David Reay

Last updated

Daved Reay

Born
David S. Reay
Education University of Essex (PhD)
Scientific career
Fields Climate change
Nitrogen
Methane
Climate education
Net zero [1]
Institutions University of Edinburgh
Thesis Temperature dependence of inorganic nitrogen utilisation by bacteria and microalgae  (1999)
Doctoral students Hannah Ritchie [2]
Website blogs.ed.ac.uk/davereay/ OOjs UI icon edit-ltr-progressive.svg

David S. Reay FRSGS is a climate change scientist, author, and professor of carbon management and education at the University of Edinburgh. [1] [3] [4] He serves as executive director of the Edinburgh Climate Change Institute and policy director of ClimateXChange. [5] [6] [7]

Contents

Education

Reay was educated at the University of Essex where he was awarded a PhD in 1999 for research on the utilisation of inorganic nitrogen by bacteria and microalgae. [8]

Research and career

Reay's research focuses on greenhouse gas fluxes and land use, [9] including national and international research projects such as CarboEurope and NitroEurope, and research council-funded work through the UK's Natural Environment Research Council (NERC). Reay's key peer reviewed publications include novel work on global carbon sinks, the soil methane sink, and nitrous oxide emissions from aquatic systems. His work on nitrous oxide featured in the Intergovernmental Panel on Climate Change (IPCC) Fourth and Fifth Assessment Reports. In addition to his contributions to the understanding of greenhouse gas fluxes, Reay has written widely on climate change policy and society, particularly on individual and community action. He now[ when? ] advises the Scottish and UK Governments on climate action, especially around climate change skills and green jobs [10]

Climate change

Reay has authored several books on climate change, including the popular science books Climate-smart Food, [11] Nitrogen and Climate Change, Climate Change Begins at Home [12] [13] [14] [15] published in 2005 by Macmillan and shortlisted for the Times Higher Young Academic Author of the Year Award, and Your Planet Needs You! published in 2009 by Macmillan Children's Books. [16] He is also lead editor of Greenhouse Gas Sinks [17] published in 2007 by CABI and creator and editor of the climate change science website Greenhouse Gas Online. [18] [19]

Service and leadership

Reay chairs the Scottish Government's Climate Emergency Skills Implementation Group, sits on the UK Government's Green Jobs Taskforce, and is the creator of the award-winning Master of Science (MSc) course in carbon management at the University of Edinburgh. [20]

He is very active in climate change knowledge exchange, both nationally and internationally, [21] [22] [23] [24] being a regular media commentator on climate change issues, advising on and appearing in the BBC's Can We Save Planet Earth Are We Changing Planet Earth? film with David Attenborough, and frequently providing expert evidence on climate change to select committees in the Westminster and Holyrood Parliaments. [25] Knowledge exchange information, University of Edinburgh. [25] His former doctoral students include Hannah Ritchie. [2]

Related Research Articles

<span class="mw-page-title-main">Greenhouse effect</span> Atmospheric phenomenon causing planetary warming

The greenhouse effect occurs when greenhouse gases in a planet's atmosphere cause some of the heat radiated from the planet's surface to build up at the planet's surface. This process happens because stars emit shortwave radiation that passes through greenhouse gases, but planets emit longwave radiation that is partly absorbed by greenhouse gases. That difference reduces the rate at which a planet can cool off in response to being warmed by its host star. Adding to greenhouse gases further reduces the rate a planet emits radiation to space, raising its average surface temperature.

<span class="mw-page-title-main">Global warming potential</span> Potential heat absorbed by a greenhouse gas

Global warming potential (GWP) is a measure of how much infrared thermal radiation a greenhouse gas added to the atmosphere would absorb over a given time frame, as a multiple of the radiation that would be absorbed by the same mass of added carbon dioxide. GWP is 1 for CO2. For other gases it depends on how strongly the gas absorbs infrared thermal radiation, how quickly the gas leaves the atmosphere, and the time frame being considered. The carbon dioxide equivalent is calculated from GWP. For any gas, it is the mass of CO2 that would warm the earth as much as the mass of that gas. Thus it provides a common scale for measuring the climate effects of different gases. It is calculated as GWP times mass of the other gas.

