Decision making and climate change
... a relatively poor use of resources. Adaptive measures that build in lower emission profiles have a better cost/benefit ratio for society. • Giving mitigation measures a higher priority than adaptation, in the absence of a global legal framework, still leaves municipalities and regions vulnerable to ...
... a relatively poor use of resources. Adaptive measures that build in lower emission profiles have a better cost/benefit ratio for society. • Giving mitigation measures a higher priority than adaptation, in the absence of a global legal framework, still leaves municipalities and regions vulnerable to ...
Intro_Clim_Sci_prelim_post
... perturbation (say, a change in greenhouse gas concentrations) is the change in net (down minus up) irradiance (solar plus long-wave in Wm-2) at the tropopause AFTER allowing for stratospheric temperatures to readjust to radiative equilibrium, but with surface and tropospheric temperatures and state ...
... perturbation (say, a change in greenhouse gas concentrations) is the change in net (down minus up) irradiance (solar plus long-wave in Wm-2) at the tropopause AFTER allowing for stratospheric temperatures to readjust to radiative equilibrium, but with surface and tropospheric temperatures and state ...
IntellBldgPart1_2009fin - University of Reading, Department of
... strength of absorption of infra-red radiation overlap of absorption with other gases lifetime in the atmosphere amount added over given period of time ...
... strength of absorption of infra-red radiation overlap of absorption with other gases lifetime in the atmosphere amount added over given period of time ...
2 x
... -There is a +trend in the mean duration of hailstone events in cont. Croatia, Počakal (2012) -But typical, standard climate models don't have those variables included yet - should be there! ...
... -There is a +trend in the mean duration of hailstone events in cont. Croatia, Počakal (2012) -But typical, standard climate models don't have those variables included yet - should be there! ...
Increasing the use and usability of participatory assessments
... • The 6-EAP target of a maximum 2 degrees global temperature increase should not be exceeded in the Sustainable Emission Pathway scenario • The rate of temperature increase per decade, proposed by WBGU, of 0.2 °C/decade could be added as an additional target • No other climate change targets have be ...
... • The 6-EAP target of a maximum 2 degrees global temperature increase should not be exceeded in the Sustainable Emission Pathway scenario • The rate of temperature increase per decade, proposed by WBGU, of 0.2 °C/decade could be added as an additional target • No other climate change targets have be ...
Slides
... energy supply, e.g. wind and nuclear • Growing new markets for insurance against losses from extreme weather • National and global greenhouse gas emissions reductions targets ...
... energy supply, e.g. wind and nuclear • Growing new markets for insurance against losses from extreme weather • National and global greenhouse gas emissions reductions targets ...
Global warming issues
... Human influence has been detected in warming of the atmosphere and the ocean, in changes in the global water cycle, in reductions in snow and ice, in global mean sea level rise, and in changes in some climate extremes. This evidence for human influence has grown since AR4. It is extremely likely tha ...
... Human influence has been detected in warming of the atmosphere and the ocean, in changes in the global water cycle, in reductions in snow and ice, in global mean sea level rise, and in changes in some climate extremes. This evidence for human influence has grown since AR4. It is extremely likely tha ...
Global warming issues - FBS-WP
... Human influence has been detected in warming of the atmosphere and the ocean, in changes in the global water cycle, in reductions in snow and ice, in global mean sea level rise, and in changes in some climate extremes. This evidence for human influence has grown since AR4. It is extremely likely tha ...
... Human influence has been detected in warming of the atmosphere and the ocean, in changes in the global water cycle, in reductions in snow and ice, in global mean sea level rise, and in changes in some climate extremes. This evidence for human influence has grown since AR4. It is extremely likely tha ...
Global Warming
... this century, and likely at least the past millennium •It is difficult to explain the recent surface warming in terms of natural climate variability •Recent surface warming is consistent with simulations of the effects of anthropogenic influence on climate ...
... this century, and likely at least the past millennium •It is difficult to explain the recent surface warming in terms of natural climate variability •Recent surface warming is consistent with simulations of the effects of anthropogenic influence on climate ...
Forest-climate interactions in an era of global change
... and the spread of invasive species—are affecting forests worldwide. Such changes threaten biodiversity and may exacerbate climate change. Understanding and predicting how forests are changing provides critical support for biodiversity conservation and climate protection. Dr. Anderson-Teixeira leads ...
