The Physical Environment
Outline of Topics
Physical Environment:
Climate and climate variation
Human impacts on climate
Peer-reviewed literature
Primary and secondary literature
Tips for reading and understanding
Applying these skills to a real paper
Ecology
Definition:
Ecology is the scientific study of how organisms interact with each other and their environment.
These interactions determine the distribution and abundance of organisms.
The Physical Environment
Role of Physical Environment:
Determines where organisms can live.
Determines resources available to organisms.
Affects the rate of population growth.
Components of the Physical Environment:
Climate: Long-term trends in temperature, wind, and precipitation.
Solar radiation drives climate systems, influenced by human impacts.
Chemical Composition:
Composition of air, water, and soil including salinity, acidity, and gas concentrations.
Energy Balance
Energy Inputs and Outputs:
Energy In: Shortwave, high energy (light + UV).
Energy Out: Longwave (IR), low energy (heat).
Greenhouse Effect
Natural Greenhouse Effect:
Greenhouse gases (GHGs) in the atmosphere absorb and re-radiate some infrared radiation.
Raises Earth’s temperature to livable range (from 0˚F to 59˚F).
Enhanced Greenhouse Effect:
Additional GHGs from human activities raise temperature further, contributing to climate change.
Latitude and Solar Radiation
Variation in Solar Radiation:
At the poles, sunlight spreads over a larger area and takes a longer path through the atmosphere.
Near the equator, sunlight strikes Earth perpendicularly.
Seasonal Distribution
Solstices and Equinoxes:
Solstice: December 21 (Southern Hemisphere summer) & June 21 (Northern Hemisphere summer).
Equinoxes: September 22 & March 20, equal day and night.
Seasonality at Different Latitudes:
Higher latitudes display greater variations in seasonal climate than lower latitudes.
Local Climate and Geography
Climate Patterns:
Horse latitudes have low precipitation, major deserts occur here.
Tropical region experiences significant and consistent precipitation.
Vertical Circulation of the Atmosphere:
Affects global wind patterns and resultant climate zones (Hadley cell, Ferrel cell, Polar cell).
Ocean Currents
Surface Currents: Warm and cool currents impacting global climate.
Upwelling:
Driven by wind, causes cool, nutrient-rich water to replace surface water.
Global Temperature Control
Temperature Influences:
Latitude, wind, ocean circulation, topography (elevation effects), and local geography.
Precipitation Patterns
Overall Trends:
Patterns driven by atmospheric circulation and topographic variations.
High precipitation near the equator, low in horse latitudes, deserts characterized by arid conditions.
Influences of Topography on Precipitation
Mechanism:
Air masses pick up moisture and release precipitation on windward slopes.
Leeward slopes experience dry conditions as descending air warms.
Continentality vs. Marine Climate
Continentality:
More extreme temperature variations; land heats and cools quickly.
Marine Climate:
More moderate temperatures; water's slow warming/cooling.
Marine Environment Characteristics
Physical Factors:
Oxygen variability, strong vertical gradients in temperature, light, nutrients, pressure.
Photic zones limit where photosynthetic organisms can survive.
Human Impact on Climate
Global Warming Trends:
Human activities have caused > 1.0°C warming since 1750.
2025 global temperature averages recorded at 1.17°C above 20th century averages.
Climate Predictions
Future Projections:
Increased frequency and intensity of extreme weather events in coming decades.
Scientific Methodology
Steps of the Scientific Method:
Developing hypotheses, designing experiments, collecting data, publishing results.
Scientific Literature
Peer-reviewed Literature:
Ensures quality and accuracy of scientific communication.
Importance of Reading Scientific Literature:
Provides foundation for fields of study and insights into research methodologies.
How to Read a Scientific Paper
Structure of Scientific Papers:
Title, abstract, introduction, methods, results, discussion, literature cited.
Reading Tips:
Skim and annotate papers, focus on methods, results, and discussions.
Practical Applications
Example Study:
Pinsky et al. (2013) explored how marine taxa track local climate velocities.
Findings indicate that climate velocity can effectively explain distribution shifts across marine species, more so than species characteristics.
Key Takeaway: Differences in climate variables lead to varied distribution shifts in marine species, indicating a complex response to climate change.