Earth Science

🏝️Earth Science Unit 2 – Earth's Systems and Cycles

Earth's systems—geosphere, hydrosphere, atmosphere, and biosphere—interact through complex cycles and processes. These systems exchange energy and matter, shaping our planet's climate, landscapes, and life. Understanding these interactions is crucial for addressing environmental challenges and managing resources sustainably. Key concepts include biogeochemical cycles, feedback loops, and human impacts on Earth's systems. The water, carbon, and rock cycles demonstrate the continuous movement of materials between Earth's spheres. Climate patterns, weather systems, and human activities all play vital roles in shaping our planet's dynamic environment.

Key Concepts and Definitions

  • Earth's systems include the geosphere (solid Earth), hydrosphere (water), atmosphere (air), and biosphere (living organisms)
  • Cycles describe the continuous movement and exchange of materials between Earth's systems
    • Examples include the water cycle, carbon cycle, and rock cycle
  • Feedback loops can amplify (positive feedback) or dampen (negative feedback) changes in Earth's systems
  • Albedo measures the reflectivity of a surface (snow has high albedo, absorbing less solar radiation)
  • Anthropogenic factors are human activities that influence Earth's systems (deforestation, fossil fuel combustion)
  • Biogeochemical cycles involve the transfer of chemical elements between living organisms and the physical environment
  • Gaia hypothesis proposes that Earth's systems interact to maintain conditions suitable for life
  • Milankovitch cycles describe long-term variations in Earth's orbit and axis tilt that affect climate

Earth's Major Systems

  • Geosphere consists of the solid Earth, including the crust, mantle, and core
    • Crust is the thin, outermost layer of the Earth (oceanic crust, continental crust)
    • Mantle is the layer between the crust and core, comprising most of Earth's volume
    • Core is the innermost layer, divided into the liquid outer core and solid inner core
  • Hydrosphere encompasses all water on Earth's surface and underground (oceans, lakes, rivers, groundwater, ice caps)
  • Atmosphere is the gaseous layer surrounding the Earth, composed primarily of nitrogen and oxygen
    • Troposphere is the lowest layer where weather occurs
    • Stratosphere contains the ozone layer, which absorbs harmful UV radiation
  • Biosphere includes all living organisms on Earth (plants, animals, microorganisms)
  • Earth's systems constantly interact and exchange energy and matter through various cycles and processes

The Water Cycle

  • Evaporation occurs when water changes from liquid to gas, primarily due to solar energy
    • Transpiration is the release of water vapor from plants through their leaves
  • Condensation happens when water vapor cools and forms liquid water droplets (clouds, fog)
  • Precipitation is the falling of water from the atmosphere to the Earth's surface (rain, snow, hail)
  • Infiltration describes the movement of water into the soil and groundwater
    • Percolation is the downward movement of water through soil and rock layers
  • Runoff is the flow of water over the Earth's surface, eventually reaching streams, rivers, and oceans
  • Groundwater storage occurs in aquifers, which are permeable rock layers that hold water
  • Sublimation is the direct change of water from solid (ice) to gas (water vapor), skipping the liquid phase

The Carbon Cycle

  • Photosynthesis is the process by which plants convert carbon dioxide and water into glucose and oxygen using solar energy
    • Carbon dioxide is absorbed from the atmosphere, and oxygen is released as a byproduct
  • Respiration releases stored energy in glucose, consuming oxygen and producing carbon dioxide (performed by plants, animals, and decomposers)
  • Decomposition breaks down dead organic matter, releasing carbon dioxide and nutrients back into the environment
  • Fossil fuel formation occurs when organic matter is buried and subjected to high pressure and temperature over millions of years (coal, oil, natural gas)
  • Combustion of fossil fuels releases stored carbon back into the atmosphere as carbon dioxide
  • Ocean absorption dissolves atmospheric carbon dioxide in seawater, forming carbonic acid and lowering ocean pH (ocean acidification)
  • Weathering of rocks consumes atmospheric carbon dioxide in chemical reactions, forming carbonate minerals
  • Volcanic eruptions release carbon dioxide from the Earth's interior back into the atmosphere

