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Effects of thinning on drought vulnerability and climate response in north temperate forest ecosystems

TLDR
Results suggest that thinning generally enhanced drought resistance and resilience; however, this relationship showed a pronounced reversal over time in stands maintained at lower tree densities, and the importance of accounting for stand structure when predicting climate-change impacts to forests is highlighted.
Abstract
Reducing tree densities through silvicultural thinning has been widely advocated as a strategy for enhancing resistance and resilience to drought, yet few empirical evaluations of this approach exist. We examined detailed dendrochronological data from a long-term (>50 years) replicated thinning experiment to determine if density reductions conferred greater resistance and/or resilience to droughts, assessed by the magnitude of stand-level growth reductions. Our results suggest that thinning generally enhanced drought resistance and resilience; however, this relationship showed a pronounced reversal over time in stands maintained at lower tree densities. Specifically, lower-density stands exhibited greater resistance and resilience at younger ages (49 years), yet exhibited lower resistance and resilience at older ages (76 years), relative to higher-density stands. We attribute this reversal to significantly greater tree sizes attained within the lower-density stands through stand development, which in turn increased tree-level water demand during the later droughts. Results from response–function analyses indicate that thinning altered growth–climate relationships, such that higher-density stands were more sensitive to growing-season precipitation relative to lower-density stands. These results confirm the potential of density management to moderate drought impacts on growth, and they highlight the importance of accounting for stand structure when predicting climate-change impacts to forests.

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On underestimation of global vulnerability to tree mortality and forest die‐off from hotter drought in the Anthropocene

TL;DR: In this article, the authors identify ten contrasting perspectives that shape the vulnerability debate but have not been discussed collectively and present a set of global vulnerability drivers that are known with high confidence: (1) droughts eventually occur everywhere; (2) warming produces hotter Droughts; (3) atmospheric moisture demand increases nonlinearly with temperature during drought; (4) mortality can occur faster in hotter Drought, consistent with fundamental physiology; (5) shorter Drought can become lethal under warming, increasing the frequency of lethal Drought; and (6) mortality happens rapidly
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Contemporary forest restoration: A review emphasizing function

TL;DR: The science underpinning contemporary approaches to forest restoration practice is synthesized and some major approaches for altering structure in degraded forest stands are presented, and approaches for restoration of two key ecosystem processes, fire and flooding are described.
Journal ArticleDOI

Potential of forest thinning to mitigate drought stress: A meta-analysis

TL;DR: In this paper, a meta-analysis was conducted to assess the potential of thinning for improving tree performance during and after a severe drought in conifers and broadleaves.
Journal ArticleDOI

Structural overshoot of tree growth with climate variability and the global spectrum of drought-induced forest dieback

TL;DR: It is shown 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, which expects forests to become increasingly structurally mismatched to water availability and thus overbuilt during more stressful episodes.
References
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Journal ArticleDOI

Little change in global drought over the past 60 years

TL;DR: It is shown that the previously reported increase in global drought is overestimated because the PDSI uses a simplified model of potential evaporation that responds only to changes in temperature and thus responds incorrectly to global warming in recent decades.
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Estimating Potential Evapotranspiration

TL;DR: In this article, four methods for estimating potential evapotranspiration are compared and evaluated: the Class A evaporation pan located in an irrigated pasture area, the Hargreaves equation, the Jensen-Haise eguation, and the Blaney-Criddle method.
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Estimating Potential Evapotranspiration

TL;DR: Thesis (B.S.) as mentioned in this paper, Massachusetts Institute of Technology, Dept. of Civil and Sanitary Engineering, 1960, Boston, Massachusetts, United States, USA, USA..
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DENDROCLIM2002: A C++ program for statistical calibration of climate signals in tree-ring chronologies ☆

TL;DR: DENDROCLIM2002 is an extension of existing task-specific software, which is mostly MS-DOS based, and of available user-supplied code for statistical packages, such as SAS, that incorporates the ability to test for temporal changes of dendroclimatic relationships by means of evolutionary and moving intervals.
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