Award Abstract # 1655189
Collaborative Research: Causes and consequences of fire-regime variability in Rocky Mountain forests

NSF Org: DBI
Division of Biological Infrastructure
Recipient: UNIVERSITY OF WYOMING
Initial Amendment Date: July 5, 2017
Latest Amendment Date: July 5, 2017
Award Number: 1655189
Award Instrument: Standard Grant
Program Manager: Reed Beaman
DBI
 Division of Biological Infrastructure
BIO
 Directorate for Biological Sciences
Start Date: August 1, 2017
End Date: July 31, 2023 (Estimated)
Total Intended Award Amount: $177,009.00
Total Awarded Amount to Date: $177,009.00
Funds Obligated to Date: FY 2017 = $177,009.00
History of Investigator:
  • Bryan Shuman (Principal Investigator)
    bshuman@uwyo.edu
Recipient Sponsored Research Office: University of Wyoming
1000 E UNIVERSITY AVE
LARAMIE
WY  US  82071-2000
(307)766-5320
Sponsor Congressional District: 00
Primary Place of Performance: University of Wyoming
1000 E. University Ave
Laramie
WY  US  82071-2000
Primary Place of Performance
Congressional District:
00
Unique Entity Identifier (UEI): FDR5YF2K32X5
Parent UEI: FDR5YF2K32X5
NSF Program(s): ECOSYSTEM STUDIES
Primary Program Source: 01001718DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 9150
Program Element Code(s): 118100
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.074

ABSTRACT

Wildfires affect more than 180,000 km2 in the Unites States every year, on average, an area 20 times the size of Yellowstone National Park. In the Rocky Mountains, the amount of area burned in large wildfires has been increasing since the mid-1980s, a trend well linked to warming spring and summer temperatures, and expected to continue in upcoming decades. The way society plans for and reacts to wildfires, for example through federal policy and land management, is strongly shaped by our understanding of the causes, ecological consequences, and historical precedence of fire in different ecosystems. Important questions in this context include: how often have fires occurred in the past and how has this varied with climate and human activity, how have fires impacted valued resources including forests and water quality, and how long does it take for ecosystems to recover to pre-fire conditions? Studying how and why forests and wildfire activity have varied in the past, over periods of varying climate and human activity, provides a critical foundation for understanding the implications of wildfires. This long-term perspective also helps inform and improve models that simulate the impacts of future environmental change, including changes in wildfire activity. Mechanisms for broader impacts include documenting and communicating research results via a journalism graduate student embedded with the research team, advancing STEM education through the development of forest and fire ecology curricula for high school educators, and training graduate and undergraduate students in field-, lab-, and modeling-based research.

This research investigates the relationships and feedbacks among changes in climate, wildfire activity, and ecosystems over the past 2500 years through a unique combination of paleoecological reconstructions and ecosystem modeling. Using an unusually dense network of lake-sediment records in two study regions (i.e., 9-12 lakes within 1000 km2 in the N. and S. Rockies), the frequency, severity, and synchrony of past fire activity will be characterized and compared to paleoclimate records to assess the drivers of past fire activity. Paleofire records will be supplemented with high-resolution records of vegetation and biogeochemical change at a subset of focal sites, to assess the ecosystem impacts of past fire activity. Coupled climate-fire-ecosystem dynamics will be examined at watershed and sub-regional spatial scales through a set of ecosystem modeling simulations that compare paleo-informed to equilibrium scenarios.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Bartowitz, Kristina J. and Higuera, Philip E. and Shuman, Bryan N. and McLauchlan, Kendra K. and Hudiburg, Tara W. "Post-Fire Carbon Dynamics in Subalpine Forests of the Rocky Mountains" Fire , v.2 , 2019 https://doi.org/10.3390/fire2040058 Citation Details
Chileen, Barrie_V and McLauchlan, Kendra_K and Higuera, Philip_E and Parish, Meredith and Shuman, Bryan_N "Vegetation response to wildfire and climate forcing in a Rocky Mountain lodgepole pine forest over the past 2500 years" The Holocene , v.30 , 2020 https://doi.org/10.1177/0959683620941068 Citation Details
Clark-Wolf, Kyra and Higuera, Philip E. and Shuman, Bryan N. and McLauchlan, Kendra K. "Wildfire activity in northern Rocky Mountain subalpine forests still within millennial-scale range of variability" Environmental Research Letters , v.18 , 2023 https://doi.org/10.1088/1748-9326/acee16 Citation Details
ClarkWolf, Kyra D. and Higuera, Philip E. and McLauchlan, Kendra K. and Shuman, Bryan N. and Parish, Meredith C. "Fireregime variability and ecosystem resilience over four millennia in a Rocky Mountain subalpine watershed" Journal of Ecology , v.111 , 2023 https://doi.org/10.1111/1365-2745.14201 Citation Details
Higuera, P. E. and Crausbay, S. and Shuman, B. N. and Wolf, K. D. "Challenges to forest restoration in an era of unprecedented climate and wildfire activity in Rocky Mountain subalpine forests." Past global changes magazine , 2022 Citation Details
Higuera, Philip E. and Shuman, Bryan N. and Wolf, Kyra D. "Rocky Mountain subalpine forests now burning more than any time in recent millennia" Proceedings of the National Academy of Sciences , v.118 , 2021 https://doi.org/10.1073/pnas.2103135118 Citation Details
Parish, Meredith C. and Calder, W. John and Shuman, Bryan N. "Millennial-scale increase in winter precipitation in the southern Rocky Mountains during the Common Era" Quaternary Research , v.94 , 2020 https://doi.org/10.1017/qua.2019.85 Citation Details
Parish, Meredith C. and Wolf, Kyra D. and Higuera, Philip E. and Shuman, Bryan N. "Holocene water levels of Silver Lake, Montana, and the hydroclimate history of the Inland Northwest" Quaternary Research , 2022 https://doi.org/10.1017/qua.2022.17 Citation Details
Pompeani, David P. and McLauchlan, Kendra K. and Chileen, Barrie V. and Calder, W. John and Shuman, Bryan N. and Higuera, Philip E. "The biogeochemical consequences of late Holocene wildfires in three subalpine lakes from northern Colorado" Quaternary Science Reviews , v.236 , 2020 https://doi.org/10.1016/j.quascirev.2020.106293 Citation Details

