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Lecture #23 - chem.uwec.edu
Lecture #23 - chem.uwec.edu

... as well properties the energy the climate system. These changes are and expressed terms… of radiative as Aerosols, landinuse forcing,2 which is used to compare how a range of human and natural factors drive warming or cooling influences on global climate. Since the TAR, new observations and related ...
Assessing Scientific Knowledge about Climate Change
Assessing Scientific Knowledge about Climate Change

... Director, NZ Climate Change Centre; Chief Scientist (Climate), NIWA; Adjunct Professor, Climate Change Research Institute, VUW. Work has now begun on the IPCC's Fifth Assessment, due for completion in 2014. This presentation will summarise significant findings from the IPCC's Fourth Assessment compl ...
climate extremes
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 ...
Língua Inglesa - Portal Sigma – Centro Educacional
Língua Inglesa - Portal Sigma – Centro Educacional

... 0.76° C since 1850. Most of the warming that has occurred over the last 50 years is very likely to have been caused by human activities. In its Fourth Assessment Report (AR4), published in 2007, the intergovernmental Panel on Climate Change (IPCC) project that, without further action to reduce green ...
Global Climate Change: New Timelines
Global Climate Change: New Timelines

... •Carbon dioxide increased by 1/3 since 1750 because of the burning fossil fuels (80%) and deforestation (20%) –Fate: 40% in atmosphere, 35% in land and 25% in ocean •The rate of increase is 100-1000 times faster than Nature can change CO2 ...
Climate Sensitivity - Earth and Environmental Sciences
Climate Sensitivity - Earth and Environmental Sciences

... the radiative forcing responsible for the climate change. Radiative forcing is the change in energy balance (in and out) at the Earth's surface. In this case we will use three known past examples of climate change to predict a forth – our future. We know that 20,000 years ago there were large ice sh ...
The current causes of climate change: the human causes
The current causes of climate change: the human causes

... changes in climate, including average temperature and precipitation. ...
Atmospheric circulation patterns in climate change
Atmospheric circulation patterns in climate change

... local circulation patterns, and are highly uncertain. In this talk I will review recent work from two projects investigating how regional changes to temperatures at the Earth's lower boundary can affect atmospheric circulation patterns, on timescales ranging from days to centuries. The first examine ...
A Safe Landing for the Climate (Chapter 2)
A Safe Landing for the Climate (Chapter 2)

... • Greenhouse gases are gases in an atmosphere that absorb and emit radiation within the thermal infrared range. This process is the fundamental cause of the greenhouse effect. Common greenhouse gases in the Earth’s atmosphere include water vapor, CO², methane, nitrous oxide, and ozone. ...
The contains tools to better understand and communicate climate science.
The contains tools to better understand and communicate climate science.

... AMERICAN CHEMICAL SOCIETY ...
Why are global temperatures changing? File
Why are global temperatures changing? File

... thought to have negative effects. ...
U3A-ClimChange01 4442KB Oct 07 2012
U3A-ClimChange01 4442KB Oct 07 2012

... assesses the most recent scientific, technical and socio-economic information produced worldwide relevant to the understanding of climatic change. It does not conduct any research nor does it monitor climate related data or parameters • Currently 195 countries are members ...
Headline goes here
Headline goes here

... WHAT IS THE GREENHOUSE EFFECT? ...
Intro/review to climate change webquest
Intro/review to climate change webquest

... Select one of them that interests you. 15. The technology I selected is __________________________________________ 16. Describe/ explain how the technology you selected works __________________________________________________________________________________________ __________________________________ ...
Unit_3-Session_2-Modern_Climate_change
Unit_3-Session_2-Modern_Climate_change

... Concentrations of CO2, N2O, CH4 (“Greenhouse Gases”) have increased dramatically over last 150 yrs. ...
Energy production outline
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... Simple and complex modelling: The kinetic theory of gases is a simple mathematical model that produces a good approximation of the behaviour of real gases. Scientists are also attempting to model the Earth’s climate, which is a far more complex system. Advances in data availability and the ability t ...
Climate Change Science
Climate Change Science

... change – no single solution, but needs major changes in human behaviour 3. Future climate change (in the next few decades) is inevitable – we need to start preparing now ...
power point - Altair-PYP-Exhibition-2010
power point - Altair-PYP-Exhibition-2010

... Ocean Current The Earth Tilt Meteorites Continental Drifts ...
Global Warming, the End of Life as We Know It?
Global Warming, the End of Life as We Know It?

