Related Experiment Video
Updated: Jun 10, 2026

11:49
Cereal Crop Ear Counting in Field Conditions Using Zenithal RGB Images
Published on: February 2, 2019
Possible changes to arable crop yields by 2050
Keith W Jaggard1, Aiming Qi, Eric S Ober
1Rothamsted Research, Broom's Barn Research Centre, Higham, Bury St Edmunds, Suffolk, UK. keith.jaggard@bbsrc.ac.uk
Summary
Future climate change may increase crop yields through carbon dioxide (CO2) enrichment, but rising temperatures and ozone levels pose challenges. Closing the yield gap is key to feeding a growing global population by 2050.
Area of Science:
- Agricultural Science
- Climate Change Biology
- Environmental Science
Background:
- Projected 2050 conditions: 9.1 billion population, 550 ppm CO2, 60 ppb ozone, 2°C warmer climate.
- Need to assess crop yield contributions to global food security under these future scenarios.
Purpose of the Study:
- To evaluate the potential impact of environmental changes on crop yields.
- To determine the role of increased crop production in feeding the future global population.
- To identify strategies for maximizing crop yields in changing environmental conditions.
Main Methods:
- Analysis of projected environmental changes (CO2, temperature, ozone).
- Modeling of crop yield responses to these changes.
- Assessment of factors influencing yield gaps and potential improvements.
Main Results:
- CO2 enrichment may increase yields by ~13%, but C4 crops may see no change.
- Increased temperatures could offer agronomic opportunities, but also increase evaporation.
- Ozone increases may decrease yields by 5% or more; soil-borne pathogens may increase.
- Closing the yield gap and improving potential yields could increase production by ~50% without extra land.
Conclusions:
- Future crop production is sensitive to CO2, temperature, and ozone levels.
- Agronomic and breeding strategies are crucial for adapting to climate change.
- Reducing the gap between achievable and actual farm yields is vital for food security.
- Bio-energy land demands are not factored into these yield increase projections.
Related Concept Videos
What is Climate?
Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
Plant Breeding and Biotechnology
Crop cultivation has a long history in human civilization, with records showing the cultivation of cereal plants beginning at around 8000 BC. This early plant breeding was developed primarily to provide a steady supply of food.
Adaptations that Reduce Water Loss
Though evaporation from plant leaves drives transpiration, it also results in loss of water. Because water is critical for photosynthetic reactions and other cellular processes, evolutionary pressures on plants in different environments have driven the acquisition of adaptations that reduce water loss.
The Calvin Benson Cycle
Ribulose 1,5- bisphosphate carboxylase/oxygenase (RuBisCo) is a critical enzyme that catalyzes carbon dioxide assimilation during photosynthesis. However, it is an inefficient enzyme, having an extremely slow catalytic rate. A typical enzyme can process about a thousand molecules per second; however, RuBisCo fixes only around three-carbon dioxides per second. Photosynthetic cells compensate for this slow rate by synthesizing very high amounts of RuBisCo, making it the most abundant single...
Responses to Drought and Flooding
Water plays a significant role in the life cycle of plants. However, insufficient or excess of water can be detrimental and pose a serious threat to plants.
Global Climate Change
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
