Topics > Soil and land management > Soil and ecosystem services > Climate change adaptation

Climate change, wheat production and erosion risk

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Summary

Projections for a warming, drying climate across the state’s agricultural zone are cause for concern, particularly where low soil moisture often presents a significant limitation to plant growth. Changes in plant growth have the potential to increase soil erosion risk and this topsoil degradation can lead to a loss in soil fertility, carbon content and soil water holding capacity as a result.

A crop simulation modelling exercise was conducted on wheat yield, to provide more information the about potential climate change impacts on dryland cereal cropping in Southern South Australia.

This page will help you understand:

  • which environments are vulnerable to poor cereal crop yield and soil erosion risk during dry years
  • which soils are more resilient for cereal cropping in dry environments
  • farm management recommendations for managing cereal crops in dry environments under climate change projections.

Wheat yield modelling study

Potential impacts to wheat grain yields and the frequency and severity of wind and water erosion risk (due to low crop stubble biomass) have been examined through a modelling exercise spanning the entire dryland cereal cropping zone.

The Agricultural Production System simulator (APSIM) was used for this study. This platform contains a suit of modules and a range of plant, animal, soil, climate and management components that can be incorporated into modelling agricultural outcomes.

This case study used the following soil properties: surface texture and plant available water holding capacity (PAWC), along with mapped attributes of water erosion and wind erosion potential. These mapped attributes were used as a basis for establishing ‘critical ground cover’ required for adequate protection against erosion.

Representative historic long-term climate datasets were used in the modelling, along with hypothetical climate change scenarios (consistent with projections to 2030) to explore simulated regional impacts under drying, warming and increasing carbon dioxide levels.

  • Shallow clayey soils are most vulnerable to poor yields and low stubble cover in dry years.
  • In low rainfall environments, higher rates of evaporation and the inherent higher wilting point moisture levels in clay surface soils increases the risk of moisture stress and terminal drought (early crop senescence), compared to sandy surface soils.
  • Sandy surface soils with large PAWC (e.g. deep sands or some sandy surfaced texture-contrast soils) are the most resilient for cropping in drier environments.
  • Low rainfall cropping environments appear most vulnerable to reducing grain yields and increasing erosion risk, if rainfall declines.
  • The modelling suggests that for some areas there will be a general trade-off between grain yield and residual crop biomass (available to protect soils) under declining rainfall. This lower biomass is the result of earlier flowering and grain production triggered in some wheat varieties by the warming climate, giving the plant less time to invest in growing its biomass (i.e. shorter growing period).
  • Meanwhile, cropping systems in the wetter parts of the State are likely to benefit from a warming, drying climate. In these situations, where moisture is not a limiting factor, the increased CO2 and temperature (in historically cool regions) have the opportunity to boost plant and crop production levels.
  • Erosion risk is a gradational problem, increasing in extent with poorer seasons and increasing in frequency with a drying climate.
  • The erosion risk maps highlight a patchwork of areas that will need to be monitored if projections of a drying climate become a reality, to identify any emerging and recurrent erosion risk issues.

If climate changes in line with current projections, farmers and other natural resource managers will need to adopt a range of adaptation strategies. These may include incremental shifts and flexible risk management approaches through to more fundamental practice changes over generational timeframes. Farm management practices

  • Continue to improve water use efficiency to optimise grain and biomass production.
  • Adopt a range of climate risk management strategies (e.g. flexible and responsive farming techniques; using seasonal indicators to base management decisions).
  • Consider soil and land types in management decisions (e.g. farming to land capability, including inherent production potential and risk; assessing required stubble cover and quality; grazing management).
  • Retain cereal stubbles for soil protection, helping to minimise erosion risk after harvest and into the following season.
  • Use crop species that leave greater amounts of protective biomass after harvest (particularly in the case of grain legumes).
  • Continue uptake of reduced tillage and ‘no-till’ farming techniques.
  • Investigate alternative land use or management on areas of land prone to higher frequencies of poor crop growth, low economic returns and elevated erosion risk.
  • Use spatial analogues to consider adaptation options (learn from what farmers are doing in warmer and drier locations).

Refer to the full report for recommendations for a) research and development, b) state and regional planning and policy development, c) industry adaptation and education, and d) future scenario modelling.

an approaching dust storm. There is no long-range visibility.
Dust storm, Mitchellville. Image Source: Craig Liddicoat