<span class="mw-page-title-main">Nitrous oxide</span> Colourless non-flammable gas

Nitrous oxide, commonly known as laughing gas, nitrous, nitro, or nos, is a chemical compound, an oxide of nitrogen with the formula N
2
O
. At room temperature, it is a colourless non-flammable gas, and has a slightly sweet scent and taste. At elevated temperatures, nitrous oxide is a powerful oxidiser similar to molecular oxygen.

Trace gases are gases that are present in small amounts within an environment such as a planet's atmosphere. Trace gases in Earth's atmosphere are gases other than nitrogen (78.1%), oxygen (20.9%), and argon (0.934%) which, in combination, make up 99.934% of its atmosphere.

<span class="mw-page-title-main">IPCC list of greenhouse gases</span> List of greenhouse gases

This is a list of the most influential long-lived, well-mixed greenhouse gases, along with their tropospheric concentrations and direct radiative forcings, as identified by the Intergovernmental Panel on Climate Change (IPCC). Abundances of these trace gases are regularly measured by atmospheric scientists from samples collected throughout the world. Since the 1980s, their forcing contributions are also estimated with high accuracy using IPCC-recommended expressions derived from radiative transfer models.

<span class="mw-page-title-main">Climate change mitigation</span> Actions to reduce net greenhouse gas emissions to limit climate change

Climate change mitigation is action to limit climate change by reducing emissions of greenhouse gases or removing those gases from the atmosphere. The recent rise in global average temperature is mostly due to emissions from burning fossil fuels such as coal, oil, and natural gas. Mitigation can reduce emissions by transitioning to sustainable energy sources, conserving energy, and increasing efficiency. It is possible to remove carbon dioxide from the atmosphere by enlarging forests, restoring wetlands and using other natural and technical processes. Experts call these processes carbon sequestration. Governments and companies have pledged to reduce emissions to prevent dangerous climate change in line with international negotiations to limit warming by reducing emissions.

<span class="mw-page-title-main">Greenhouse gas emissions</span> Sources and amounts of greenhouse gases emitted to the atmosphere from human activities

Greenhouse gas emissions from human activities strengthen the greenhouse effect, contributing to climate change. Most is carbon dioxide from burning fossil fuels: coal, oil, and natural gas. The largest emitters include coal in China and large oil and gas companies. Human-caused emissions have increased atmospheric carbon dioxide by about 50% over pre-industrial levels. The growing levels of emissions have varied, but have been consistent among all greenhouse gases. Emissions in the 2010s averaged 56 billion tons a year, higher than any decade before. Total cumulative emissions from 1870 to 2017 were 425±20 GtC from fossil fuels and industry, and 180±60 GtC from land use change. Land-use change, such as deforestation, caused about 31% of cumulative emissions over 1870–2017, coal 32%, oil 25%, and gas 10%.

<span class="mw-page-title-main">Greenhouse gas emissions by the United States</span> Climate changing gases from the North American country

The United States produced 5.2 billion metric tons of carbon dioxide equivalent greenhouse gas (GHG) emissions in 2020, the second largest in the world after greenhouse gas emissions by China and among the countries with the highest greenhouse gas emissions per person. In 2019 China is estimated to have emitted 27% of world GHG, followed by the United States with 11%, then India with 6.6%. In total the United States has emitted a quarter of world GHG, more than any other country. Annual emissions are over 15 tons per person and, amongst the top eight emitters, is the highest country by greenhouse gas emissions per person. However, the IEA estimates that the richest decile in the US emits over 55 tonnes of CO2 per capita each year. Because coal-fired power stations are gradually shutting down, in the 2010s emissions from electricity generation fell to second place behind transportation which is now the largest single source. In 2020, 27% of the GHG emissions of the United States were from transportation, 25% from electricity, 24% from industry, 13% from commercial and residential buildings and 11% from agriculture. In 2021, the electric power sector was the second largest source of U.S. greenhouse gas emissions, accounting for 25% of the U.S. total. These greenhouse gas emissions are contributing to climate change in the United States, as well as worldwide.

