b). Therefore, the equation of interest was the impact of the extreme weather on crop diversification:
$$S=f(C, X)$$
(1)
in which vectors of climate variables (C) and control variables (X) affected the Brazilian municipal crop diversification. The climate specifications include five-year moving averages of extreme climate indices for each period of the Agricultural Census 95/96, 2006, and 2017. The five-year moving average was chosen to consider the impact of the medium-term climate on perennial and temporary crops because a more extended period could dilute the effect on these crops (Piedra-Bonilla et al. 2020a, b). This study considers the following extreme events: frosts, droughts, hot days, and extreme precipitation days because they are linked to abiotic stresses in agriculture (Taiz and Zeiger 2006). Thus, five extreme climate indices were used, recommended by the World Meteorological Organization—WMO's Expert Team on Sector-Specific Climate Indices (ET-SCI) for the agriculture sector. The definition of the extreme climate indices for this study is presented in Table 1. These indices were calculated using daily values of precipitation and maximum and minimum temperature with data from the Terrestrial Hydrology Research Group (THRG) (Sheffield et al. 2006), obtaining results of annual values considering the base period (1985–2016) and using standardized software (ClimPACT2) (Alexander & Herold 2015). The base period was considered a minimum period of 30 years that included agricultural census periods.
Table 1
Definition of extreme weather indices
Index code
Name
Definition
Unit
Event type
FD
Frost days
Annual count of days when TN < 0ºC
Days
Frosts
CDD
Consecutive Dry Days
Maximum number of consecutive days with PR < 1,0 mm
Days
Maximum length of dry spell
Rn1mma
Number of dry days
Annual count of days when PR < 1,0 mm
Days
Dry days
R20mm
Number of very heavy rainy days
Annual count of days when PR ≥ 20 mm
Days
Extreme precipitation days
TX90p
Amount of hot days
Percentage of days when TX > 90th percentile
%
Hot days
TN minimum temperature, TX maximum temperature, PR precipitation
a. The Rnnmm index originally indicates the number of personalized rainy days in which rainfall has a minimum number of mm specified by the user to account for rainy days. We adapted to quantify dry days in the Rn1mm index. However, there is a caveat of showing rain where there is not since there are pixel resolution problems
Source: Adapted from Alexander and Herold 2015
The daily available temperature and precipitation data were up to 2016. The data source section provides more details.

2.1 Extreme events

Frost days (FD) were considered only for the South region since it is located below the tropical zone, and frost is commonly found in winter (Bitencourt et al. 2020; Wrege et al. 2018). Figure 1.a shows the erratic behavior of frosts in the southern region of Brazil over three periods (1987–1996, 1997–2006, and 2007–2016). We also used the consecutive dry days (CDD) and the number of dry days (Rn1mm) to analyze the effect of prolonged drought and intermittent drought on agricultural diversification, respectively (Table 1). Severe drought conditions can cause premature plant death, while batch drought conditions affect plant growth and development (Oshunsanya et al. 2019; Kopecká et al. 2023). In Brazil, the drought due to the severe El Niño phenomenon (2015–2016) caused high mortality of cocoa trees (15%) and decreased cocoa yield by 89% in Bahia (Gateau-Rey et al. 2018). The severe drought in 2012–2013 in Ceará led to a 43% reduction in planted area, resulting in average losses of 75% in crops, and caused losses in livestock, with the cattle herd mortality rate of 0.33% in 2010 to 3.05% in 2013 (Ceará, 2013). Figure 1.b shows the expansion of drought periods between 30 and 61 days in the Midwest, Southeast, and South regions, while the Northeast shows an increase in the dispersion of high CDD values (> 122 days) over the 1987–2016 years. Figure 1. c highlights that the days without precipitation have increased in the North and Center-West. Conversely, Fig. 2.d shows the decrease in very heavy rainy days from 2007 to 2016. Flood-sensitive crops are harmed, considerably reducing their productivity.
Fig. 1
Extreme climate indices in Brazil over 1987–1996, 1997–2006, and 2007–2016. Source: Research results based on data from the Global Meteorological Forcing Dataset for land surface modeling using the methodology of Sheffield et al. (2006)
Fig. 2
Evolution of agricultural diversification (Simpson Index) in 1995/1996, 2006, and 2017 Agricultural Censuses.
Source: Research results
Furthermore, prolonged exposure to extreme temperatures, significantly during flowering, harms most plants, which can cause losses in agricultural production (Taiz and Zeiger 2006). In Brazil, the study by Gusso et al. (2014) showed that heatwaves can increase the effects of drought and reduce soybean productivity in the South. Thermal stress also affects livestock production. For example, severe exposure to thermal stress can cause reductions in productivity (20%) of cow's milk in southern Brazil (Garcia et al. 2015). Figure 2.e shows that the number of hot days has increased over the three periods (1987–1996, 1997–2006, and 2007–2016), especially in the last period (2007–2016).
Although abiotic stresses in agriculture can significantly impact crops' phenological cycles (Oshunsanya et al. 2019; Kopecká et al. 2023) and analyzing extreme events within a single year might provide valuable insights, the overall perspective over multiple years can offer a more comprehensive understanding. Considering a broader timescale, as well as understanding climate conditions and future projections (Oshunsanya et al. 2019), can help assess the long-term effects of these events on crops, allowing for better planning and adaptation strategies to mitigate their adverse impacts. Thus, while immediate correlations between extreme events and crop phenology are vital, a temporal view provides a more robust grounding for agricultural planning and management.

2.2 Econometric model

The empirical analysis was based on a panel econometric model with fixed effects in which the agricultural diversification of Brazilian municipalities is affected by the climate and other socioeconomic, agricultural, and market characteristics. This approach follows a general model developed by Benin et al. (2004) and Van Dusen & Taylor (2005). Thus, the complete version of the equation of interest (1), previously presented, is:
$${S}_{it}={\beta C}_{it}+\gamma {SE}_{it}+\delta {A}_{it}+{\zeta M}_{it}+{\mu }_{i}+{\theta }_{rt}+{\varepsilon }_{it},$$
(2)
which \({S}_{it}\) represents the Simpson crop diversification index in municipality \(i\) and year \(t\), \({C}_{it}\) represents various specifications of extreme weather in municipality \(i\) and year \(t\). \({SE}_{it}\) is the vector of the socioeconomic characteristics of the municipality \(i\) and year \(t\), \({A}_{it}\) is the vector of the agricultural characteristics of the municipality \(i\) and year \(t\), \({M}_{it}\) is the vector of the market characteristics of the municipality \(i\) and year \(t\), \({\mu }_{i}\) represents the effects municipalities, capturing fixed spatial characteristics, observed or not, removing the shock of many possible sources of omitted variable bias (Dell et al. 2014). \({\theta }_{rt}\) represents the fixed effects of year \(t\) and state \(r\), neutralizing any common state trends and ensuring that relationships of interest are identified by idiosyncratic local shocks. \({\varepsilon }_{it}\) is the independent and identically distributed error term (iid) in municipality \(i\) and year \(t\), with mean 0 and variance σ. The fixed-effects model proved to be the most suitable after testing the model specification, heteroscedasticity, and autocorrelation using the Hausman, Modified Wald, and Wooldridge tests, respectively (Table 3).
The Simpson index is adapted from ecological species diversity indexes, representing species concentration (Magurran 2004). This index considers how much each on-farm activity contributes to the total on-farm income of the municipality (Sambuichi et al. 2016). Thus, we considered agricultural, livestock, and forestry products:
$$\begin{array}{cc}{S}_{t}=1-{\sum }_{j=1}^{N}{\alpha }_{k}^{2}& 0\le {S}_{t}\le 1\end{array}$$
(3)
where \({\alpha }_{k}\) is the proportion of the Gross Value Production of each agricultural, livestock, and forestry product in the municipality's total on-farm Gross Value Production in t year. Agricultural products can be classified into two types: temporary and permanent crops. Temporary crops are grown for a short period, usually less than a year. These crops need to be replanted after each harvest. On the other hand, permanent crops last for several years and do not need to be replanted after harvesting. Crop diversification involves the possibility of growing successive or simultaneous crops (simple or intercropping) in the same location and year. Livestock products include cattle, pigs, and poultry in each municipality every year. Forestry products include planted forests and plant extraction, which involves extracting native forest resources.
In the Simpson index, 1 indicates perfect diversification, and 0 indicates perfect specialization (a single product). According to Sambuichi et al. (2016), there are four categories of crop diversification. The first category is Very Specialized (\(S=0\)), which includes municipalities that produce only one product. The second category is Specialized (\(0<S\le 0.35)\), which includes municipalities where at least 80% of income depends on one product, although they also produce other products. The third category is Diversified ((\(0.35<S\le 0.65)\), where a single product represents less than 80% of income. Lastly, the fourth category is Very Diversified (\(S>0.65)\), indicating that at least three products are produced with similar weights in income.
Six specifications were used for climate variables to analyze the effect of extreme weather events (\({C}_{it}\)):
i.
Frosts: five-year moving average of the FD index and the five-year moving average of winter precipitation since there is a correlation (0.52 ***) between temperature and precipitation (Auffhammer et al. 2013). We used winter precipitation because most of the frosts occur in that season. These variables were only used for the South region.
 