... adaptation and mitigation” – This agency does NOT carry out research or monitor climate data – The basic assessments made are on peer reviewed and published scientific/ technical literature. – Divided into three Working Groups and a Task Force – Getting ready to release their Fourth Assessment Repor ...
Headline Statements from the Summary for
Headline Statements from the Summary for

... Understanding the Climate System and its Recent Changes Human influence on the climate system is clear. This is evident from the increasing greenhouse gas concentrations in the atmosphere, positive radiative forcing, observed warming, and understanding of the climate system. Climate models have impr ...
Climate Change Notes
Climate Change Notes

... CH4, nitrous oxides N20, aerosols (small particles tend to reflect solar radiation), water vapor Our Earth is warmed by absorbed solar energy. The warm earth radiates heat away into frigid space and this heat energy must pass upward through the atmosphere. As it passes through the atmosphere some of ...
A meteorological Pearl Harbor
A meteorological Pearl Harbor

... itself.  But  heating  up  the  planet  has   "juiced"  our  weather,  making  heat   waves  hotter  and  longer,  and  storms   more  violent  and  numerous.  Juiced  is   an  apt  word,  because  warmer  air   holds  more  water,  p ...
Climate Change
Climate Change

... been adjusted down by almost 2C and a declining temperature trend over 65 years in the raw data had been transformed into a sharply warming trend” (Oz 28 Jan 2015) ...
IPCC Fifth Assessment Report: Climate Change 2013/14
IPCC Fifth Assessment Report: Climate Change 2013/14

... Projections of future global mean temperature change and sea level rise confirm the potential for human activities to alter the Earth's climate to an extent unprecedented in human history; The long time-scales governing both the accumulation of greenhouse gases in the atmosphere and the response of ...
Climate Change - University of West Georgia
Climate Change - University of West Georgia

... • Sulfur dioxide reacts with water vapor causing haze • Combined with ejected particulate matter • One of the coldest years in the last two centuries was 1816, the “Year Without a Summer” • Caused by eruption of Tambora in ...
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Attribution of recent climate change



Attribution of recent climate change is the effort to scientifically ascertain mechanisms responsible for recent changes observed in the Earth's climate, commonly known as 'global warming'. The effort has focused on changes observed during the period of instrumental temperature record, when records are most reliable; particularly in the last 50 years, when human activity has grown fastest and observations of the troposphere have become available. The dominant mechanisms (to which recent climate change has been attributed) are anthropogenic, i.e., the result of human activity. They are: increasing atmospheric concentrations of greenhouse gases global changes to land surface, such as deforestation increasing atmospheric concentrations of aerosols.There are also natural mechanisms for variation including climate oscillations, changes in solar activity, and volcanic activity.According to the Intergovernmental Panel on Climate Change (IPCC), it is ""extremely likely"" that human influence was the dominant cause of global warming between 1951 and 2010. The IPCC defines ""extremely likely"" as indicating a probability of 95 to 100%, based on an expert assessment of all the available evidence.Multiple lines of evidence support attribution of recent climate change to human activities: A basic physical understanding of the climate system: greenhouse gas concentrations have increased and their warming properties are well-established. Historical estimates of past climate changes suggest that the recent changes in global surface temperature are unusual. Computer-based climate models are unable to replicate the observed warming unless human greenhouse gas emissions are included. Natural forces alone (such as solar and volcanic activity) cannot explain the observed warming.The IPCC's attribution of recent global warming to human activities is a view shared by most scientists, and is also supported by 196 other scientific organizations worldwide (see also: scientific opinion on climate change).
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