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Lecture 1: Understanding the Greenhouse Lecture 1
Lecture 1: Understanding the Greenhouse Lecture 1

... Since the temperature of the earth varies with date, time of day, latitude, longitude and elevation, monitoring “Global Temperature” is highly problematic. The National Oceanic and Atmospheric Administration performs this function for the US. See www.noaa.gov Land, ship, buoy and satellite based sen ...
An introduction to climate change
An introduction to climate change

... Without trying to labour this point, we are changing it. Mankind is causing the globe to heat up. It would perhaps be useful to prefix ‘global warming’ and ‘climate change’ with ‘anthropogenic’ or ‘man-made’. The medieval warm period and little ice ages are examples of how regional climate in Europe ...
No immediate reason to expect another Ice Age.
No immediate reason to expect another Ice Age.

... record since 1860: 22% and falling. • Sunspots’ correlation with earth’s temps: 79% and rising for past decade. Argues for solar cause. • Could the “consensus” be wrong? ...
II. Current Stresses and Future Climate Impacts on Key Economic
II. Current Stresses and Future Climate Impacts on Key Economic

... mortality from insect outbreaks, probability of an increase of large fires, and changes caused by thawing of permafrost. The effects of a projected warming would depend critically on accompanying changes in precipitation. One of the characteristic features of the boreal forest is that insect outbrea ...
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... the tropical cyclone climate record to date, no firm conclusion can be made on this point. 2. No individual tropical cyclone can be directly attributed to climate change. 3. The recent increase in societal impact from tropical cyclones has largely been caused by rising concentrations of population a ...
Climate Change
Climate Change

... Finally atmospheric chemistry is considered in the 2007 report along with reflectivity changes on the Earth due to changing vegetation patterns ...
Circulation
Circulation

... equatorial Pacific. This is caused by oscillations in the atmospheric pressure systems in the Southern Hemisphere which results in: -Weakening of southwest trades wind leading to weak upwelling off the coast of Peru. This causes the presence of warm water, reversal of local climate, low primary prod ...
Global Warming Effects on Extreme Weathers
Global Warming Effects on Extreme Weathers

... sun heats the earth's atmosphere and its surface causing air and water to move around the planet. The result can be as simple as a slight breeze or as complex as the formation of a tornado ...
what is the right target for co2?: 350 ppm is a death sentence for
what is the right target for co2?: 350 ppm is a death sentence for

... too high to prevent the extinction of coral reefs (which can take no further warming, since most corals have died in the last 20 years from heat shock) and the disappearance of all low lying islands and coastlines where billions of people live. Even a target of 350 ppm is UNACCEPTABLE if we are to a ...
Source: http://climateprogress - Tearfund International Learning Zone
Source: http://climateprogress - Tearfund International Learning Zone

... headed to 1000 ppm” and Study: Water-vapor feedback is “strong and positive,” so we face “warming of several degrees Celsius”). That’s why it is such a big deal when the UK’s official provider of climate and weather-related analysis — located within the UK’s Ministry of Defence — starts telling it l ...
Climate Change and Cocoa Output: Evidence from CCR
Climate Change and Cocoa Output: Evidence from CCR

... are two closely related threats facing mankind (Human Induced). Climate change due to anthropogenic factors has shown that the globe is warming (Odingo, 2009, IPCC, 2007). Studies have shown that the trend is accelerating such that the average temperature is rising at 0.20C every decade (IPCC, 2007 ...
Diapositiva 1
Diapositiva 1

... ARCTIC Coburg Island and Pond Inlet, CA next picture ...
Brief Overview of Climate Change
Brief Overview of Climate Change

... Greenhouse gases are necessary to live as we know it, because they keep the planet's surface warmer than it otherwise would be. But, as the concentrations of these gases continue to increase in the atmosphere, the Earth's temperature is climbing above past levels. According to NOAA and NASA data, th ...
Global Warming Quiz
Global Warming Quiz

... 6. Rising temperatures allow mosquitoes to survive at higher altitudes, potentially bringing them to regions that lack population immunity. In addition, the transmission period for vector-borne diseases is increased with expanded warm seasons (source: World Health Organization) 7. Insurance companie ...
Climate Control and Ozone Depletion
Climate Control and Ozone Depletion

... – CO2, CH4, and N2O emissions higher – Main sources: agriculture, deforestation, and burning of fossil fuels • Correlation of rising CO2 and CH4 with rising global temperatures ...
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... Climate change is occurring far faster than even the worst predictions of the UN's Nobel Prize-winning scientific panel on climate change foresaw, Al Gore warned. New evidence shows "the climate crisis is significantly worse and unfolding more rapidly than those on the pessimistic side of the IPCC p ...
Global Warming: Will Human-Induced Climate Change Destroy the
Global Warming: Will Human-Induced Climate Change Destroy the

... Global warming may make the sea level become higher. Warmer weather makes glaciers melt. Some melting glaciers add more water to the ocean. Warmer temperatures also make water expand. When water expands in the ocean, it takes up more space and the level of the sea rises. A 2℃ increase in earth's ave ...
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... ...
Climate Change through time
Climate Change through time

... L.O. To describe how the earth’s climate has changed through time. ...
20090831_Analysis_Climate_Change_India
20090831_Analysis_Climate_Change_India

... • The process of warming by these greenhouse gases is well known, simple, and easily quantified. • The response of the Earth to this warming is complex. ...
17.1 Structure of the Atmosphere
17.1 Structure of the Atmosphere

... - At sea level, there is 1 atm of pressure. (this is all the gas molecules are above your head weighing down on you) ...
Top Level Figure Choices
Top Level Figure Choices

... Global Climate Change Impacts in the United States How has climate already changed? How is it likely to change in the future? How is climate change affecting us now where we live and work? ...
PowerPoint - Columbia University
PowerPoint - Columbia University

... GHGs & ice sheet area, as feedbacks. 2. Chief instigator of climate change was earth orbital change, a very weak forcing. 3. Climate on long time scales is very sensitive to even small forcings. 4. Human-made forcings dwarf natural forcings that drove glacial-interglacial climate change. 5. Humans n ...
Global warming and poverty
Global warming and poverty

... (MDGs) for poverty reduction unachievable. Industrialized countries must lead the switch from polluting fossil-fuel based energy systems to clean energy – they have the biggest historical and present share of emissions, the best investment possibilities, and a large, highly skilled workforce. The ne ...
Warming climate drives human conflict
Warming climate drives human conflict

... Floods and drought also have an effect, although it is smaller than that of temperature, the researchers report. And the effects are apparent worldwide, in developed and developing countries. “The level of consistency in how people are responding was surprising to ...
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Instrumental temperature record



The instrumental temperature record shows fluctuations of the temperature of earth's climate system. Initially the instrumental temperature record only documented land and sea surface temperature, but in recent decades instruments have also begun recording ocean temperature. Data is collected from thousands of meteorological stations around the globe and through satellite observations. The longest-running temperature record is the Central England temperature data series, that starts in 1659. The longest-running quasi-global record starts in 1850.
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