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PPT file - Regional Climate Modeling Laboratory
PPT file - Regional Climate Modeling Laboratory

... something other than “tomorrow’s problem”  We are committed to a warming over the next 40 years regardless of what policy path we choose  Policy decisions today will affect global warming and associated environmental changes in the latter half of the 21st century and ...
Good Paris goal, bad Canadian target : King Weekly Sentinel : http
Good Paris goal, bad Canadian target : King Weekly Sentinel : http

... Canadian target), would cause a global average temperature change relative to pre-industrial times of 2.7 to 3.5 degrees. Canada's target was “only ahead of Kazakhstan, Australia, and Saudi Arabia which is a sad place to be as one of the top 10 emitters in the world” (Dr. Karen Farbridge, former May ...
Global warming and the Carbon Cycle
Global warming and the Carbon Cycle

... Early Warning signs from the Arctic: • The poles are heating faster than the rest of the earth ...
Slow-motion catastrophe Slow-motion catastrophe | ajc.com
Slow-motion catastrophe Slow-motion catastrophe | ajc.com

... from elevated water temperatures and disease, and entire island nations are poised to be swallowed by rising sea levels. The Arctic Climate Impact Assessment recently released by scientists from eight nations noted that winter temperatures in parts of the Arctic have risen by up to 7 degrees F, melt ...
Climate Change and Ozone Depletion
Climate Change and Ozone Depletion

... little time to deal with its harmful effects.  As a prevention strategy scientists urge to cut global CO2 emissions in half over the next 50 years. ...
ESYS 10 Introduction to Environmental Systems February 26
ESYS 10 Introduction to Environmental Systems February 26

... Observed temperature changes: are they due to anthropogenic forcing? Temperature increases can be due to: (1) Solar radiation changes (cools or warms) - 11year cycle 0.6 to 0.7 W/m2. All reconstructions indicate that the direct effect of variations in solar forcing over the 20th century was about 2 ...
What is climate change?
What is climate change?

... However, human activities are increasing the levels of methane being released into the atmosphere in several ways: - Industry – methane is produced during the production, processing, storage and distribution of natural gas - Increase in cattle rearing – cows naturally produce methane, but an increas ...
lecture 13 for 351 - Department of Atmospheric Science
lecture 13 for 351 - Department of Atmospheric Science

... the Milankovitch cycles • Eccentricity of the earth’s orbit happens on a cycle of about 100,000 years • Precession of earth’s axis has a 23,000 year ...
Climate change
Climate change

... However, human activities are increasing the levels of methane being released into the atmosphere in several ways: - Industry – methane is produced during the production, processing, storage and distribution of natural gas - Increase in cattle rearing – cows naturally produce methane, but an increas ...
What is climate change?
What is climate change?

... • These trap heat in the earths atmosphere – known as the greenhouse effect • Over time, there has been a considerable build up of greenhouse gases which scientists state is caused by human behavior ...
Strand 3 Multiple Choice Questions
Strand 3 Multiple Choice Questions

... 12. A business claims to be doing "everything possible" to reduce greenhouse gas emissions. Which company practice would cause a consumer to question this claim? A. The company purchases recycled paper products B. The building lights are triggered by motion C. The building is powered by geothermal ...
Creation care
Creation care

... • Over the last 40 years, the earth has been warming, mostly due to increased emissions of CO2 from burning fossil fuels • Seven thousand million tonnes of CO2 are emitted globally per annum • A warmer earth leads to a changing climate ...
Slide 1 - climateknowledge.org
Slide 1 - climateknowledge.org

... • More clouds mean more infrared to surface  warmer • More or less clouds? • Does this stabilize? • Water in all three phases essential to stable climate ...
The Carbon Cycle and Global Warming
The Carbon Cycle and Global Warming

... breathe and from burning fossil fuels Methane- comes from cattle as they digest their food. The gas also comes from fields where rice is grown in paddy fields. nitrous oxide - when plants die and rot, nitrous oxide is produced. Ozone- occurs naturally in the atmosphere. CFC’s ...
CASE STUDY - Climate change
CASE STUDY - Climate change

... environmental stress is holding back the efforts of the world’s poor to build a better life for themselves and their children. ...
climate change and south africa everyone can make a
climate change and south africa everyone can make a

