PowerPoint 프레젠테이션
... Date : 25 May, 2007 Venue: National Fisheries Research & Development Institute ...
... Date : 25 May, 2007 Venue: National Fisheries Research & Development Institute ...
now - Fiona`s Red Kite
... A presentation by Fiona Hewer MSc FRMetS for Henley College 13 February 2008 ...
... A presentation by Fiona Hewer MSc FRMetS for Henley College 13 February 2008 ...
climate models
... may have increased lately Current estimate of forcing: very small Note: Evidence is very weak! ...
... may have increased lately Current estimate of forcing: very small Note: Evidence is very weak! ...
The Haitian Scientific Society (HSS)
... BRUTUS - Section 3 Where does Global Warming come from? Pierre-Richard Cornely – Section 3 The Earth's climate changes in response to external forces, including variations in its orbit around the Sun (orbital forces), changes in solar luminosity, volcanic eruptions, and atmospheric greenhouse gas co ...
... BRUTUS - Section 3 Where does Global Warming come from? Pierre-Richard Cornely – Section 3 The Earth's climate changes in response to external forces, including variations in its orbit around the Sun (orbital forces), changes in solar luminosity, volcanic eruptions, and atmospheric greenhouse gas co ...
WORD - war changes climate
... the earth's climate system must surely be the greatest scientific challenge yet to be faced by humankind. It is a worthy banner under which the nations of the world can unite" (IPCC, Working Group I, p. 328). Certainly not a bad thing for science. The 1992 Earth Summit resulted in an unprecedented ...
... the earth's climate system must surely be the greatest scientific challenge yet to be faced by humankind. It is a worthy banner under which the nations of the world can unite" (IPCC, Working Group I, p. 328). Certainly not a bad thing for science. The 1992 Earth Summit resulted in an unprecedented ...
- The Population Policy of South Africa
... distribution of weather events around an average (for example, greater or fewer extreme weather events). Climate change may be limited to a specific region, or may occur across the whole Earth2. Priority concerns for Climate Change in South Africa. A few areas of particular concern where global clim ...
... distribution of weather events around an average (for example, greater or fewer extreme weather events). Climate change may be limited to a specific region, or may occur across the whole Earth2. Priority concerns for Climate Change in South Africa. A few areas of particular concern where global clim ...
2.6.4bcd Ocean Acidification and Sea Level Rise Piper
... Sea Level and Climate change Between 1870 and 2004, Global average sea levels have risen _______cm. _________ main factors contributed to observed sea level rise. The first is thermal expansion: as ocean water warms, it ______________. The second is from the contribution of land-based ice du ...
... Sea Level and Climate change Between 1870 and 2004, Global average sea levels have risen _______cm. _________ main factors contributed to observed sea level rise. The first is thermal expansion: as ocean water warms, it ______________. The second is from the contribution of land-based ice du ...
Studying Climate Change: Proxy Indicators
... Relative changes in precipitation (in percent) for the period 2090–2099, relative to 1980–1999. Values are multi-model averages based on the SRES A1B scenario for December to February (left) and June to August (right). White areas are where less than 66% of the models agree in the sign of the change ...
... Relative changes in precipitation (in percent) for the period 2090–2099, relative to 1980–1999. Values are multi-model averages based on the SRES A1B scenario for December to February (left) and June to August (right). White areas are where less than 66% of the models agree in the sign of the change ...
A Christian Apporach to Climate Change
... impacts of increasing land temperatures, rising sea levels, and a change in the frequency of extreme climatic events. ...
... impacts of increasing land temperatures, rising sea levels, and a change in the frequency of extreme climatic events. ...
Regionalkonferenz der Metropolregion Hamburg
... • avoiding man-made changes („mitigation“) – this has different dimensions, namely avoiding elevated levels of GHG concentrations by reduced emissions; by intensified sinks; by geo-engineering the global albedo, or regional and local conditions. • adapting to man-made changes („adaptations“) of clim ...
... • avoiding man-made changes („mitigation“) – this has different dimensions, namely avoiding elevated levels of GHG concentrations by reduced emissions; by intensified sinks; by geo-engineering the global albedo, or regional and local conditions. • adapting to man-made changes („adaptations“) of clim ...
Bridging The Divide Between Climate Change and Human
... to be flooded every year due to sea-level rise by the 2080s. Those denselypopulated and low-lying areas where adaptive capacity is relatively low, and which already face other challenges such as tropical storms or local coastal subsidence, are especially at risk. The numbers affected will be largest ...
... to be flooded every year due to sea-level rise by the 2080s. Those denselypopulated and low-lying areas where adaptive capacity is relatively low, and which already face other challenges such as tropical storms or local coastal subsidence, are especially at risk. The numbers affected will be largest ...
What Climate Change Means for Florida
... has warmed more than one degree (F) during the last century. The sea is rising about one inch every decade, and heavy rainstorms are becoming more severe. In the coming decades, rising temperatures are likely to increase storm damages, harm coral reefs, increase the frequency of unpleasantly hot day ...
... has warmed more than one degree (F) during the last century. The sea is rising about one inch every decade, and heavy rainstorms are becoming more severe. In the coming decades, rising temperatures are likely to increase storm damages, harm coral reefs, increase the frequency of unpleasantly hot day ...
Climate Change LECTURE
... Climate Change LECTURE Following on the success of the climate change lecture series during 2007 and 2008 the Environmental Protection Agency will host a number of occasional climate change lectures in autumn 2008 and spring 2009. The occasional lectures are aimed at providing updates from the scien ...
