Conifer radial growth response to recent seasonal warming and drought from the southwestern USA

Charles Truettner, William R.L. Anderegg, Franco Biondi, George W Koch, Kiona Ogle, Christopher R Schwalm, Marcy E. Litvak, John D. Shaw, Emanuele Ziaco

Research output: Contribution to journalArticle

4 Citations (Scopus)

Abstract

Future droughts are expected to become more severe and frequent under future climate change scenarios, likely causing widespread tree mortality in the western USA. Coping with an uncertain future requires an understanding of long-term ecosystem responses in areas where prolonged drought is projected to increase. Tree-ring records are ideally suited for this task. We developed 24 tree-ring chronologies from 20 U.S. Forest Service Forest Inventory and Analysis (FIA) plots in the southwestern USA. Climate variables were derived from the PRISM climate dataset (800-m grid cells) to capture the bimodal precipitation regime of winter snow and summer monsoonal rainfall, as well as warm-season vapor-pressure deficit (VPD) and winter minimum temperature. Based on mixed linear models, radial growth from 1948 to 2013 for four conifer species (Pinus edulis, Juniperus osteosperma, Pinus ponderosa, and Picea engelmannii) responded negatively to warm-season VPD and positively to cold-season precipitation. Pinus spp. benefited from warm-season precipitation linked to the North American monsoon, and Pinus spp. and J. osteosperma radial growth increased with warmer cold-season minimum temperature. However, warmer cold-season minimum temperatures countered the beneficial influence of cold-season precipitation for radial growth in Pinus spp. and J. osteosperma, while P. engelmannii was unaffected. Also, enhanced drying effects of warm-season VPD associated with decreased cold-season precipitation negatively affected radial growth of Pinus spp. and P. engelmannii. Of the four conifer species studied, Pinus spp. are most affected by droughts since 1948, while P. engelmannii and J. osteosperma appear to be more resilient. Investigating seasonal climate responses and interaction effects on radial growth in areas impacted by severe drought helps identify species that may be particularly at risk from climate change impacts in the Anthropocene.

Original languageEnglish (US)
JournalForest Ecology and Management
DOIs
StateAccepted/In press - Jan 1 2018

Fingerprint

warm season
Juniperus osteosperma
growth response
cold season
conifers
coniferous tree
Picea engelmannii
warming
drought
Pinus
vapor pressure
growth rings
climate
Pinus edulis
climate change
tree ring
temperature
USDA Forest Service
winter
tree mortality

Keywords

  • Climate change
  • Climate interactions
  • Conifers
  • Dendroclimatology
  • Forest drought severity index
  • Southwest USA

ASJC Scopus subject areas

  • Forestry
  • Nature and Landscape Conservation
  • Management, Monitoring, Policy and Law

Cite this

Conifer radial growth response to recent seasonal warming and drought from the southwestern USA. / Truettner, Charles; Anderegg, William R.L.; Biondi, Franco; Koch, George W; Ogle, Kiona; Schwalm, Christopher R; Litvak, Marcy E.; Shaw, John D.; Ziaco, Emanuele.

In: Forest Ecology and Management, 01.01.2018.

Research output: Contribution to journalArticle

Truettner, Charles ; Anderegg, William R.L. ; Biondi, Franco ; Koch, George W ; Ogle, Kiona ; Schwalm, Christopher R ; Litvak, Marcy E. ; Shaw, John D. ; Ziaco, Emanuele. / Conifer radial growth response to recent seasonal warming and drought from the southwestern USA. In: Forest Ecology and Management. 2018.
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AU - Shaw, John D.

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AB - Future droughts are expected to become more severe and frequent under future climate change scenarios, likely causing widespread tree mortality in the western USA. Coping with an uncertain future requires an understanding of long-term ecosystem responses in areas where prolonged drought is projected to increase. Tree-ring records are ideally suited for this task. We developed 24 tree-ring chronologies from 20 U.S. Forest Service Forest Inventory and Analysis (FIA) plots in the southwestern USA. Climate variables were derived from the PRISM climate dataset (800-m grid cells) to capture the bimodal precipitation regime of winter snow and summer monsoonal rainfall, as well as warm-season vapor-pressure deficit (VPD) and winter minimum temperature. Based on mixed linear models, radial growth from 1948 to 2013 for four conifer species (Pinus edulis, Juniperus osteosperma, Pinus ponderosa, and Picea engelmannii) responded negatively to warm-season VPD and positively to cold-season precipitation. Pinus spp. benefited from warm-season precipitation linked to the North American monsoon, and Pinus spp. and J. osteosperma radial growth increased with warmer cold-season minimum temperature. However, warmer cold-season minimum temperatures countered the beneficial influence of cold-season precipitation for radial growth in Pinus spp. and J. osteosperma, while P. engelmannii was unaffected. Also, enhanced drying effects of warm-season VPD associated with decreased cold-season precipitation negatively affected radial growth of Pinus spp. and P. engelmannii. Of the four conifer species studied, Pinus spp. are most affected by droughts since 1948, while P. engelmannii and J. osteosperma appear to be more resilient. Investigating seasonal climate responses and interaction effects on radial growth in areas impacted by severe drought helps identify species that may be particularly at risk from climate change impacts in the Anthropocene.

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KW - Forest drought severity index

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