🏝️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.
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