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Climate change impacts on the biophysics and economics of world fisheries
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Global marine fisheries are underperforming economically because of overfishing, pollution and habitat degradation. Added to these threats is the looming challenge of climate change. Observations, experiments and simulation models show that climate change would result in changes in primary productivity, shifts in distribution and changes in the potential yield of exploited marine species, resulting in impacts on the economics of fisheries worldwide. Despite the gaps in understanding climate change effects on fisheries, there is sufficient scientific information that highlights the need to implement climate change mitigation
and adaptation policies to minimize impacts on fisheries.
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Dissecting insect responses to climate warming: overwintering and post-diapause performance in the southern green stink bug, Nezara viridula, under simulated climate-change conditions
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The effect of simulated climate change on overwintering and postdiapause
reproductive performance is studied in Nezara viridula (L.) (Heteroptera:
Pentatomidae) close to the species’ northern range limit in Japan. Insects are reared
from October to June under quasi-natural (i.e. ambient outdoor) conditions and in
a transparent incubator, in which climate warming is simulated by adding 2.5 ◦
C to
the ambient temperatures. Despite the earlier assumption that females of N. viridula
overwinter in diapause, whereas males do so in quiescence, regular dissections show
that the two sexes overwinter in a state of true diapause. During winter, both sexes are
dark-coloured and have undeveloped reproductive organs. Resumption of development
does not start until late March. During winter, the effect of simulated warming on the
dynamics and timing of physiological processes appears to be limited. However, the
warming significantly enhances winter survival (from 27–31% to 47–70%), which
is a key factor in range expansion of N. viridula. In spring, the effect of simulated
warming is complex. It advances the post-diapause colour change and transition from
dormancy to reproduction. The earlier resumption of development is more pronounced
in females: in April, significantly more females are already in a reproductive state
under the simulated warming than under quasi-natural conditions. In males, the
tendency is similar, although the difference is not significant. Warming significantly
enhances spring survival and percentage of copulating adults, although not the percentage
of ovipositing females and fecundity. The results suggest that, under the expected
climate-warming conditions, N. viridula will likely benefit mostly as a result of
increased winter and spring survival and advanced post-diapause reproduction. Further
warming is likely to allow more adults to survive the critical cold season and contribute
(both numerically and by increasing heterogeneity) to the post-overwintering population
growth, thus promoting the establishment of this species in newly-colonized
area
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The Holocene`
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Combining nine tree growth proxies from four sites, from the west coast of Norway to the Kola Peninsula of NW Russia, provides a well replicated
(> 100 annual measurements per year) mean index of tree growth over the last 1200 years that represents the growth of much of the northern pine
timberline forests of northern Fennoscandia. The simple mean of the nine series, z-scored over their common period, correlates strongly with mean
June to August temperature averaged over this region (r = 0.81), allowing reconstructions of summer temperature based on regression and variance
scaling. The reconstructions correlate significantly with gridded summer temperatures across the whole of Fennoscandia, extending north across Svalbard
and south into Denmark. Uncertainty in the reconstructions is estimated by combining the uncertainty in mean tree growth with the uncertainty in
the regression models. Over the last seven centuries the uncertainty is < 4.5% higher than in the 20th century, and reaches a maximum of 12% above
recent levels during the 10th century. The results suggest that the 20th century was the warmest of the last 1200 years, but that it was not significantly
different from the 11th century. The coldest century was the 17th. The impact of volcanic eruptions is clear, and a delayed recovery from pairs or multiple
eruptions suggests the presence of some positive feedback mechanism. There is no clear and consistent link between northern Fennoscandian summer
temperatures and solar forcing.
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The Wheel of Life Food, Climate, Human Rights, and the Economy
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The links between climate change and industrial agriculture create a nexus of crises—food
insecurity, natural resource depletion and degradation, as well as human
rights violations and inequities.
While it is widely recognized that greenhouse gas (GHG) emissions due
to human activity are detrimental to the natural environment, it can be difficult to
untangle the cascading effects on other sectors. To unravel some of the effects, this
paper focuses on three interrelated issues:
1) What are the critical links between climate change and agriculture?
2) How is the nexus of agriculture and climate change affecting human societies
particularly regarding food and water, livelihoods, migration, gender
equality, and other basic survival and human rights?
3) What is the interplay between economic and finance systems, on the one
hand, and food security, climate change, and fundamental human rights, on
the other?
In the process of drawing connections among these issues, the report will identify
the commonality of drivers, or “push” factors, that lead to adverse impacts.
A central theme throughout this report is that policies and practices must
begin with the ecological imperative in order to ensure authentic security and stability
on all fronts including food, water, livelihoods and jobs, climate, energy, and
economic. In turn this engenders equity, social justice, and diverse cultures. This
imperative, or ethos of nature, is a foundation that serves as a steady guide when
reviewing mitigation and adaptation solutions to climate change.
Infused within this theme is the sobering recognition that current consumption
and production patterns are at odds with goals of reducing GHGs and attaining
global food security. For instance, consumption and production levels, based on the
global average, are 25 percent higher than the earth’s ecological capacity.1
As societies
address the myriad ecological and social issues at the axis of global warming,
a central task will be to re-align consumption and production trends in a manner
that can fulfill economic and development requirements. This will require a major
shift away from present economic growth paradigms based on massive resource
extraction and toward creating prosperous and vital societies and economies that
preserve the planet’s environmental capacity
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Missing feedbacks, asymmetric uncertainties, and the underestimation of future warming
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Historical evidence shows that atmospheric greenhouse
gas (GhG) concentrations increase during periods of
warming, implying a positive feedback to future climate
change. We quantified this feedback for CO2 and CH4 by
combining the mathematics of feedback with empirical icecore
information and general circulation model (GCM)
climate sensitivity, finding that the warming of 1.5 –4.5C
associated with anthropogenic doubling of CO2 is amplified
to 1.6– 6.0C warming, with the uncertainty range deriving
from GCM simulations and paleo temperature records.