ii.
Maximum length of dry spell: the five-year moving average of the CDD index and the five-year moving average of the annual average temperature. The correlation between these two variables was 0.35 ***.
 
iii.
Dry days: the five-year moving average of the Rn1mm index and the five-year moving average of the annual average temperature. The correlation between these two variables was 0.01*.
 
iv.
Extreme precipitation days: the five-year moving average of the R20mm index (number of very heavy rain days) and the five-year moving average of the annual average temperature. The correlation between these two variables was −0.37 ***.
 
v.
Hot days: the five-year moving average of the TX90p index (number of hot days) and annual accumulated precipitation. The correlation between these two variables was −0.12 ***.
 
The independent variables were measurements of the vectors shown in the right part of the equation (2), according to the Summary Statistics in Table 2. The technical assistance variable is considered an essential resource for disseminating information on agricultural practices (Rahman 2016), which can influence the adoption of new technologies and diversifying cultures. Benin et al. (2004) state that large farms can produce more crops. The irrigation variable can decrease diversity through uniform humidity conditions (BENIN et al. 2004) and be an investment directed to intensive crops. In the market variable, the number of farms that produce corn was used, which was considered a proxy to control the effect of the demand for the main crops. The value of soy production was not considered because only 1877, 1360, and 1832 Brazilian municipalities in the 1995/1996, 2006, and 2017 censuses, respectively, reported these data, causing a considerable loss of observations. However, most Brazilian corn production is carried out in double-cropping systems (soybean-corn) (Abraão; Costa, 2018), so we indirectly consider soybean.
Table 2
Summary Statistics
Variable
1996
2006
2017
Mean
SD
Mean
SD
Mean
SD
Simpson Index
0.69
0.20
0.61
0.22
0.63
0.21
Socioeconomic characteristics
    
Technical assistance (unit)
238.62
494.99
299.25
556.35
262.99
488.34
Legal status of farms (unit)
941.76
1390.97
1031.22
1563.97
1072.78
1739.89
Agricultural characteristics
     
Farm size (ha)
95.62
178.97
77.18
135.03
77.62
127.05
Irrigation (unit)
74.26
180.83
86.76
216.69
132.04
335.30
Market characteristics
     
Maize farms (unit)
663.61
1187.94
530.45
983.90
432.35
863.44
Climate characteristics
     
FD (days)
0.10
0.36
0.02
0.09
0.26
0.77
Rn1mm (days)
229.62
35.29
227.05
34.74
208.48
33.58
R20mm (days)
17.86
8.02
16.45
7.03
8.20
7,0.94
TX90 (% days)
7.07
2.96
9.96
4.19
19.95
14.84
CDD (days)
36.80
23.86
33.74
21.31
41.01
27.75
Annual temperature ºC
23.77
2.60
24.16
2.54
24.06
2.66
Annual rainfall (mm)
1407.93
469.22
1359.94
424.30
1337.29
511.09
Source: Research results

2.3 Simulations of the impact of climate change on crop diversification

To analyze how the diversification of municipal agricultural production will respond in future periods to the climate change scenarios expected by the IPCC, we simulated the consequences of these scenarios on crop diversification behavior, using the parameters estimated by the equation of interest of this research (1) (Seo and Mendelsohn 2008). Thus, according to Eq. (4), the crop diversification index of the Brazilian municipalities (\({\widehat{S}}_{iBASE}\)) was estimated, considering extreme climate indexes projected for the base year (\({C}_{i,BASE}\)), along with the parameters estimated by Eq. (2):
$${\widehat{S}}_{iBASE}={\beta C}_{i,BASE}+\gamma {SE}_{it}+\delta {A}_{it}+{\zeta M}_{it}+{\mu }_{i}+{\theta }_{rt}+{\varepsilon }_{it}$$
(4)
The base year was the last year of the period included in this study, 2016. This way, the existing bias between the expected ​​and observed values ​​of the considered climatic variables was eliminated. In addition, the estimate was made between 1986 and 2005, the base period specified by the IPPC's Fifth Assessment Report (AR5). The baseline scenario assumes that farmers will continue producing their crops if the climate remains unchanged. In other words, no other possible reasons have been modeled for why the choice of cultures may change in the future. Only the effects of climate change were observed separately from the effects of the other variables, although the other variables are expected to vary over time (Seo and Mendelsohn 2008).
Then, the agricultural diversification index (\({\widehat{S}}_{iFUTURE}\))) was estimated, considering the temperature and precipitation averages and the extreme climate indices projected for future scenarios (\({C}_{i,FUTURE}\)), established by the IPCC (2013) for the averages of two periods: beginning (2016–2035) and mid (2046–2065) of the twenty-first century, according to the following equation:
$${\widehat{S}}_{iFUTURO}={\beta C}_{i,FUTURO}+\gamma {SE}_{it}+\delta {A}_{it}+{\zeta M}_{it}+{\mu }_{i}+{\theta }_{rt}+{\varepsilon }_{it}$$
(5)
When using the parameters estimated in Eq. (5) to estimate the future crop diversification index, we assumed that the relationship between climatic variables and the diversification index would remain constant until the last future period used in the simulations. We used average data for periods to avoid using a year projection with an outlier. Finally, the rate of change in diversification was calculated in response to changes in temperature and precipitation expected by the following equation:
$$\%\Delta {S}_{it}=\frac{({\widehat{S}}_{iFUTURE}-{\widehat{S}}_{iBASE})}{{S}_{iBASE}}\times 100$$
(6)
Thus, we examined a set of climate change scenarios predicted by the IPCC based on population size, economic activity, lifestyle, energy use, land use patterns, technology, and climate policy. The projections used in this study were based on Representative Concentration Pathways (RCPs), which were used to make projections according to the abovementioned factors. The RCPs describe four categories of Greenhouse Gas (GHG) emissions and atmospheric concentrations, air pollutant emissions, and land use. These categories include a rigorous mitigation scenario (RCP2.6), two intermediate scenarios (RCP4.5 and RCP6.0), and a scenario with very high GHG emissions (RCP8.5). Scenarios without additional efforts to constrain emissions ("baseline scenarios") lead to paths that vary between RCP6.0 and RCP8.5. RCP2.6 represents a scenario that aims to keep global warming below two °C above pre-industrial temperatures (IPCC, 2013). For this research, the future scenarios for the simulations were RCP4.5 and RCP8.5, as they represent intermediate and extreme climate change projections.
To perform the simulations for the scenarios RCP4.5 and RCP8.5, we obtained the climate data from three General Circulation Models (GCM): HadGEM2-ES—Hadley Center Global Environmental Model version 2; MIROC-ESM—Model for Interdisciplinary Research on Climate; and MRI-CGCM3—Meteorological Research Institute Coupled Atmosphere – Oceans General Circulation Model version 3. According to Pires et al. (2016), the HadGEM2-ES model can correctly simulate precipitation seasonality in several Brazilian regions, according to simulated historical precipitation evaluations.

