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Climate change is a significant and lasting change in the statistical
distribution of weather patterns over periods ranging from decades to
millions of years. It may be a change in average weather conditions or the
distribution of events around that average (e.g., more or fewer extreme
weather events). Climate change may be limited to a specific region or may
occur across the whole Earth.

Table of Contents
1        Terminology
2        Causes
                  Internal forcing mechanisms
                           Ocean variability
                 External forcing mechanisms
                           Orbital variations
                           Solar output
                           Volcanism
                           Plate tectonics
                           Human influences
Physical evidence for and examples of climatic change
            Temperature measurements and proxies
            Historical and archaeological evidence
            Glaciers
            Arctic sea ice loss
            Vegetation
            Pollen analysis
            Precipitation
            Dendroclimatology
            Ice cores
            Animals
            Sea level change
The most general definition of climate change is a change in the statistical
properties of the climate system when considered over long periods of
time, regardless of cause.[1] Accordingly, fluctuations over periods shorter
than a few decades, such as El Niño, do not represent climate change.
The term sometimes is used to refer specifically to climate change caused
by human activity, as opposed to changes in climate that may have resulted
as part of Earth's natural processes.[2] In this latter sense, used especially in
the context of environmental policy, the term climate change today is
synonymous with anthropogenic global warming. Within scientific
journals, however, global warming refers to surface temperature
increases, while climate change includes global warming and everything else
that increasing greenhouse gas amounts will affect.[3]
Causes
Climate changes in response to changes in the global energy balance. On
the broadest scale, the rate at which energy is received from the sun and the
rate at which it is lost to space determine the equilibrium temperature and
climate of Earth. This energy is then distributed around the globe by winds,
ocean currents, and other mechanisms to affect the climates of different
regions.
Factors that can shape climate are called climate forcings or "forcing
mechanisms".[4] These include such processes as variations in solar
radiation, deviations in the Earth's orbit, mountain-building and continental
drift, and changes in greenhouse gas concentrations. There are a variety of
climate change feedbacks that can either amplify or diminish the initial
forcing. Some parts of the climate system, such as the oceans and ice caps,
respond slowly in reaction to climate forcings, while others respond more
quickly.
Forcing mechanisms can be either "internal" or "external". Internal forcing
mechanisms are natural processes within the climate system itself (e.g., the
meridional overturning circulation). External forcing mechanisms can be
either natural (e.g., changes in solar output) or anthropogenic (e.g.,
increased emissions of greenhouse gases).
on climate change, deals, exclusively with the exploration of the causes
of climate change. The increase in the emission of green house gases
and the subsequent enhanced greenhouse effect, is the root of this
problem and the human activities and processes which cause these are
quite comprehensively discusses. Trends in the increase in the
concentrations of these green house gases are detailed with the use of
tables and graphs and pie-charts have also been included to show the
contribution of different gases to global warming.
The scientific chemical processes to show the production of these
gases, also find cover here further illustrations and photographs to
ascertain the impacts of these gases a are also included. In addition the
consequences of the actions of these causes are discussed and critical
insights into combating these causes one listed.
1. Causes of Global Climate Change
2. Ozone Depletion
3. International Carbon Market
4. Global Warming
5. Sea Level Rise
6. Effects of Climate Extremes
7. International Emission Trading
8. Climate Change and Health
9. Impacts of Climate Change to Coral Reefs
10. Climate Change and Adaption
11. Climate Change Mitigation
12. International Effort against Climate Change
Climate
Climate

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Climate

  • 1.
  • 2.
  • 3.
  • 4.
  • 5.
  • 6. Climate change is a significant and lasting change in the statistical distribution of weather patterns over periods ranging from decades to millions of years. It may be a change in average weather conditions or the distribution of events around that average (e.g., more or fewer extreme weather events). Climate change may be limited to a specific region or may occur across the whole Earth. Table of Contents 1 Terminology 2 Causes Internal forcing mechanisms Ocean variability External forcing mechanisms Orbital variations Solar output Volcanism Plate tectonics Human influences
  • 7.
  • 8. Physical evidence for and examples of climatic change Temperature measurements and proxies Historical and archaeological evidence Glaciers Arctic sea ice loss Vegetation Pollen analysis Precipitation Dendroclimatology Ice cores Animals Sea level change
  • 9. The most general definition of climate change is a change in the statistical properties of the climate system when considered over long periods of time, regardless of cause.[1] Accordingly, fluctuations over periods shorter than a few decades, such as El Niño, do not represent climate change. The term sometimes is used to refer specifically to climate change caused by human activity, as opposed to changes in climate that may have resulted as part of Earth's natural processes.[2] In this latter sense, used especially in the context of environmental policy, the term climate change today is synonymous with anthropogenic global warming. Within scientific journals, however, global warming refers to surface temperature increases, while climate change includes global warming and everything else that increasing greenhouse gas amounts will affect.[3] Causes
  • 10. Climate changes in response to changes in the global energy balance. On the broadest scale, the rate at which energy is received from the sun and the rate at which it is lost to space determine the equilibrium temperature and climate of Earth. This energy is then distributed around the globe by winds, ocean currents, and other mechanisms to affect the climates of different regions. Factors that can shape climate are called climate forcings or "forcing mechanisms".[4] These include such processes as variations in solar radiation, deviations in the Earth's orbit, mountain-building and continental drift, and changes in greenhouse gas concentrations. There are a variety of climate change feedbacks that can either amplify or diminish the initial forcing. Some parts of the climate system, such as the oceans and ice caps, respond slowly in reaction to climate forcings, while others respond more quickly. Forcing mechanisms can be either "internal" or "external". Internal forcing mechanisms are natural processes within the climate system itself (e.g., the meridional overturning circulation). External forcing mechanisms can be either natural (e.g., changes in solar output) or anthropogenic (e.g., increased emissions of greenhouse gases).
  • 11.
  • 12.
  • 13. on climate change, deals, exclusively with the exploration of the causes of climate change. The increase in the emission of green house gases and the subsequent enhanced greenhouse effect, is the root of this problem and the human activities and processes which cause these are quite comprehensively discusses. Trends in the increase in the concentrations of these green house gases are detailed with the use of tables and graphs and pie-charts have also been included to show the contribution of different gases to global warming. The scientific chemical processes to show the production of these gases, also find cover here further illustrations and photographs to ascertain the impacts of these gases a are also included. In addition the consequences of the actions of these causes are discussed and critical insights into combating these causes one listed.
  • 14.
  • 15. 1. Causes of Global Climate Change 2. Ozone Depletion 3. International Carbon Market 4. Global Warming 5. Sea Level Rise 6. Effects of Climate Extremes 7. International Emission Trading 8. Climate Change and Health 9. Impacts of Climate Change to Coral Reefs 10. Climate Change and Adaption 11. Climate Change Mitigation 12. International Effort against Climate Change