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Gordon_SCS_ITF_GRL12_2012GL052021.pdf
Gordon_SCS_ITF_GRL12_2012GL052021.pdf

climate change WG II
climate change WG II

... hazardous climate events occurring within a specific time period and the vulnerability of an exposed society or system. Impacts are also referred to as consequences and outcomes. The impacts of climate change on geophysical systems, including floods, droughts, and sea level rise, are a subset of imp ...
Significant decrease in yield under future climate conditions
Significant decrease in yield under future climate conditions

... and [O3 ] to increase by 25% compared to the concentrations experienced today (32–62 ppb). The latest assessment report of IPCC, working group I, also considered three other climate scenarios with lower increase in the anthropogenic emission of greenhouse gases leading to less elevated temperature, ...
Diagnosing Present and Future Permafrost from Climate Models
Diagnosing Present and Future Permafrost from Climate Models

... Permafrost is a characteristic aspect of the terrestrial Arctic and the fate of near-surface permafrost over the next century is likely to exert strong controls on Arctic hydrology and biogeochemistry. Using output from the fifth phase of the Coupled Model Intercomparison Project (CMIP5), the author ...
Annex I Annex D in the Convention
Annex I Annex D in the Convention

... In the review of new POPs regional differences in climate change as observed and projected by IPCC should be taken into account. Climate change is predicted by the UNEP/AMAP expert group (2011) to increase the transport of POPs to the Arctic and other remote regions. Climate change is also predicted ...
Summary for Policymakers
Summary for Policymakers

... hazardous climate events occurring within a specific time period and the vulnerability of an exposed society or system. Impacts are also referred to as consequences and outcomes. The impacts of climate change on geophysical systems, including floods, droughts, and sea level rise, are a subset of imp ...
van Hooidonk et al. 2013. Opposite latitudinal gradients in projected
van Hooidonk et al. 2013. Opposite latitudinal gradients in projected

... presented in Chan & Connolly (2013) of 15%. We also show the extreme ends of the meta-analysis outcomes in that study, the mean  1SD; 7% and 23% per unit reduction in Ωarag. Previously, a latitudinal gradient was found in the projected onset of annual bleaching (van Hooidonk et al., 2013); therefor ...
Climate Extremes Communications Guidebook
Climate Extremes Communications Guidebook

... January 2013 draft of the National Climate Assessment 2014 (draft NCA 2014) report: “Some extreme weather and climate events have increased in recent decades, and there is new and stronger evidence that many of these increases are related to human activities… Human-induced climate change has already ...
Climate Change, Agricultural Adaptation and Fairtrade
Climate Change, Agricultural Adaptation and Fairtrade

Vulnerability of Marine Turtles to Climate Change
Vulnerability of Marine Turtles to Climate Change

Regional: Glacial Melt and Downstream Impacts on Indus
Regional: Glacial Melt and Downstream Impacts on Indus

... weather and hydrological stations in glacial areas, (ii) a lack of basin-wide and transboundary models to provide trends and future scenario in water supply situation, (iii) the shortage of basin-wide data on glaciers and their dynamics including changes in mass and their impacts on meltwater river ...
SEEKING CLIMATE JUSTICE: A CRITICAL RESPONSE TO SINGER
SEEKING CLIMATE JUSTICE: A CRITICAL RESPONSE TO SINGER

Basic physical mechanisms for monsoon failure in past and future
Basic physical mechanisms for monsoon failure in past and future

... CLIMBER-3α, that project monsoon rainfall around the world to increase quasi–linearly with global warming in the coming centuries. While this is generally consistent with many other studies, the atmospheric component of CLIMBER-3α is based on a simplified statistical–dynamical approach, and may not ...
the knowledge base. Updating what we know about ocean
the knowledge base. Updating what we know about ocean

... on Sustainable Development. Ocean issues featured more highly than ever before. In the outcome document The Future We Want, world leaders observed (paragraph 166): ‘We call for support to initiatives that address ocean acidification and the impacts of climate change on marine and coastal ecosystems ...
Ocean Acidification THE KNOWLEDGE BASE 2012
Ocean Acidification THE KNOWLEDGE BASE 2012

... on Sustainable Development. Ocean issues featured more highly than ever before. In the outcome document The Future We Want, world leaders observed (paragraph 166): ‘We call for support to initiatives that address ocean acidification and the impacts of climate change on marine and coastal ecosystems ...
Temperature Shocks and Economic Growth: Evidence from the Last Half Century
Temperature Shocks and Economic Growth: Evidence from the Last Half Century

... headway in exploring potential impacts of shifts in climate by examining medium-term temperature shifts within countries. Mean global land temperatures have risen nearly 1◦C since 1970 (Brohan et al. 2006), but countries have not warmed equally. We therefore examine whether those countries that expe ...
Impacts of Climate Related Geo-engineering on Biological
Impacts of Climate Related Geo-engineering on Biological

