Award Abstract # 2411570
Collaborative Research: Resolving Uncertainty in Past Delta-14C Spikes from Tree Rings

NSF Org: AGS
Division of Atmospheric and Geospace Sciences
Recipient: MONTANA STATE UNIVERSITY
Initial Amendment Date: August 27, 2024
Latest Amendment Date: August 27, 2024
Award Number: 2411570
Award Instrument: Standard Grant
Program Manager: Tai-Yin Huang
thuang@nsf.gov
 (703)292-4943
AGS
 Division of Atmospheric and Geospace Sciences
GEO
 Directorate for Geosciences
Start Date: October 1, 2024
End Date: September 30, 2027 (Estimated)
Total Intended Award Amount: $185,538.00
Total Awarded Amount to Date: $185,538.00
Funds Obligated to Date: FY 2024 = $185,538.00
History of Investigator:
  • Rachael Filwett (Principal Investigator)
    rachael.filwett@montana.edu
Recipient Sponsored Research Office: Montana State University
216 MONTANA HALL
BOZEMAN
MT  US  59717
(406)994-2381
Sponsor Congressional District: 01
Primary Place of Performance: Montana State University
216 MONTANA HALL
BOZEMAN
MT  US  59717
Primary Place of Performance
Congressional District:
01
Unique Entity Identifier (UEI): EJ3UF7TK8RT5
Parent UEI:
NSF Program(s): SOLAR-TERRESTRIAL,
AGS-ATM & Geospace Sciences
Primary Program Source: 01002425DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 1523, 4444, 6897, 9150
Program Element Code(s): 152300, 689700
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

This collaborative project will use field- and model-based experiments to evaluate how different species of tree from different locations on earth take up and store carbon. Cosmic radiation, including particles from the sun, poses a serious threat to satellites, space stations, and human space exploration. Direct observations of extreme cosmic particle events are limited to the last several decades but environmental archives like tree rings and ice cores suggest that rare events can be ~50 times more severe than those documented by the instrumental record. Tree rings are globally common and record past events through isotopic tracers, yet the precision of these records may be affected by both latitude and the way different species take up and store carbon from the atmosphere. Results of this study will create an upper limit on extreme solar events critical for safeguarding space-based infrastructure from harmful cosmic events. This award support early-career researchers, graduate and undergraduate students, and women PIs from ESPSCoR states.

Understanding past variability in Solar energetic particle events (SEPs) is critical for space-weather forecasting and safeguarding modern infrastructure. A well-replicated history of spikes in 14C from tree rings would provide an upper limit on severe space-based hazards yielding improvements in forecasting and risk assessment. However, inferences about the timing and magnitude of past 14C production is hampered by uncertainties associated with the role of non-structural carbohydrates (NSC) in the age of carbon allocated to wood. This project uses three of the best-replicated 14C spikes (663 BCE, 774 CE, and 993 CE) as global pulse-labeling experiments to quantify physiological sources of uncertainty on ?14C measurements from tree rings with the goal of improving estimates of the nature of past 14C production spikes. Using living trees at three sites, the team will determine the age of carbon allocated to wood across three tree life strategies: evergreen conifers, deciduous conifers and deciduous angiosperms. The team will then pair these modern field measurements with new time series of past extreme 14C production events from the same sites and the global dataset of annual tree ring ?14C measurements, to determine impacts of tree physiology and geomagnetic latitude on estimates of timing, duration, magnitude, and solar phase using a Bayesian framework for modeling 14C production from tree rings. Resolving sources of uncertainty in ?14C in tree rings will yield better estimates of the magnitude past SEPs and create an upper limit on extreme solar events critical for safeguarding space-based infrastructure from harmful cosmic events.

The Solar-Terrestrial Research Program, Paleoclimate Program, and GEO directorate co-fund this project.

This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

Please report errors in award information by writing to: awardsearch@nsf.gov.

Print this page

Back to Top of page