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Climate Sensitivity - Home page 350.me.uk
Climate Sensitivity - Home page 350.me.uk

... d i f f e r e n t physical processes to the cooling of the l a s t ice age (18K years ago), and (3) by using estimated changes in global temperature and the abundance of atmospheric greenhouse gases to deduce an empirical climate sensitivity for the period 1850-1980. Our 3-D global climate model yie ...
How far are biodiversity loss and climate change similar as policy
How far are biodiversity loss and climate change similar as policy

... are therefore of direct importance to some of the world’s largest corporations, with highly developed technical and financial planning and executive capacity. On the other hand, the impact of biodiversity loss on industrial sectors is less immediately significant and more diffuse. There are numerous ...
Understanding Uncertainties in Future Colorado River Streamflow
Understanding Uncertainties in Future Colorado River Streamflow

... concentrations translate to larger temperature increases especially in the latter part of the 21st century. ...
Public Perception of Climate Change Adaptation
Public Perception of Climate Change Adaptation

... motivating factor for individuals to reduce greenhouse gas emissions and to adopt adaptation measures to reduce health risks. However, it is not clear if the health frame would suffice to engage the pubic in adaptation and mitigation steps, since they hinge on public appreciation of the health threa ...
Climate Change and San Francisco Bay-Delta Tidal
Climate Change and San Francisco Bay-Delta Tidal

... salt in brackish and freshwater tidal systems, in addition to causing increases in atmospheric CO2 concentration, warmer temperatures, and shifts in precipitation. In the San Francisco Bay–Delta, the areas most likely to be affected—brackish and freshwater tidal wetlands—are also the sites with the ...
An ecohydrological sketch of climate change impacts on water and
An ecohydrological sketch of climate change impacts on water and

... approach (sensu Allen et al., 2005; Feddes, 1987) may be preferred for model simplicity, but such factors can only be applied under the climate conditions for which they were www.hydrol-earth-syst-sci.net/16/3945/2012/ ...
exemplar - ESPACE Project
exemplar - ESPACE Project

... planning. The strategy – “Planning in a Changing Climate” aims to influence the philosophy and practice of spatial planning by recommending how adaptation to climate change can be incorporated. b. Influence on policies A key debate at the 2nd ESPACE Conference in November 2005 “Blueprint for a Chang ...
Evaluating sun–climate relationships since the Little Ice Age
Evaluating sun–climate relationships since the Little Ice Age

... perhaps 9[7>C[ Solar variability may account for part of this warming which\ during the past 249 years\ generally tracks ~uctuating solar activity levels[ While increases in greenhouse gas concentrations are widely assumed to be the primary cause of recent climate change\ surface temperatures nevert ...
From Words to Facts: Acting on climate change
From Words to Facts: Acting on climate change

... Central America little contributes to climate change, but it [ill endure some of its most negative conseUuences The global [arming [ill increase the magnitude and freUuency of extreme climate events such as droughts that [ill impact the region This is [hy during the upcoming CO4 that [ill be hel ...
Climate Change Planning in Alaska`s National Parks
Climate Change Planning in Alaska`s National Parks

... Many areas will experience drying conditions despite increased precipitation, due to higher temperature and increased rates of evapotranspiration. More freezing rain events affect foraging success and survival of wildlife, travel safety, and utility transmission. Avalanche hazards increase in some a ...
Rapid thinning of the late Pleistocene Patagonian Ice Sheet
Rapid thinning of the late Pleistocene Patagonian Ice Sheet

Yurok Tribe and Climate Change:
Yurok Tribe and Climate Change:

... “The term Climate Change is used to refer to changes in the Earth's climate. In the most general sense, it can be taken to mean changes over all timescales and in all of the components of climate, including precipitation and clouds as well as temperature. Climate changes can be caused both by natura ...
COP21 at Paris: What to expect
COP21 at Paris: What to expect

... 2015 has been an unexpectedly positive year for climate change efforts, as the long-floundering U.N. process has finally begun to deliver some of what is needed. Make no mistake: We are still on track to overshoot the limits of our planet’s ability to absorb the fossil pollutants we are pumping into ...
Assessing the Impacts of Climate Change on Urban Forests in the
Assessing the Impacts of Climate Change on Urban Forests in the

... Climate change creates both challenges and opportunities for sustaining urban forests. The recent Washington Climate Change Impacts Assessment projected sea level rise, temperature increase, and change in precipitation for Washington State (UW-CIG, 2009). Little research, however, has been done to g ...
Building Place-Based Climate Change Education
Building Place-Based Climate Change Education

... effort focused on gathering information and conducting social-science research that could be used to develop an interagency communication strategy to more effectively communicate about climate change across agency boundaries. ...
StudyQuestions4
StudyQuestions4