2.4 Data source

The data for constructing the Simpson Index were extracted from the Agricultural Censuses 1995/1996, 2006, and 2017 from the Brazilian Institute of Geography and Statistics – IBGE (IBGE 2017). We considered the Gross Value Production of horticulture, permanent crops, temporary crops, forestry, and plant extraction and the Gross Value Sold of heads of cattle, pigs, and poultry at the municipal level. However, several MCAs did not display data on agricultural products at all periods, resulting in an unbalanced panel. Data on agricultural, livestock, and forestry products were extracted from the 1995/1996 Census of Agriculture, resulting in 3,809 MCAs, constituting 3,798 MCAs and 3,813 MCAs in 2006 and 2017, respectively.
The daily georeferenced maximum and minimum temperature and precipitation data were extracted from the Terrestrial Hydrology Research Group (THRG) following the methodology of Sheffield et al. (2006) using the Coupled Model Intercomparison Project 5 (CMIP52). The database was built by combining global data based on surface observations with the NCEP – NCAR (National Center for Environmental Prediction / National Center for Atmospheric Research) reanalysis. The original data used have a resolution of 0.25º × 0.25º (spatial resolution 28 km) of daily precipitation (mm) and daily temperature (C) for the period from 1985 to 2016. However, for the analysis at the MCA level, the data were interpolated to a resolution of 30 m. It is worth mentioning that the temperature and precipitation data provided by THRG are up to 2016. Thus, the impact of the climate did not consider the year 2017. However, the moving averages from five years ago can model the farmers' crop choices concerning climate variability (Cho and McCarl 2017).
The data for the socioeconomic, agricultural, and market characteristics of the Brazilian municipalities were also extracted from the Agricultural Censuses 1995/1996, 2006, and 2017.
Future climate data were extracted from the General Circulation Models: HadGEM2-ES, MIROC-ESM, and MRI-CGCM3. Like the observed climatic data, the future data used have a resolution of 0.25º × 0.25º of daily precipitation (mm) and daily temperature (C) from 2016 to 2065.

3 Results

3.1 Descriptive statistics

Table 2 summarizes the data for the variables in Eq. (2) for the years 1996, 2006, and 2017. Regarding the variables of socioeconomic, agricultural, and market characteristics, it is noteworthy that the mean of producers with the legal status of the farm has increased. The number of producers who received technical assistance increased in 2006 but declined slightly in 2017. In addition, the average farm size decreased over the period, and at the same time, the number of farms with corn production in 2017 was reduced by more than 55% compared to 1996. In the last three decades, corn production has been concentrated in regions with higher productivity, especially in the Midwest, South, and the MATOPIBA3 area (Oliveira & Gasques 2019).
The Simpson index decreased over the years of interest, showing only a slight increase in 2017. The Brazilian crop diversification rate decreased by −8.7% from 1996 to 2017. However, despite the decreasing trend, the index values ​​were still found in the Diversified category. Furthermore, the regions showed changes in crop diversification (Fig. 2). The South and Northeast regions maintained the highest values ​​of diversification in the three Agricultural Censuses, while the Mid-West region maintained the opposite. These results are related to the farm size because the South and Northeast regions have a strong presence of family farming with small production, contrary to the Midwest region, which has large farms specialized in a few cultures (De Castro 2014).
Regarding the climate variables, it is worth noting that the moving averages of dry days (below 1 mm of precipitation daily) decreased slightly in Brazil. Likewise, the days with heavy rain decreased considerably in the last period. Nevertheless, hot days grew considerably, especially in 2017, increasing by around 182% compared to the 1996 moving average. Similarly, the consecutive dry day moving average has increased. On the other hand, the moving averages of frosts in the South region have also been increasing. The means of annual temperature are similar over the period, but the annual rainfall has decreased in the same period.

3.2 Impacts of extreme weather events on crop diversification

Table 3 shows the effects of extreme weather events on crop diversification in Brazil for the first time. It is seen that there were very few differences between the models with controls and any controls in terms of the values of the coefficients of the weather indexes, which shows that the relationship between extreme events and crop diversification in Brazilian municipalities is treated randomly. In models (1) and (2), it was observed that frosts (FD) had a negative relationship with crop diversification in the South, but the variable was not statistically significant. Nevertheless, this was the only weather extreme index that shows significance considering nonlinear effects and interaction terms between some climate variables on crop diversification, as shown in Table 9 in the Appendix. So, the change in crop diversification depends on the amounts of frost days; the effects of FD are not constant.
Table 3
Effects of extreme weather indices on crop diversification in Brazil
Variable
(1)
(2)
(3)
(4)
(5)
(6)
(7)
(8)
(9)
(10)
Technical assistance
1.45e-05
 
9.22e-06
 
1.91e-05**
 
1.96e-05**
 
2.00e-05**
 
 
(1.00e-05)
 
(7.75e-06)
 
(8.36e-06)
 
(8.32e-06)
 
(8.36e-06)
 
Legal status of farms
2.85e-06
 
4.01e-06
 
−3.20e-06
 
−2.46e-06
 
−2.51e-06
 
 
(1.40e-05)
 
(3.80e-06)
 
(4.30e-06)
 
(4.31e-06)
 
(4.30e-06)
 
Irrigation
4.14e-05
 
3.90e-05***
 
1.52e-05
 
1.34e-05
 
1.38e-05
 
 
(3.96e-05)
 
(1.04e-05)
 
(1.01e-05)
 
(9.99e-06)
 
(1.00e-05)
 
Farm Size
−0.000284
 
−0.000236***
 
−0.000243***
 
−0.000245***
 
−0.000243***
 
 
(0.00030)
 
(3.53e-05)
 
(3.56e-05)
 
(3.59e-05)
 
(3.58e-05)
 
Maize farm
6.34e-06
 
6.21e-06*
 
1.19e-05***
 
1.21e-05***
 
1.18e-05***
 
 
(8.71e-06)
 
(3.32e-06)
 
(3.80e-06)
 
(3.82e-06)
 
(3.80e-06)
 
FD
−0.00541
−0.00579
        
 
(0.00496)
(0.00504)
        
CDD
  
0.000161*
0.000142
      
   
(9.46e-05)
(9.59e-05)
      
Rn1mm
    
0.000229***
0.000244***
    
     
(7.82e-05)
(7.97e-05)
    
R20mm
      
−1.20e-05
−3.41e-05
  
       
(0.000358)
(0.000361)
  
TX90p
        
0.000704***
0.000729***
         
(0.000179)
(0.000180)
Annual temperature
  
0.00182*
0.00138
0.00346***
0.00355***
0.00371***
0.00380***
  
   
(0.00103)
(0.00104)
(0.00107)
(0.00108)
(0.00109)
(0.00110)
  
Annual rainfall
        
−3.93e-06
−4.15e-06
         
(6.63e-06)
(6.69e-06)
Winter precipitation
0.000178*
0.000188*
        
 
(0.00010)
(0.000103)
        
Constant
0.681***
0.685***
0.648***
0.650***
0.508***
0.493***
0.550***
0.538***
0.630***
0.621***
 
