Climate Change

Climate Change Report Warns of Dramatically Warmer World This Century
The World Bank - Climate Change - Climate Change Report Warns of Dramatically Warmer World This Century

Highlights:

New World Bank-commissioned report warns the world is on track to a “4°C world” marked by extreme heat-waves and life-threatening sea level rise.

Adverse effects of global warming are “tilted against many of the world's poorest regions” and likely to undermine development efforts and goals.

Bank eyes increased support for adaptation, mitigation, inclusive green growth and climate-smart development.
 
Blennow K, Persson J, Tome M, Hanewinkel M. Climate Change: Believing and Seeing Implies Adapting. PLoS ONE 2012;7(11):e50182. PLOS ONE: Climate Change: Believing and Seeing Implies Adapting

Knowledge of factors that trigger human response to climate change is crucial for effective climate change policy communication. Climate change has been claimed to have low salience as a risk issue because it cannot be directly experienced. Still, personal factors such as strength of belief in local effects of climate change have been shown to correlate strongly with responses to climate change and there is a growing literature on the hypothesis that personal experience of climate change (and/or its effects) explains responses to climate change. Here we provide, using survey data from 845 private forest owners operating in a wide range of bio-climatic as well as economic-social-political structures in a latitudinal gradient across Europe, the first evidence that the personal strength of belief and perception of local effects of climate change, highly significantly explain human responses to climate change. A logistic regression model was fitted to the two variables, estimating expected probabilities ranging from 0.07 (SD ±0.01) to 0.81 (SD ±0.03) for self-reported adaptive measures taken. Adding socio-demographic variables improved the fit, estimating expected probabilities ranging from 0.022 (SD ±0.008) to 0.91 (SD ±0.02). We conclude that to explain and predict adaptation to climate change, the combination of personal experience and belief must be considered.
 
Choat B, Jansen S, Brodribb TJ, et al. Global convergence in the vulnerability of forests to drought. Nature;advance online publication. http://www.nature.com/nature/journal/vaop/ncurrent/full/nature11688.html

Shifts in rainfall patterns and increasing temperatures associated with climate change are likely to cause widespread forest decline in regions where droughts are predicted to increase in duration and severity1. One primary cause of productivity loss and plant mortality during drought is hydraulic failure2, 3, 4. Drought stress creates trapped gas emboli in the water transport system, which reduces the ability of plants to supply water to leaves for photosynthetic gas exchange and can ultimately result in desiccation and mortality. At present we lack a clear picture of how thresholds to hydraulic failure vary across a broad range of species and environments, despite many individual experiments. Here we draw together published and unpublished data on the vulnerability of the transport system to drought-induced embolism for a large number of woody species, with a view to examining the likely consequences of climate change for forest biomes. We show that 70% of 226 forest species from 81 sites worldwide operate with narrow (<1?megapascal) hydraulic safety margins against injurious levels of drought stress and therefore potentially face long-term reductions in productivity and survival if temperature and aridity increase as predicted for many regions across the globe5, 6. Safety margins are largely independent of mean annual precipitation, showing that there is global convergence in the vulnerability of forests to drought, with all forest biomes equally vulnerable to hydraulic failure regardless of their current rainfall environment. These findings provide insight into why drought-induced forest decline is occurring not only in arid regions but also in wet forests not normally considered at drought risk7, 8.
 
Climate change, impacts and vulnerability in Europe 2012
http://www.eea.europa.eu/pressroom/publications/climate-impacts-and-vulnerability-2012/

This European Environment Agency (EEA) report presents information on past and projected climate change and related impacts in Europe, based on a range of indicators. The report also assesses the vulnerability of society, human health and ecosystems in Europe and identifies those regions in Europe most at risk from climate change. Furthermore, the report discusses the principle sources of uncertainty for the indicators and notes how monitoring and scenario development can improve our understanding of climate change, its impacts and related vulnerabilities.
 
Tallis H, Mooney H, Andelman S, et al. A Global System for Monitoring Ecosystem Service Change. BioScience 2012;62(11):977-86. JSTOR: An Error Occurred Setting Your User Cookie

Earth’s life-support systems are in flux, yet no centralized system to monitor and report these changes exists. Recognizing this, 77 nations agreed to establish the Group on Earth Observations (GEO). The GEO Biodiversity Observation Network (GEO BON) integrates existing data streams into one platform in order to provide a more complete picture of Earth’s biological and social systems. We present a conceptual framework envisioned by the GEO BON Ecosystem Services Working Group, designed to integrate national statistics, numerical models, remote sensing, and in situ measurements to regularly track changes in ecosystem services across the globe. This information will serve diverse applications, including stimulating new research and providing the basis for assessments. Although many ecosystem services are not currently measured, others are ripe for reporting. We propose a framework that will continue to grow and inspire more complete observation and assessments of our planet’s life-support systems.
 
