Climate Change, Carbon and Wildfires

Similar documents
Wildfires Mitigation Strategy and Incentives in Northern and Central Australia: Dr. Jeremy Russell-Smith

Agricultural Application of Mycorrhizal Fungi to Increase Crop Yields, Promote Soil Health and Combat Climate Change

Carbon Sequestration Why and How?

Hydraulic Fracturing Is Industry Standard Practice the Best Practice? The Case for Waterless Fracking

Figure 1 - Global Temperatures - A plot from the EarthScience Centre at

Forestry and carbon sequestration.

Climate Change: The Debate

In 2011 burning of fossil fuels provided 83% of mankind s energy resource while nuclear electric power provided 9%, and renewable energy 8% (1).

Prof Brendan Mackey, PhD

The Forgotten Resource: Groundwater in Australia 1

INTRO TO GREENHOUSE GAS EMISSIONS


Earth s energy balance and the greenhouse effect

Curbing Greenhouse Gases: Agriculture's Role

UN Climate Council Words in red are defined in vocabulary section (pg. 9)

2. Climate change and forests

MANUAL FOR REDD PROGRAM

Climate Change Specialist Report final

THE INTRODUCTION THE GREENHOUSE EFFECT

Teacher Guide Climate Change: The Debate A Structured Controversy

Building a Global Agenda of Action. in support of sustainable livestock sector development

Main Anthropogenic Sources of Greenhouse Gases Agriculture, Fire, Change in Land Use and Transport

The Economics of the Kyoto Protocol

Wood and Paper Products Store Greenhouse Gases

Cool Farming Climate impacts of agriculture and mitigation potential

GLOBAL WARMING AND THE EFFECT ON AGRICULTURE

CLIMATE ACTON PLANNING & MITIGATION: Base Year 2016 Greenhouse Gas Inventory Results

Chapter 19 Global Change

SINKS IN THE CDM? IMPLICATIONS AND LOOPHOLES

LIVING IN THE ENVIRONMENT, 18e G. TYLER MILLER SCOTT E. SPOOLMAN. Climate Disruption. Cengage Learning 2015

Chapter 19 Global Change

Scope and methodology for measuring the Greenhouse Gas (GHG) and Carbon Profile of the Canadian Forestry Industry

Fertilizing biofuel crops may cause release of greenhouse gases Featured scientist: Leilei Ruan from Michigan State University

Topic A2. Wetlands in the IPCC processes

FOREST MEASUREMENT AND MONITORING WORKSHOP September 4-5 Puyo, Ecuador

Web-quest Exploration Guide

CAN THE UNITED NATIONS KEEP CLIMATE CHANGE UNDER CONTROL?

Greenhouse Effect. The Greenhouse Effect

Agriculture and Greenhouse Gas Mitigation: Who, What, How, Where and When?

TECHNICAL NOTE #08. Carbon Footprint in the context of clay brick masonry walling TECHNICAL CONTRIBUTOR

HU-205: Geography. Geography 04: Biogeochemical Cycles & Biosphere. Biomes. Global patterns in the biosphere

content of the atmosphere. In 2011 about 90% of total CO 2

Climate Change Policy and Economics: Implications and Opportunities for Agriculture. KSU Extension Conference Global Climate Change Session

Narration: The presentation consists of three parts.

Joint Submission from Beef + Lamb New Zealand and Deer Industry New Zealand to:

FCRN Soil Carbon Workshop The potential for soil carbon sequestration, including the role of nitrogen. Keith Goulding, David Powlson and Andy Whitmore

The atmosphere is warming

Teaching Time: 1 hour and 15 minutes

Bushfires, Prescribed Burning and Global Warming

Background Brief for Outcomes Australia Forum on Vegetation-Rainfall Relationships

Estimating the Overall Impact of A Change In Agricultural Practices on Atmospheric CO 2

IRELAND S EMISSIONS OF GREENHOUSE GASES FOR THE PERIOD

- Changes in the concentration of gases can increase or decrease Earth s temperature.

