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Paleoclimatology
Study of Earth's past climate changes.
Earth/Sun Geometry
Arrangement affecting climate through solar radiation.
Sun Angle
Angle of sunlight impacting temperature and climate.
Latitude
Distance from equator influencing climate variations.
U-Shaped Valleys
Glacially carved valleys with steep sides and flat floors.
Glaciers
Masses of ice that shape landscapes during ice ages.
Buried Soils
Ancient soils covered by sediments indicating past climates.
Interglacial Periods
Warmer climate phases between glacial periods.
Dendrochronology
Tree ring study for dating and climate analysis.
Annual Growth Rings
Yearly tree growth indicators influenced by climate.
Factors Affecting Growth
Temperature and moisture influence tree ring width.
Precipitation
Water availability affecting tree growth and ring size.
Drought Indicators
Narrow tree rings signal dry conditions.
Extreme Weather Events
Impact of storms or fires reflected in tree rings.
Pollen Analysis
Study of pollen to infer past climates.
Palynology
Scientific study of pollen grains in sediments.
Pollen Preservation
Durable pollen remains in sediment for millennia.
Species-Specific Pollen
pollen grains that exhibit unique characteristics, such as shape, size, and surface markings, that are characteristic of a particular plant species
Environmental Requirements
Conditions needed for plant growth affecting pollen types.
Sediment Layers
Stratified deposits containing preserved pollen over time.
Carbon Dating
Method for dating sediment layers to establish timelines.
Climate Indicators
Pollen types reveal historical climate conditions.
Chronology
Dating sediment layers to correlate with climate events.
Pollen Records
Used to track global and regional climate changes.
Ice Cores
Drilled from glaciers, preserve ancient atmospheric samples.
Air Bubbles
Trapped in ice, contain historical gas concentrations.
Greenhouse Gases
Gases like CO₂ and CH₄ that trap heat.
Isotopic Composition
Ratio of oxygen isotopes indicates past temperatures.
Annual Layers
Counted layers in ice cores indicate ice age.
Correlation of CO₂ and Temperature
Strong link between CO₂ levels and global temperatures. For instance, during ice ages, CO2 levels were much lower, and global temperatures were cooler. During interglacial periods, CO2 levels were higher, and temperatures were warmer.
Ice Ages
Periods of lower CO₂ and colder temperatures.
Interglacial Periods
Warmer periods with higher CO₂ levels.
Tree Rings
Provide high-resolution annual climate data.
Local Climate Influence
Tree growth affected by temperature and precipitation.
Pollen Analysis
Indicates past vegetation and climate conditions.
Carbon Cycle
The process by which carbon is exchanged between the Earth’s atmosphere, oceans, soil, and living organisms.
Carbon Reservoirs
Are natural or artificial systems that store carbon and prevent it from being released into the atmosphere. Includes atmosphere, oceans, land, and organisms.
Greenhouse Effect
the process by which certain gases in Earth’s atmosphere trap heat, keeping the planet warm enough to support life
Human Impact on CO₂
Burning fossil fuels, deforestation, industrialization, and agricultural practices increases atmospheric CO₂.
Natural CO₂ Sources
Includes photosynthesis (respiration), decomposition, and volcanic activity releases co2 when magma rises to the surface
U-shaped Valleys
Evidence of past glacial activity in landscapes.
Buried Soils
Indicate past interglacial periods and climate.
Climate Variability
Short-term climate changes like droughts or wet years.
Proxy Data
Indirect measures indicating past climate conditions such as ice cores, tree rings, sediment cores, pollen, and fossils
Atmospheric Composition
Refers to the types and relative amounts of gases present in Earth's atmosphere. Historical gases analyzed from ice core samples.
Drought Indicators
Pollen shifts signal changes in climate moisture.
Greenhouse Effect
Gases trap solar heat, maintaining Earth's temperature.
Solar Radiation
Energy emitted by the Sun, mainly visible light.
Industrial Revolution
Late 18th century shift to machinery and fossil fuels.