... • If a "100-year flood" happened last year, could another one happen this year on the same river? Explain. 5. How can human activities cause the frequency of flooding to get worse and increase the size of floods at the same time? 6. How can human activities also increase the potential costs and cons ...
Report - UNHCR
Report - UNHCR

... (e.g., shared waters) or the sudden expansion of shared or undemarcated resources. In the latter category is the possibility of exploiting newly accessible natural resource deposits and transport routes through the Arctic. 19. Of these five channels, the first is well researched and documented, incl ...
Modelling the response of glaciers to climate warming
Modelling the response of glaciers to climate warming

Glaciers and climate change in the Karakoram
Glaciers and climate change in the Karakoram

... From: The Economist, June 2008: “…Mr Hasnain estimates that Himalayan glaciers will be gone in 20-30 years. That would leave many great rivers depending on seasonal rainfall. According to the IPCC. this may be the fate of the Indus…by 2035…” The Guardian 2008 “…The problem is perhaps most acute in A ...
NASA faked the moon landing—therefore
NASA faked the moon landing—therefore

... who espouse science denial is not entirely surprising because if an overwhelming scientific consensus cannot be accepted as the result of researchers independently converging on the same evidence-based view, then the very existence of the consensus calls for an alternative explanation. The ideation ...
Global food security under climate change
Global food security under climate change

... improvements will be less pronounced and are expected to set in later. Over the next 15 years, for instance, the prevalence of undernourishment will decline less than in other regions, from ⬇33% to a still worrisome 21%, as significant constraints (soil nutrients, water, infrastructure, etc.) will l ...
the results of the scientific congress
the results of the scientific congress

... society and economy have developed and thrived. These indicators include global mean surface temperature, sea-level rise, global ocean temperature, Arctic sea ice extent, ocean acidification, and extreme climatic events. With unabated emissions, many trends in climate will likely accelerate, leading ...
The language of climate change adaptation
The language of climate change adaptation

- The University of Liverpool Repository
- The University of Liverpool Repository

... argued that two-and-a-half planets would be maintain the lifestyle of the average Merseysider. It argued that the best way to shrink the city’s ecological footprint would be to focus on the areas of greatest pressure, including transport, waste, water treatment, and energy use, and recomended an aw ...
Plants and climate change: complexities and
Plants and climate change: complexities and

... ‘To achieve the ultimate objective of the Convention to stabilize greenhouse gas concentration in the atmosphere at a level that would prevent dangerous anthropogenic interference with the climate system, we shall, recognizing the scientific view that the increase in global temperature should be bel ...
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Global warming



Global warming and climate change are terms for the observed century-scale rise in the average temperature of the Earth's climate system and its related effects.Multiple lines of scientific evidence show that the climate system is warming. Although the increase of near-surface atmospheric temperature is the measure of global warming often reported in the popular press, most of the additional energy stored in the climate system since 1970 has gone into ocean warming. The remainder has melted ice, and warmed the continents and atmosphere. Many of the observed changes since the 1950s are unprecedented over decades to millennia.Scientific understanding of global warming is increasing. The Intergovernmental Panel on Climate Change (IPCC) reported in 2014 that scientists were more than 95% certain that most of global warming is caused by increasing concentrations of greenhouse gases and other human (anthropogenic) activities. Climate model projections summarized in the report indicated that during the 21st century the global surface temperature is likely to rise a further 0.3 to 1.7 °C (0.5 to 3.1 °F) for their lowest emissions scenario using stringent mitigation and 2.6 to 4.8 °C (4.7 to 8.6 °F) for their highest. These findings have been recognized by the national science academies of the major industrialized nations.Future climate change and associated impacts will differ from region to region around the globe. Anticipated effects include warming global temperature, rising sea levels, changing precipitation, and expansion of deserts in the subtropics. Warming is expected to be greatest in the Arctic, with the continuing retreat of glaciers, permafrost and sea ice. Other likely changes include more frequent extreme weather events including heat waves, droughts, heavy rainfall, and heavy snowfall; ocean acidification; and species extinctions due to shifting temperature regimes. Effects significant to humans include the threat to food security from decreasing crop yields and the abandonment of populated areas due to flooding.Possible societal responses to global warming include mitigation by emissions reduction, adaptation to its effects, building systems resilient to its effects, and possible future climate engineering. Most countries are parties to the United Nations Framework Convention on Climate Change (UNFCCC),whose ultimate objective is to prevent dangerous anthropogenic climate change. The UNFCCC have adopted a range of policies designed to reduce greenhouse gas emissions and to assist in adaptation to global warming. Parties to the UNFCCC have agreed that deep cuts in emissions are required, and that future global warming should be limited to below 2.0 °C (3.6 °F) relative to the pre-industrial level.
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