... and the spread of invasive species—are affecting forests worldwide. Such changes threaten biodiversity and may exacerbate climate change. Understanding and predicting how forests are changing provides critical support for biodiversity conservation and climate protection. Dr. Anderson-Teixeira leads ...
What the 2007 Reports of the IPCC mean Gordon J. Aubrecht
... The global atmospheric concentration of methane has increased from a preindustrial value of about 715 ppb to 1732 ppb in the early 1990s, and was 1774 ppb in 2005. The atmospheric concentration of methane in 2005 exceeds by far the natural range of the last 650,000 years (320 to 790 ppb) as determi ...
... The global atmospheric concentration of methane has increased from a preindustrial value of about 715 ppb to 1732 ppb in the early 1990s, and was 1774 ppb in 2005. The atmospheric concentration of methane in 2005 exceeds by far the natural range of the last 650,000 years (320 to 790 ppb) as determi ...
Science of climate change
... The atmosphere is not behaving as models would predict. Climate is mainly influenced by the sun. A carbon dioxide rise has always come after a temperature increase not before. 8. Long-term data on hurricanes and arctic ice is too poor to assess trends. 9. Water vapour is the major greenhouse gas; co ...
... The atmosphere is not behaving as models would predict. Climate is mainly influenced by the sun. A carbon dioxide rise has always come after a temperature increase not before. 8. Long-term data on hurricanes and arctic ice is too poor to assess trends. 9. Water vapour is the major greenhouse gas; co ...
climate change
... weather patterns that are occurring because of an increase in the earth's average temperature. ...
... weather patterns that are occurring because of an increase in the earth's average temperature. ...
Politics and Greenhouse Climate Change
... ‘Most of the observed increase in global average temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations.’ ...
... ‘Most of the observed increase in global average temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations.’ ...
Global warming - u
... Two millennia of mean surface temperatures according to different reconstructions. ...
... Two millennia of mean surface temperatures according to different reconstructions. ...
Global Climate Change
... to human activities since 1750 and now far exceed previous levels • Carbon dioxide has increased by approximately 80% since 1970 ...
... to human activities since 1750 and now far exceed previous levels • Carbon dioxide has increased by approximately 80% since 1970 ...
climate extremes
... Changes in Radiation Absorbing Gases -- Increases may warm the lower troposphere and cool the stratosphere. • Carbon Dioxide and other Green House Gases • Gases such as methane, nitrous oxide, and chlorofluorocarbons combined, produce as large an effect as carbon dioxide but carbon dioxide gets mos ...
... Changes in Radiation Absorbing Gases -- Increases may warm the lower troposphere and cool the stratosphere. • Carbon Dioxide and other Green House Gases • Gases such as methane, nitrous oxide, and chlorofluorocarbons combined, produce as large an effect as carbon dioxide but carbon dioxide gets mos ...
Summary for Policy Makers
... • For the next two decades a warming of about 0.2°C per decade is projected for a range of SRES emission scenarios. • Even if the concentrations of all greenhouse gases and aerosols had been kept constant at year 2000 levels, a further warming of about 0.1°C per decade would be expected. • Earlier I ...
... • For the next two decades a warming of about 0.2°C per decade is projected for a range of SRES emission scenarios. • Even if the concentrations of all greenhouse gases and aerosols had been kept constant at year 2000 levels, a further warming of about 0.1°C per decade would be expected. • Earlier I ...
Weekly Sustainability News Summary May 22, 2015 Company Initiatives:
... that there’s going to be a breakthrough on the Republican side, and that we’ll finally achieve consensus to take action. Full Article: The Washington Post Global businesses must lead the way on climate action — Major business leaders will gather in Paris this week for the Business and Climate Summ ...
... that there’s going to be a breakthrough on the Republican side, and that we’ll finally achieve consensus to take action. Full Article: The Washington Post Global businesses must lead the way on climate action — Major business leaders will gather in Paris this week for the Business and Climate Summ ...
Diapositiva 1
... economic, demographic and cultural will of people. These models were named A1, A2, B1, B2. ...
... economic, demographic and cultural will of people. These models were named A1, A2, B1, B2. ...