Study | Geography | Forest type | Forecast time period | Elevation (m) | Study extent (km) | GCMs in model | Climate scenario | Climate Variables used in model | Model Used |
---|---|---|---|---|---|---|---|---|---|
Cassell et al. 2019. Widespread severe wildfires under climate change lead to increased forest homogeneity in dry mixed-conifer forests | Southern Blue Mountains of central Oregon | Mixed conifer | 2010–2100 | 719–2744 | 9388 | Range of 20 CIMP5 | Contemporary, RCP 4.5 and RCP 8.5 | maximum temperature, minimum temperature, average precipitation, daily average wind speed, wind direction | LANDIS II Dynamic Fire and Fuels extension |
Hansen et al. 2020. Can wildland fire management alter 21st-century subalpine fire and forests in Grand Teton National Park, Wyoming, USA? | Grand Teton NP, WY | Mixed conifer | 2018–2098 | 1600–3400 | 400 | CNRM-CM5, GFDL-ESM2M | RCP 4.5 and RCP 8.5 | KBDI, daily temperature, precipitation, vapor pressure deficit, solar radiation | iLand |
Honig and Fulé 2012. Simulating effects of climate change and ecological restoration on fire behavior in a southwestern USA ponderosa pine forest | Kaibab National Forest, AZ | P. pine | 2070–2099 | 2067–2184 | 7 | CSIRO:MK3 (least extreme model); MPIM:ECHAM5 (most extreme model) | A1B | temperature, relative humidity, 1-h fuel moisture, 10-h fuel moisture, 100-h fuel moisture, wind speed | ANOVA, Tukey HSD mean comparison |
Hurteau 2017. Quantifying the Carbon Balance of Forest Restoration and Wildfire under Projected Climate in the Fire-Prone Southwestern US | Northern AZ, Camp Navajo | P. pine | Early (2010–2019), mid (2050–2059), and late (2090–2099) century | 2164 | 116 | Range of 41 CIMP5 | RCP 8.5 | Mean monthly minimum temperature, mean monthly maximum temperature, mean monthly precipitation | LANDIS II Dynamic Fire and Fuels extension |
Krofcheck et al. 2017a. Prioritizing forest fuels treatments based on the probability of high-severity fire restores adaptive capacity in Sierran forests | Sierra Nevada, CA | Oak, p. pine, mixed conifer | 1950–2100 | 300–3000 | 875 | CIMP5: CCSM4, CNRM-CM5, FGOAL-g2S, GFDL, MICROC5-ESM 2 | RCP 8.5 | temperature, precipitation | LANDIS II Dynamic Fire and Fuels extension |
Krofcheck et al. 2017b. Restoring surface fire stabilizes forest carbon under extreme fire weather in the Sierra Nevada | Sierra Nevada, CA | Mixed conifer | 1980–2015 to 2100 | 300–3000 | 875 | NA | contemporary, extreme | temperature, precipitation | LANDIS II Dynamic Fire and Fuels extension |
Krofcheck et al. 2019. Optimizing Forest Management Stabilizes Carbon Under Projected Climate and Wildfires | Sangre De Cristo mtns, NM | PJ, P. Pine, Mixed conifer | 2000–2050 | 1900–3700 | 450 | CIMP5: CCSM4, CNRM-CM5, FGOAL-g2S, GFDL, MICROC5-ESM 2 | RCP 8.5 | temperature, precipitation | LANDIS II Dynamic Fire and Fuels extension |
Liang et al. 2018. Large-scale restoration increases carbon stability under projected climate and wildfire regimes | Sierra Nevada, CA | Forested areas | 2010–2100 | 165–4230 | 34,000 | GFDL, CCSM3, CNRM | A2 | temperature, precipitation | LANDIS II Dynamic Fire and Fuels extension |
