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House science testimony apr 15 final - Climate Etc.
House science testimony apr 15 final - Climate Etc.

... the climate is to these increases. Climate sensitivity is defined as the global surface warming that occurs when the concentration of carbon dioxide in the atmosphere doubles. If climate sensitivity is high, then we can expect substantial warming in the coming century as emissions continue to increa ...
ORIGINAL ARTICLE GLOBAL WARMING: ITS IMPLICATIONS
ORIGINAL ARTICLE GLOBAL WARMING: ITS IMPLICATIONS

... warming.Less than 50% of the students were willing to contribute through one or the other means of stopping global warming. Only around 50% of the students were ready to convey the message to others. INTRODUCTION: Warming of the climate system is unequivocal, as is now evident from the observations ...
Climate change and freshwater ecosystems: impacts
Climate change and freshwater ecosystems: impacts

... availability are climate-dependent; and (iii) many systems are already exposed to numerous anthropogenic stressors. Most climate change studies to date have focused on individuals or species populations, rather than the higher levels of organization (i.e. communities, food webs, ecosystems). We prop ...
Climate Change Adaptation Plan
Climate Change Adaptation Plan

... Note: Uncertainty around the projected amount of future sea level rise may or may not offset the amount of current and future vertical land motion, thereby resulting in a broad range of scenarios. This uncertainty is an issue for coastal zone planning. Any new initiative or project must be flexible ...
Climate Risk Assessment for Water Resources
Climate Risk Assessment for Water Resources

... 3 The runoff elasticity of a performance indicator (e.g. hydro-energy production) defines the response (as a multiplier) of the indicator to changes in runoff; for example, a runoff elasticity of hydro-energy of 1.2 indicates that a 10% decrease in runoff would cause a 12% decrease in generated hydr ...
The distributional impact of climate change on rich and poor countries
The distributional impact of climate change on rich and poor countries

Climate change science and the climate change scare Contents
Climate change science and the climate change scare Contents

... be otherwise. CO2 is also changing. It was 15 times higher than now in the Cambrian period 550 million years ago (which saw the most glorious proliferation of life forms in the Earth’s history). It dropped to half as low as now in the last Ice Age (which saw misery). These dramatic changes in CO2 ha ...
Climate change beliefs and perceptions of weather
Climate change beliefs and perceptions of weather

... Public perception research in different countries has suggested that real and perceived periods of high temperature strengthen people’s climate change beliefs. Such findings raise questions about the climate change beliefs of people in regions with moderate climates. Relatively little is known about ...
McCarty, 2001. Ecological consequences of recent climate change.
McCarty, 2001. Ecological consequences of recent climate change.

... Abstract: Global climate change is frequently considered a major conservation threat. The Earth’s climate has already warmed by 0.5⬚ C over the past century, and recent studies show that it is possible to detect the effects of a changing climate on ecological systems. This suggests that global chang ...
Climate Change Planning in Alaska`s National Parks
Climate Change Planning in Alaska`s National Parks

... to late-21st Century. Relative proportions of moisture deposited as snow, ice or rain change as temperature increases. Many areas will experience drying conditions despite increased precipitation, due to higher temperature and increased rates of evapotranspiration. More freezing rain events affect f ...
The National strategy on climate change was issued by Prime
The National strategy on climate change was issued by Prime

... 2139/QĐ-TTg on December 05, 2011. The following is its full content (for reference): National strategy on climate change I. Climate change – Challenge and chance 1. Challenges Climate change is one of biggest challenges to the human beings. Climate change can lead to serious impacts on production, l ...
Adapting to climate change: A perspective from evolutionary
Adapting to climate change: A perspective from evolutionary

... respectively, than either is to the mean temperature. Thus changes in mean environmental temperatures might have played a smaller role in the evolution of performance curves than have changes in thermal extremes and their interactions with precipitation (and likely cloud cover). In a similar vein, t ...
This article was originally published in a journal published by
This article was originally published in a journal published by

David R. Legates, Ph.D. Center for Climatic Research
David R. Legates, Ph.D. Center for Climatic Research

... (1993 to 2003). This was regarded as further confirmation the IPCC’s AGW hypothesis. Their expectation was that the Earth’s climate system would continue accumulating heat more or less monotonically. Now that heat accumulation has stopped (and perhaps even reversed), the tables have turned. The same ...
Neelin, 2011. Climate Change and Climate Modeling, Cambridge
Neelin, 2011. Climate Change and Climate Modeling, Cambridge

... ozone hole formation (the stratospheric polar vortex, stratospheric ice clouds), vegetation affects absorption of sunlight and evaporation from land surfaces, ... Neelin, 2011. Climate Change and Climate Modeling, Cambridge UP ...
Aasprang.Brita.Envir..
Aasprang.Brita.Envir..

