1. Projecting future changes in U.S. forest fuel and fire conditions using NARCCAP regional climate change scenarios Yongqiang Liu Center for Forest Disturbance Science USDA Forest Service, Athens, GA 2012 NARCCAP Users’ Meeting April 10 – 11, 2012. NCAR, Boulder, CO

2. The Lower North Fork Fire 20 miles west of Denver on March 26, 2012 4140 acres burned 27 home destroyed 3 fatalities About 400 firefighters from several states A prescribed burning by Colorado Forest Service escaped into a wildfire Warm winds and highs in the 70s are expected to further dry out brush and other potential fire fuel along the Front Range and Colorado plains., and residents are being discouraged from lighting campfires or burning trash (NWS).

3. 750,000 acres (3,000 km 2 ) burned 22 human lives lost 4,000 homes destroyed Billions of dollars in damage 12,000 firefighters in suppression 2005 Southern California Fires

4. Wildfire in the U.S. Hundreds of thousands of fires each year 4 million acres (16,000 km 2 ) burned annually in past 50 years. 6 million acres in past decade Low frequency and high severity in the west, high frequency and low severity in the east

5. Mega-fires Big fires – Very large burned areas Big impacts – smoke transported to major metro areas Big efforts – forest management options for risk prevention and impact mitigation prevention and impact mitigation Occurring mostly under drought conditions -1988 Yellowstone fires. About 800,000 acres affected - The northern U.S. drought was among the driest of the 20th century -2011 TX and SE fires. About 4.3 million acres burned. -Worst ever one-year drought -2011 GA/FL Okefenokee fires. About 600,000 acres burned. -Worst drought in Georgia in a century

6. Fire Potential and Fire Danger Prevent activities leading to fire ignition Fire management planning (e.g., suppression) Condition for prescribed burning

7. What is fire potential in future under changing climate? What is fire potential in future under changing climate? Atmospheric condition is one of environmental factors for individual wildfires Climate models have projected overall increase in temperature and more frequent droughts in many mid-latitude regions due to the greenhouse effect. Thus, it is likely wildfires will increase in frequency and intensity in these regions including the U.S. (IPCC 2007). The impact of climate change on fire is already occurring (Westerling et al., 2006) and will become more remarkable by middle of this century in the western U.S. (Spracklen et al. 2009)

8. Prediction of future U.S. wildfire trends and impacts Project future mega-fire activity under changing climateProject future mega-fire activity under changing climate Assess impacts on air quality in major metropolitan areasAssess impacts on air quality in major metropolitan areas Help mangers develop forest management options for mitigationHelp mangers develop forest management options for mitigation - A research project supported by the USDA and USDOI Joint Fire Science Program (JFSP)

9. Special values of NARCCAP Data 1. Calculating fire danger rating and fire indices such as Keetch-Byram Drought Index (KBDI)

10. 2. Driving Dynamic Land Ecosystem Model DLEM - a process-based terrestrial ecosystem model (Tian et al., 2010) Project fuel change in fuel loading, which is a factor for fire emissions

11. 3. Driving smoke and air quality models Wildfires emit large amounts of PM 2.5 and O 3 precursors that lead to regional haze, smog, and visibility degradation Biomass burning contributes to about 40% of total BC emissions, which play a key role in the smoke- snow feedback mechanism. Radiative forcing of smoke particles reduces surface temperature, cloud and precipitation. Fire events could enhance climate anomalies such as droughts. Simulations using regional air quality models such as CMAQ and WRF-Chem need full meteorology. Smoke prediction system for air quality prediction (NOAA ARL).

12. 4. Calculating windows for prescribed burning Prescribed burning is a management tool for reducing wildfire risk by removing the accumulating dead fuels. One of management tools for mitigation of future wildfire increase However, there is increasing risk for fire escaping (a control burning becomes a wildfire) due to global warming. Preferred weather conditions for prescribed burning in the southern U.S.: - wind speed at 20-foot above the ground of 6-20 mph; - relative humidity of 30-55%; - temperature of <60oF in winter; - fine fuel (1-hour) moisture of 10-20%, and - KBDI of 250-400.

13. Large values of over 600 (extreme fire potential) all seasons in the inter-Mountains KBDI increases from winter to fall in the East, up to 500 Using HadCM3-HRM3 projection Using HadCM3-HRM3 projection

14. RegionPresentFuture winterspringsummerfallwinterspringsummerfall PS 0.50 0.50 2.13 2.13 2.24 2.240.95 1.97 1.97 1.49 1.49 0.01 0.01 0.07 0.07 PW 0.43 0.43 0.06 0.06 0.80 0.800.17 0.56 0.56 1.25 1.25 1.24 1.24 1.57 1.57 SW 4.15 4.15 4.32 4.32 4.48 4.484.00 -1.44 -1.44-1.83-0.37-0.09 NW 2.58 2.58 2.83 2.83 2.39 2.392.68 2.61 2.61 2.03 2.03 2.87 2.87 3.34 3.34 SC 2.17 2.17 0.79 0.79 4.57 4.574.04 -3.56 -3.56-1.18 1.13 1.13 0.03 0.03 NC 2.64 2.64 1.86 1.86 1.42 1.422.98 0.34 0.34-0.22 1.90 1.90 3.37 3.37 SE -0.30 -0.30 -0.25 -0.25 2.71 2.713.20 -2.20 -2.20 0.61 0.61 1.61 1.61 1.76 1.76 NE 1.09 1.09 0.35 0.35 1.48 1.482.92 -1.37 -1.37 0.03 0.03 2.61 2.61 1.73 1.73 US 1.95 1.95 1.64 1.64 2.77 2.773.03 1.11 1.11 0.40 0.40 1.38 1.38 1.49 1.49 Slopes of fitting lines of KBDI curves over 30-year periods

15. Increase in Rocky Mountains all seasons Increase in Southeast and Pacific coast in Summer and Fall Decrease in the inter-Mountains all seasons in Winter and Spring

16. Fire potential increases by one level, from low to moderate or from moderate to high in southern eco-regions

17. Also most remarkable during summer and fall seasons, but with different spatial patterns. Change in KBDI calculated using HadCM3 projection

18. Future change in southern fuel loading (Zhang et al., 2009)

19. Future change in fuel moisture

20. Available days for burns are reduced in most areas. Largest reduction in southeast by up to 30% during summer. Increase slightly in the west coast and inter-mountains. Change in burning window for prescribed burning

21. Conclusions Climate is the most important environmental factor for long- term wildfire variability. Large change in future U.S. wildfire is expected under a changing climate. Climate is the most important environmental factor for long- term wildfire variability. Large change in future U.S. wildfire is expected under a changing climate. High-resolution climate change scenarios are necessary for projection of future wildfire trends. Dynamical downscaling adds values to traditionally used statistical downscaling by providing unique information for integrated fire projection and impact research. High-resolution climate change scenarios are necessary for projection of future wildfire trends. Dynamical downscaling adds values to traditionally used statistical downscaling by providing unique information for integrated fire projection and impact research. With the application of NARCCAP data, we were able to understand the impacts of climate change on U.S. fire potential, forest fuel conditions, and forest management. The data will be further applied to understanding the air quality impacts of changing wildfire. With the application of NARCCAP data, we were able to understand the impacts of climate change on U.S. fire potential, forest fuel conditions, and forest management. The data will be further applied to understanding the air quality impacts of changing wildfire.

22. Thanks!