Thus, anthropogenic emissions result in higher final GhG
concentrations, and therefore more warming, than would be
predicted in the absence of this feedback. Moreover, a
symmetrical uncertainty in any component of feedback,
whether positive or negative, produces an asymmetrical
distribution of expected temperatures skewed toward higher
temperature. For both reasons, the omission of key positive
feedbacks and asymmetrical uncertainty from feedbacks, it
is likely that the future will be hotter than we think.
Citation: Torn, M. S., and J. Harte (2006), Missing feedbacks,
asymmetric uncertainties, and the underestimation of future
warming.
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TRY – a global database of plant traits
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Plant traits – the morphological, anatomical, physiological, biochemical and phenological characteristics of plants and
their organs – determine how primary producers respond to environmental factors, affect other trophic levels,
influence ecosystem processes and services and provide a link from species richness to ecosystem functional diversity.
Trait data thus represent the raw material for a wide range of research from evolutionary biology, community and
functional ecology to biogeography. Here we present the global database initiative named TRY, which has united a
wide range of the plant trait research community worldwide and gained an unprecedented buy-in of trait data: so far
93 trait databases have been contributed. The data repository currently contains almost three million trait entries for
69 000 out of the world’s 300 000 plant species, with a focus on 52 groups of traits characterizing the vegetative and
regeneration stages of the plant life cycle, including growth, dispersal, establishment and persistence. A first data
analysis shows that most plant traits are approximately log-normally distributed, with widely differing ranges of
variation across traits. Most trait variation is between species (interspecific), but significant intraspecific variation is
also documented, up to 40% of the overall variation. Plant functional types (PFTs), as commonly used in vegetation
models, capture a substantial fraction of the observed variation – but for several traits most variation occurs within
PFTs, up to 75% of the overall variation. In the context of vegetation models these traits would better be represented by
state variables rather than fixed parameter values. The improved availability of plant trait data in the unified global
database is expected to support a paradigm shift from species to trait-based ecology, offer new opportunities for
synthetic plant trait research and enable a more realistic and empirically grounded representation of terrestrial
vegetation in Earth system models.
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U.S. Forest Carbon and Climate Change Controversies and Win-Win Policy Approaches
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As consensus grows about the serious impacts of global climate change, the role of
forests in carbon storage is increasingly recognized. Terrestrial vegetation worldwide
currently removes about 24 percent of the greenhouse gases released by industrial
processes. Unfortunately, this contribution is approximately cancelled out by carbon
released as a result of global deforestation and other ecosystem changes. Slowing or
halting the rate of deforestation is thus one of the prime strategies to mitigate global
climate change.
The U.S. situation differs from the global one in several ways. Since both forest acres
and average biomass per forest acre are currently increasing, as U.S. forests recover
from past clearing or heavy harvest, our forest carbon stores are growing larger over
time. However, our high rate of industrial emissions means that only about 10 percent
of the carbon released from burning fossil fuels in the United States is captured by our
forests. Moreover, net U.S. forest carbon sequestration has begun to slow in recent
years as reforestation reaches its limits and development sprawls into more rural forested
areas. U.S. forests could possibly capture a much higher portion of our industrial
emissions, but only if we prevent forest conversion and development and manage our
forests to maximize carbon stores.
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Unburnable Carbon – Are the world’s financial markets carrying a carbon bubble?
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The Carbon Tracker initiative is a new way of looking at the carbon emissions
problem. It is focused on the fossil fuel reserves held by publically listed
companies and the way they are valued and assessed by markets. Currently
financial markets have an unlimited capacity to treat fossil fuel reserves
as assets. As governments move to control carbon emissions, this market
failure is creating systemic risks for institutional investors, notably the
threat of fossil fuel assets becoming stranded as the shift to a low-carbon
economy accelerates.
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Scenario Planning: a Tool for Conservation in an Uncertain World
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: Conservation decisions about how, when, and where to act are typically based on our expectations
for the future. When the world is highly unpredictable and we are working from a limited range of expectations,
however, our expectations will frequently be proved wrong. Scenario planning offers a framework for
developing more resilient conservation policies when faced with uncontrollable, irreducible uncertainty. A
scenario in this context is an account of a plausible future. Scenario planning consists of using a few contrasting
scenarios to explore the uncertainty surrounding the future consequences of a decision. Ideally, scenarios
should be constructed by a diverse group of people for a single, stated purpose. Scenario planning can
incorporate a variety of quantitative and qualitative information in the decision-making process. Often, consideration
of this diverse information in a systemic way leads to better decisions. Furthermore, the participation
of a diverse group of people in a systemic process of collecting, discussing, and analyzing scenarios
builds shared understanding. The robustness provided by the consideration of multiple possible futures has
served several groups well; we present examples from business, government, and conservation planning that
illustrate the value of scenario planning. For conservation, major benefits of using scenario planning are (1)
increased understanding of key uncertainties, (2) incorporation of alternative perspectives into conservation
planning, and (3) greater resilience of decisions to surprise.
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Call Off the Quest
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Over the past 30 years, the climate research community has made valiant efforts to answer the “climate sensitivity” question: What is the long-term equilibrium warming response to a doubling of atmospheric carbon dioxide? Earlier this year, the Intergovernmental Panel on Climate Change (1) concluded that this sensitivity is likely to be in the range of 2° to 4.5°C, with a 1-in-3 chance that it is outside that range. The
lower bound of 2°C is slightly higher than the 1.6°C proposed in the 1970s (2).
26 OCTOBER 2007 VOL 318 SCIENCE
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