Lead Supervisor: Richard P. Allan, University of Reading, Department of Meteorology
Co-supervisors: Michaela Hegglin, University of Reading, Department of Meteorology; Alejandro Bodas-Salcedo, Met Office; Viju John, EUMETSAT
The tiny quantities of water vapour in the air many kilometres above our heads is of central importance to the Earth’s greenhouse effect and ongoing climate change. It regulates the planet’s natural cooling system through absorption of outgoing infrared radiation and where the humidity exceeds saturation point determines the distribution and thickness of high altitude clouds. Upper tropospheric humidity is an essential climate variable because it controls key atmospheric processes, including water vapour and cloud feedbacks that can amplify the climate system’s response to increases in other greenhouse gases such as carbon dioxide. It is therefore vital to understand past variability and change in upper tropospheric humidity and evaluate these key processes in complex climate prediction models.
This project will exploit state of the art global satellite measurements and novel diagnostic tools to evaluate dataset quality, quantify the variability of atmospheric humidity in space and time and use this information to advance understanding of important atmospheric processes as well interrogate and improve detailed weather and climate prediction models that are of great benefit to society. The research will provide a valuable interface between Earth Observation and climate modelling, as well elucidating feedback processes fundamental to climate change and therefore of great relevance to policymakers. The supervision team provides a broad expertise across climate science and Earth Observation and there will be the opportunity to work with scientists from the UK Met Office involved in the development of weather and climate models and with scientists stationed at EUMETSAT who are directly involved in producing and extending key satellite observing systems.
The project will tackle important questions relating to the climate system including:
- How much does upper tropospheric humidity amplify climate change?
- Can state of the art climate models capture the processes determining variability and change in upper tropospheric humidity?
- Will signatures from upper tropospheric humidity provide new insight into high altitude cloud feedbacks?
- How does upper tropospheric humidity control Earth’s radiative energy balance and is there a tropical super greenhouse effect?
There will be opportunities to liaise and learn from EUMETSAT partners involved in developing Upper Tropospheric Humidity datasets and Met Office partners on using and evaluating climate model simulations. This will provide comprehensive training in cross-disciplinary data analysis skills applied to models and Earth observations.
The candidate will have a background in physical science with good numerical skills. An interest in observing the Earth and monitoring ongoing climate change as well as an interest in meteorology and climate science will be an advantage as will knowledge of programming and experience in developing numerical models: all of these aspects are desirable but not essential.
There is the possibility to gain support to undertake a trip to the EUMETSAT partners in Darmstaad, Germany.
Lang, T., Buehler, S.A., Burgdorf, M. et al. A new climate data record of upper-tropospheric humidity from microwave observations. Sci Data 7, 218 (2020).
Sherwood, S. C. et al. (2020). An assessment of Earth’s climate sensitivity using multiple lines of evidence. Reviews of Geophysics, 58, e2019RG000678.
Soden B. J., et al. (2005). The Radiative Signature of Upper Tropospheric Moistening, Science 310, 841