Information on LULUCF actions by Sweden. First progress report

FIGURE SET HEADER for Set #5. Figure Set 5: Global Warming Potential Temperate Agriculture

Asia and Pacific Commission on Agricultural Statistics

GLOBAL WARMING IS HAPPENING GLOBAL WARMING WILL BE VERY HARD TO STOP (By John B. Wheeler, member Potomac River Association)

Farming Sustainability Series Part II: Sustainability in Australian Farming Systems Professor Kadambot Siddique

FACT SHEET IMPACTS OF USING NATIVE FOREST BIOMASS FOR ENERGY

2. Why the Level of Ambition Must Be Raised

INTRODUCTION FORESTS & GREENHOUSE GASES

FACTS ABOUT GL BAL WARMING. gogreen. Shop visit An Ekotribe Initiative

Understanding tropical deforestation

Heating up: bushfires and climate change

FIRE MANAGEMENT OF CONSERVATION RESERVES IN THE KIMBERLEY

LAND COURT OF QUEENSLAND

FAO S work on climate change Soils, land and water. SOILS, LAND AND WATER for climate change adaptation and mitigation

AGRICULTURE & FORESTRY

THE CARBON CRISIS: IT S NOW OR NEVER TO SAVE CORAL REEFS

Farming Sustainability Series Part III: Sundrop Farms- Growing with Seawater and Sunlight Philipp Saumweber, Founder and CEO, Sundrop Farms

Carbon at risk. B.C. s Unprotected Old-Growth Rainforest. Logging on Vancouver Island Photo: TJ Watt

Fact sheet 18 June Selecting and Using GWP values for Refrigerants

Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore

The Management of Soil Nutrients: Chemical Fertilisers or Not?

Forest industries. National Association of Forest Industries. and climate change

Climate Change Science: Where are we now and where are we heading?

Greenhouse gas emissions during the 2003 World Summit

INVEST SMART. TRADE WISE. THINK GREEN.

Duke Energy s Low Carbon Strategy Initiatives for West Virginia December 8, 2009

Introduction and Methodology

Global warming. Models for global warming Sand analogy

CALIFORNIA EDUCATION AND THE ENVIRONMENT INITIATIVE

Peatland Ecosystem and Global Change

What does IPCC AR5 say? IPCC as a radical inside the closet

LONG TERM (OPERATION) IMPACTS AND POTENTIAL MITIGATION

Weather has always been a hot topic of conversation. We talk about whether it is hot or cold, windy or calm, snowy or dry. We listen to the radio to

Climate MRV for Africa Phase 2 Development of National GHG Inventory Grassland

Carbon Dioxide and Global Warming Case Study

Dr David Karoly School of Meteorology

Policy Briefing Paper: Australian Food Systems

2.0 Climate Change Response

Chapter 19: Global Change

Perspectives on Carbon Emissions from uanadian arest Fire

The carbon impacts of choices with the body after death: four scenarios

Tropical Forests and Atmospheric Carbon Dioxide: Current Knowledge and Potential Future Scenarios

Permaculture Design Masterclass EBook. 3. Production

Discussion Paper. Voluntary Carbon Offsets

Informal Meeting of Agriculture Ministers

Clark University Greenhouse Gas Emissions Update: Clark University on Track for Carbon Reduction and Carbon Neutrality Goals.

Chapter 2. Climate Change: Scientific Basis

Transcription:

12 7 October 2014 Climate Change, Carbon and Wildfires Christopher D. Johns Research Analyst Climate Change Key Points Recent evidence indicates that as much as 10% of wildfire produced carbon remains in the atmosphere contributing to global warming. Even in circumstances where carbon sequestering does achieve balanced levels, for around seven months of the year the carbon released by wildfires still contributes to the total amount of greenhouse gas (GHG) in the atmosphere. There is a growing body of evidence suggesting that, as the planet warms, wildfires are becoming more frequent and more intense. While measures to curb industrial GHG emissions have proved difficult and divisive, reductions achieved by the control of wildfires have been largely ignored and may provide a less controversial way of contributing GHG reductions. Summary Until recently, carbon released into the atmosphere from wildfires was not considered a significant component of atmospheric greenhouse gas (GHG). It was assumed that over the climatic cycle this carbon would be sequestered back into vegetative re-growth. A growing body of evidence however, now suggests that carbon produced by wildfires is making a significant contribution to the volume of GHG in the atmosphere in both the short and long term. In the future, atmospheric carbon estimates should include wildfires as a significant GHG source and effort to reduce atmospheric carbon must include measures to curb wildfires.

