Potential decline in carbon carrying capacity under projected climate-wildfire interactions in the Sierra Nevada

Ecosystem carbon carrying capacity (CCC) is determined by prevailing climate and natural disturbance regimes, conditions that are projected to change significantly. The interaction of changing climate and its effects on disturbance regimes is expected to affect forest regeneration and growth, which...

Celý popis

Uloženo v:
Podrobná bibliografie
Vydáno v:Scientific reports Ročník 7; číslo 1; s. 2420 - 7
Hlavní autoři: Liang, Shuang, Hurteau, Matthew D., Westerling, Anthony LeRoy
Médium: Journal Article
Jazyk:angličtina
Vydáno: London Nature Publishing Group UK 25.05.2017
Nature Publishing Group
Nature Portfolio
Témata:
21st century
631/158/2165
631/158/2454
631/158/2465
Carbon
Carrying capacity
Climate change
Climate effects
Disturbances
Ecosystems
Forests
Growing season
Humanities and Social Sciences
Mountains
multidisciplinary
Natural disturbance
Science
Science (multidisciplinary)
Vegetation type
Wildfires
United States > US
Sierra Nevada Mountain Range
ISSN:2045-2322, 2045-2322
On-line přístup:Získat plný text
Tagy: Přidat tag
Žádné tagy, Buďte první, kdo vytvoří štítek k tomuto záznamu!
Popis
Shrnutí:Ecosystem carbon carrying capacity (CCC) is determined by prevailing climate and natural disturbance regimes, conditions that are projected to change significantly. The interaction of changing climate and its effects on disturbance regimes is expected to affect forest regeneration and growth, which may diminish forest carbon (C) stocks and uptake. We modeled landscape C dynamics over 590 years along the latitudinal gradient of the U.S. Sierra Nevada Mountains under climate and area burned by large wildfires projected by late 21 st century. We assumed climate and wildfire stabilize at late-21 st century conditions (2090–2100) to facilitate analysis of lags between warming and changing CCC. We show that compared with historical (1980–2010) climate and wildfire conditions, projected scenarios would drive a significant decrease of up to 73% in mean total ecosystem carbon (TEC) by the end of the 590-year simulation. Tree regeneration failure due to intensified growing season dryness and increased area burned would substantially decrease forested area, transitioning the system from C sink to source. Our results demonstrate the potential for a lower CCC in the system due to extensive vegetation type conversion from forest to non-forest types, and suggest a decline in the contribution of Sierra Nevada forests to U.S. C sink.
Bibliografie:ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 14
content type line 23
ISSN:2045-2322
2045-2322
DOI:10.1038/s41598-017-02686-0