ch9Lecture
Earth's climate is warming
Yearly average temperatures increased in the Arctic twice as fast as the tropics and temperate areas
90% of Arctic glaciers are retreating at fast rates
Sea ice has been declining
Permafrost is melting during summers
Fires are more common
Animal populations are decreasing
Public perceptions on climate change
In the U.S. 2016 study, only 48% believe climate change is caused by humans
Opinion is political and financial
International and scientific consensus on climate change
Based on "facts" that support agendas, in some cases
2015 Paris Agreement is flawed and limited in its scope
Long-term climate patterns
Earth's climate has been dynamic over the past millions of years
In the past 10,000 years, Earth has grown warmer with ups and downs
Pleistocene period: Earth cycled between colder and warmer periods
Holocene period: Earth in a warm interglacial period, with shifts in climate
Measuring global warming
Earth has warmed significantly since the Industrial Revolution
Difficult to measure global annual surface air temperature
Models, sampling stations, and examining patterns are used
Causes of natural climate variation
Solar forcing
Regional variation in annual temperatures (land vs. water)
El Niño/Southern Oscillation, which changes ocean currents and alters weather patterns
Volcanic eruptions cool the atmosphere
Causes of global warming
Temperature of Earth's atmosphere affected by the amount of solar radiation, Earth's orbit, and human influences
Human influences include the chemical composition of the troposphere, such as carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O)
Greenhouse effect
Gas molecules absorb heat, known as greenhouse gases
Water vapor (H2O) is the most abundant naturally occurring greenhouse gas
Other greenhouse gases include carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O)
Human impacts on global warming
Anthropogenic (human-caused) increases in greenhouse gases, such as CO2
Deforestation, fossil fuel use, and synthetic greenhouse gases like chlorofluorocarbon (CFC) compounds
Impact of anthropogenic greenhouse gases
Global warming potential (GWP) measures the long-term impact and capacity to absorb infrared light/retain heat
Gases like CO2, methane (CH4), and nitrous oxide (N2O) trap heat from Earth's surface
Sources of greenhouse gases
Total greenhouse emissions expressed in carbon dioxide equivalents (CO2e)
Burning fossil fuels and industrial processes contribute to greenhouse gas emissions
Consequences of global warming
Climate patterns are changing, leading to drier and wetter conditions
Melting glaciers and ice sheets, with over 80% of Earth's glaciers retreating
Rising sea levels due to thermal expansion and glacial meltwater
Changing populations and ecosystems
Climate plays
Earth's climate is warming
Yearly average temperatures increased in the Arctic twice as fast as the tropics and temperate areas
90% of Arctic glaciers are retreating at fast rates
Sea ice has been declining
Permafrost is melting during summers
Fires are more common
Animal populations are decreasing
Public perceptions on climate change
In the U.S. 2016 study, only 48% believe climate change is caused by humans
Opinion is political and financial
International and scientific consensus on climate change
Based on "facts" that support agendas, in some cases
2015 Paris Agreement is flawed and limited in its scope
Long-term climate patterns
Earth's climate has been dynamic over the past millions of years
In the past 10,000 years, Earth has grown warmer with ups and downs
Pleistocene period: Earth cycled between colder and warmer periods
Holocene period: Earth in a warm interglacial period, with shifts in climate
Measuring global warming
Earth has warmed significantly since the Industrial Revolution
Difficult to measure global annual surface air temperature
Models, sampling stations, and examining patterns are used
Causes of natural climate variation
Solar forcing
Regional variation in annual temperatures (land vs. water)
El Niño/Southern Oscillation, which changes ocean currents and alters weather patterns
Volcanic eruptions cool the atmosphere
Causes of global warming
Temperature of Earth's atmosphere affected by the amount of solar radiation, Earth's orbit, and human influences
Human influences include the chemical composition of the troposphere, such as carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O)
Greenhouse effect
Gas molecules absorb heat, known as greenhouse gases
Water vapor (H2O) is the most abundant naturally occurring greenhouse gas
Other greenhouse gases include carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O)
Human impacts on global warming
Anthropogenic (human-caused) increases in greenhouse gases, such as CO2
Deforestation, fossil fuel use, and synthetic greenhouse gases like chlorofluorocarbon (CFC) compounds
Impact of anthropogenic greenhouse gases
Global warming potential (GWP) measures the long-term impact and capacity to absorb infrared light/retain heat
Gases like CO2, methane (CH4), and nitrous oxide (N2O) trap heat from Earth's surface
Sources of greenhouse gases
Total greenhouse emissions expressed in carbon dioxide equivalents (CO2e)
Burning fossil fuels and industrial processes contribute to greenhouse gas emissions
Consequences of global warming
Climate patterns are changing, leading to drier and wetter conditions
Melting glaciers and ice sheets, with over 80% of Earth's glaciers retreating
Rising sea levels due to thermal expansion and glacial meltwater
Changing populations and ecosystems
Climate plays