Linking drought legacy effects across scales: From leaves to tree rings to ecosystems
Abstract
Abstract Severe drought can cause lagged effects on tree physiology that negatively impact forest functioning for years. These “drought legacy effects” have been widely documented in tree‐ring records and could have important implications for our understanding of broader scale forest carbon cycling. However, legacy effects in tree‐ring increments may be decoupled from ecosystem fluxes due to (a) postdrought alterations in carbon allocation patterns; (b) temporal asynchrony between radial growth and carbon uptake; and (c) dendrochronological sampling biases. In order to link legacy effects from tree rings to whole forests, we leveraged a rich dataset from a Midwestern US forest that was severely impacted by a drought in 2012. At this site, we compiled tree‐ring records, leaf‐level gas exchange, eddy flux measurements, dendrometer band data, and satellite remote sensing estimates of greenness and leaf area before, during, and after the 2012 drought. After accounting for the relative abundance of tree species in the stand, we estimate that legacy effects led to ~10% reductions in tree‐ring width increments in the year following the severe drought. Despite this stand‐scale reduction in radial growth, we found that leaf‐level photosynthesis, gross primary productivity (GPP), and vegetation greenness were not suppressed in the year following themore »
- Authors:
-
[1];
[2];
[3];
[5];
[2];
[1]
- Univ. of Utah, Salt Lake City, UT (United States)
- Indiana Univ., Bloomington, IN (United States)
- Midwest Dendro, LLC, Naperville, IL (United States)
- Indiana Univ., Bloomington, IN (United States); Harvard Univ., Petersham, MA (United States). Harvard Forest
- Univ. of Arizona, Tucson, AZ (United States)
- Publication Date:
- Research Org.:
- Princeton Univ., NJ (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC), Biological and Environmental Research (BER); National Inst. of Food and Agriculture; National Science Foundation (NSF)
- OSTI Identifier:
- 1612378
- Alternate Identifier(s):
- OSTI ID: 1560215
- Grant/Contract Number:
- SC0016011; 1714972; 2017-67013-26191; 2018-67019-27850; 1802880
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Global Change Biology
- Additional Journal Information:
- Journal Volume: 25; Journal Issue: 9; Journal ID: ISSN 1354-1013
- Publisher:
- Wiley
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; Biodiversity & conservation; environmental sciences & ecology; carbon allocation; dendroecology; drought recovery; eddy covariance; remote sensing
Citation Formats
Kannenberg, Steven A., Novick, Kimberly A., Alexander, M. Ross, Maxwell, Justin T., Moore, David J. P., Phillips, Richard P., and Anderegg, William R. L. Linking drought legacy effects across scales: From leaves to tree rings to ecosystems. United States: N. p., 2019.
Web. doi:10.1111/gcb.14710.
Kannenberg, Steven A., Novick, Kimberly A., Alexander, M. Ross, Maxwell, Justin T., Moore, David J. P., Phillips, Richard P., & Anderegg, William R. L. Linking drought legacy effects across scales: From leaves to tree rings to ecosystems. United States. https://doi.org/10.1111/gcb.14710
Kannenberg, Steven A., Novick, Kimberly A., Alexander, M. Ross, Maxwell, Justin T., Moore, David J. P., Phillips, Richard P., and Anderegg, William R. L. Mon .
"Linking drought legacy effects across scales: From leaves to tree rings to ecosystems". United States. https://doi.org/10.1111/gcb.14710. https://www.osti.gov/servlets/purl/1612378.
@article{osti_1612378,
title = {Linking drought legacy effects across scales: From leaves to tree rings to ecosystems},
author = {Kannenberg, Steven A. and Novick, Kimberly A. and Alexander, M. Ross and Maxwell, Justin T. and Moore, David J. P. and Phillips, Richard P. and Anderegg, William R. L.},
abstractNote = {Abstract Severe drought can cause lagged effects on tree physiology that negatively impact forest functioning for years. These “drought legacy effects” have been widely documented in tree‐ring records and could have important implications for our understanding of broader scale forest carbon cycling. However, legacy effects in tree‐ring increments may be decoupled from ecosystem fluxes due to (a) postdrought alterations in carbon allocation patterns; (b) temporal asynchrony between radial growth and carbon uptake; and (c) dendrochronological sampling biases. In order to link legacy effects from tree rings to whole forests, we leveraged a rich dataset from a Midwestern US forest that was severely impacted by a drought in 2012. At this site, we compiled tree‐ring records, leaf‐level gas exchange, eddy flux measurements, dendrometer band data, and satellite remote sensing estimates of greenness and leaf area before, during, and after the 2012 drought. After accounting for the relative abundance of tree species in the stand, we estimate that legacy effects led to ~10% reductions in tree‐ring width increments in the year following the severe drought. Despite this stand‐scale reduction in radial growth, we found that leaf‐level photosynthesis, gross primary productivity (GPP), and vegetation greenness were not suppressed in the year following the 2012 drought. Neither temporal asynchrony between radial growth and carbon uptake nor sampling biases could explain our observations of legacy effects in tree rings but not in GPP. Instead, elevated leaf‐level photosynthesis co‐occurred with reduced leaf area in early 2013, indicating that resources may have been allocated away from radial growth in conjunction with postdrought upregulation of photosynthesis and repair of canopy damage. Collectively, our results indicate that tree‐ring legacy effects were not observed in other canopy processes, and that postdrought canopy allocation could be an important mechanism that decouples tree‐ring signals from GPP.},
doi = {10.1111/gcb.14710},
journal = {Global Change Biology},
number = 9,
volume = 25,
place = {United States},
year = {Mon May 27 00:00:00 EDT 2019},
month = {Mon May 27 00:00:00 EDT 2019}
}
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