Get our free book (in Spanish or English) on rainwater now - To Catch the Rain.
|See also the Climate change category.|
for subtopics, how-tos, project pages, designs, organization pages and more.
Climate changeW is a significant and lasting change in the Earth's climate over an extended period. In this article we discuss the impact of a rise in the average temperature of the Earth's atmosphere and oceans from the 19th century to the present.  Climate change is expected to have far greater negative effects on developing countries than on developed countries due to numerous factors including exposure to extreme weather and infrastructure considerations.
- 1 The science of climate change
- 2 The impact of climate change
- 3 Historic changes in the earth's climate
- 4 Climate change mitigation
- 5 Climate change chain reactions
- 6 Climate Change on the Ocean
- 7 Impact of climate change on species
- 8 Notes
- 9 See also
- 10 Interwiki links
- 11 External Links
The science of climate change
Although the existence of the greenhouse effect has been largely understood since 1896, there are still a tiny minority of scientists who remain critical of specifics written in some reports of the IPCCW and other organisations. These so-called climate change skepticsW are generally misinformed or are deliberately attempting to create doubt and uncertainty about the science.
Certain politicians, lobbyists and economists refer to disinformation from climate change 'skeptics' for their own advantage, portraying an image that climate change does not exist, poses but a minor problem, or may even be beneficial so as to be able to prevent action to reduce greenhouse gases (mostly resulting from the burning of fossil fuels). The GWPF in the UK is an example of a political lobbying group, which is secretly funded by fossil fuel interests.Guardian article on the secret funding of the GWPF
The impact of climate change
Although climate change itself has been proven, uncertainties still exist regarding predicting the effects. The IPCC is highly confident that impacts will increase as greenhouse gases and associated positive feedback effects kick in (e.g. methane release from melting permafrost, changing albedo), though their severity and the timescales may differ to some extent. Examples of impacts include:
- Increasing heat stresses as global temperatures rise. While some regions such as Canada may benefit to some degree from rising temperatures, the overall effects on the ability of the planet to support life will be negative. As temperatures rise, many equatorial regions will become hostile to life;
- Changing weather patterns, especially more extreme weather events and changing rainfall patterns, specifically increasing or decreasing precipitation levels. Increasing floods and drought periods will have a generally negative effect on farming;
- Natural disasters (ie mud slides, hurricanes, ...) are expected to increase in their severity. Death toll in 2003 = 150,000 people :
- Sea level rise will contaminate a very large percentage of the planets' agricultural fields with sea salt and make them no longer suitable for continued food production. In addition, many low-lying islands and coastlines will need to be abandoned, forcing many people to move.
- Increasing ocean acidity. As the pH of water decreases due to the input of carbonic acid (resulting from CO2 dissolving in water), life forms which rely on a chalk shell will find it increasingly impossible to survive. This will have negative effects on many ocean ecosystems, especially coral reefs which are the most bio-diverse of any ecosystem on the planet.
Historic changes in the earth's climate
The term "climate change" is often used to describe the impact of human-caused pollution on the earth's climate, but is important to understand that climate change is also caused by natural phenomena.
History of Ice Ages
The earth's climate is subject to large fluctuations. The climate is dominated by ices ages, which reduce the earth's surface temperature and cover large parts of the surface in ice sheets. There have only been five ice ages to date, that have lasted from 30 million up to 300 million years. The most recent one occurred during to "Quaternary", which started about 2.5 million years ago and is still lasting. In between ice ages, the poles are not covered by glaciers and the temperature is higher. The climate is quite stable in these periods, however during ice ages strong variations occur. These variations are called glacial (cold) and interglacial (hot) periods. Glacial and interglacial periods alternate every 5,000-15,000 years. The current interglacial period started 14,000 years ago.