... succulent Karoo where a high level of extinction is predicted Some predictions suggest that maize production in summer rainfall areas and fruit and cereal production in winter rainfall areas may be badly affected Commercial forestry is vulnerable to an increased frequency of wildfires and changes in ...
climate change and south africa
climate change and south africa

... succulent Karoo where a high level of extinction is predicted Some predictions suggest that maize production in summer rainfall areas and fruit and cereal production in winter rainfall areas may be badly affected Commercial forestry is vulnerable to an increased frequency of wildfires and changes in ...
Rapid accumulation of committed sea-level rise from global warming
Rapid accumulation of committed sea-level rise from global warming

... m assuming today’s trends continue or to 2.1 m under an aggressive emissions cutting and atmospheric carbon dioxide removal scenario. Both scenarios threaten the future viability of many hundreds of coastal municipalities in the United States alone, but the low emissions path would likely spare hund ...
Climate Change
Climate Change

... and accelerating ever since, the human consumption of fossil fuels has elevated CO2 levels from a concentration of ~280 ppm (parts per million) in the atmosphere to more than 380 ppm today. • These increases are projected to reach more than 560 ppm before the end of the 21st century. It is known tha ...
Climate Change - American Museum of Natural History
Climate Change - American Museum of Natural History

... 3. Making a Difference What can you do to conserve energy and reduce CO2 in the atmosphere? There are many ways to reduce you and your family’s energy use. Switch to compact fluorescent light bulbs, install energyefficient appliances, and turn off appliances and electronics when not in use. Take sho ...
BOPP_WP17_highlights_+
BOPP_WP17_highlights_+

... Impact of climate change on regional carbon uptake (gC/m2/°C) ...
www.dec.ny.gov/docs/administration_pdf/0807climchange.pdf
www.dec.ny.gov/docs/administration_pdf/0807climchange.pdf

... Scientists predict that this higher sea level could double the likelihood of a storm that produces a 100year flood in New York City. Rising sea waters may also increase saltwater intrusion into drinking water supplies near the coast, and could inundate tidal marshes and sensitive shallow habitats th ...
Belanger – Earth climate past present future – week 1
Belanger – Earth climate past present future – week 1

... 5 key elements and their interrelationships: 1. Atmosphere 2. Hydrosphere 3. Biosphere 4. Cryosphere 5. Lithosphere The sun is key to linking all these through water. Feedbacks: positive and negative 1. Water vapor 2. Ice albedo 3. Radiation feedback ...
No Slide Title
No Slide Title

... in terms of natural climate variability •Recent surface warming is largely consistent with simulations of the effects of anthropogenic ...
Climate Change - Englishcenter
Climate Change - Englishcenter

... a ___ A change in the Earth’s orbit can start or finish an ice age. b ___ People can never change the Earth’s climate. c ___ Methane and carbon dioxide are greenhouse gases. d ___ Ice is now melting in glaciers in different parts of the world. e ___ Monsoon rains will be shorter and less heavy ...
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Climate change feedback



Climate change feedback is important in the understanding of global warming because feedback processes may amplify or diminish the effect of each climate forcing, and so play an important part in determining the climate sensitivity and future climate state. Feedback in general is the process in which changing one quantity changes a second quantity, and the change in the second quantity in turn changes the first. Positive feedback amplifies the change in the first quantity while negative feedback reduces it.The term ""forcing"" means a change which may ""push"" the climate system in the direction of warming or cooling. An example of a climate forcing is increased atmospheric concentrations of greenhouse gases. By definition, forcings are external to the climate system while feedbacks are internal; in essence, feedbacks represent the internal processes of the system. Some feedbacks may act in relative isolation to the rest of the climate system; others may be tightly coupled; hence it may be difficult to tell just how much a particular process contributes. Forcings, feedbacks and the dynamics of the climate system determine how much and how fast the climate changes. The main positive feedback in global warming is the tendency of warming to increase the amount of water vapor in the atmosphere, which in turn leads to further warming. The main negative feedback comes from the Stefan–Boltzmann law, the amount of heat radiated from the Earth into space changes with the fourth power of the temperature of Earth's surface and atmosphere.Some observed and potential effects of global warming are positive feedbacks, which contribute directly to further global warming. The Intergovernmental Panel on Climate Change's (IPCC) Fourth Assessment Report states that ""Anthropogenic warming could lead to some effects that are abrupt or irreversible, depending upon the rate and magnitude of the climate change.""
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