The Rock Cycle

  • Igneous rocks form from the cooling and solidification of magma (intrusive) or lava (extrusive)
    • Examples include granite (intrusive) and basalt (extrusive)
  • Sedimentary rocks form from the compaction and cementation of sediments (rock fragments, organic matter, chemical precipitates)
    • Examples include sandstone, limestone, and shale
  • Metamorphic rocks form when pre-existing rocks are subjected to high pressure and temperature, causing physical and chemical changes
    • Examples include marble (metamorphosed limestone) and gneiss (metamorphosed granite)
  • Weathering breaks down rocks into smaller fragments through physical (mechanical) and chemical processes
    • Physical weathering includes freeze-thaw cycles and abrasion
    • Chemical weathering involves dissolution and reactions with water and acids
  • Erosion is the transport of weathered rock fragments by water, wind, or ice
  • Deposition occurs when eroded sediments settle and accumulate in layers (deltas, floodplains, ocean floors)
  • Uplift and exposure bring buried rocks back to the surface through tectonic processes (mountain building)

Climate and Weather Patterns

  • Climate describes the long-term average weather conditions in a specific area
    • Factors influencing climate include latitude, altitude, ocean currents, and atmospheric circulation patterns
  • Weather refers to short-term atmospheric conditions (temperature, humidity, precipitation, wind)
  • Global wind patterns are driven by uneven heating of the Earth's surface and the Coriolis effect
    • Examples include trade winds, westerlies, and polar easterlies
  • Ocean currents redistribute heat and moisture globally, influencing regional climates (Gulf Stream, Kuroshio Current)
  • Jet streams are fast-moving air currents in the upper atmosphere that steer weather systems
  • El Niño and La Niña are periodic fluctuations in ocean temperatures and atmospheric pressure in the Pacific Ocean, affecting global weather patterns
  • Monsoons are seasonal wind patterns that bring heavy rainfall to tropical regions (South Asia, West Africa)
  • Greenhouse effect is the warming of the Earth's surface due to the absorption of infrared radiation by atmospheric gases (carbon dioxide, water vapor)

Human Impact on Earth's Systems

  • Deforestation removes trees, reducing carbon storage and altering local water cycles and biodiversity
    • Causes include agriculture, logging, and urbanization
  • Fossil fuel combustion releases greenhouse gases, contributing to global warming and climate change
    • Effects include rising sea levels, more frequent extreme weather events, and shifts in species distributions
  • Urbanization alters local climates through the urban heat island effect and changes in surface runoff and infiltration
  • Agriculture can lead to soil erosion, nutrient depletion, and water pollution from fertilizers and pesticides
    • Irrigation diverts water from natural systems and can cause salinization of soils
  • Overfishing disrupts marine food webs and can lead to the collapse of fish populations
  • Invasive species introduced by human activities can outcompete native species and alter ecosystem dynamics
  • Habitat fragmentation due to human infrastructure (roads, dams) can isolate populations and hinder species migration
  • Conservation efforts aim to protect and restore natural systems (protected areas, sustainable resource management)

Practical Applications and Case Studies

  • Studying Earth's systems helps predict and mitigate natural hazards (earthquakes, volcanic eruptions, hurricanes)
    • Example: monitoring seismic activity and volcano deformation to issue early warnings
  • Understanding the water cycle informs water resource management and flood control
    • Example: constructing dams and levees to regulate river flow and prevent flooding
  • Knowledge of the carbon cycle is crucial for developing strategies to reduce greenhouse gas emissions and combat climate change
    • Example: implementing carbon taxes and investing in renewable energy sources
  • Analyzing the rock cycle helps locate and extract valuable mineral resources (ores, fossil fuels)
    • Example: using seismic surveys and geological mapping to identify oil and gas reserves
  • Climate and weather data are used in agriculture, transportation, and energy production
    • Example: using seasonal forecasts to optimize crop planting and harvesting schedules
  • Recognizing human impacts on Earth's systems informs environmental policies and conservation efforts
    • Example: establishing marine protected areas to restore coral reefs and fisheries
  • Interdisciplinary research combines knowledge from multiple fields to address complex environmental challenges
    • Example: collaborations between geologists, ecologists, and social scientists to develop sustainable land-use plans


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© 2024 Fiveable Inc. All rights reserved.
AP® and SAT® are trademarks registered by the College Board, which is not affiliated with, and does not endorse this website.