Climate change and the future occurrence of moorland wildfires in the Peak District of the UK

We investigated the impact of climate change on the number of wildfires in the Peak District uplands of northern England. Wildfires in peat can result in severe carbon loss and damage to water supplies, and fighting such fires is difficult and costly in such a remote location. The Peak District is expected to experience warmer, wetter winters and hotter, drier summers. Local weather simulations from a weather generator were used to predict the future incidence and timing of fires. Wildfire predictions were based on past fire occurrence and weather over 27.5 yr. A Probit model of wildfire incidence was applied to simulated weather data, which were generated by a Markov pro- cess and validated against actual baseline weather data using statistical criteria and success in repli- cating past fire patterns. The impact of climate change on the phenology and ecology of moorland and on visitor numbers was considered. Simulations suggest an overall increase in occurrence of summer wildfires. The likelihood of spring wildfires is not reduced by wetter winter conditions; how- ever, the chance of wildfires rises as rainfall decreases. Temperature rise has a non-linear impact, with the risk of wildfire occurrence rising disproportionately with temperature. Recreation use is a major source of ignition. Little change in wildfire incidence is projected in the near future, but as cli- mate change intensifies, the danger of summer wildfires is projected to increase from 2070; therefore, fire risk management will be necessary in future. In addition, moorlands may have to be managed to reduce the chance of summer wildfires becoming catastrophic, with consequent damage to eco- system services such as water supplies and peat carbon storage. Management measures may include controlled burning, grazing or mowing to remove fuel.

[1]  C. Harpham,et al.  A daily weather generator for use in climate change studies , 2007, Environ. Model. Softw..

[2]  P. Jones,et al.  Observed trends in the daily intensity of United Kingdom precipitation. , 2000 .

[3]  Stephen J. Cornell,et al.  Modelling the coupled dynamics of moorland management and upland vegetation , 2009 .

[4]  D A Stainforth,et al.  Confidence, uncertainty and decision-support relevance in climate predictions , 2007, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.

[5]  R. Milne,et al.  Carbon in the Vegetation and Soils of Great Britain , 1997 .

[6]  Benjamin P. Bryant,et al.  Climate change and wildfire in California , 2008 .

[7]  Jean Palutikof,et al.  Impacts of short-term climate variability in the UK on demand for domestic and international tourism , 2006 .

[8]  Scott L. Stephens,et al.  Fire and sustainability: considerations for California’s altered future climate , 2008 .

[9]  D. Wilks,et al.  The weather generation game: a review of stochastic weather models , 1999 .

[10]  Jürgen P. Kropp,et al.  Trend assessment: applications for hydrology and climate research , 2005 .

[11]  Simon J. Brown,et al.  An extreme value analysis of UK drought and projections of change in the future , 2010 .

[12]  M. Flannigan,et al.  Climate change and forest fires. , 2000, The Science of the total environment.

[13]  J. Rothwell,et al.  The role of wildfire and gully erosion in particulate Pb export from contaminated peatland catchments in the southern Pennines, U.K. , 2007 .

[14]  P. Waggoner Anticipating the frequency distribution of precipitation if climate change alters its mean , 1989 .

[15]  J. Mayes SPATIAL AND TEMPORAL FLUCTUATIONS OF MONTHLY RAIDFALL IN THE BRITISH ISLES AND VARIATIONS IN THE MID‐LATITUDE WESTERLY CIRCULATION , 1996 .

[16]  G. Behn,et al.  Fuel dynamics and fire behaviour in spinifex grasslands of the Western Desert , 2006 .

[17]  G. Cavan,et al.  The Best Strategy for Mitigating Moorland Wildfire Risk A Report to Moors for the Future , 2007 .

[18]  P. White,et al.  Environmental drivers of large, infrequent wildfires: the emerging conceptual model , 2007 .

[19]  Jay D. Miller,et al.  Quantitative Evidence for Increasing Forest Fire Severity in the Sierra Nevada and Southern Cascade Mountains, California and Nevada, USA , 2009, Ecosystems.

[20]  T. Dawson,et al.  Potential effects of climate change on plant communities in three montane nature reserves in Scotland, UK , 2008 .

[21]  J. Holden,et al.  Ecosystems Services in Dynamic and Contested Landscapes: The Case of UK Uplands , 2009 .

[22]  J. Keith Gilless,et al.  Predicting the effect of climate change on wildfire behavior and initial attack success , 2008 .

[23]  T. Brown,et al.  The Impact of Twenty-First Century Climate Change on Wildland Fire Danger in the Western United States: An Applications Perspective , 2004 .

[24]  J. R. Wallis,et al.  Noah, Joseph, and Operational Hydrology , 1968 .

[25]  Roger Stern,et al.  Fitting Models to Daily Rainfall Data , 1982 .

[26]  Roy Thompson,et al.  A time-series analysis of the changing seasonality of precipitation in the British Isles and neighbouring areas , 1999 .

[27]  Peter Chapman,et al.  Environmental change in moorland landscapes , 2007 .

