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45 Terms
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Evidence of Climate Change
Global average surface temperature has risen; greenhouse gases have increased; heat waves are more common; warm seasons are longer; water cycles are changing; sea levels are rising; ice caps are shrinking; ocean acidification is increasing; and extreme events are becoming more frequent.
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Milankovitch Cycles
Changes in Earth's orbit and tilt that naturally influence climate over long periods.
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Solar Radiation
Changes in the intensity of energy received from the Sun can influence Earth's climate.
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Volcanic Eruptions
Volcanic eruptions release particles that can reflect sunlight and cause temporary cooling.
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Industrial Revolution
Human activities increased dramatically, especially fossil fuel burning, causing large increases in atmospheric CO2.
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Global Mean Surface Temperature (GMST)
The average temperature of Earth's surface; it is about 1.1°C warmer than before the Industrial Revolution.
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Climate Change
Climate naturally fluctuates, but human activities have greatly increased the rate of recent warming.
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Greenhouse Gases
Gases such as CO2 that trap heat in Earth's atmosphere and contribute to warming.
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Carbon Cycle
The movement of carbon among the atmosphere, organisms, oceans, and Earth; human activities are increasing atmospheric CO2.
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Keeling Curve
A graph showing atmospheric CO2 concentration in parts per million (ppm) over time; it shows a long-term increase in CO2.
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Keeling Curve Seasonal Pattern
CO2 changes seasonally because plants photosynthesize more during the growing season and less during winter.
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Human Activities and Climate Change
Burning fossil fuels and cutting down forests increase atmospheric CO2, which traps heat and warms Earth.
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Positive Feedback
When warming causes changes that create even more warming, such as warming releasing additional CO2.
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Changing Water Cycle
Climate change can intensify floods and droughts, alter rainfall patterns, and contribute to rising sea levels.
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Effects of Climate Change
More heat waves, longer warm seasons, shorter cold seasons, melting ice, rising sea levels, ocean acidification, coral loss, and more extreme events.
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Linear Regression
A statistical method used to examine the relationship between two variables using a line of best fit.
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Scatterplot
A graph used to display the relationship between two variables before performing linear regression.
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Slope
The rate and direction of change between two variables in a linear regression.
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R-squared (R²)
A value showing how much of the variation in one variable is explained by the other variable.
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P-value
A statistical value used to determine whether a relationship is likely statistically significant.
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Independent Variable
The variable that is changed or controlled by the researcher; the possible cause.
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Dependent Variable
The variable that is measured; the possible effect.
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Replicates
Repeated trials of an experiment used to increase reliability and confidence in results.
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Photosynthesis
The process plants use to absorb CO2 and solar energy and convert it into organic matter.
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Photosynthesis as a Carbon Sink
Photosynthesis removes CO2 from the atmosphere and stores carbon in organic matter.
Higher CO2 can initially increase the rate of photosynthesis.
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How Heat Affects Photosynthesis
Too much heat can damage plant systems, reduce growth, and lower photosynthesis.
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How Drought Affects Photosynthesis
Drought and extreme weather can stress plants and reduce photosynthesis.
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Respiration
Metabolic process that uses oxygen and releases CO2 and energy from organic molecules.
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How Respiration Affects Climate Change
Respiration releases CO2 into the atmosphere.
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How Climate Change Affects Respiration
Climate change can alter respiration rates and the balance between CO2 released by respiration and CO2 removed by photosynthesis.
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Climate Change and Biomes
Climate change can alter temperature, water cycles, photosynthesis, species distributions, and the structure of biomes.
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Wildfire and Climate Change
Higher temperatures and changing conditions can increase wildfire risk.
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Biome Movement
As climate changes, forests and other biomes may shift toward higher latitudes or elevations.
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Acclimation
An individual organism adjusts to environmental changes during its lifetime.
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Adaptation
An inherited trait that becomes more common because it helps organisms survive and reproduce in their environment.
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Extinction
The permanent loss of a species when all of its members die.
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Climate Change and Species
Species may adapt, acclimate, move to new areas, or become extinct as environmental conditions change.
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Greenhouse Gases and Biomes
Increased greenhouse gases warm Earth and can shift temperature and precipitation patterns, changing where different biomes can exist.
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CO2 and Temperature Relationship
Increasing atmospheric CO2 traps more heat, contributing to increases in global temperature.
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Natural vs. Human Climate Change
Natural drivers include orbital changes, solar intensity, and volcanic eruptions; humans have greatly accelerated recent warming through fossil fuel use and deforestation.
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Carbon Feedback Loop
Human CO2 emissions increase warming; warming can release additional CO2, which can cause further warming.
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Long-Term Climate Data
Carbon dioxide and temperature data collected over decades and millennia can be compared to identify long-term climate patterns and changes.