<span class="mw-page-title-main">Global Carbon Project</span>

The Global Carbon Project (GCP) is an organisation that seeks to quantify global greenhouse gas emissions and their causes. Established in 2001, its projects include global budgets for three dominant greenhouse gases—carbon dioxide, methane, and nitrous oxide —and complementary efforts in urban, regional, cumulative, and negative emissions.

<span class="mw-page-title-main">Carbon dioxide removal</span> Removal of atmospheric carbon dioxide through human activity

Carbon dioxide removal (CDR), also known as carbon removal, greenhouse gas removal (GGR) or negative emissions, is a process in which carbon dioxide gas is removed from the atmosphere by deliberate human activities and durably stored in geological, terrestrial, or ocean reservoirs, or in products. In the context of net zero greenhouse gas emissions targets, CDR is increasingly integrated into climate policy, as an element of climate change mitigation strategies. Achieving net zero emissions will require both deep cuts in emissions and the use of CDR. CDR can counterbalance emissions that are technically difficult to eliminate, such as some agricultural and industrial emissions.

<span class="mw-page-title-main">Greenhouse gas</span> Gas in an atmosphere that absorbs and emits radiation at thermal infrared wavelengths

A greenhouse gas (abbreviated as GHG) is a gas that absorbs radiant energy at thermal infrared wavelengths. Greenhouse gases cause the greenhouse effect by trapping some of the heat a planet's surface radiates in response to light from its host star (which is the sun in the case of planet Earth). The primary greenhouse gases in Earth's atmosphere are water vapor (H2O), carbon dioxide (CO2), methane (CH4), nitrous oxide (N2O), and ozone (O3). Without greenhouse gases, the average temperature of Earth's surface would be about −18 °C (0 °F), rather than the present average of 15 °C (59 °F).

<span class="mw-page-title-main">Atmospheric methane</span> Methane in Earths atmosphere

Atmospheric methane is the methane present in Earth's atmosphere. The concentration of atmospheric methane—one of the most potent greenhouse gases—is increasing due to methane emissions, and is causing climate change.

<span class="mw-page-title-main">Greenhouse gas monitoring</span> Measurement of greenhouse gas emissions and levels

Greenhouse gas monitoring is the direct measurement of greenhouse gas emissions and levels. There are several different methods of measuring carbon dioxide concentrations in the atmosphere, including infrared analyzing and manometry. Methane and nitrous oxide are measured by other instruments. Greenhouse gases are measured from space such as by the Orbiting Carbon Observatory and networks of ground stations such as the Integrated Carbon Observation System.

Greenhouse gas emissions from wetlands of concern consist primarily of methane and nitrous oxide emissions. Wetlands are the largest natural source of atmospheric methane in the world, and therefore remain a major area of concern with respect to climate change. They contribute approximately 167 Tg of methane to the atmosphere per year. Wetlands account for approximately 20 percent of atmospheric methane through emissions from soils and plants. Wetlands are characterized by water-logged soils and distinctive communities of plant and animal species that have evolved and adapted to the constant presence of water. This high level of water saturation creates conditions conducive to methane production.

<span class="mw-page-title-main">Carbon-neutral fuel</span> Type of fuel which have no net greenhouse gas emissions

Carbon-neutral fuel is fuel which produces no net-greenhouse gas emissions or carbon footprint. In practice, this usually means fuels that are made using carbon dioxide (CO2) as a feedstock. Proposed carbon-neutral fuels can broadly be grouped into synthetic fuels, which are made by chemically hydrogenating carbon dioxide, and biofuels, which are produced using natural CO2-consuming processes like photosynthesis.

<span class="mw-page-title-main">Global surface temperature</span> Average temperature of the Earths surface

In earth science, global surface temperature is calculated by averaging the temperature at the surface of the sea and air temperature over land. Periods of global cooling and global warming have alternated during Earth's history.

<span class="mw-page-title-main">Climate-friendly gardening</span> Low greenhouse gases gardening

Climate-friendly gardening is a form of gardening that can reduce emissions of greenhouse gases from gardens and encourage the absorption of carbon dioxide by soils and plants in order to aid the reduction of global warming. To be a climate-friendly gardener means considering both what happens in a garden and the materials brought into it and the impact they have on land use and climate. It can also include garden features or activities in the garden that help to reduce greenhouse gas emissions elsewhere.