... effect of accumulating greenhouse gases. They would introduce a new dynamic between the warming effects of greenhouse gases and the cooling effects of SRM with uncertain climatic implications, especially at the regional scale. SRM would not directly address ocean acidification. SRM proposals ...
adaptation to climate change: key terms
adaptation to climate change: key terms

... At its meeting on 23 March 2005, the Annex I Expert Group requested the Secretariat to prepare a paper on key adaptation concepts and terms that have entered the UNFCCC lexicon such as ‘adaptation’, ‘vulnerability’, ‘adverse effect’, ‘adaptive capacity’, and others. The aim of the task is to collect ...
Ecosystem Processes and Human Influences
Ecosystem Processes and Human Influences

... Analyses of long-term records at 35 headwater basins in the United States and Canada indicate that climate change effects on streamflow are not as clear as might be expected, perhaps because of ecosystem processes and human influences. Evapotranspiration was higher than was predicted by temperature ...
Ecosystem Processes and Human Influences Regulate Streamflow Response to Climate Change at
Ecosystem Processes and Human Influences Regulate Streamflow Response to Climate Change at

... Analyses of long-term records at 35 headwater basins in the United States and Canada indicate that climate change effects on streamflow are not as clear as might be expected, perhaps because of ecosystem processes and human influences. Evapotranspiration was higher than was predicted by temperature ...
Climate Change curriculum
Climate Change curriculum

... Students begin the Climate Change Unit with an oli (chant). The oli sets a tone of respect and reverence for the elements as we seek to understand the changes to climate that are occurring all around us. Climate change is a complex topic that provides opportunities for students to explore many inter ...
Regional Climate Information – Evaluation and Projections
Regional Climate Information – Evaluation and Projections

... RCMs driven by observed boundary conditions show areaaveraged temperature biases (regional scales of 105 to 106 km2) generally within 2ºC and precipitation biases within 50% of observations. Statistical downscaling demonstrates similar performance, although greatly depending on the methodological im ...
Climate Projections FAQ
Climate Projections FAQ

... Our main objective is to develop a shared understanding within the Forest Service of what climate projections are, their strengths and limitations, and to provide some guidance regarding how climate projections might be used for climate change impact analyses by Forest Service units and partner or ...
Climate projections FAQ - Eastern Forest Environmental Threat
Climate projections FAQ - Eastern Forest Environmental Threat

... Our main objective is to develop a shared understanding within the Forest Service of what climate projections are, their strengths and limitations, and to provide some guidance regarding how climate projections might be used for climate change impact analyses by Forest Service units and partner or ...
CLIMATE CHANGE VULNERABILITY ASSESSMENTS: AN
CLIMATE CHANGE VULNERABILITY ASSESSMENTS: AN

... and uses them to illustrate the evolution of integrated assessments. This evolution is reflected in the following trends: – From linear to more complex chains of analysis, – From non-adaptive to perfectly adaptive to realistically adaptive agents, – From simplistic to sophisticated to pluralistic co ...
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Global warming hiatus



A global warming hiatus, also sometimes referred to as a global warming pause or a global warming slowdown, is a period of relatively little change in globally averaged surface temperatures. In the current episode of global warming many such periods are evident in the surface temperature record, along with robust evidence of the long term warming trend.The exceptionally warm El Niño year of 1998 was an outlier from the continuing temperature trend, and so gave the appearance of a hiatus: by January 2006 assertions had been made that this showed that global warming had stopped. A 2009 study showed that decades without warming were not exceptional, and in 2011 a study showed that if allowances were made for known variability, the rising temperature trend continued unabated. There was increased public interest in 2013 in the run-up to publication of the IPCC Fifth Assessment Report, and despite concerns that a 15-year period was too short to determine a meaningful trend, the IPCC included a section on a hiatus, which it defined as a much smaller increasing linear trend over the 15 years from 1998 to 2012, than over the 60 years from 1951 to 2012. Various studies examined possible causes of the short term slowdown. Even though the overall climate system had continued to accumulate energy due to Earth's positive energy budget, the available temperature readings at the earth's surface indicated slower rates of increase in surface warming than in the prior decade. Since measurements at the top of the atmosphere show that Earth is receiving more energy than it is radiating back into space, the retained energy should be producing warming in at least one of the five parts of Earth's climate system.A July 2015 paper on the updated NOAA dataset cast doubt on the existence of this supposed hiatus, and found no indication of a slowdown. This analysis incorporated the latest corrections for known biases in ocean temperature measurements, and new land temperature data. Scientists working on other datasets welcomed this study, though the view was expressed that the short term warming trend had been slower than in previous periods of the same length.
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