Santer BD, Painter JF, Mears CA, et al. Identifying human influences on atmospheric temperature. Proceedings of the National Academy of Sciences. Identifying human influences on atmospheric temperature

We perform a multimodel detection and attribution study with climate model simulation output and satellite-based measurements of tropospheric and stratospheric temperature change. We use simulation output from 20 climate models participating in phase 5 of the Coupled Model Intercomparison Project. This multimodel archive provides estimates of the signal pattern in response to combined anthropogenic and natural external forcing (the fingerprint) and the noise of internally generated variability.

Using these estimates, we calculate signal-to-noise (S/N) ratios to quantify the strength of the fingerprint in the observations relative to fingerprint strength in natural climate noise. For changes in lower stratospheric temperature between 1979 and 2011, S/N ratios vary from 26 to 36, depending on the choice of observational dataset. In the lower troposphere, the fingerprint strength in observations is smaller, but S/N ratios are still significant at the 1% level or better, and range from three to eight. We find no evidence that these ratios are spuriously inflated by model variability errors. After removing all global mean signals, model fingerprints remain identifiable in 70% of the tests involving tropospheric temperature changes. Despite such agreement in the large-scale features of model and observed geographical patterns of atmospheric temperature change, most models do not replicate the size of the observed changes.

On average, the models analyzed underestimate the observed cooling of the lower stratosphere and overestimate the warming of the troposphere. Although the precise causes of such differences are unclear, model biases in lower stratospheric temperature trends are likely to be reduced by more realistic treatment of stratospheric ozone depletion and volcanic aerosol forcing.
 
Villarini G, Vecchi GA. Projected Increases in North Atlantic Tropical Cyclone Intensity from CMIP5 Models. Journal of Climate. An Error Occurred Setting Your User Cookie

Tropical cyclones – particularly intense ones – are a hazard to life and property, so an assessment of the changes in North Atlantic tropical cyclone intensity has important socio-economic implications. In this study we focus on the seasonally integrated Power Dissipation Index (PDI) as a metric to project changes in tropical cyclone intensity. Based on a recently developed statistical model, we examine projections in North Atlantic PDI using output from 17 state-of-the-art global climate models and three radiative forcing scenarios. Overall, we find that North Atlantic PDI is projected to increase with respect to the 1986-2005 period across all scenarios. The difference between the PDI projections and those of the number of North Atlantic tropical cyclones, which are not projected to increase significantly, indicates an intensification of North Atlantic tropical cyclones in response to both greenhouse gas (GHG) increases and aerosol changes over the current century. At the end of the 21st century, the magnitude of these increases shows a positive dependence on projected GHG forcing. The projected intensification is significantly enhanced by non-GHG (primarily aerosol) forcing in the first half of the 21st century.
 
Peters GP, Andrew RM, Boden T, et al. The challenge to keep global warming below 2 [deg]C. Nature Clim Change;advance online publication. http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate1783.html

The latest carbon dioxide emissions continue to track the high end of emission scenarios, making it even less likely global warming will stay below 2 °C. A shift to a 2 °C pathway requires immediate significant and sustained global mitigation, with a probable reliance on net negative emissions in the longer term.
 
Policy Implications Of Warming Permafrost
http://www.unep.org/pdf/permafrost.pdf

Permafrost is perennially frozen ground occurring in about 24% of the exposed land surface in the Northern Hemisphere. The distribution of permafrost is controlled by air temperature and, to a lesser extent, by snow depth, vegetation, orientation to the sun and soil properties. Any location with annual average air temperatures below freezing can potentially form permafrost.

Snow is an effective insulator and modulates the effect of air temperature, resulting in permafrost temperatures up to 6°C higher than the local mean annual air temperature. Most of the current permafrost formed during or since the last ice age and can extend down to depths of more than 700 meters in parts of northern Siberia and Canada. Permafrost includes the contents of the ground before it was frozen, such as bedrock, gravel, silt and organic material. Permafrost often contains large lenses, layers and wedges of pure ice that grow over many years as a result of annual freezing and thawing of the surface soil layer.