(0.0249)
(0.00838)
(0.0250)
(0.0242)
(0.0299)
(0.0298)
(0.0278)
(0.0273)
(0.0124)
(0.0110)
Fixed effects state/year
YES
YES
NO
NO
YES
YES
YES
YES
YES
YES
Hausman test
3008.26***
-
137.48***
96.27***
1263.87***
29352.***
8835.13***
28029.52***
83.86***
24936***
Modified Wald test
9.5e + 30***
6.5e + 30***
5.7e + 32***
3.1e + 32***
2.0e + 61***
6.6e + 5***
1.0e + 61***
1.0e + 61***
2.0e + 61***
1.0e + 6***
Wooldridge test
1.997
0.809
1.429
0.982
2.204
1.803
1.048
0.765
1.270
1.012
N
2,009
2,009
11,42
11,42
11,42
11,42
11,42
11,42
11,42
11,42
R-squared
0.088
0.083
0.083
0.072
0.144
0.136
0.143
0.135
0.144
0.136
F Statistic
12.75***
17.59***
11.34***
19.44***
236.09***
163.86***
237.29***
26.51***
236.66***
84.24***
Number of MCA
671
671
3,818
3.818
3,818
3,818
3,818
3,818
3,818
3,818
Robust standard errors are in parentheses. Significance: *** p < 0,01, ** p < 0,05, * p < 0,1
Considering the 3,818 MCAs from Brazil, in the mean, the consecutive dry day’s index (CDD) positively affected crop diversification at the 10% significance level in the model (3) with controls. This model only used fixed effects of year and municipalities (Table 2). However, specific models for each region show that the North and South regions exhibit no significant effect of Dry Spells (Table 5 in Appendix), possibly because, as shown in Fig. 1.c, these regions experienced fewer days with consecutive dry days. Moreover, the southeast region has a negative effect. The dry day’s variable (Rn1mm) was also positive and statistically significant at 1% in models (5) and (6), considering all the MCAs (Table 3). We found similar results in specific models for the northeast, southeast, and south regions. Nevertheless, it was not statistically significant in the models of the Northern region (Table 6 in Appendix), which has fewer days without rainfalls (Fig. 1.c). In the models of the Midwest region, the effects were negative, with a p-value less than 0.5 (Table 6 in Appendix).
The very rainy days (R20mm) negatively affected crop diversification; however, it was not statistically significant in models (7) and (8) considering the whole country. This result may be related to the fact that measures to reduce the negative effects of extreme precipitation days are more linked to other methods, such as flood forecasting systems, channel infrastructures, and, or agricultural drains, and the location of the productive systems that avoid being in areas of recurrent flooding. Despite this, the models of the Southeast region indicate the R20mm index significantly positively impacts crop diversification, contrary to the models of the Northeast regions, where the effects are negative (Table 6 in Appendix). This result may be explained since the Northeast region is associated with less rainfall (Figs. 1 b and c). The Brazilian semi-arid region occupies most of the northeast region and is associated with prolonged droughts. Between 2012 and 2015, the drought intensified, and in terms of future projections, a trend toward more extended periods with consecutive dry days (CDD) is expected in this region (Marengo et al., 2017).
On average, the increase in the amount of Hot Days (TX90p) produces an increase of 0.000704 and 0.000729 in the level of diversification in models (9) and (10), respectively. The coefficients of the variable of interest (TX90p) were higher than the rest. Similarly, the results by Dillon et al. (2015) revealed that the number of crop groups harvested positively correlates with the degree days shocks. In the same way, the specific models for the Northeast and Southeast regions show positive effects on crop diversification (Table 8 in Appendix). On the contrary, the models of the Midwest region exhibit negative effects, where there was less crop diversification (Fig. 2).
Generally, it is emphasized that some controls, such as technical assistance, size of the farm, and the demand Proxy for important crops (corn), were statistically significant in all models, except for the frosts. Therefore, they are important factors in the allocation of crops in Brazil. Access to technical assistance and corn production positively affected diversification across all models. Thus, the role of rural extension services becomes important, especially on small farms, to disseminate agroecological practices that are resilient to extreme weather events, which are expected to increase in intensity and frequency in the future. Furthermore, the results show that diversification is not contrary to the production of main crops, such as corn.
Furthermore, it was observed that the farm size negatively influences diversification in all estimated econometric models (except when the model includes frosts). Then, the small producer is more likely to diversify to reduce its income variability, which is much greater than the large one, which is less vulnerable to shocks in its agricultural production. For detailed effects of the control by region, please refer to Tables 5, 6, 7 and 8 the Appendix.

3.3 Future projections of the impact of climate change on agricultural diversification

For the analysis, only the extreme weather events that obtained statistically significant coefficients in the models estimated in the previous section were considered, such as consecutive dry days (CDD), dry days (Rn1mm), and hot days (TX90p). We did not project future scenarios for frosts (FD) in the South as the effects are not constant in nonlinear analyses and have no significance in linear regression. Similarly, there were no statistically significant effects on diversification for very rainy days (R20mm) in Brazil.
Figure 3 shows the expected evolution (2016–2065) of Brazil's average annual temperature and accumulated precipitation. It is noteworthy that there is an increasing temperature trend in the three projections of the global climate models (HadGEM2-ES; MIROC-ESM and MRI-CGCM3) and the two GHG emissions scenarios (intermediate—RCP4.5 and extreme—RCP8.5). The MRI-CGCM3 projections show the worst temperature scenario and the lowest accumulated precipitation values compared to other climate models. According to the IPCC (2023), there is expected to be an increase in the frequency and occurrence of compound heatwaves and droughts, which may happen simultaneously in multiple locations. We also observed no trend in the expected evolution of annual accumulated precipitation. The changes in precipitation will not be uniform throughout the twenty-first century. However, an increase in the contrast in precipitation between wet and dry regions and between rainy and dry seasons is expected (IPCC, 2013).
Fig. 3
Expected evolution of the average annual temperature (ºC) and accumulated precipitation (mm) in Brazil (2016–2065). Source: Research results, based on data from HadGEM2-ES - Hadley Center Global Environmental Model version 2; MIROC-ESM - Model for Interdisciplinary Research on Climate; MRI-CGCM3 - Meteorological Research Institute Coupled Atmosphere-Ocean General Circulation Model version 3
To simulate the impacts of climate change on future crop diversification in Brazil, we used the statistically significant estimates of the parameters in the previous section. Thus, the CDD, Rn1mm, and TX90p indices were considered. Most of the simulations with the climate specifications were obtained from the estimated coefficients of the econometric models that included the fixed effects for municipalities and state/year since they showed better adjustment, according to Eq. (2), except for the CDD model. Finally, the base (\({\widehat{S}}_{iBASE}\)) and future (\({\widehat{S}}_{iFUTURE}\)) crop diversification indices were estimated using Eqs. (4) and (5), respectively.
Table 4 summarizes the impact of climate change on crop diversification in Brazil in the periods 2016–2035 and 2046–2065 in the three projections of the General Circulation Models (HadGEM2-ES; MIROC-ESM and MRI-CGCM3) and two scenarios of GHG emission (RCP4.5 and RCP8.5). The results were calculated using Eq. (6) of the rate variation in crop diversification (\(\%\Delta {S}_{it}\)) considering CDD, Rn1mm, and TX90p indices projected for the base year and future scenarios. Additionally, the t-test was applied to compare the equality of means in the variation of diversification between different climate specifications in both emission scenarios. The specification of hot days was chosen as a basis for comparison with the other climatic variables since the estimated coefficients of the TX90p index were statistically significant at 1% in Table 3, as well as that there is a high probability that the maximum extreme temperatures will be more frequent (IPCC 2023). Notably, most cases have no statistically significant difference in the means. Thus, the econometric models used in the simulations are shown to be robust.
Table 4
Effect of climate change scenario on the variation in crop diversification ( \(\%\Delta {S}_{it}\)) in Brazil
Climate models
Rate variation crop diversification (\(\%\Delta {S}_{it}\))
CDD
Rn1mm
TX90p
RCP4.5
RCP8.5
RCP4.5
RCP8.5
RCP4.5
RCP8.5
2016–2035
      
HadGEM2-ES
0.212
−0.037
9.462
0.062
0.427
0.599
 
(0.542)
(0.488)
(520.197)
(1.649)
(11.57)
(239.048)
MIROC-ESM
−0.293
0.387
0.027
−0.213
−0.087
−1.069
 
(0.538)
(0.583)
(1.754)
(40.744)
(20.474)
(87.886)
MRI-CGCM3
0.04
−0.2***
−0.199
−0.42***
−0.35
−0.06***
 
(0.467)
(0.713)
(7.144)
(3.886)
(23.564)
(1.444)
Mean
−0.014
0.038
3.097
−0.189
−0.003
−0.176
 
