The long-term warming of the planet's overall temperature
Global warming
Pace has significantly increased in the last hundred years due to the burning of fossil fuels
As the human population has increased, so has the volume of fossil fuels burned
Greenhouse effect
The Sun's rays penetrate the atmosphere, but when that heat is reflected off the surface cannot escape back into space
Greenhouse gases
Carbon dioxide
Chlorofluorocarbons
Water vapor
Methane
Nitrous oxide
Climate change
Changes in weather patterns and growing seasons around the world
Sea level rise caused by the expansion of warmer seas and melting ice sheets and glaciers
Global warming causes climate change, which poses a serious threat to life on earth in the forms of widespread flooding and extreme weather
In 2013 the IPCC reported that the interval between 1880 and 2012 saw an increase in global average surface temperature of approximately 0.9 °C (1.5 °F)
The increase is closer to 1.1 °C (2.0 °F) when measured relative to the preindustrial (i.e., 1750–1800) mean temperature
Human beings and human activities have been responsible for a worldwide average temperature increase of between 0.8 and 1.2 °C (1.4 and 2.2 °F) of global warming since preindustrial times
Most of the warming observed over the second half of the 20th century could be attributed to human activities
The global mean surface temperature would increase between 3 and 4 °C (5.4 and 7.2 °F) by 2100 relative to the 1986–2005 average should carbon emissions continue at their current rate
Significant societal, economic, and ecological damage would result if global average temperatures rose by more than 2 °C (3.6 °F) in such a short time
Such damage would include increased extinction of many plant and animal species, shifts in patterns of agriculture, and rising sea levels
By 2015 all but a few national governments had begun the process of instituting carbon reduction plans as part of the Paris Agreement
Should carbon emissions continue at their present rate, the increase in average near-surface air temperatures would reach 1.5 °C sometime between 2030 and 2052
The global average sea level rose by some 19–21 cm (7.5–8.3 inches) between 1901 and 2010 and that sea levels rose faster in the second half of the 20th century than in the first half
The global average sea level would rise 26–77 cm (10.2–30.3 inches) relative to the 1986–2005 average by 2100 for global warming of 1.5 °C
Modern global warming is the result of an increase in magnitude of the greenhouse effect, a warming of Earth's surface and lower atmosphere caused by the presence of greenhouse gases
In 2014 the IPCC reported that concentrations of carbon dioxide, methane, and nitrous oxides in the atmosphere surpassed those found in ice cores dating back 800,000 years
At the beginning of the industrial age in the mid-18th century, carbon dioxide concentrations in the atmosphere were roughly 280 parts per million (ppm)
By the middle of 2018 they had risen to 406 ppm, and, if fossil fuels continue to be burned at current rates, they are projected to reach 550 ppm by the mid-21st century—essentially, a doubling of carbon dioxide concentrations in 300 years
Climate change
Broader set of changes that go along with global warming, including changes in weather patterns, the oceans, ice and snow, and ecosystems
Greenhouse effect
A natural process that helps make the Earth warm enough for us to live
Greenhouse gases in the atmosphere trap some of the energy from the sun before it escapes to outer space, warming the atmosphere
The "ozone hole" refers to a decrease in the layer of ozone gas found high in the Earth's atmosphere, which helps to shield the planet from the sun's harmful ultraviolet rays
The Earth's climate changed many times in the distant past as a result of natural causes, but today's climate change is different because people's activities are the main cause
Even a one- to two-degree increase in global temperature can lead to a much greater risk of wildfires
The average temperature around the world is rising, and 2001–2010 was the warmest decade on record
As the Earth's climate gets warmer over time, most places will experience more days with record high temperatures and fewer days with record low temperatures
The average sea level around the world has risen by nearly 7 inches in the last 100 years, glaciers all over the world are shrinking, and many bird species are shifting northward
Any change in the climate of an area can affect the plants and animals that live there
Things you can do to reduce greenhouse gas emissions
Turn off the lights when you leave a room
Turn off your computer and other electronic devices when you're not using them
Drive less. Instead, walk, ride your bike, or use public transportation if you can
Use less water
Create less waste
Recycle used paper, cans, bottles, and other materials
Visual Impacts of Climate Change Evidence
Melting Glaciers
Rising Sea Levels
Flooding
Worsening Drought
Supercell Storms
Increasing Tornadoes
Patterns affecting weather and climate of the Philippines
Weather disturbance
A term used to describe a change in atmospheric conditions or weather patterns
Types of weather disturbances
Tropical cyclones
Intense tropical cyclones
Low-pressure areas
Very intense tropical cyclones
Tropical waves
Tropical disturbances
Tropical depressions
Extra-tropical disturbances
Subtropical disturbances
Moderate tropical storms
Severe tropical storms
Zones of disturbed weather
Weather disturbances
Hurricanes
Cyclones
Thunderstorms
Tornadoes
Tropical cyclone
Warm-core low pressure system associated with a spiral inflow of mass at the bottom level and spiral outflow at the top level, forming over oceans where sea surface temperature and air temperatures are greater than 26°C
Typhoon
A tropical cyclone that occurs in the part of the Northwest Pacific Ocean that is west of the dateline and reaches wind speeds of at least 74 mph
Hurricane
A tropical cyclone of that intensity that occurs in the North Atlantic, in the Northeast Pacific east of the dateline or the South Pacific east of the 160th meridian east
Oceans and seas have great influence on the weather of continental masses