A change of climate which is attributed directly or indirectly to human activity that alters the composition of the global atmosphere and which is in addition to natural climate variability observed over comparable time periods
Earth's climate has stabilized only in the tens of thousands of years
Complex physicochemical processes in our atmosphere, oceans, and the sun support life on earth
Role of the atmosphere
Protects us from harmful ultraviolet solar radiation
Warms the planet
Prevents extremes between day and night temperatures
Keeps the Earth habitable
Factors that influence an area's weather
Latitude
Altitude
Geography (large bodies of water, mountains, urban areas)
Factors that influence an area's climate
Location
Large-scale climate system (El Niño Southern Oscillation)
Climate of the Philippines
Type I (two pronounced seasons)
Type II (pronounced peak in wet season)
Type III (no pronounced seasonal cycle)
Type IV (rainfall more or less distributed throughout the year)
Natural greenhouse effect
Naturally occurring concentrations of atmospheric gases trap enough heat from the sun to sustain life
Earth's atmospheric gases
Nitrogen
Oxygen
Water
Carbon dioxide
Methane
Greenhouse gases
Absorb the energy of specific wavelengths of electromagnetic radiation (i.e. light) and transfer parts of that energy to the atmosphere as heat
Natural greenhouse effect
1. Solar radiation reaches the Earth's atmosphere - some is reflected back into space
2. The rest of the sun's energy is absorbed by the land and the oceans, heating the Earth
3. Heat radiates from Earth towards space
4. Some of this radiative heat is trapped by greenhouse gases in the atmosphere, keeping the Earth warm enough to sustain life
Enhanced greenhouse effect
Human activities increase the amount of greenhouse gases released into the atmosphere, trapping extra heat and causing the Earth's temperature to rise
Natural sources of carbon dioxide emissions
Decomposition of vegetation
Ocean release
Volcanic eruptions
Naturally occurring wildfires
Respiration
Anthropogenic sources of carbon dioxide emissions
Production
Land use land cover change
Deforestation
Burning of fossil fuels (coal, oil, and natural gas)
Climate change is a change of climate which is attributed directly or indirectly to human activity that alters the composition of the global atmosphere and which is in addition to natural climate variability observed over comparable time periods
Bill Nye, "The Science guy": '"It's not that the world hasn't had more carbon dioxide, it's not that the world hasn't been warmer. The problem is the speed at which things are changing. We are inducing a sixth mass extinction event kind of by accident, and we don't want to be the extinctee"'
Global and local indicators of climate change
Changes in weather extremes and variability (extreme temperatures, prolonged droughts, severe storms, typhoons, flooding)
A collective series of extreme events (beyond normal, how frequent, how strong)
What climatologists monitor
Temperature
Precipitation
Sea-level rise
Ocean and atmospheric currents
Incident solar radiation
Clouds
Water budget in the biosphere and atmosphere
Impacts of climate change
Biodiversity loss
Agriculture
Coastal zones
Economy
Fisheries
Human health
Food security
Terrestrial ecosystems & forests
Water resources
Saltwater intrusion
Sea level rise
Coral bleaching & Ocean acidification
Drought
Flooding
Abnormal weather patterns
A 2-degree rise in global temperature is considered a critical threshold above which dangerous and cascading effects of human-generated climate change will occur
At 1.5°C, 69 million people will be directly affected or displaced by rising seas, while at 2.0°C, 80 million people will be affected
At 1.5°C, 14% of the population will be exposed to deadly heat waves at least once every five years, while at 2.0°C, 37% will be exposed
At 1.5°C, 350 million people will be exposed to drought, while at 2.0°C, 411 million people will be exposed
At 1.5°C, there will be a 6% more insects, 4% fewer invertebrates, and 8% fewer plants, while at 2.0°C, there will be 18% more insects, 8% fewer invertebrates, and 16% fewer plants
At 1.5°C, we will lose 70-90% of coral reefs, while at 2.0°C, 99% of our coral reefs will be lost
The numbers are global averages, and different areas around the world will have the worst experience than others
To keep temperatures from rising higher than 1.5 degrees, global emissions need to be reduced to 45% by 2030 and cut to 0% by 2050
Main objective of the United Nations Framework Convention on Climate Change (UNFCC)
Stabilization of atmospheric GHG concentration at a level that would prevent dangerous anthropogenic interference with the climate system, give enough time for ecosystems to adapt to climate change, and ensure food security and sustainable economic development
GHG emitting activities
Energy
Industrial processes
Agriculture
Land use change
Forestry
Waste
Stopping emissions is not enough, as carbon dioxide concentration will not respond immediately due to the residence times of GHGs
The Philippines is vulnerable to climate change due to environmental impacts, rapid urbanization, higher population density, and incidence of poverty