(0.289)
(0.291)
(173.329)
(12.981)
(11.713)
(30.266)
2046–2065
      
HadGEM2-ES
0.724
0.545
20.111
1.172
1.317
1.368
 
(0.831)
(0.614)
(1141.966)
(4.217)
(25.165)
(53.669)
MIROC-ESM
−0.117*
0.82
0.304
−0.583
0.623
−0.026
 
(0.584)
(0.799)
(3.069)
(137.809)
(26.557)
(121.3)
MRI-CGCM3
0.324***
0.437***
0.515***
0.873***
0.932
1.541
 
(0.562)
(0.728)
(3.888)
(8.908)
(2.178)
(7.922)
Mean
0.31***
0.600
6.977
0.487
0.957
0.961
 
(0.404)
(0.487)
(380.693)
(48.934)
(12.429)
(47.792)
The results indicate that in 2016–2035, crop diversification in Brazil would increase little and even decrease, especially in the extreme scenario (RCP8.5). In the results of the simulations presented in Table 4, it is observed that the increase in the rate of hot days in the first period could lead to a slight decline in the level of diversification of −0.003% and −0.176% in the scenarios RCP4.5 and RCP8.5, respectively. To illustrate, Fig. 4 shows the diversification changes that could occur in the early and mid-twenty-first century under future TX90p climate scenarios. The TX90p index was chosen as the main analysis specification because the increase in temperature is the global trend with the highest probability of occurrence.
Fig. 4
Rate variation in crop diversification in Brazil under future TX90p climate scenarios. Note: The values were calculated from the average of the three projections of the global climate model (HadGEM2-ES; MIROC-ESM and MRI-CGCM3) and in two emission scenarios (RCP4.5 and RCP8.5) from the calculated averages of the TX90p index.
Source: Research results
On the other hand, in 2045–2065, diversification would have a positive variation, albeit of low magnitude, in most cases (Table 4). In simulations of the TX90p increment, the average percentage variation of crop diversification would be 0.957% and 0.961% in the scenarios RCP4.5 and RCP8.5, respectively. As shown in Fig. 4, the greatest increase in diversification in this period would occur in the scenario of global warming with high GHG emissions (RCP8.5). It is also notable that the greatest rate variation in the level of crop diversification would occur in the Midwest and North regions.
In general, it is observed that the scenario without additional efforts to restrict GHG emissions (RCP8.5) predicts the lowest values ​​in the rate variation of diversification in the first period. In contrast, the variation would show the highest values in the second period. Municipalities would tend to diversify further as the climate scenario becomes more severe. Additionally, the HadGEM2-ES model anticipates the highest percentage values ​​in the variation of diversification in both periods and emission scenarios.
Standard deviations are in parentheses; Significance in the difference between model means: *** p < 0.01, ** p < 0.05, * p < 0.1. Source: Research results

4 Discussion

Regarding the impact of frosts in the South, non-statistically significant parameters can be justified since the diversification strategy is not considered standard practice to manage this type of risk. It would imply, above all, using species or varieties that are tolerant at low temperatures or trees with taller species to help reduce heat-related losses. This would limit the selection of species diversity only for that extreme climatic event. Thus, crop diversification is not the primary strategy to mitigate the risks of frosts. Additionally, we found ambiguous results in nonlinear analyses.
Regarding prolonged droughts (CDD), crop diversification is not considered the main response to the adverse effects of this extreme event in Brazil. Irrigation is the leading practice in reducing the risks of droughts since evidence has responded to the reduction of precipitation in Brazil (Cunha et al. 2015). However, it is worth mentioning that adequate adaptation planning should include synergy between adaptive practices (Teklewold et al. 2017). For example, adopting diversification with irrigation can help overcome prolonged drought shocks. According to Renard and Tilman (2019), the diversity of agricultural species associated with irrigation increases the temporal stability of national crop production, contrary to the instability of precipitation and temperature. Besides, crop diversification is more relevant in areas with less precipitation, such as the Northeast region, unlike the North region, which receives higher rainfall. The Northeast region has approximately 46% of Brazilian farms, mostly family farms (79,2%) (IBGE 2017), and it falls into the highly diversified category (Fig. 2).
Dry days promote crop diversification in Brazil and most regions. However, the results show a negative relation in the Midwest, characterized by a significant area of specialized crops. (Fig. 2). In this region, the most important agricultural practice is the double cropping of soy-maize, a type of diversification. Still, soy-maize cropping is negatively impacted by reduced rainfall during the growing season, making this form of diversification irrelevant in mitigating drought risks (Brumatti et al. 2020). According to Piedra-Bonilla et al. (2020a, b), there is a negative correlation between farm size and crop diversification in Brazil, and the farms in the Midwest tend to be the largest.
The study results indicate that diversification is not used to reduce agricultural vulnerability caused by extreme precipitation days in Brazil. Moreover, diversification may not be influenced by the decreasing trend in days with heavy rains in all Brazilian regions (as shown in Fig. 2.d). However, the agroforestry system, a form of crop diversification, has been recognized as a practice that mitigates the effects of heavy precipitation. Forests are less susceptible to flooding and soil erosion, which reduces water flow (Baldwin et al. 2022). Despite this, the southern region exhibits a significant positive effect. The region has experienced heavy rainfall for about 20 to 30 days from 1987 to 2016, as shown in Fig. 1.c. During the same period, the South had the highest crop diversification level, according to Piedra-Bonilla et al. (2020a, b). Small farms and family farming characterize the region, as IBGE (2017) reported.
Our results suggest that municipalities adopting the diversity of on-farm activities as a strategy for adapting to heat shocks considerably increased on average in Brazil and most regions. These results are similar to those found in the study by Birthal and Hazrana (2019), in which the thermal stress shocks of the previous year increased the diversification of cultures of Indian farmers. Similarly, the results of Dillon et al. (2015) revealed that the number of crop groups harvested has a positive relationship with the degree days shocks.
The channels of extreme weather's impact on crop diversification may take different forms. First, diversification is related to managing risks so that farmers can reduce revenue risk depending on more than a single output (Chavas 2023). Different types of crop diversification are effective technologies for enhancing the resilience of crop yields after a weather-related shock. These technologies include crop rotation (Renwick et al. 2021; Marini et al. 2020), intercropping (Aslam et al. 2020; Amanullah et al. 2021), and livestock-crop systems (Peterson et al. 2020; Delandmeter et al. 2024). Finally, climate change has global agricultural price impacts (Yusifzada 2023), which can increase volatility and encourage farmers and regions to diversify production (Roest et al. 2018).
For future climate change simulations, crop diversification would decrease from 2016 to 2035 (Table 4 and Fig. 4). This would reflect a continuation of the past evolution, decreasing from 1995/96 to 2017. According to Parré and Chagas (2022), the growth rates of agricultural diversification indexes were negative in Brazil between 2002 and 2018. However, in the second period (2046–2065), there would be a change in direction in which diversification would increase in Brazil, albeit slightly (Table 4 and Fig. 4). Then, in this period, crop diversification would start to gain prominence as a strategy for adapting to climate change. These results are similar to those found in Latin America by Seo and Mendelsohn (2008), whose simulations indicate that the increase in crop-livestock integrations would occur in hot, dry, and humid scenarios until 2060.
Furthermore, the increase in the rate variation in diversification in the Midwest in the period 2045–2060 in both scenarios of GHG emissions (RCP 4.5 and RCP8.5) (Fig. 4) shows that this region that has been characterized by the specialization of cultures, such as corn, soy, sugar cane, would change their technologies to more resilient agricultural practices. For example, this region has adopted the system of no-till in grain crops (Romeiro 2014) that requires the rotation of diversified crops for its correct functioning in the long term.
However, the slight growth in crop diversification from the middle of the twenty-first century would not be enough to reduce vulnerability in the face of climatic scenarios. The benefits of resilience acquired from diversification improve in the long term (Bowles et al. 2020; Birthal & Hazrana 2019), so pressing public policies are needed to help increase the diversity of cultures in Brazil to improve its potential to reduce climate risks over time. In this context, it is essential to discuss, on the one hand, the factors that have favored the concentration of crops from the public sector. Still, on the other hand, different current public strategies can encourage agricultural diversification as a Brazilian agricultural adaptation to climate change.
In Brazil, monocultures on large farms destined for export have had economic importance since colonial times, except in the Northeast, because their climatic conditions have been less favorable (Fausto 1994). However, after 1980, the country stopped depending on food imports only after several public policies. Credit, research, and the rural extension of various institutions consolidated agricultural production around the 70 s of the last century (Vieira Filho and Fishlow 2017). However, agricultural technology development was mainly focused on grain production with intensive mechanization, fertilizers, and pesticides, especially in the Southeast and Midwest regions (Alves et al. 2013). This logic was influenced by the practices and technologies of the Green Revolution, which expanded in industrialized countries through the improvement of new varieties of grains, the intensive use of pesticides, mechanization, and irrigation (De Andrades & Ganimi 2007). Thus, the Research and Development (R&D) focused on crop specialization, influencing technical assistance and rural credit equally. So, public policies have promoted this logic of monocultures and a reduction in the diversity of cultures.
However, after pressure from civil society and scientists, R&D has started to focus on developing sustainable technologies, indicating the negative environmental impact, monocultures, and the intensive use of chemical inputs and machinery. In 2009, Brazil established the National Policy on Climate Change, in which the agricultural sector is contemplated through the Low Carbon Emission Agriculture Plan (ABC Plan), established in the following year until 2020. The ABC Plan has organized actions to adopt sustainable production technologies to meet the country's GHG emissions reduction commitments in the agricultural sector. Within the actions, the concept of diversification is not considered as such. Still, several forms of diversification are used in the programs, such as Crop-Livestock-Forest Integration, Agroforestry Systems, and rotation, intercropping, or crop succession as part of the No-Tillage Systems. According to Manzatto et al. (2018), it is observed that the ABC Plan has driven agricultural diversification through its programs, even exceeding the commitments established at the beginning of the programs, since the Crop-Livestock-Forest Integration reached 146% of its goals. So, the ABC Plan must continue in a new phase to reinforce and expand resilient and mitigation technologies, such as diversification. According to Souza Piao et al. (2021) and Vinholis et al. (2021), to strengthen the adoption of the ABC Plan technologies, it is necessary to improve the rural extension service in the diffusion of sustainable technologies to producers. These results accompany the positive effects of technical assistance on agricultural diversification observed in most climate specifications.
On the other hand, remembering that smaller farms are more willing to diversify their agricultural production in Brazil, discussing public policies focused on family farming is important. Firstly, there are public food purchases, as instruments to encourage the purchase of products from family farming, such as the Food Acquisition Program (Programa de Aquisação de Alimentos—PAA), Institutional Purchases, and the National School Feeding Program (Programa Nacional de Alimentação Escolar—PNAE). These programs aim to support sustainable agricultural production and the acquisition of diversified foods considered to be of food value (Grisa et al. 2020). Therefore, public policies have contributed to the increase in the sale of diversified products in family farming.