<span class="mw-page-title-main">Peter Smith (biologist)</span> Scottish climate change scientist

Pete Smith is Professor of Soils and Global change at the University of Aberdeen where he directs the Scottish Climate Change Centre of Expertise, ClimateXChange.

Top contributors to climate change are the companies, sources, and countries on Earth causing climate change through greenhouse gas emissions, which are mainly: Carbon dioxide, Methane, Nitrous oxide and the fluorinated gases bromofluorocarbon, chlorofluorocarbon, hydrochlorofluorocarbon, hydrofluorocarbon, nitrogen trifluoride, perfluorocarbons and sulfur hexafluoride

<span class="mw-page-title-main">Greenhouse gas emissions from agriculture</span> Agricultures effects on climate change

Agriculture contributes towards climate change through greenhouse gas emissions and by the conversion of non-agricultural land such as forests into agricultural land. The agriculture, forestry and land use sector contribute between 13% and 21% of global greenhouse gas emissions. Emissions of nitrous oxide, methane make up over half of total greenhouse gas emission from agriculture. Animal husbandry is a major source of greenhouse gas emissions.

References

  1. 1 2 David Reay publications indexed by Google Scholar OOjs UI icon edit-ltr-progressive.svg
  2. 1 2 Ritchie, Hannah (2018). Global food systems : addressing malnutrition through sustainable system pathways. ed.ac.uk (PhD thesis). University of Edinburgh. hdl:1842/33270. OCLC   1085199475. EThOS   uk.bl.ethos.764079. Open Access logo PLoS transparent.svg
  3. David Reay publications from Europe PubMed Central
  4. Dave Reay's ORCID   0000-0001-5829-9007
  5. "Edinburgh Climate Change Institute". Edinburgh Climate Change Institute (ECCI). Retrieved 23 February 2022.
  6. "Home". climatexchange.org.uk. ClimateXChange. Retrieved 23 February 2022.
  7. David Reay on Twitter OOjs UI icon edit-ltr-progressive.svg
  8. Reay, David S. (1999). Temperature dependence of inorganic nitrogen utilisation by bacteria and microalgae. exlibrisgroup.com (PhD thesis). University of Essex. OCLC   556727590. EThOS   uk.bl.ethos.265190.
  9. "Welcome to nginx!". Archived from the original on 9 June 2009. Retrieved 9 June 2009.
  10. "Dave Reay – Dave Reay, University of Edinburgh".
  11. https://www.palgrave.com/gp/book/9783030182052 [ ISBN missing ]
  12. Chris Goodall. Book Review: Going in the right direction, Nature Reports Climate Change, doi : 10.1038/climate.2007.45.
  13. Brian Clegg. Review - Climate Change Begins at Home Popular Science.
  14. Chew Hung Chang. BOOK REVIEW: "Climate Change Begins at Home" The Singapore Economic Review, 2008, vol. 53, issue 02, pages 337-338.
  15. Irena Dingley. Cut Your Carbon BBC.
  16. "Your Planet Needs You!". Archived from the original on 24 January 2009. Retrieved 14 July 2009.
  17. "Greenhouse Gas Sinks". Archived from the original on 19 October 2008. Retrieved 9 June 2009.
  18. "Home". ghgonline.org.
  19. "Dave Reay – Dave Reay, University of Edinburgh".
  20. "University of Edinburgh Business School - Carbon Management". Archived from the original on 28 January 2010. Retrieved 9 June 2009.
  21. "The Royal Society of Edinburgh". Archived from the original on 24 December 2012. Retrieved 14 July 2009.
  22. "ScienceLive - Climate Change Begins at Home with David Reay". Archived from the original on 20 August 2008. Retrieved 14 July 2009.
  23. "The Royal Institution of Great Britain | Dr Dave Reay". Archived from the original on 22 June 2010. Retrieved 14 July 2009.
  24. "Reap what we sow". Archived from the original on 5 July 2009. Retrieved 14 July 2009.
  25. 1 2 "Dave Reay – Dave Reay, University of Edinburgh".