Atmospheric CO2 Levels
Stable before Industrial Revolution, now significantly increased.
Current CO2 Levels
Surpassed 420 ppm, highest in 3 million years.
Rate of Climate Change
Current changes occur faster than historical shifts.
Historical Climate Shifts
Triggered by Earth's orbit, volcanic activity, asteroid impacts.
Temperature Increase
Earth warmed 2.2°F since the 19th century.
Recent Temperature Rise
0.5°F increase in last 20 years.
Plastic Pollution Locations
Found in North Pacific, Asia, Arctic, and Antarctic.
Microplastics
Tiny plastic particles from larger plastics or manufactured.
Microplastics Sources
Include microbeads in cosmetics and synthetic clothing fibers.
NIH Research on Microplastics
Indicates health risks include inhalation and cancer.
Paris Climate Agreement
Legally binding treaty to combat climate change globally in 2015
COP 21
Conference where the Paris Agreement was adopted.
Global Warming Limit
refers to the target set by the Paris Climate Agreement to limit the increase in Earth's average temperature as a result of human activities
Well below 2°C above pre-industrial levels, and
Pursue efforts to limit the temperature increase to 1.5°C above pre-industrial levels.
Pre-Industrial Levels
Reference point for measuring global temperature rise.
Climate Change Indicators
Include wildfires, rising sea levels, Gulf Stream impacts.
Heatwaves
Increased frequency due to climate change.
Hurricanes
More intense and frequent due to warming.
Droughts
Increased occurrence linked to climate change.
Climate Change Evidence
Natural events indicating ongoing climate shifts.
Ice Age
Historical period of significant temperature decline.
Montreal Protocol
1987 treaty to phase out ozone-depleting substances.
Ozone Layer
Protects Earth from harmful UV radiation.
Greenhouse Gas Emissions
Gases contributing to global warming and climate change.
Universal Agreement
Treaty signed by all UN member countries.
Legally Binding Targets
Mandatory goals for phasing out harmful substances. In climate agreements like the Paris Climate Agreement, legally binding targets would typically involve specific emission reduction goals, financial contributions, or other commitments that a country agrees to meet.
Environmental Success
Significant reduction of ozone-depleting substances achieved.
Industry Adaptation
Industries adjusted practices to comply with environmental standards.
Science-Driven Policy
Policies based on scientific research and findings.
Rising Temperatures
Increased heat and shorter winters in Michigan.
Extreme Weather
More frequent heavy rains and drought risks.
Great Lakes Impacts
Rising water levels and erosion affecting ecosystems.
Agricultural Disruptions
Negative effects on crop production and farming.
Public Health Risks
Increased health issues due to climate change.
Economic Disruptions
Financial instability from climate-related challenges
e.g: increasing the frequency of extreme weather events, reducing agricultural productivity, and damaging infrastructure
Energy Demand Strain
Increased energy needs impacting infrastructure.
Colorado River
Major water source for seven U.S. states.
American Nile
Nickname for Colorado River due to its importance.
Cradle of Civilization
Regions where early complex societies emerged.
Mesopotamia
Fertile area known for early agriculture and governance.
Las Vegas Population Growth
Rapid increase began in the 20th century.
Annual Visitors to Las Vegas
Approximately 40 million tourists each year.
Average Rainfall in Vegas
About 4.2 inches annually, mostly in winter.
Colorado River Compact
1922 agreement dividing Colorado River water rights.
Water Storage in SW U.S.
Stored in reservoirs, dams, and aquifers.
Water Management
Strategies to optimize limited water resources.
Dams
Structures generating electricity and controlling floods.
Anasazi Indians
Ancient civilization in SW U.S. from 200-1300 CE.
Four Corners Region
Area where Arizona, New Mexico, Colorado, Utah meet.
Civilization Decline
Migration into Pueblo tribes around 1300 CE.
Tree Ring Analysis
Method to study historical climate through tree growth.
Sediment Cores
Samples used to analyze past environmental conditions.