5 Conclusions

Here, we show the impact of extreme weather events on crop diversification in Brazil for the first time. First, the results showed that Brazilian municipalities adopted diversification as an adaptation strategy when the climatic shocks were dry spells (CDD), days without precipitation (Rn1mm), and hot days (TX90p). Notably, the evolution of the percentage of hot days and the average annual temperature had increasing trends from 1985 to 2016. In the Southern region, diversification was not considered a practice to mitigate the vulnerability caused by frosts and heavy rainfall in the country. However, the heavy rainy days decreased in all Brazilian regions over the same period, while the frosts were erratic. Thus, the response to diversification as an adaptive strategy would depend on the type of climate shock and the characteristics of the climate and agricultural technologies of the regions. Each region's specific models show that extreme climate indices' impact on crop diversification varies across the Brazilian regions, so other adaptative strategies should accompany it.
The results of simulations of the rate variation in Brazilian crop diversification in the beginning (2016–2035) and mid (2046–2065) of the twenty-first century show the following forecast. In the first period, all-climate specifications showed a decrease in the percentage variation of Brazilian agricultural diversification, especially in the RCP8.5 scenarios. However, the decrease in Brazilian diversification in 2016–2035 would be less than the historical average observed (−8.7%) from 1996 to 2017. Next, the variation in diversification would increase in the scenario of high GHG emissions (RCP8.5) in the second period (2046–2065). These forecasts of changes in agricultural land use in Brazil indicate convergence to agricultural systems that are more resilient to climate change.
The findings of this study must be considered in light of some limitations. First, a change in diversification at municipality levels may not necessarily imply a similar change in the degree of diversification at the scale of farms. Nevertheless, it is assumed that the contribution of individual activities impacts diversification with data at the municipality level. Furthermore, the municipality analyses help focus on providing credit and technical assistance through administrative levels (Birthal & Hazrana 2019). Second, it was not possible to empirically estimate which form of diversification would be projected in the future. But discusses the concentration of on-farm products that could increase with the increase of some extreme weather events. We recommend that upcoming studies take into consideration these concerns.
Finally, promoting sustainable agricultural practices, such as crop diversification, is essential through extension and rural credit. However, based on the research results discussed above, it can be concluded that crop diversification is not a one-size-fits-all solution to mitigate the risks of extreme weather events in Brazil and should not be the only adaptive practice adopted. Instead, it should be complemented with other adaptive strategies such as irrigation and a no-till system. Public policies should focus on providing support and incentives for farmers to adopt these practices and invest in research and development to identify new and more effective strategies to cope with climate change. Furthermore, policymakers should also consider the regional differences in Brazil and tailor their policies accordingly to meet the specific challenges faced by farmers in each region.

Declarations

Conflicts of interest/Competing interests

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Appendix

Appendix

Tables 5, 6, 7, 8 and 9.
Table 5
Effects of Consecutive Dry Days (CDD) on crop diversification in the Brazilian regions
 
(1)
(2)
(3)
(4)
(5)
(6)
(7)
(8)
(9)
(10)
VARIABLES
Northa
Northeast
Midwest
South East
South
Technical assistance
-3.60e-05
 
1.92e-05
 
-4.88e-05
 
2.19e-05
 
2.19e-05**
 
 
(2.52e-05)
 
(2.14e-05)
 
(4.81e-05)
 
(2.16e-05)
 
(1.03e-05)
 
Legal status of farms
-2.13e-06
 
-1.62e-05**
 
3.26e-06
 
8.83e-05***
 
2.31e-06
 
 
(9.51e-06)
 
(6.56e-06)
 
(3.32e-05)
 
(1.63e-05)
 
(1.31e-05)
 
Irrigation
2.95e-05
 
4.83e-06
 
-9.36e-06
 
3.07e-05
 
4.60e-05
 
 
(3.84e-05)
 
(1.52e-05)
 
(0.000126)
 
(1.94e-05)
 
(3.91e-05)
 
Farm Size
-7.97e-05
 
-0.00035***
 
-2.57e-05
 
-0.00028***
 
-0.000390
 
 
(0.000102)
 
(6.91e-05)
 
(7.89e-05)
 
(7.85e-05)
 
(0.000280)
 
Maize farm
3.97e-06
 
1.76e-05***
 
3.01e-05
 
-2.96e-06
 
3.41e-05***
 
 
(1.15e-05)
 
(5.75e-06)
 
(4.50e-05)
 
(1.74e-05)
 
(7.03e-06)
 
CDD
0.00129
0.00132
0.000322***
0.000344***
0.000935
0.00101*
-0.000451*
-0.000613**
-1.99e-05
-0.000134
 
(0.000795)
(0.000801)
(0.000124)
(0.000124)
(0.000589)
(0.000584)
(0.000237)
(0.000255)
(0.000220)
(0.000221)
Annual temperature
  
-0.00129
-0.00124
-0.0130***
-0.0135***
0.0113***
0.0112***
-0.00219
-0.00397**
   
(0.00181)
(0.00183)
(0.00499)
(0.00506)
(0.00202)
(0.00214)
(0.00167)
(0.00165)
Constant
0.631***
0.610***
0.707***
0.687***
0.858***
0.854***
0.413***
0.447***
0.710***
0.780***
 
