Future of Continental Heatwaves

Overview

Climate change is the critical challenge facing modern societies. The impacts of global warming will predominantly be experienced on continents, where the rapidly increasing risk of severe heatwaves (Figure 1) represents an existential threat to societies and ecosystems. The exceptional summers of 2018 (the UK’s joint hottest on record) and 2019 (which featured the UK’s hottest-ever day) represent ominous portents of the future.

Despite their societal importance, our fundamental understanding of continental heatwaves remains strikingly limited. We know that carbon dioxide-induced global warming over continents will be substantially larger than over oceans on average (Sutton et al 2007), and that this enhanced warming over land is tightly linked to aridity (Byrne & O’Gorman 2013; Byrne & O’Gorman 2018). But how climate change will affect heatwaves over continents is uncertain (Fischer & Knutti 2015), with no robust theory to interpret or corroborate predictions from complex and imperfect climate models.

Click on an image to expand

Image Captions

Figure 1: A schematic figure showing how global warming increases the occurrence of extreme heat events. (figure courtesy of the Climate Commission of Australia)

Methodology

During this project you will take a new approach to (a) transforming our fundamental understanding of continental heatwaves and (b) narrowing uncertainty in how these heatwaves will respond to a changing climate. Three key objectives will be tackled:

1. A NEW THEORY FOR CONTINENTAL HEATWAVES: A new theory for continental heatwaves and their response to climate change will be developed. This work will build on influential research linking average continental temperatures to land aridity and ocean warming (Byrne & O’Gorman 2013; Byrne & O’Gorman 2018). The goal is to build a robust, conceptual understanding of the mechanics of continental heatwaves. The new theory will challenge the current heatwave paradigm based on complex computational models and will fill a notable gap in our knowledge of how the climate system operates.

2. INNOVATIVE CLIMATE SIMULATIONS TO ADVANCE UNDERSTANDING: A novel hierarchy of climate models, from simplified continental configurations to state-of-the-art simulations, will be performed and analysed to investigate continental heatwaves under climate change. The goal is to test and refine the theory for continental heatwaves developed in Objective 1 in a systematic manner. Simulations will also be designed to probe the processes controlling how continental heatwaves in different regions (e.g. low versus high latitudes) respond to global warming.

3. EMERGENT CONSTRAINTS FOR CONTINENTAL HEATWAVES: The theory and simulations from Objectives 1 and 2 will be combined to develop emergent constraints for continental heatwaves for the first time. Emergent constraints are observable quantities in the current climate that have great potential to provide a new pathway to narrowing uncertainty in future predictions, but have not yet been developed for continental heatwaves. Potential emergent constraints will be tested using the simulations described in Objective 2 and, if successful, will be applied to narrow uncertainty in heatwave predictions from state-of-the-art climate models.

For Objective 2, you will perform novel climate simulations using the Community Earth System Model (CESM). These simulations will be designed to investigate the dynamics of continental heatwaves and their response to climate change. For Objective 3, you will analyse heatwaves in state-of-the-art climate simulations from the CMIP6 data archives, with the aim of narrowing the large uncertainty in future projections.

Project Timeline

Year 1

Year 1 will involve a literature review to enable you to develop your understanding of heatwave dynamics and physical aspects of climate change. The ingredients of a new theory for continental heatwaves will also be built up. You will begin using the CESM climate model and setting up the simulations to continental heatwaves in a changing climate. You will attend a training course on how to run the CESM model at the National Center for Atmospheric Research (NCAR) in Boulder, Colorado.

Year 2

Year 2 will focus on (a) running the set of idealised climate simulations to investigate continental heatwaves in different climates and (b) using the simulations to test and refine the new theory for heatwaves. You will draft a research article on this portion of the project and will present the key results at the American Geophysical Union’s annual meeting in San Francisco (or at a comparable international conference).

Year 3

Year 3 will involve applying the insights into heatwave dynamics developed in Years 1 and 2 to state-of-the-art climate simulations from the CMIP6 archive. This will involve substantial Big Data analyses using Python, with the objective of narrowing the large uncertainty in future heatwave projections. You will attend and present your research at an international conference on monsoon dynamics.

Year 3.5

Year 3.5 will focus on writing the PhD thesis and drafting a research article on the analyses conducted during Year 3.

Training
& Skills

You will be trained on several aspects of physical climate science including atmospheric dynamics, heatwaves, climate modelling and climate change. You will also be trained in highly sought-after technical skills in computational modelling, high-performance computing, and Big Data analyses using Python. You will attend a training course on using the CESM climate model at NCAR in Colorado, and will complete an internship with the CASE partner on this project – a leading catastrophe risk modelling company based in London (CASE support pending).

References & further reading

[1] Byrne & O’Gorman (2013): Land-ocean warming contrast over a wide range of climates: convective quasi-equilibrium theory and idealized simulations,
Journal of Climate, vol. 29, pp. 9045-9061.[2] Byrne & O’Gorman (2018): Trends in continental temperature and humidity directly linked to ocean warming, Proceedings of the National Academy of Sciences, vol. 115, pp. 4863-4868.[3] Fischer & Knutti (2015): Anthropogenic contribution to global occurrence of heavy-precipitation and high-temperature extremes, Nature Climate Change, vol. 5, pp. 560-564.[4] Sutton et al (2007): Land/sea warming ratio in response to climate change: IPCC AR4 model results and comparison with observations. Geophysical Research Letters, vol. 34, L02701.

Further Information

For further details on this project, please contact Dr Michael Byrne by email mpb20@st-andrews.ac.uk or by phone at 07472179331.

Apply Now