Analysis Introduction In December 2014 the United Nations Intergovernmental Panel on Climate Change (IPCC) is expected to present its 5 th Assessment Report. The Climate Change Council of Australia has summarised preliminary key findings that emphasise the ever-increasing body of evidence supporting the judgement that climate change is occurring as a result of human activities. This confirms the findings of the previous assessment report (AR4) published in 2007. The Climate Change Council also acknowledges the scientific findings that support the view that climate change is already affecting many natural and human systems and poses significant risks to human health, ecosystems, infrastructure, agricultural production and communities. Bearing in mind that the IPCC is the most authoritative international body on climate change science, and that its assessments are subject to an extremely rigorous review process, statements as categorical as those above must be viewed with the utmost seriousness. It is possible, however, that the IPCC has overlooked a significant source of atmospheric GHG. Each year wildfires release large quantities of carbon into the atmosphere. Currently this carbon this is not considered a major contributor to GHG influenced climate change. It may be time to reconsider this policy. Greenhouse Gas The principle cause of human induced climate change is the release of GHG into the atmosphere, largely from the burning of fossil fuels. This process was brought about by the industrial revolution and has increased exponentially with developments in technology and the spread of industrialisation. Perhaps, not surprisingly, efforts to curb the burning of fossil fuels in order to reduce atmospheric GHG have been largely unsuccessful. The considerable achievements of the United Nations Framework Convention on Climate Change notwithstanding, coordinated controls and reduction targets appear to be beyond the capacity of the international community at this time. Industrialised nations with highly developed capitalist economies depended upon growth driven by consumerism. Developing nations with large workforces and markets defend with vigour their right to pursue the lifestyles of the nations who were once seen as their exploiters. It is not surprising, therefore, that other sources of GHG have not received similar consideration. One significant source of GHG that, until recently, has been overlooked in GHG emission calculations has been the CO2 produced by wildfires and recent scientific research suggests this exclusion may have been a mistake. Wildfires Definitions of wildfires differ slightly but they are commonly defined as a fire that burns quickly and uncontrolled in areas of grass, bush or woodland. The most common cause of wildfires is lightning strike. A wildfire can also be deliberately lit if it is not appropriately authorised as in the case of arson or if control of an authorised fire is lost. In Australia wildfires are often referred to as bushfires, a general term that refers to the woodland fires that occur in the southeast of the nation and the savannah fires of more northern regions. It is important to differentiate wildfires from the deliberate burning of stubble following the Page 2 of 5

harvesting of crops and from the use of fire as a land management practice as often attributed to Australian Aboriginal culture. Under this definition, wildfires would not include the use of fire for land clearance for agriculture, as has occurred on a huge scale in South America, Africa and Asia. This practice is believed to have contributed significantly to climate change both in the direct production of GHG and in the loss of natural capacity to draw carbon back out of the atmosphere by forests. For a graphic depiction of global fire activity since the year 2000, refer to the NASA Earth Observatory link: linkhttp://earthobservatory.nasa.gov/globalmaps/view.php?d1=mod14a1_m_fire For millennia fire has been a feature of the natural environment. An equilibrium existed whereby the quantity of CO2 released into the atmosphere by burning and the quantity stored in plant material by photosynthesis remained neutral. In 1997, when the Kyoto protocols set rules for the international accounting of GHG emissions, it was assumed that much of the GHG produced by wildfires, such as CO 2, would be recycled back into vegetation as regrowth and did not significantly contribute to global warming. Accordingly, the Australian Greenhouse Office s National Greenhouse Gas Inventory estimates that the accountable, greenhouse gas emissions from wildfires contributed less than 2% of Australia s total emissions as only methane and nitrous oxide, and not CO2, were considered. This view, while appropriately conservative in the context of the Kyoto protocols in 1997, now understates the importance of wildfire related GHG emission in two ways. Firstly, CO2 released into the atmosphere by wildfires can remain there for a period of approximately seven months before it is re-captured by photosynthesis. During this time it will contribute to the warming of the planet. Secondly, and most importantly, there is compelling evidence from a number of sources that the incidence and intensity of wildfires is increasing. Research from the United States indicates that wildfires are getting bigger, more destructive, and more expensive 1. A recent report by the US Union of Concerned Scientists stated as the world warms, we can expect more seasons with higher wildfire potential, seasons are projected to lengthen, with the Southwest s [of the United States] season of fire potential lengthening from seven months to all year long. Additionally, wildfires themselves are likely to be more severe. Similarly, a recent Australian report submitted to the IPCC, recommended wildfire emissions of CO 2 be integrated into future climate change models as the body of scientific evidence against wildfires being neutral for CO 2 GHG emissions grows. Current Australian research indicates that even in environments where significant regrowth is able to occur, some 10% of CO 2 is remaining in the atmosphere after sequestration. This figure is almost certainly a conservative assessment. Globally, forested areas are being burnt more regularly and are unable to sequester as much CO 2 as they have in the past. Wildfires may now, or may become, an amplifier of global warming. Higher temperatures create conditions where wildfires are more likely for longer periods and will burn with greater intensity with less capacity for regeneration of vegetation. The resultant CO 2 emissions contribute to higher temperatures and the cycle continues. 1 Bonnicksen, Thomas M. Texas AM University, 2009. Page 3 of 5

