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Climate Change?
Climate Change?

... greenhouse gas emissions are created by land clearing • Forests absorb carbon dioxide from the air • Burnt and rotting timber gives off greenhouse gases ...
Global warming in context - NIS Aktobe Global Perspectives
Global warming in context - NIS Aktobe Global Perspectives

... of fuels increase nitric acid that rapidly converts into soluble nitrogen that are washed out by rain stimulating plant growth and increasing NPP. Land use management- in northern and mid-latitudes forests where logging occurs there is evidence of rapid re growth. Although this year-year increase in ...
Document
Document

... The preceding comment does not disqualify O’Brien’s observations but it does mean that his comments should be read within a certain context and for a certain effect. In response to these skeptics, I have two main lines of argument. First, the Intergovernmental Panel on Climate Change (IPCC) has issu ...
Climate Change Importance and Implication on Conservation
Climate Change Importance and Implication on Conservation

... The burning of fossil fuels for transpiration and industrial purposes has typically been regarded as the chief contributors to the emissions of greenhouse gases and climate change. However, in recent past, FAO (2006) has highlighted a crucial role of the farm animal production sector on global warm ...
Chapter 9 Air: Climate and Pollution
Chapter 9 Air: Climate and Pollution

... review scientific evidence on the causes and likely effects of climate change. • In 2007, the IPCC issued its 4th Assessment Report. The conclusion is a 90% certainty that observed climate change is caused by human activity. • Subsequent reports raised that to a 99% certainty. ...
21st century climate change in West Africa
21st century climate change in West Africa

... Sahelian 21st century Precipitation anomalies ...
ppt
ppt

...  Ice-Albedo Effect: Cooling  Cooling causes more snow  Snow reflects sunlight Ground cools, radiates little IR Atmosphere cools Snow doesn’t melt More precipitation falls as snow  Feedback Mechanism: Ocean absorbs CO2  CO2 builds up over icy world, warming starts  “Ice House Earth” ...
Presentation Title, Arial Regular 29pt Sub title
Presentation Title, Arial Regular 29pt Sub title

... More heat-related deaths for people aged over 65 1115 deaths per year at present in the 5 largest capital cities, increasing to 2300-2500 per year by 2020 ...
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... and storms may impact the fishing industry in southeast Alaska. However, since fisheries in other parts of the world may be impacted also, it is hard to predict the relative competitiveness of Alaska fisheries. Tourism is a major source of revenue in southeast Alaska, and longer and warmer summers m ...
Equilibrium response of a climate model when feedbacks are
Equilibrium response of a climate model when feedbacks are

... They based their assessment on the results from two global climate models, one with a relatively low sensitivity to CO2 doubling (PCM), and the other with a relatively high sensitivity (HADCM3). They looked at outcomes in California for two scenarios. One is “business as usual” scenario, that envisa ...
A Scientific Guide to the `Skeptics Handbook`
A Scientific Guide to the `Skeptics Handbook`

... Skeptics claim that much of the measured global warming is due to weather stations positioned near air conditioners and car parks. We know this isn’t true for several reasons. For starters, we can compare temperatures from good weather stations to the poorly sited weather stations. Both good and bad ...
Modeling and Predicting Climate Change
Modeling and Predicting Climate Change

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The New York Times 18th May 2050
The New York Times 18th May 2050

... climate change recognition, the research also represents a new mechanism for analyzing events in world history. The paper reports on the near coincidence of major tidal fluctuations with worldwide phenomena, including the Little Ice Age of 1400 A.D. to 1700 A.D., major dust layers in Minnesota lake ...
Climate Change Floods and Droughts
Climate Change Floods and Droughts

... from four to eight inches, an increase in precipitation by approximately one percent, changes in the ecosystem altering the amount of snow in the north, a rise from five to ten percent in rainfall, and summers becoming increasingly dry while ice in the Artic Ocean decreases. Climate change can bring ...
Climate Change & Agriculture - Agricultural Marketing Policy Center
Climate Change & Agriculture - Agricultural Marketing Policy Center

... change and are more cost effective than adaptation ...
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chapter19

... 1. Considerable scientific evidence indicates that the earth’s atmosphere is warming, mostly because of human activities, and that this is likely to lead to significant climate disruption during this century that could have severe and long-lasting harmful ...
Water vapor feedback
Water vapor feedback

... Uncertainty about the future: This plot shows the upper and lower limits of the global mean warming over the coming century predicted by current GCM simulations. ...
Knutti - Institute for Atmospheric and Climate Science
Knutti - Institute for Atmospheric and Climate Science

... NATURE|Vol 458|30 April 2009 ...
Global warming on Jupiter
Global warming on Jupiter

... poles will become cooler. Average temperature at some latitudes could change by as much as 5.5° Celsius (Marcus 2006). In other words, what is predicted is not global warming on Jupiter but a change in the distribution of heat with the equator getting hotter and the poles cooling. It's also worth me ...
Met 112: Final Exam Study Guide
Met 112: Final Exam Study Guide

... and sea-ice, carbon cycle, atmospheric chemistry, etc) 3. What is the approach for you to know the future climate? (climate modeling) 4. Why Ocean is critical in climate system? ...
Global Climate Change International Collaborations through STEM
Global Climate Change International Collaborations through STEM

... As scientists have accumulated evidence and strengthened their understanding of climate change, the public has become greatly divided (IPCC, 2007; National Research Council, 2010)  In Pew Research Center poll (2009), 49% of nonscientists and 84% of scientists agreed with the statement, “the earth i ...
Document
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... Global surface temperature (Ts) depends on three main factors: a) Solar flux b) Albedo (on Earth mostly clouds) c) Greenhouse Effect (CO2, H2O , CH4, O3 etc.) • We can calculate Te from the “Energy balance equation” and add the greenhouse warming: Ts = Te + ∆Tg ...
Y11GeUC7 Fragile PPwk26 - the InterHigh IGCSE Geography
Y11GeUC7 Fragile PPwk26 - the InterHigh IGCSE Geography

... delta is then not able to grow rice once salt water has infiltrated it. The precipitation brought by the Monsoons and the spring melt from the Himalayas is less reliable than before, which means sometimes there are floods when more turns up that expected, while at other times there are equally unexp ...
Chap 6 Forcing and feedback
Chap 6 Forcing and feedback

... Define: RF = ΔEin - ΔEout : positive radiative forcings warm the planet Ex 1: How much does Ein change if S increases by 5%? Answer: Ein = 1360(1-0.3)/4 = 238; Ein=1360*1.05*(1-0.3)/4=250; change = 12 W/m2. Note: time independent Ex 2: What increase in solar constant would cause a radiative forcing ...
Preventing dangerous climate change
Preventing dangerous climate change

... place over the last 50 years. Whilst the extent of climate change is often expressed in a single figure – global temperature – the effects of climate change (such as temperature, precipitation and the frequency of extreme weather events) will vary greatly from place to place. Increasing atmospheric ...
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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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