Loehman et al. 2018. Can Land Management Buffer Impacts of Climate Changes and Altered Fire Regimes on Ecosystems of the Southwestern United States? | Jemez Mountains, NM; Kaibab Plateau, AZ | Ponderosa pine; dry-mixed conifer | 2015–2115 | 1500–3500 (Jemez), 1439–2830 (Kaibab) | 1800 (Jemez), 3350 (Kaibab) | CCSM4 (warm-dry), HadGEM2ES (hot-arid) | RCP 4.5 and RCP 8.5 | temperature, precipitation | LANDIS II Dynamic Fire and Fuels extension, FireBGCv2 |
Loudermilk et al. 2017. Bending the carbon curve: fire management for carbon resilience under climate change | Lake Tahoe Basin, CA, NV | Jeffrey pine and dry-mixed-conifer | 2010–2110 | 1897–3320 | 850 | GFDL | A2 (high), B1 (moderate) | temperature, precipitation | LANDIS II Dynamic Fire and Fuels extension |
Lutz et al. 2009. Climate, lightning ignitions, and fire severity in Yosemite National Park, California, USA | Yosemite NP, CA | P. pine, dry mixed conifer | 2020–2049 | 657–3997 | 30.27 | HadCM3 | B1 | 1 April SWE | Linear regression |
O’Conner et al. 2020. Projected Climate-Fire Interactions Drive Forest to Shrubland Transition on an Arizona Sky Island | Sky islands. Huachuca mtns and Madrean Sky islands, AZ | Forests and woodlands | 2005–2055 | 1199–2855 | not specified — Huachuca Mountains | CanESM2, HadGEM2-CC, HadGEM2-ES | RCP 8.5 | maximum temperature, minimum temperature, average precipitation | FireBGCv2 |
O’Donnell et al. 2018. Forest restoration as a strategy to mitigate climate impacts on wildfire, vegetation, and water in semiarid forests | Kaibab Plateau, AZ | Forests and woodlands | 2010–2110 | 1439–2830 | 330 | 17 GCMs | RCP 4.5 and RCP 8.5 | temperature, wind speed, wind direction, relative humidity, precipitation | LANDIS II Dynamic Fire and Fuels extension |
Parks et al. 2016. How will climate change affect wildland fire severity in the western US? | Western US | Forested ecosystems | 2040–2069 | Conterminous | 500km2 hexels; 27 ecoregions | 20 GCMs | RCP 8.5 | Actual Evapotranspiration (AET), water deficit (WD), Annual precipitation (PPT), soil moisture (SMO), snow water equivalent (SWO) | Boosted regression trees |
Parks et al. 2018b. Analog-based fire regime and vegetation shifts in mountainous regions of the western US | Western US | Forested ecosystems in mountainous regions | Early (2011–2040,) mid (2041–2070), late (2071–2100) | Conterminous | 1km2; 17 ecoregions | 15 CMIP5 GCMs | RCP 8.5 | Climatic moisture deficit (CMD) and Evapotranspiration (ET); focus on water balance | LANDFIRE data. Next Gen Fire Severity Mapping |
Parks et al. 2019. Living on the edge: trailing edge forests at risk of fire-facilitated conversion to non-forest | Western US | Forested ecosytems | Mid-century 2040–2070 | Conterminous | 1 km pixel; 8 ecoregions | 15 CMIP5 GCMs | RCP 8.5 | Climatic moisture deficit (CMD) and Evapotranspiration (ET); focus on water balance | LANDFIRE data. Next Gen Fire Severity Mapping |
Serra-Diaz et al. 2018. Disequilibrium of fire-prone forests sets the stage for a rapid decline in conifer dominance during the 21st century | Klamath, OR and CA | Mixed conifer | 2015–2100 | 100–2000 | 29,400 | ACCESS 8.5 (much hotter-drier), CanESM2 (much hotter-wetter), CNRM-CM5 4.5 (hotter-wetter), MIROC5 2.6 (mild hot-wetter) | RCP 4.5 and RCP 8.5 | temperature, precipitation | LANDIS II Dynamic Fire and Fuels extension |