(0.0365)
(0.0238)
(0.0462)
(0.0461)
(0.140)
(0.127)
(0.0462)
(0.0464)
(0.0406)
(0.0331)
Fixed effects state/year
NO
NO
YES
YES
NO
NO
NO
NO
NO
NO
Hausman test
17.39***
6,01*
416.75***
530.26***
12.87*
5,56*
120.91***
148,42***
51.57***
0.23
Modified Wald test
7.7e + 05***
3.8e + 05***
1.0e + 61***
6.2e + 59***
1.2e + 06***
7.8e + 05***
5.6e + 31***
6.9e + 32***
1.0e + 09***
1.3e + 31***
Wooldridge test
0.014
0.367
3.457*
2.126
6.414**
5.377**
1.538
4.843
2.409
0.761
Observations
519
519
3,964
3,964
768
768
4,160
4,160
2,009
2,009
R-squared
0.064
0.056
0.105
0.091
0.033
0.023
0.165
0.143
0.034
0.007
F Statistic
6.40***
6.48***
13.75***
15.06***
6.40***
6.48***
62.18***
122.48***
9.52***
5.27***
Number of MCA
173
173
1,322
1,322
256
256
1,396
1,396
671
671
Robust standard errors are in parentheses. Significance: *** p < 0,01, ** p < 0,05, * p < 0,1; a: No correlation between CDD and annual temperature
Table 6
Effects of Number of dry days index (Rn1mm) on crop diversification in the Brazilian regions
 
(1)
(2)
(3)
(4)
(5)
(6)
(7)
(8)
(9)
(10)
VARIABLES
North
Northeast
Midwesta
South East
South
Technical assistance
-3.24e-05
 
1.97e-05
 
-6.28e-05
 
1.79e-05
 
2.08e-05**
 
 
(2.49e-05)
 
(2.14e-05)
 
(4.73e-05)
 
(2.17e-05)
 
(1.02e-05)
 
Legal status of farms
-3.59e-06
 
-1.67e-05**
 
1.64e-05
 
9.28e-05***
 
-2.77e-06
 
 
(9.63e-06)
 
(6.58e-06)
 
(3.49e-05)
 
(1.64e-05)
 
(1.34e-05)
 
Irrigation
3.22e-05
 
6.03e-06
 
-3.43e-05
 
3.22e-05
 
4.84e-05
 
 
(3.94e-05)
 
(1.55e-05)
 
(0.000127)
 
(2.06e-05)
 
(3.93e-05)
 
Farm Size
-9.24e-05
 
-0.000349***
 
-1.37e-05
 
-0.000274***
 
-0.000375
 
 
(9.87e-05)
 
(6.94e-05)
 
(9.08e-05)
 
(7.74e-05)
 
(0.000284)
 
Maize farm
5.51e-06
 
1.74e-05***
 
3.30e-05
 
-7.14e-06
 
3.31e-05***
 
 
(1.14e-05)
 
(5.76e-06)
 
(4.70e-05)
 
(1.76e-05)
 
(6.97e-06)
 
Rn1mm
0.000106
6.58e-05
0.000289***
0.000295***
-0.00120**
-0.00123**
0.000392*
0.000456**
0.000276**
0.000419***
 
(0.000307)
(0.000308)
(0.000106)
(0.000106)
(0.000519)
(0.000481)
(0.000205)
(0.000215)
(0.000115)
(0.000111)
tmedia_ano_ma
0.00321
0.00324
-0.000898
-0.000805
  
0.0105***
0.0102***
-0.00212
-0.00403***
 
(0.00785)
(0.00775)
(0.00181)
(0.00183)
  
(0.00188)
(0.00192)
(0.00148)
(0.00142)
Constant
0.481**
0.471**
0.649***
0.627***
0.824***
0.829***
0.324***
0.345***
0.655***
0.687***
 
(0.214)
(0.212)
(0.0505)
(0.0503)
(0.107)
(0.103)
(0.0631)
(0.0648)
(0.0459)
(0.0396)
Fixed effects state/year
NO
NO
YES
YES
NO
NO
NO
NO
NO
NO
Hausman test
14.39***
1.90
335.32***
696.05***
19.97***
1.63
54.10***
69.90***
52.49***
7.27**
Modified Wald test
1.1e + 06***
6.5e + 05***
2.5e + 30***
3.2e + 31***
6.3e + 05***
2.3e + 05***
7.3e + 32***
2.4e + 32***
7.3e + 30***
1.3e + 31***
Wooldridge test
0.112
0.674
4.228***
2.779*
12.915***
11.912***
2.239
5.173
2.239
0.817
Observations
519
519
3,964
3,964
768
768
4,160
4,160
2,009
2,009
R-squared
0.060
0.050
0.105
0.091
0.027
0.016
0.165
0.142
0.037
0.015
F Statistic
5.20***
4.35***
13.70***
14.96***
2.27**
6.55**
61.87***
123.09***
10.16***
11.68***
Number of MCA
173
173
1,322
1,322
256
256
1,396
1,396
671
671
Robust standard errors are in parentheses. Significance: *** p < 0,01, ** p < 0,05, * p < 0,1; a: No correlation Rn1mm with annual temperature
Table 7
Effects of the Number of Very Heavy Rainy Days Index (R20mm) on Crop Diversification in the Brazilian Regions
 
(1)
(2)
(3)
(4)
(5)
(6)
(7)
(8)
(9)
(10)
VARIABLES
North
Northeast
Midwest
South East
South
Technical assistance
-3.12e-05
 
2.32e-05
 
-4.76e-05
 
2.06e-05
 
1.44e-05
 
 
(2.49e-05)
 
(2.15e-05)
 
(5.04e-05)
 
(2.15e-05)
 
(9.70e-06)
 
Legal status of farms
-3.77e-06
 
-1.65e-05**
 
4.93e-06
 
8.89e-05***
 
1.67e-05
 
 
(9.86e-06)
 
(6.57e-06)
 
(3.49e-05)
 
(1.63e-05)
 
(1.41e-05)
 
Irrigation
3.34e-05
 
1.61e-06
 
-5.88e-05
 
2.96e-05
 
4.00e-05
 
 
(4.02e-05)
 
(1.55e-05)
 
(0.000143)
 
(1.94e-05)
 
(4.02e-05)
 
Farm Size
-9.30e-05
 
-0.000348***
 
-1.39e-05
 
-0.000278***
 
-0.000342
 
 
(9.90e-05)
 
(6.99e-05)
 
(8.79e-05)
 
(7.86e-05)
 
(0.000288)
 
Maize farm
6.22e-06
 
1.66e-05***
 
3.73e-05
 
-6.18e-06
 
3.15e-06
 
 
(1.14e-05)
 
(5.81e-06)
 
(4.89e-05)
 
(1.73e-05)
 
(8.44e-06)
 
R20mm
0.000269
0.000131
-0.00126*
-0.00140**
-0.00109
-0.000681
0.00135*
0.00209***
-0.000590
-0.000574
 
(0.00101)
(0.000993)
(0.000668)
(0.000663)
(0.00126)
(0.00105)
(0.000724)
(0.000742)
(0.000486)
(0.000483)
Annual temperature
0.00291
0.00303
-0.00124
-0.00121
-0.0107**
-0.0117**
0.0118***
0.0121***
0.00244
0.00285*
 
(0.00769)
(0.00757)
(0.00183)
(0.00185)
(0.00502)
(0.00501)
(0.00197)
(0.00203)
(0.00173)
(0.00173)
Constant
0.582***
0.559***
0.730***
0.711***
0.866***
0.875***
0.358***
0.363***
0.664***
0.675***
 
