Earth’s Major Spheres
Core Idea: We all are connected
Earth has four major spheres that constantly interact with each other
Hydrosphere-water
Lithosphere-land/rock
Atmosphere-air
Biosphere-all living things
Big Idea: Nothing on earth works in isolation, everything affects everything else
Concept of interconnectedness is central to Indigenous worldviews
Became mainstream with modern environmental movement in 1970
Earth’s four spheres
At any moment, matter exists in one of the four spheres
If one sphere is disturbed, the others are affected too
Hydrosphere
All forms of water on earth including
Oceans
Lakes
Rivers
Snow
Glaciers
Water underneath the surface
Water vapour in air
Cycles through ecosystems through 3 processes
Evaporation-water turns to vapour (heat)
Condensation-vapour turns to clouds
Precipitation-rain, snow falls back down
Geosphere
Contains all of the solid, rocky parts of the Earth
Planet’s surface (crust)
Semi solid land underneath crust (mantle)
Liquid land near the center of the planet (core)
Lithosphere/Major landforms
Contains the crust and uppermost part of the mantle
Includes various landforms like mountains, valleys, rocks, minerals, soil
Lithosphere is constantly being shaped by external forces such as the sun, wind, ice, water and chemical changes
Atmosphere
The gaseous part of Earth
Upper portion protects living things from the sun’s harmful UV radiation and absorbs and emits heat
Further away from the earth=lower air pressure
The Sun’s role in Earth Sphere
Solar energy is absorbed (taken in) and reflected (bounced back) by the atmosphere and surface
Heats earth’s surface unevenly
Global winds and ocean currents move heat around planet and redistribute heat
Solar energy enters the biosphere through photosynthesis and cellular respiration
At the equator sun rays hit directly-more heat concentrated
At the poles sun rays hit at an angle-heat spreads over a larger area-less warm
Because the earth is curved…
Strikes earth at different angles
Lower latitudes (near equator) receive more direct solar energy
Higher latitudes (near poles) receive less enrgy
Global winds system
How wind is created (convection currents)
Warm air near earth’s surface rises (warm air is lighter)
As it rises it cools down
Cool air is denser so it sinks back down
This sinking cool air creates wind that pushes warm air around
Coriolis effect- a change in the direction of moving air, water or other objects due to Earth’s rotation
When air temperature changes-weather occurs
Trade winds-near equator
Westerlies-mid latitudes
Polar easterlies-near the poles
Ocean currents
Move thermal energy around Earth
Surface currents are created by wind
Five major sets of surface currents (one in each ocean basin)