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

The Big Burns project was a multi-institution collaboration studying how climate, wildfire, and ecosystems in high-elevation forests in the Rocky Mountains changed over the past 2500 years. The project focused on understanding the causes and ecological impacts of historical variability in fire activity, explicitly comparing the past to the present. The collaboration among the University of Montana, University of Idaho, University of Wyoming, and Kansas State University was funded through a four-year grant from the NSF’s Ecosystem Studies program, which was extended to span six years with no-cost extensions. 

During the project's six-year duration (2017-2023), the societal impacts of wildfires gained heightened relevance, sparking urgent discussions from local to global scales. The Big Burns project made significant scientific contributions directly influencing these conversations. By combining paleoecological reconstructions and ecosystem modeling, the project provided context for current changes in wildfire activity, comparing them to historical variability. This approach revealed essential mechanisms and impacts of change, offering valuable insights for anticipating the future.

The Big Burns project focused on two Rocky Mountain landscapes with a history of extensive wildfires. In the Northern Rockies (Idaho and Montana), major wildfires in 1910 influenced national wildfire policy, and recent decades have seen increased burning. The Southern Rockies (Colorado and Wyoming) have also experienced significant wildfire activity, including extensive burning around 1000 years ago during the Medieval Climate Anomaly, and the extraordinary 2020 fire season.

 

Major findings from the Big Burns project revealed that high-elevation forests in the southern Rocky Mountains are now burning at rates surpassing those of the past 2000 years, driven by unprecedented climate conditions and accidental human ignitions. These findings gained widespread media attention and were featured in NSF's 2021 Year in Discovery summary. The study built upon almost a decade of prior work, funded by other NSF projects, providing extensive spatial coverage and detail to contextualize contemporary wildfires. 

Newly developed records of climate, wildfire, and ecosystem change in the northern Rocky Mountains underscore the sensitivity of fire activity and ecosystems to climate change over the past 4000+ years. Remarkably, these ecosystems have consistently demonstrated resilience, rebounding from repeated wildfires during this time. While high-elevation forests throughout the Rocky Mountains have historically evolved under the influence of fire, the current heightened fire activity is attributed to global warming and human activities, posing increased risks to human lives and property.

In contrast to the Southern Rockies, contemporary wildfire activity in Northern Rockies' high-elevation forests has not surpassed levels experienced over past millennia. The Big Burns project shed light on the potential impact of future burning, revealing the threshold beyond which these forests may be pushed, surpassing experiences in recent millennia.

The project achieved success on multiple fronts, including the training of one postdoc, two PhD students, two MS students, all earning degrees and publishing in the scientific literature. Notable outcomes include career progressions, with one MS student advancing to a PhD program, another securing employment with the USGS, and both PhDs pursuing postdoctoral research. PhD students each earned additional fellowships, which supplemented and expanded the scope of their graduate work. For example, PhD student Clark-Wolf expanded her work to study post-fire tree regeneration after recent wildfires, integrating contemporary and paleo ecology perspectives into her dissertation and publication record. PhD student Bartowitz earned an NSF INTERN award to work on forest carbon cycling with The Nature Conservancy. 

The project resulted in 25 publications in scientific journals. Graduate students and the postdoc played significant roles, serving as lead authors on 11 and co-authors on seven papers directly tied to the project. These 18 papers have amassed over 230 citations in scientific literature as of August 2023. Additionally, seven papers contributing invited perspectives from paleoecology to contemporary ecology garnered over 1200 citations by the same date. Project findings were disseminated to scientific audiences through presentations at numerous national and international conferences, as well as invited seminars.

Our team also shared project findings widely, reaching the public, managers, and policymakers through articles in The Washington Post, Global Change Biology, and The Conversation. We also contributed to podcasts like NSF's Discovery Files and gave public presentations to make our research more accessible beyond academia.

Finally, discoveries from the Big Burns project have been integrated into undergraduate curriculum in ecology and climate change at the University of Montana, University of Idaho, and University of Wyoming. The project supported over a dozen undergraduate students in lab and field work, and it partially supported one graduate student in environmental journalism, who embedded with the project for one field season. Several undergraduate students involved in the project have gone on to pursue graduate degrees in biological or physical sciences. 


 

 


Last Modified: 09/26/2024
Modified by: Bryan N Shuman

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