(0.213)
(0.207)
(0.0478)
(0.0476)
(0.145)
(0.126)
(0.0514)
(0.0513)
(0.0459)
(0.0403)
Fixed effects state/year
NO
NO
YES
YES
NO
NO
NO
NO
NO
NO
Hausman test
14.54**
1.45
441.82***
1179.95***
18.56***
2.83
85.07***
89.59***
49.14***
5.38
Modified Wald test
4.8e + 05***
5.2e + 05***
2.7e + 31***
2.5e + 30***
1.5e + 06***
6.1e + 05***
2.0e + 32***
4.1e + 31***
6.1e + 30***
5.7e + 30***
Wooldridge test
0.114
0.709
2.517
1.290
1.578
0.979
0.060
0.409
2.145
0.522
Observations
519
519
3,964
3,964
768
768
4,160
4,160
2,009
2,009
R-squared
0.057
0.048
0.104
0.090
0.028
0.016
0.165
0.143
0.066
0.058
F Statistic
5.13***
4.33**
13.42***
14.73***
1.60
3.30**
62.18***
123.67***
11.67***
21.21***
Number of MCA
173
173
1,322
1,322
256
256
1,396
1,396
671
671
Robust standard errors are in parentheses. Significance: *** p < 0,01, ** p < 0,05, * p < 0,1
Table 8
Effects of Amount of hot days index (TX90p) on crop diversification in the Brazilian regions
 
(1)
(2)
(3)
(4)
(5)
(6)
(7)
(8)
(9)
(10)
VARIABLES
Northa
Northeast
Midwesta
South East
South
Technical assistance
-3.27e-05
 
2.09e-05
 
5.39e-05*
 
1.40e-05
 
1.47e-05
 
 
(2.44e-05)
 
(2.12e-05)
 
(3.23e-05)
 
(2.13e-05)
 
(9.74e-06)
 
Legal status of farms
-2.72e-06
 
-1.64e-05**
 
-4.93e-05*
 
4.75e-05***
 
1.72e-05
 
 
(9.82e-06)
 
(6.49e-06)
 
(2.61e-05)
 
(1.55e-05)
 
(1.41e-05)
 
Irrigation
2.92e-05
 
2.20e-06
 
-8.83e-06
 
2.66e-05
 
3.96e-05
 
 
(3.88e-05)
 
(1.52e-05)
 
(0.000121)
 
(2.03e-05)
 
(4.01e-05)
 
Farm Size
-8.88e-05
 
-0.00034***
 
-0.00024***
 
-0.00023***
 
-0.000354
 
 
(9.96e-05)
 
(6.89e-05)
 
(8.12e-05)
 
(7.26e-05)
 
(0.000289)
 
Maize farm
5.19e-06
 
1.73e-05***
 
-4.84e-05
 
2.53e-05
 
4.58e-06
 
 
(1.13e-05)
 
(5.75e-06)
 
(4.18e-05)
 
(1.71e-05)
 
(8.43e-06)
 
TX90p
-0.00118
-0.00131
0.000823**
0.000832**
-0.00240**
-0.00241**
0.00159***
0.00166***
-5.58e-06
9.07e-05
 
(0.00144)
(0.00146)
(0.000343)
(0.000348)
(0.00100)
(0.00100)
(0.000290)
(0.000292)
(0.000276)
(0.000273)
Annual rainfall
  
-8.91e-06
-1.04e-05
  
1.41e-05
1.68e-05
-2.26e-05**
-1.99e-05*
   
(9.57e-06)
(9.56e-06)
  
(1.40e-05)
(1.43e-05)
(1.14e-05)
(1.12e-05)
Constant
0.672***
0.652***
0.687***
0.670***
0.785***
0.637***
0.560***
0.569***
0.737***
0.753***
 
(0.0326)
(0.0128)
(0.0162)
(0.0134)
(0.0604)
(0.00945)
(0.0258)
(0.0233)
(0.0310)
(0.0208)
Fixed effects state/year
NO
NO
YES
YES
YES
YES
NO
NO
NO
NO
Hausman test
14.68**
0.37
541.90***
803.54***
30.66***
41.14***
81.86***
25.68***
38.56***
23.29***
Modified Wald test
1.0e + 06***
4.2e + 05***
2.8e + 31***
6.7e + 30***
6.8e + 05***
7.9e + 05***
1.7e + 32***
2.2e + 32***
8.2e + 30***
1.4e + 07***
Wooldridge test
0.249
1.121
3.568*
2.277
33.705***
35.320***
2.456
5.479**
2.195
0.592
Observations
519
519
3,964
3,964
768
768
4,160
4,160
2,009
2,009
R-squared
0.058
0.049
0.107
0.092
0.187
0.161
0.188
0.177
0.066
0.057
F Statistic
5.83***
6.01***
13.97**
15.35***
16.88***
39.14***
41.94***
59.55***
11,49***
20,28***
Number of MCA
173
173
1,322
1,322
256
256
1,396
1,396
671
671
Robust standard errors are in parentheses. Significance: *** p < 0,01, ** p < 0,05, * p < 0,1; a: No correlation between TX90p and annual rainfall
Table 9
Nonlinear effects of Frost Days (FD) on crop diversification in the South region
 
(1)
(2)
VARIABLES
Sul
Technical assistance
1.32e-05
 
 
(9.96e-06)
 
Legal status of farms
-2.41e-07
 
 
(1.39e-05)
 
Irrigation
3.99e-05
 
 
(3.94e-05)
 
Farm Size
-0.000300
 
 
(0.000289)
 
Maize farm
1.01e-05
 
 
(8.39e-06)
 
FD
-0.0892*
-0.0944**
 
(0.0466)
(0.0462)
FD square
0.0445**
0.0442**
 
(0.0203)
(0.0202)
Winter precipitation
0.000270**
0.000271**
 
(0.000110)
(0.000110)
FD x Winter precipitation
0.000347
0.000385
 
(0.000313)
(0.000311)
FD square x Winter precipitation
-0.000230*
-0.000229*
 
(0.000129)
(0.000128)
Constant
0.684***
0.687***
 
(0.0243)
(0.00878)
Fixed effects state/year
YES
YES
Hausman test
75.10***
13.20**
Modified Wald test
6.6e + 06***
7.0e + 30***
Wooldridge test
1.831
0.709
Observations
2,009
2,009
R-squared
0.097
0.092
F Statistic
11.26***
14.21***
Number of AMC
671
671
Robust standard errors are in parentheses. Significance: *** p < 0,01, ** p < 0,05, * p < 0,1
Footnotes
1
This study used, as units of observation, the Minimum Comparable Areas (MCA) for intertemporal comparisons of the same geographic area since the number of Brazilian municipalities increased over the years. Following the methodology proposed by Ehrl (2017), we made compatible municipalities in the three Agricultural Censuses used in this research (95/96, 2006, and 2017), i.e., the MCA developed in our research considered the municipalities that were created or merged during the analyzed period. Because MCAs represent the municipality observations, we will simplify the exposition by referring to them as municipalities.
 
2
Studies suggest that using General Circulation Models (GCM) from CMIP6 (last phase) does not invalidate the results found by CMIP5. The GCMs from CMIP do not substantially improve the representation of precipitation climate extremes for Brazil (Medeiros et al. 2022). Besides, CMIP5 projected temperature increases align with the observations that show global warming over land areas (Carvalho et al. 2022). Furthermore, according to Seneviratne and Hauser (2020), there is a notable convergence in regional climate sensitivity between CMIP5 and CMIP6 multimodel ensembles, indicating consistency in projections for extreme temperatures, heavy precipitation, and specific climate events in response to global warming.
 
3
MATOPIBA is the area that stretches across the territories of four Brazilian states: Maranhão, Tocantins, Piauí, and Bahia.
 
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Metadata
Title
Extreme weather events and crop diversification: climate change adaptation in Brazil
Authors
Elena Beatriz Piedra-Bonilla
Dênis Antônio Da Cunha
Marcelo José Braga
Laís Rosa Oliveira
Publication date
01-06-2025
Publisher
Springer Netherlands
Published in
Mitigation and Adaptation Strategies for Global Change / Issue 5/2025
Print ISSN: 1381-2386
Electronic ISSN: 1573-1596
DOI
https://doi.org/10.1007/s11027-025-10211-2

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