Title: The Nature of Physical Geography
Course: Geography 102: Physical Geography
Institution: Fullerton College
Definition:
Geography originates from the Greek terms:
geo meaning "Earth"
graphein meaning "to write"
Characteristics of Geography:
It is a method rather than just a body of knowledge
Holistic approach: considers entire systems
Eclectic: incorporates various disciplines
Utilizes spatial analysis: examining the arrangement of phenomena across space
Employs Earth systems science: interdisciplinary approach combining physical and human geography
Understanding Science:
Science encompasses more than just the scientific method
Example contrast: Science can explain technical capabilities (like cloning a T. rex)
Humanities provide perspectives on ethical considerations (such as the implications of cloning)
Scientific Method Steps:
Observe phenomena
Formulate a hypothesis
Design an experiment
Predict outcomes
Conduct the experiment
Draw conclusions
Achieve scientific “proof”
Scientific Theory:
Explanation of natural events validated through repeated observations
Scientific Law:
A statement of observed phenomena consistently holding true
Examples often misinterpreted as mere theory (e.g., gravity and evolution)
Systems Theory:
A system is interrelated components working together for a process
All systems need an energy source
Types of systems:
Open Systems: interact with surroundings
Closed Systems: isolated from external influences
Feedback and Equilibrium:
System feedback mechanisms and maintaining equilibrium
Inputs:
Energy and material (e.g., fuel, oxygen, water)
Outputs:
Products/resulting matter (e.g., exhaust gases, waste, mechanical motion)
Automobile Example:
Inputs: fuel, oil, tires, resources
Outputs: heat loss, waste, debt
Water Cycle Processes:
Involves various stages: precipitation, evaporation, condensation, etc.
Examples of storage: in ice, atmosphere, oceans, groundwater, etc.
Highlight the interconnectedness and flow of water through systems
Plant Processes:
Input of CO2 and H2O, conversion into sugars (energy)
Photosynthesis: harnessing sunlight and transforming it into chemical energy
Respiration: breaking down sugars for energy release
Water transpiration's role in maintaining plant health
Concepts:
Positive Feedback: reinforces the initial stimulus, accelerating change
Negative Feedback: counteracts the initial stimulus, promoting stability
Equilibrium refers to a stable state of a system
Example:
Florida's Atlantic coast demonstrates dynamic equilibrium through continuous sand erosion and deposition by ocean currents
Indicates balance and interaction of natural forces
Four Primary Spheres:
Atmosphere: air and gases
Lithosphere: Earth's solid structure
Hydrosphere: water in all forms
Cryosphere: ice domains
Additional Sphere:
Biosphere: all living organisms
Anthrosphere: human influence on the environment
Circumference Measurements:
Polar: 40,008 km
Equatorial: 40,075 km
North and South Pole measurements indicate geoidal bulge variations
Importance of Location:
Accurate location is critical for geographic analysis
Based on Earth's rotation axis leading to the definition of coordinate systems such as latitude and longitude
Graticule: grid overlay for map representation
Latitudes:
Parallels measure angles north/south of equator
Significant latitudes:
Tropic of Cancer (23.5° N)
Equator (0°)
Poles (90° N/S)
Arctic/Antarctic Circles (66.5° N/S)
Latitude zones defined by these markers
Zones Defined:
Arctic: 66.5° N to North Pole
Subarctic: 55° N to 66.5° N
Midlatitude: 35° N to 55° N
Subtropical: 23.5° N to 35° N
Equatorial/Tropical: 23.5° N to 23.5° S
Antarctic Zones similarly defined
Longitudes:
Meridians measure angle east/west from Prime Meridian in Greenwich
They converge at poles, critical for geographic description and navigation
Definition:
Great circles bisect the sphere and pass through its center
They indicate the shortest path between two points on the globe
Circle of illumination and small circles also explained
Visual Differentiation:
Each pair of meridians creates a great circle; parallels (except the equator) form small circles
Great circles provide equal halves, whereas small circles divide the globe unequally