FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2582977415> ?p ?o ?g. }

• W2582977415 endingPage "3757" @default.
• W2582977415 startingPage "3742" @default.
• W2582977415 abstract "Ongoing climate change poses significant threats to plant function and distribution. Increased temperatures and altered precipitation regimes amplify drought frequency and intensity, elevating plant stress and mortality. Large-scale forest mortality events will have far-reaching impacts on carbon and hydrological cycling, biodiversity, and ecosystem services. However, biogeographical theory and global vegetation models poorly represent recent forest die-off patterns. Furthermore, as trees are sessile and long-lived, their responses to climate extremes are substantially dependent on historical factors. We show that periods of favourable climatic and management conditions that facilitate abundant tree growth can lead to structural overshoot of aboveground tree biomass due to a subsequent temporal mismatch between water demand and availability. When environmental favourability declines, increases in water and temperature stress that are protracted, rapid, or both, drive a gradient of tree structural responses that can modify forest self-thinning relationships. Responses ranging from premature leaf senescence and partial canopy dieback to whole-tree mortality reduce canopy leaf area during the stress period and for a lagged recovery window thereafter. Such temporal mismatches of water requirements from availability can occur at local to regional scales throughout a species geographical range. As climate change projections predict large future fluctuations in both wet and dry conditions, we expect forests to become increasingly structurally mismatched to water availability and thus overbuilt during more stressful episodes. By accounting for the historical context of biomass development, our approach can explain previously problematic aspects of large-scale forest mortality, such as why it can occur throughout the range of a species and yet still be locally highly variable, and why some events seem readily attributable to an ongoing drought while others do not. This refined understanding can facilitate better projections of structural overshoot responses, enabling improved prediction of changes in forest distribution and function from regional to global scales." @default.
• W2582977415 created "2017-02-03" @default.
• W2582977415 creator A5031803026 @default.
• W2582977415 creator A5038386497 @default.
• W2582977415 creator A5053563490 @default.
• W2582977415 creator A5057169216 @default.
• W2582977415 creator A5064086810 @default.
• W2582977415 creator A5070185002 @default.
• W2582977415 creator A5070307451 @default.
• W2582977415 creator A5083816257 @default.
• W2582977415 date "2017-03-03" @default.
• W2582977415 modified "2023-10-06" @default.
• W2582977415 title "Structural overshoot of tree growth with climate variability and the global spectrum of drought‐induced forest dieback" @default.
• W2582977415 cites W1483518999 @default.
• W2582977415 cites W1488616880 @default.
• W2582977415 cites W1491310250 @default.
• W2582977415 cites W1494272296 @default.
• W2582977415 cites W1502566860 @default.
• W2582977415 cites W1516902267 @default.
• W2582977415 cites W1550857001 @default.
• W2582977415 cites W1575234955 @default.
• W2582977415 cites W1759372127 @default.
• W2582977415 cites W1800247335 @default.
• W2582977415 cites W1834239181 @default.
• W2582977415 cites W1867465844 @default.
• W2582977415 cites W1900769509 @default.
• W2582977415 cites W1902001896 @default.
• W2582977415 cites W1902238321 @default.
• W2582977415 cites W1925309871 @default.
• W2582977415 cites W1951564719 @default.
• W2582977415 cites W1968502959 @default.
• W2582977415 cites W1981213426 @default.
• W2582977415 cites W1983188825 @default.
• W2582977415 cites W1984941255 @default.
• W2582977415 cites W1986994835 @default.
• W2582977415 cites W1993071761 @default.
• W2582977415 cites W1994369651 @default.
• W2582977415 cites W1994499934 @default.
• W2582977415 cites W1997118727 @default.
• W2582977415 cites W1997242076 @default.
• W2582977415 cites W1998251298 @default.
• W2582977415 cites W1998638849 @default.
• W2582977415 cites W1998918998 @default.
• W2582977415 cites W2005867148 @default.
• W2582977415 cites W2010443544 @default.
• W2582977415 cites W2010784770 @default.
• W2582977415 cites W2014088742 @default.
• W2582977415 cites W2017583521 @default.
• W2582977415 cites W2019170188 @default.
• W2582977415 cites W2024649846 @default.
• W2582977415 cites W2028971361 @default.
• W2582977415 cites W2029075357 @default.
• W2582977415 cites W2031925862 @default.
• W2582977415 cites W2033013208 @default.
• W2582977415 cites W2034385655 @default.
• W2582977415 cites W2034424367 @default.
• W2582977415 cites W2035008438 @default.
• W2582977415 cites W2042909031 @default.
• W2582977415 cites W2044201741 @default.
• W2582977415 cites W2045081268 @default.
• W2582977415 cites W2049642839 @default.
• W2582977415 cites W2052486546 @default.
• W2582977415 cites W205279106 @default.
• W2582977415 cites W2053894538 @default.
• W2582977415 cites W2056640260 @default.
• W2582977415 cites W2058466775 @default.
• W2582977415 cites W2060960912 @default.
• W2582977415 cites W2061411772 @default.
• W2582977415 cites W2063681704 @default.
• W2582977415 cites W2071454092 @default.
• W2582977415 cites W2072264207 @default.
• W2582977415 cites W2078169978 @default.
• W2582977415 cites W2079742492 @default.
• W2582977415 cites W2080870934 @default.
• W2582977415 cites W2081184087 @default.
• W2582977415 cites W2086154193 @default.
• W2582977415 cites W2086522048 @default.
• W2582977415 cites W2093127583 @default.
• W2582977415 cites W2093498564 @default.
• W2582977415 cites W2095018643 @default.
• W2582977415 cites W2095051989 @default.
• W2582977415 cites W2096061806 @default.
• W2582977415 cites W2096870124 @default.
• W2582977415 cites W2097647145 @default.
• W2582977415 cites W2098469025 @default.
• W2582977415 cites W2099501065 @default.
• W2582977415 cites W2103818866 @default.
• W2582977415 cites W2105122814 @default.
• W2582977415 cites W2105287424 @default.
• W2582977415 cites W2105511799 @default.
• W2582977415 cites W2106080357 @default.
• W2582977415 cites W2106632946 @default.
• W2582977415 cites W2106966676 @default.
• W2582977415 cites W2107101214 @default.
• W2582977415 cites W2108008160 @default.
• W2582977415 cites W2109737638 @default.
• W2582977415 cites W2110239639 @default.
• W2582977415 cites W2113290704 @default.

• next