[28]  M. Hulme,et al.  Evidence for trends in heavy rainfall events over the UK , 2002, Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences.

[29]  E. Mills,et al.  The Impact of Climate Change on Wildfire Severity: A Regional Forecast for Northern California , 2004 .

[30]  John E. Walsh,et al.  Assessing the response of area burned to changing climate in western boreal North America using a Multivariate Adaptive Regression Splines (MARS) approach , 2009 .

[31]  Annette Menzel,et al.  Observed changes in seasons: an overview , 2002 .

[32]  C. Legg,et al.  The future of fire management in the British uplands , 2008 .

[33]  E. Chuvieco,et al.  Human-caused wildfire risk rating for prevention planning in Spain. , 2009, Journal of environmental management.

[34]  J. Tallis Fire and flood at Holme Moss: erosion processes in an upland blanket mire , 1987 .

[35]  Richard Coe,et al.  A Model Fitting Analysis of Daily Rainfall Data , 1984 .

[36]  S. Page,et al.  The amount of carbon released from peat and forest fires in Indonesia during 1997 , 2002, Nature.

[37]  J. Craddock Annual rainfall in England since 1725 , 1976 .

[38]  A. Mackay,et al.  Summit-type blanket mire erosion in the Forest of Bowland, Lancashire, UK: Predisposing factors and implications for conservation , 1996 .

[39]  Richard W. Katz,et al.  Precipitation as a Chain-Dependent Process , 1977 .

[40]  A. Watt CONTRIBUTIONS TO THE ECOLOGY OF BRACKEN (PTERIDIUM AQUILINUM). VI. FROST AND THE ADVANCE AND RETREAT OE BRACKEN , 1954 .

[41]  P. Jones,et al.  UK Climate Projections Briefing Report , 2010 .

[42]  A. Thomas,et al.  Sediment Stratigraphy and Heavy Metal Fluxes to Reservoirs in the Southern Pennine Uplands, UK , 2006 .

[43]  Timothy E H Allott,et al.  Drivers of Change in Upland Environments , 2009 .

[44]  J. Radley Significance of Major Moorland Fires , 1965, Nature.

[45]  A. McGuire,et al.  Assessing the response of area burned to changing climate in western boreal North America using a Multivariate Adaptive Regression Splines (MARS) approach , 2009 .

[46]  Drake Circus Thermal shock and germination in North-West European Genisteae: implications for heathland management and invasive weed control using fire , 2009 .

[47]  T. Swetnam,et al.  Warming and Earlier Spring Increase Western U.S. Forest Wildfire Activity , 2006, Science.

[48]  Jim W. Hall,et al.  Climate scenarios and decision making under uncertainty , 2007 .

[49]  J. P. Grime,et al.  A Comparison of Plant Responses to the Extreme Drought of 1995 in Northern England , 1997 .

[50]  Daniel C. Donato,et al.  Forest Fire Impacts on Carbon Uptake, Storage, and Emission: The Role of Burn Severity in the Eastern Cascades, Oregon , 2009, Ecosystems.

[51]  Jonathan Aylen,et al.  Forecasting the outbreak of moorland wildfires in the English Peak District. , 2009, Journal of environmental management.

[52]  Jonathan Aylen,et al.  Climate Change and the Visitor Economy: the challenges and opportunities for England?s Northwest , 2006 .

[53]  Jeff Warburton,et al.  Eroding blanket peat catchments : global and local implications of upland organic sediment budgets. , 2006 .

[54]  M. Hoosbeek,et al.  Raised atmospheric CO2 levels and increased N deposition cause shifts in plant species composition and production in Sphagnum bogs , 2001 .

[55]  J. Tallis Mass movement and erosion of a southern Pennine blanket peat , 1985 .

[56]  M. Moritz,et al.  Global Pyrogeography: the Current and Future Distribution of Wildfire , 2009, PloS one.

[57]  Marc B. Parlange,et al.  STATISTICS OF EXTREMES: MODELING ECOLOGICAL DISTURBANCES , 2005 .

[58]  C. Legg,et al.  Fuel Moisture Thresholds in the Flammability of Calluna vulgaris , 2011 .

[59]  Iain Brown,et al.  Climate change in the uplands: a UK perspective on safeguarding regulatory ecosystem services. , 2008 .

[60]  T. Webb, Is vegetation in equilibrium with climate? How to interpret late-Quaternary pollen data , 1986, Vegetatio.

[61]  Jonathan Aylen,et al.  Modelling the Great Lakes Freeze: forecasting and seasonality in the market for ferrous scrap , 1996 .

[62]  M. Reed,et al.  Predicting the future carbon budget of an upland peat catchment , 2007 .

[63]  Douglas Maraun,et al.  United Kingdom daily precipitation intensity: improved early data, error estimates and an update from 2000 to 2006 , 2008 .

[64]  D. Wilks Maximum Likelihood Estimation for the Gamma Distribution Using Data Containing Zeros , 1990 .