... the fall (Höglind et al., 2009:72). Increased amounts of rain can lead to increased erosion and a loss of nutrition in the soil (Deelstra, Øygarden, Blankenberg, & Eggestad, 2012). The effects of climate change is expected to have different impacts in different places around the country (O'Brien et ...
PLATE TECTONICS AND CLIMATE CHANGE
PLATE TECTONICS AND CLIMATE CHANGE

... atmospheric pressure pattern is dominated by the Walker Circulation. The Walker Circulation is driven by the longitudinal distribution of diabatic heating over land and sea, with Africa, South America, and the warm waters surrounding Indonesia providing sources of heating. On today’s Earth, easterly ...
4b. GCOS-indicators_WDAC6 - World Climate Research Programme
4b. GCOS-indicators_WDAC6 - World Climate Research Programme

... Ø Planning for adaptation needs an understanding of future risk and how it may change: What would a one in a hundred-year storm look like in 100 years’ time? Ø Planning for future impacts needs an understanding now of worst-case scenarios, e.g. highest possible sea level rise, largest flood or big ...
Integrating Climate Information and Adaptation in Project
Integrating Climate Information and Adaptation in Project

... Analysing and Explaining Risks, Costs and Benefits a. A range of adaptation measures to address the identified climate risks should be explained and analysed. These should be compared in terms of cost and benefits in order to inform decision making. b. The costs (if any) associated with adaptation m ...
Chapter One - Brookings Institution
Chapter One - Brookings Institution

... have always had to hedge their bets to protect public health and ensure a reliable water supply in the face of climate variability and numerous other sources of variability. Some of the sources of variability include changes that derive from the choices humans make, such as demographic shifts and ch ...
Citation
Citation

... geographical species distributions are correlated with changes in climatic factors (Parmesan and Yohe 2003). This provides important proof for climate change effects, and sometimes evidence for the extent and urgency of the problem (Thomas et al. 2006). But the sort of information is not what scienc ...
Assessing the Relative Roles of Initial and Boundary Conditions in
Assessing the Relative Roles of Initial and Boundary Conditions in

... boundary conditions, such as explosive volcanic eruptions, are unlikely ever to be predictable in a deterministic sense, but their role still needs to be understood since it places limits on attainable forecast skill. 2. Comparing two kinds of predictability The question of predictability of the sec ...
Climate Change News 27 April 12
Climate Change News 27 April 12

... UNDP/SPC Introduces GIS Mapping for Land and Forest in Solomon Islands 23 March 2012: The UN Development Programme (UNDP) and the South Pacific Geoscience Commission (SOPAC) Division of the South Pacific Community (SPC) in partnership with the Solomon Islands Government, plan to introduce a remote s ...
LEIF CHRISTIAN STIGE, Dr. scient.
LEIF CHRISTIAN STIGE, Dr. scient.

... Nordic Centre of Excellence: Climate Change Effects on Marine Ecosystems and Resource Economics (Nordic Council top-level research initiative; 66 mill. NOK). Co-author and PhD supervisor. Adaptive management of living marine resources by integrating different data sources and key ecological processe ...
Climate impacts on the health of remote northern Australian
Climate impacts on the health of remote northern Australian

... The Garnaut review has indicated a limited range of emission scenarios to be considered in this impact assessment. 1 Climate projections for the near-term (2030) show similar patterns of regional change with small variation between climate models due to the influence of greenhouse gases already emit ...
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Effects of global warming



The effects of global warming are the environmental and social changes caused (directly or indirectly) by human emissions of greenhouse gases. There is a scientific consensus that climate change is occurring, and that human activities are the primary driver. Many impacts of climate change have already been observed, including glacier retreat, changes in the timing of seasonal events (e.g., earlier flowering of plants), and changes in agricultural productivity.Future effects of climate change will vary depending on climate change policies and social development. The two main policies to address climate change are reducing human greenhouse gas emissions (climate change mitigation) and adapting to the impacts of climate change. Geoengineering is another policy option.Near-term climate change policies could significantly affect long-term climate change impacts. Stringent mitigation policies might be able to limit global warming (in 2100) to around 2 °C or below, relative to pre-industrial levels. Without mitigation, increased energy demand and extensive use of fossil fuels might lead to global warming of around 4 °C. Higher magnitudes of global warming would be more difficult to adapt to, and would increase the risk of negative impacts.
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