... Climate Change LECTURE Following on the success of the climate change lecture series during 2007 and 2008 the Environmental Protection Agency will host a number of occasional climate change lectures in autumn 2008 and spring 2009. The occasional lectures are aimed at providing updates from the scien ...
IEAGHG Information Paper; 2013-IP5: Lord Nicholas Stern Identifies... Climate Action
... By Stern’s own admission, the Stern Review greatly underestimated climate change’s risks and impacts. “Emissions are at the top or above the projections we talked about six or seven years ago. Some effects are coming through faster,” he said. “We didn’t say enough about the interactions between clim ...
... By Stern’s own admission, the Stern Review greatly underestimated climate change’s risks and impacts. “Emissions are at the top or above the projections we talked about six or seven years ago. Some effects are coming through faster,” he said. “We didn’t say enough about the interactions between clim ...
Chapter 23: The Atmosphere, Climate and Global Warming
... can make to the threat of global warming: – Adapt: Learn to live with future global climatic change. – Mitigate: Work to reduce emissions of ...
... can make to the threat of global warming: – Adapt: Learn to live with future global climatic change. – Mitigate: Work to reduce emissions of ...
Mechanisms of Quaternary climate change: Stability of warm phases
... Figure 1: Recent results from the LOTRED-South America 2k effort. Climate variations in the Northern Patagonian Andes during the past four centuries. a) Summer (Nov - Mar) temperature changes (expressed as departure from calibration period 1908-2003) inferred from a regional network of Fitzroya cupr ...
... Figure 1: Recent results from the LOTRED-South America 2k effort. Climate variations in the Northern Patagonian Andes during the past four centuries. a) Summer (Nov - Mar) temperature changes (expressed as departure from calibration period 1908-2003) inferred from a regional network of Fitzroya cupr ...
Detection and attribution of climate change for the Baltic Sea Region
... • Example: N European warming trend “April to July” as part of the seasonal cycle. • It does not imply that the trend will continue into the future (beyond the time scale of serial correlation). • Example: Usually September is cooler than July. ...
... • Example: N European warming trend “April to July” as part of the seasonal cycle. • It does not imply that the trend will continue into the future (beyond the time scale of serial correlation). • Example: Usually September is cooler than July. ...
Climate Change and Hawaii
... The waters surrounding Hawaii contain coral reefs that are home to thousands of species and provide estimated economic benefits of $360 million per year. Rising sea temperatures threaten these amazing ecosystems: coral bleaching and disease outbreaks occur more frequently with high temperatures, and ...
... The waters surrounding Hawaii contain coral reefs that are home to thousands of species and provide estimated economic benefits of $360 million per year. Rising sea temperatures threaten these amazing ecosystems: coral bleaching and disease outbreaks occur more frequently with high temperatures, and ...
Derivation of the temperature increase equation: ΔT = 1.66 ln (C/Co)
... surface about 33oC warmer than it would otherwise be. How much warming does carbon dioxide itself contribute to the current surface temperature of the Earth? We can calculate the CO2 flux density (F) at concentration C in the current atmosphere using Equation 16, F = 5.35 ln C, from Section 2 above. ...
... surface about 33oC warmer than it would otherwise be. How much warming does carbon dioxide itself contribute to the current surface temperature of the Earth? We can calculate the CO2 flux density (F) at concentration C in the current atmosphere using Equation 16, F = 5.35 ln C, from Section 2 above. ...
Global Warming and Its Effect on the Arctic
... oceans • The oceans density, currently at 1.03*10^3, is expected to decrease which could shut down the deep ocean currents, such as the Thermohaline Circulation. Since this current modifies Europe's weather, if it shuts down, Europe could go into an ice age. • With more water in liquid state, more w ...
... oceans • The oceans density, currently at 1.03*10^3, is expected to decrease which could shut down the deep ocean currents, such as the Thermohaline Circulation. Since this current modifies Europe's weather, if it shuts down, Europe could go into an ice age. • With more water in liquid state, more w ...
Climate Change: Its Causes, Effects and Control
... 7. Archaeological/historical/oral evidence: These offer insight into climate changes in the past; how changes in climate have been linked with the rise and fall of some great civilizations. 4. Causes of climate change According to Speelman (2009), climate change may either be human-induced, or a nat ...
... 7. Archaeological/historical/oral evidence: These offer insight into climate changes in the past; how changes in climate have been linked with the rise and fall of some great civilizations. 4. Causes of climate change According to Speelman (2009), climate change may either be human-induced, or a nat ...
Coastal systems and low- lying areas
... • RSLR can be much larger than projected GMSLR. • Non-climate change local processes include subsidence, glacial isostatic adjustment, sediment transport, coastal development. • Changes in storms & associated storm surges may further contribute to sea level extremes. • Under present levels of global ...
... • RSLR can be much larger than projected GMSLR. • Non-climate change local processes include subsidence, glacial isostatic adjustment, sediment transport, coastal development. • Changes in storms & associated storm surges may further contribute to sea level extremes. • Under present levels of global ...
iced - clivar
... The marine cryosphere and its interactions with high latitude oceans and atmosphere What will be the nature of changes in sea-ice distribution and mass balance in both polar regions in response to climate change and variability? ...
... The marine cryosphere and its interactions with high latitude oceans and atmosphere What will be the nature of changes in sea-ice distribution and mass balance in both polar regions in response to climate change and variability? ...
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.