Wildfire GHG emissions vary significantly depending upon the intensity and the fuel burnt. The savannah fires of northern Australia differ greatly from woodland fires of the southeast of the country. Woodland fires are often categorised as either crown or surface fires. Crown fires are characterised by their large size and high-intensity that take out all of the aboveground living material. Surface fires burn with mixed-intensity and typically burn forests with low, moderate, and high-severity burn patches. For this reason it is difficult to make accurate calculations of the quantities of CO 2 produced by a specific wildfire. This variation notwithstanding, the contribution of wildfires to Australia s greenhouse gas emission calculations even at the lower estimates, remains significant as illustrated by the following analysis: Wildfires burn on average 30 million hectares per year but, on occasion, may burn up to 120 million hectares. Wildfires emit between 5 and 30 tonnes of carbon per hectare. This would be a total of between 150 and 900 million tonnes of carbon in an average year and, on occasion, between 600 and 3600 tonnes of carbon a year. Australia s industrial GHG emissions average 155 million tonnes of carbon per year 2. In an average year (30 million hectares), wildfire emissions would range from slightly less than industrial emissions (150 vs. 155 million tonnes) to 6 times that of industrial emissions. In an exceptional year, when 120 million hectares are burnt, wildfire emissions would range from 4 to 23 times industrial emissions. When this calculation is applied globally, the proportion of wildfire to industrial production carbon is reduced but remains significant: It is estimated that annually between 350 and 450 million hectares of forest and grassland are burnt by wildfires 3. As stated above, wildfires emit between 5 and 30 tonnes of carbon per hectare; therefore, annually wildfires globally will produce between 1.75 and 13.5 billion metric tonnes of carbon. In 2012, 35.425 billion metric tonnes of CO 2 were produced from industrial sources 4 or 9.668 billion metric tonnes of carbon. Note: 3.664 million tonnes of CO 2 equals 1 million tonnes of carbon. These figures clearly demonstrate the potential for significant reduction of GHG emissions by reducing the incidence of wildfires. Any measures that reduce the release of CO 2 and other greenhouse gases into the atmosphere will result in an improvement in the greenhouse gas budget 5. 2 This figure does not include aircraft and shipping emissions or emissions from fossil fuels exported to countries with development status. 3 Power, Lauren. 2013. Global Wildfires, Carbon Emissions and the Changing Climate. FDI SAP 22 November 2013. 4 http://www.globalcarbonatlas.org/?q=emissions 5 http://www.savanna.org.au/ Page 4 of 5

One option for reducing wildfires may be to restore the former natural ecological grazing that limited fuel levels and fire impacts up to 20,000 years ago and helped regenerate unique resilient bio-systems 6. Changing land-management techniques in savannah and scrubland could dramatically decrease the risk of large, carbon emitting fires, reducing the global GHG burden 7. In summary, the control and reduction of wildfires is significant to the GHG equation for three reasons: Globally, wildfires will produce huge volumes of GHG which, from the most conservative estimates will remain in the atmosphere for seven months contributing to global warming. The theory that the CO 2 produced by wildfires is ultimately GHG neutral is no longer correct. Global warming has created conditions where wildfires are becoming more intense and more frequent producing greater volumes of CO 2 in the atmosphere, while reducing regrowth and hence the capacity to sequester carbon back into vegetation. By preventing wildfires, and enhancing the growth of stable vegetation, carbon is drawn out of the atmosphere and stored organically by photosynthesis and actively reduces GHG in the atmosphere. As IPCC Assessment Report 5 states, the concentration of greenhouse gases in the atmosphere has increased to levels unprecedented on earth in 800,000 years. Future surface temperatures will largely be determined by cumulative CO 2, which means climate change will continue even if CO 2 emissions are stopped. Therefore, if the effect of climate change is to be avoided, there is a need not only to stop producing CO 2 at current rates but also reduce the levels of CO 2 currently in the atmosphere. ***** Any opinions or views expressed in this paper are those of the individual author, unless stated to be those of Future Directions International. Published by Future Directions International Pty Ltd. 80 Birdwood Parade, Dalkeith WA 6009, Australia. Tel: +61 8 9389 9831 Fax: +61 8 9389 8803 E-mail: info@futuredirections.org.au Web: www.futuredirections.org.au 6 Jehne, Walter. 2014. The Role of Wildfires in the Ecology of the Australian Landscape and its Regeneration. FDI Associate Paper 9 April 2014. 7 Power, Lauren. 2013. Global Wildfires, Carbon Emissions and the Changing Climate. FDI SAP 22 November 2013. Page 5 of 5