Thawing of Permafrost Expected to Cause Significant Additional Global Warming, Not Yet Accounted for in Climate Predictions
Thawing of permafrost expected to cause significant additional global warming, not yet accounted for in climate predictions
 
Lewandowsky S, Oberauer K, Gignac CE. (in press). NASA faked the moon landing-therefore (climate) science is a hoax: An anatomy of the motivated rejection of science. Psychological Science. http://websites.psychology.uwa.edu.au/labs/cogscience/Publications/LskyetalPsychScienceinPressClimateConspiracy.pdf

Although nearly all domain experts agree that human CO2 emissions are altering the world's climate, segments of the public remain unconvinced by the scientific evidence. Internet blogs have become a vocal platform for climate denial, and bloggers have taken a prominent and influential role in questioning climate science. We report a survey (N > 1100) of climate blog users to identify the variables underlying acceptance and rejection of climate science. Paralleling previous work, we find that endorsement of a laissez-faire conception of free-market economics predicts rejection of climate science (r ~ 0.80 between latent constructs). Endorsement of the free market also predicted the rejection of other established scientific findings, such as the facts that HIV causes AIDS and that smoking causes lung cancer. We additionally show that endorsement of a cluster of conspiracy theories (e.g., that the CIA killed Martin-Luther King or that NASA faked the moon landing) predicts rejection of climate science as well as the rejection of other scientific findings, above and beyond endorsement of laissez-faire free markets. This provides empirical confirmation of previous suggestions that conspiracist ideation contributes to the rejection of science. Acceptance of science, by contrast, was strongly associated with the perception of a consensus among scientists.


What Do Aliens, Climate Change And Princess Di Have In Common?
Climate Change Denial Linked To Conspiratorial Thinking : 13.7: Cosmos And Culture : NPR


Lewandowsky to Remove All Blog Based References
Lewandowsky to Remove All Blog Based References
 
Winkelmann R, Levermann A, Martin MA, Frieler K. Increased future ice discharge from Antarctica owing to higher snowfall. Nature 2012;492(7428):239-42. http://www.nature.com/nature/journal/v492/n7428/full/nature11616.html

Anthropogenic climate change is likely to cause continuing global sea level rise1, but some processes within the Earth system may mitigate the magnitude of the projected effect. Regional and global climate models simulate enhanced snowfall over Antarctica, which would provide a direct offset of the future contribution to global sea level rise from cryospheric mass loss2, 3 and ocean expansion4. Uncertainties exist in modelled snowfall5, but even larger uncertainties exist in the potential changes of dynamic ice discharge from Antarctica1, 6 and thus in the ultimate fate of the precipitation-deposited ice mass. Here we show that snowfall and discharge are not independent, but that future ice discharge will increase by up to three times as a result of additional snowfall under global warming. Our results, based on an ice-sheet model7 forced by climate simulations through to the end of 2500 (ref. 8), show that the enhanced discharge effect exceeds the effect of surface warming as well as that of basal ice-shelf melting, and is due to the difference in surface elevation change caused by snowfall on grounded versus floating ice. Although different underlying forcings drive ice loss from basal melting versus increased snowfall, similar ice dynamical processes are nonetheless at work in both; therefore results are relatively independent of the specific representation of the transition zone. In an ensemble of simulations designed to capture ice-physics uncertainty, the additional dynamic ice loss along the coastline compensates between 30 and 65 per cent of the ice gain due to enhanced snowfall over the entire continent. This results in a dynamic ice loss of up to 1.25 metres in the year 2500 for the strongest warming scenario. The reported effect thus strongly counters a potential negative contribution to global sea level by the Antarctic Ice Sheet.
 
[ame=http://www.youtube.com/watch?v=YoA_Z7y8f6Q]Chasing Ice movie reveals largest iceberg break-up ever filmed. - YouTube[/ame]
 
Gao Y, Fu JS, Drake JN, Liu Y, Lamarque J-F. Projected changes of extreme weather events in the eastern United States based on a high resolution climate modeling system. Environmental Research Letters 2012;7(4):044025. Projected changes of extreme weather events in the eastern United States based on a high resolution climate modeling system - Abstract - Environmental Research Letters - IOPscience

