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Seasons and Life Cycles
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A conceptual framework. This table is a guide to determining how individual species are responding to an extended growing
season by observing the duration of peak season. The life history of a species—from the onset of greening through the end of
senescence—is illustrated by the length of the solid lines. Each case represents a shift in the timing (columns) and duration
(rows) of one or more species in a hypothetical three-species community that includes an early-, mid-, and late-season species.
The growing season begins when the first species greens and ends when the last species senesces. The peak season (gray shaded
area) occurs when all species have started and none have completed their life history. Reproductive life history events likely
begin before the peak season and are completed before its end. The final row and column list changes that can be observed
through frequent observations of surface greenness.
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SECAS April 2024 Newsletter
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Logo sneak peek, Summit and Caribbean CoP reflections, Southeast CASC collaboration
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Southeast Conservation Adaptation Strategy (SECAS) Newsletter
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SECAS Newsletter October 2023
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SECAS October newsletter: 2023 Southeast Blueprint and SECAS goal report released, introducing the Midwest Blueprint
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Southeast Conservation Adaptation Strategy (SECAS) Newsletter
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SECAS Third Thursday Web Forum May 16th 10:00 am ET
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Web Forum on Thursday: Understanding coastal wetland change from multiple perspectives.
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Events
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SECAS Third Thursday Web Forum January 18th 10:00 am ET
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Join us on Thursday for a special webinar co-hosted with the Southeast Climate Adaptation Science Center! This web forum features multiple staff of the Atlanta Botanical Garden and the Southeast Plant Conservation Alliance.
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SECASC Applications open for Dec 7-14 Winter Institute on Invasive Vines
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Applications are now open for the upcoming "Integrative Approaches to Investigate Invasive Species and Landscapes Winter Institute: Vines." This all-expenses paid graduate student program is being led by faculty at the University of Puerto Rico at Río Piedras from December 7-14, 2024.
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Sectoral contributions to surface water stress in the coterminous United States
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Here, we assess current stress in the freshwater system based on the best available data in order to understand possible risks and vulnerabilities to regional water resources and the sectors dependent on freshwater. We present watershed-scale measures of surface water supply stress for the coterminous United States (US) using the water supply stress index (WaSSI) model which considers regional trends in both water supply and demand. A snapshot of contemporary annual water demand is compared against different water supply regimes, including current average supplies, current extreme-year supplies, and projected future average surface water flows under a changing climate. In addition, we investigate the contributions of different water demand sectors to current water stress. On average, water supplies are stressed, meaning that demands for water outstrip natural supplies in over 9% of the 2103 watersheds examined. These watersheds rely on reservoir storage, conveyance systems, and groundwater to meet current water demands. Overall, agriculture is the major demand-side driver of water stress in the US, whereas municipal stress is isolated to southern California. Water stress introduced by cooling water demands for power plants is punctuated across the US, indicating that a single power plant has the potential to stress water supplies at the watershed scale. On the supply side, watersheds in the western US are particularly sensitive to low flow events and projected long-term shifts in flow driven by climate change. The WaSSI results imply that not only are water resources in the southwest in particular at risk, but that there are also potential vulnerabilities to specific sectors, even in the ‘water-rich’ southeast.
Keywords: water resources, surface water, water stress
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SECURITY_ CC.pdf
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Sediment Trapping by Dams Creates Methane Emission Hot Spots
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Inland waters transport and transform sub- stantial amounts of carbon and account for ∼18% of global methane emissions. Large reservoirs with higher areal methane release rates than natural waters contribute significantly to freshwater emissions. However, there are millions of small dams worldwide that receive and trap high loads of organic carbon and can therefore potentially emit significant amounts of methane to the atmosphere. We evaluated the effect of damming on methane emissions in a central European impounded river. Direct comparison of riverine and reservoir reaches, where sedimentation in the latter is increased due to trapping by dams, revealed that the reservoir reaches are the major source of methane emissions (∼0.23 mmol CH4 m−2 d−1 vs ∼19.7 mmol CH4 m−2 d−1, respectively) and that areal emission rates far exceed previous estimates for temperate reservoirs or rivers. We show that sediment accumulation correlates with methane production and subsequent ebullitive release rates and may therefore be an excellent proxy for estimating methane emissions from small reservoirs. Our results suggest that sedimentation- driven methane emissions from dammed river hot spot sites can potentially increase global freshwater emissions by up to 7%.
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Seeds of Change for Restoration Ecology
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FORESTS PROVIDE A WIDE VARIETY OF ECOSYSTEM SERVICES, INCLUDING PROVISIONS SUCH AS
food and fuel and services that affect climate and water quality (1). In light of the increasing
global population pressure, we must not only conserve, but also restore forests to meet the
increasing demands for ecosystem services and goods
that they provide (2). Ecological restoration has recently
adopted insights from the biodiversity-ecosystem function
(BEF) perspective (3). This emphasis on functional
rather than taxonomic diversity (3, 4), combined with
increasing acceptance of perennial, global-scale effects
on the environment (5, 6) and the associated species
gains and losses (“Terrestrial ecosystem responses to
species gains and losses,” D. A. Wardle et al., Review,
10 June, p. 1273), may be the beginning of a paradigm
shift in forest conservation and restoration ecology. As
a result, we may see increased tolerance toward and the
use of nonnative tree species in forests worldwide
8 JULY 2011 VOL 333 SCIENCE
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