Climate change mitigation
Several options are available to reduce the impacts of a changing climate. Most of these (the most efficient ones) are lifestyle changes (i.e. stop the burning of fossil fuels, stop eating meat etc.) and can be put in place today. We also do not need to wait for any specific technology to became available. Rather, the essential technology is already here today. Politicians often portray a different picture but it is rarely based in reality. Selected options include:
- Reducing the release of greenhouse gasesW (GHG's) into the atmosphere (ie through energy efficiency, ...)
- Prevent carbon dioxide from being released into the atmosphere (ie through carbon capture and storage (CCS), biochar, ...). With Carbon sequestration/CCS, after combusting a fuel, the CO2 is stored in a cavity underground.
- Remove carbon dioxide from the atmosphere, e.g. through geo-engineering ocean fertilisation, planting extra trees, ...
- Shield some of the planet from the sun, or reflect a proportion of sunlight back into space (i.e. by painting roads, parking spaces and roofs white, spraying sulphate aerosols into the stratosphere, ...)
- Climate change mitigation: build heat tolerant houses (passive solar with suitable insulation), flood control barriers, ...
- Grin and bear it: put up with the inconveniences and the expected loss of biodiversity and increases in certain types of natural disasters and wait for extinction.
The IPCC already considers a 2°C temperature rise to be almost inevitable. In addition, it also advises the use of most other measures, yet stays critical of geoengineering options, due to the risks involved.
Climate change chain reactions
The change in temperature and weather has a huge impact on wildlife which can become dangerous if the change stays the same.Even the minor change of temperature can lead to earlier hatching of insects or melting of snow which protects snow rabbits from their natural hunters.These effects cause problems like insect overpopulation or too less surviving rabbits to reproduce sustainably.The insects are dangerous because they consume crops and other plans and in huge amounts they are even able to consume a whole field of possible food.Because this problem is getting bigger and even endangers species and if it goes on like this many species will die out and even our own food capacity may shrink exponentionally.
Climate Change on the Ocean
Earth is called the blue planet because approximately 72 percent of it is covered by oceans. The oceans influence the weather on local to global scales, while changes in climate can fundamentally alter many properties of the oceans.
Ocean conveyor system
The thermohaline circulation also called the great ocean conveyor belt or global ocean conveyor belt, is a large scale ocean circulation that distributes vast quantities of heat and moisture around on a planetary scale.
Gulf stream has the length of 10.000 km. It is one of the largest and fastest ocean current on earth. Originating from the tip of Florida, at 2 m/s, it brings 100.000.000 m3/s water towards Europe.
Sea level rise
As water gets warmer, it takes up more space. Each drop of water only expands by a little bit, but when you multiply this expansion over the entire depth of the ocean, it all adds up and causes sea level to rise. But that's not the only cause of the rise of sea level. The rise of sea level also caused by the melting of glaciers and polar ice caps and ice loss from Greenland and West Antarctica.
Ocean acidification is the ongoing decrease on ocean pH cause by human CO2 Emission. Ocean pH has decreased by about 30% already and if we continue emitting CO2 at the same rate by 2100 ocean acidity will increase by about 150%, a rate that has not been experienced for at least 400,000 years. Such a monumental alteration in basic ocean chemistry is likely to have wide implications for ocean life, especially for those organisms that require calcium carbonate to build shells or skeletons.
Impact of climate change on species
Through rising temperatures resulting in a shift of climate zones forces species to adapt to the new climatic conditions. By a rapidly increased temperature the risk for especially plants not to find areas with suitable living conditions early enough is higher. Observations of several species conclude that they are moving their ranges polewards to keep up with changing climate.
- http://earthobservatory.nasa.gov/Features/Water/images/precipitation_intensity_map.png Precipitation changes
- One solution is to grow more resilient crops, i.e. more resistant to changes in rainfall and disease
- 150000 people killed by global warming up to 2003
- Sea level rise: 2m rise expected by the year 2100, 6.5m by 2200
- Earth under water documentary
- Note: this direct temperature reduction does not reduce carbon levels, so ocean acidification from higher carbon dioxide is still a problem
- Renewable energy
- Incentives for sustainability
- Sea level rise
- Measures to stop global warming