This study is the first evaluation of dynamical downscaling using the Weather Research and Forecasting (WRF) Model on a 4 km × 4 km high resolution scale in the eastern US driven by the new Community Earth System Model version 1.0 (CESM v1.0). First we examined the global and regional climate model results, and corrected an inconsistency in skin temperature during the downscaling process by modifying the land/sea mask. In comparison with observations, WRF shows statistically significant improvement over CESM in reproducing extreme weather events, with improvement for heat wave frequency estimation as high as 98%. The fossil fuel intensive scenario Representative Concentration Pathway (RCP) 8.5 was used to study a possible future mid-century climate extreme in 2057–9. Both the heat waves and the extreme precipitation in 2057–9 are more severe than the present climate in the Eastern US. The Northeastern US shows large increases in both heat wave intensity (3.05?°C higher) and annual extreme precipitation (107.3 mm more per year).
 
When the Ice Melts, the Earth Spews Fire
When the ice melts, the Earth spews fire

The basic evidence for the discovery came from the work of the Collaborative Research Centre "Fluids and Volatiles in Subduction Zones (SFB 574). For more than ten years the project has been extensively exploring volcanoes of Central America. "Among others pieces of evidence, we have observations of ash layers in the seabed and have reconstructed the history of volcanic eruptions for the past 460,000 years," says GEOMAR volcanologist Dr Steffen Kutterolf, who has been with SFB 574 since its founding. Particular patterns started to appear. "There were periods when we found significantly more large eruptions than in others" says Kutterolf, the lead author of the Geology article.After comparing these patterns with the climate history, there was an amazing match. The periods of high volcanic activity followed fast, global temperature increases and associated rapid ice melting.

To expand the scope of the discoveries, Dr Kutterolf and his colleagues studied other cores from the entire Pacific region. These cores had been collected as part of the International Integrated Ocean Drilling Program (IODP) and its predecessor programmes. They record more than a million years of Earth's history. "In fact, we found the same pattern from these cores as in Central America" says geophysicist Dr Marion Jegen from GEOMAR, who also participated in the recent study. Together with colleagues at Harvard University, the geologists and geophysicists searched for a possible explanation. They found it with the help of geological computer models. "In times of global warming, the glaciers are melting on the continents relatively quickly. At the same time the sea level rises. The weight on the continents decreases, while the weight on the oceanic tectonic plates increases. Thus, the stress changes within in the Earth to open more routes for ascending magma" says Dr Jegen.

The rate of global cooling at the end of the warm phases is much slower, so there are less dramatic stress changes during these times. "If you follow the natural climate cycles, we are currently at the end of a really warm phase. Therefore, things are volcanically quieter now. The impact from human-made warming is still unclear based on our current understanding" says Dr Kutterolf. The next step is to investigate shorter-term historical variations to better understand implications for the present day.


Kutterolf S, Jegen M, Mitrovica JX, Kwasnitschka T, Freundt A, Huybers PJ. A detection of Milankovitch frequencies in global volcanic activity. Geology. A detection of Milankovitch frequencies in global volcanic activity

A rigorous detection of Milankovitch periodicities in volcanic output across the Pleistocene-Holocene ice age has remained elusive. We report on a spectral analysis of a large number of well-preserved ash plume deposits recorded in marine sediments along the Pacific Ring of Fire. Our analysis yields a statistically significant detection of a spectral peak at the obliquity period. We propose that this variability in volcanic activity results from crustal stress changes associated with ice age mass redistribution. In particular, increased volcanism lags behind the highest rate of increasing eustatic sea level (decreasing global ice volume) by 4.0 ± 3.6 k.y. and correlates with numerical predictions of stress changes at volcanically active sites. These results support the presence of a causal link between variations in ice age climate, continental stress field, and volcanism.
 
In need of action. Nature Clim Change 2012;3(1):1. In need of action : Nature Climate Change : Nature Publishing Group

Over the past twenty years of United Nations (UN) talks about climate change, little progress has been made in coordinating national efforts to cut the growth of carbon dioxide emissions. In a Commentary on http://www.nature.com/nclimate/journal/v3/n1/full/nclimate1783.html Glen Peters and colleagues show that humankind will probably face a rise in temperature of between 4–6 °C by the end of this century if significant mitigation actions do not happen now. They have contributed an estimate of the 2012 global CO2 emissions pathways to the Global Carbon Budget (Carbon Budget) — a report produced by the Global Carbon Project, an international cooperation of scientists working to support policymakers in slowing down the rate at which greenhouse-gas concentrations are increasing in the atmosphere.
 

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