The earth's surface is a vast area of 500millionsquarekilometers where four vast open systems interact
System
A functional whole, composed of organized, Interacting, Interdependentparts
Physical systems
Also known as the natural systems
Spheres
Atmosphere
Hydrosphere
Lithosphere
Biosphere
Environmental Spheres
Abiotic (non-living)
Biotic (living)
AbioticSpheres
Atmosphere
Hydrosphere
Lithosphere
Biotic Sphere
Biosphere (ecosphere)
Earth's four major spheres or systems
Hydrosphere
Biosphere
Lithosphere
Atmosphere
Atmosphere
The gaseous blanket of air that envelops, shields, and insulates the earth
The movements and processes of the atmosphere create the changing conditions that we know as weather and climate
Biosphere
Composed of all living things: people, other animals and plants
Lithosphere
Comprised of the solid earth-rocks, soil, landforms and the minerals
Hydrosphere
Comprised of the waters of the earth-oceans, lakes,rivers & the glaciers
It is the nature of these four major subsystems and the interactions among them that create and nurture the conditions necessary for life on Earth
The impact and intensity of interactions among earth's subsystems are not identical everywhere on our planet, and it is these variations that lead to the geographic patterns of environmental diversity
Physical Systems
Atmosphere
Lithosphere
Hydrosphere
Biosphere
Processes in the physical system
Atmospheric processes
Geomorphic processes
Tectonic Plate Movements
Biotic processes
Hydrologic processes
The atmosphere of the earth extends nearly 563 km (350 miles out) from the solid surface of the Earth
The atmosphereismadeupofamixtureofdifferentgasesthatcombine to allow life to exist on the planet
Gases in the lower layer atmosphere
Nitrogen (78%)
Oxygen (21%)
Carbon dioxide (vital to plant growth)
Layers of the atmosphere
Troposphere
Stratosphere
Mesosphere
Thermosphere
Troposphere
The lowest of the atmospheric layers and extendsfromtheearth'ssurfaceuptoabout14km in altitude
It extends to about 17km above the sea level at the equator and about 8km over the poles
The thickness of the troposphere varies with altitude and the seasons
The outer boundary of the troposphere is the tropopause
All human activities occur in the troposphere
It is the layer where all weatherweexperiencetakesplace
Stratosphere
Beyond the tropopause
Temperature remains constant to a height of about 20 km and then begins a gradual increase that continues until the stratosphere
Temperatures increase in the stratosphere because it is in this layer that the atmosphere's ozone is concentrated
The ozone absorbs ultraviolet radiation from the sun as a result, the stratosphere is heated
Most commercial aircrafttraveltakesplace in the lowerpart of the stratosphere
Ozone Layer
Contained within the stratosphere, mainly located in the lower portion from about 15-35 km
Absorbs most of the sun's ultraviolet radiation, especially UVB
Mesosphere
Above the stratosphere, a middle layer separating the lower stratosphere from the Thermosphere, extending from 80to90km
Military aircraft travel at much higher altitude with some classified stealth aircraft
Thermosphere
The change over from the Mesosphere begins at the height of 80km
The temperature in this layer is very high due to gases moving at very high speeds
The Aurora Borealis (northern lights) and Aurora Australis (southern lights) occur in this layer
Ionosphere
Part of the atmosphere that is ionized by solar radiation
Overlaps both the exosphere and the thermosphere
Forms the inner edge of the magnetosphere
Influences radio propagation on Earth
Responsible for auroras
Hydrosphere
The combined mass of water found on, under, and over the surface of the earth
Water is the most distinctive substance found on earth, it set the stage for the evolution of life and is still an essential ingredient of all life today
Surface water occupies 97% of the surface area of the earth
Forms of water on Earth
Liquid (seas, rivers)
Solid (ice)
Gas (water vapour)
The great majority of the world's moisture is in the form of liquid
Water Cycle
The circulation system which carries water from the oceans, through the atmosphere, to the land and backtothesea
The water cycle is a closed system, no water actually leaves the circulation system
The water cycle is powered by the energy from the sun
Water is a renewable resource, if used and managed properly it can be replaced or renewed
Processes in the water cycle
Evaporation
Condensation
Precipitation
Infiltration
Runoff
Transpiration
Evaporation
The process by which water changes from a liquid into a gas and becomes water vapor
Condensation
The reverse of evaporation, when water vapor changes from a gas to a liquid
Transpiration
The process by which plants discharge water vapour into the atmosphere
Evapotranspiration
The combined water loss into the atmosphere from evaporation and transpiration