Bishop Bio 103 greenhouse effect
Energy Conversion and Greenhouse Effect
Energy loss through various mediums.
Example: Energy lost when a car passes through glass or atmosphere due to interaction with gas molecules.
Accumulation of gas molecules increases difficulty for radiation (heat) to escape.
Greenhouse Gases
Examples of greenhouse gases:
Carbon dioxide (CO₂)
Methane (CH₄)
Hydrofluorocarbons (HFCs)
Nitrous oxide (NOₓ)
Fluorinated compounds
Impact of greenhouse gases:
Increase in global temperatures and greenhouse effect.
Global Warming Potential (GWP)
Definition: A measure of how much heat a greenhouse gas traps in the atmosphere compared to CO₂ over a specific time period.
Significance:
Indicates the potential of a gas to contribute to global warming.
Baseline Comparison:
GWP is compared to CO₂ as the standard (GWP of CO₂ = 1).
Examples of GWP:
Methane has a GWP of 21 (it is 21 times more effective than CO₂ in trapping heat).
HFCs can have a GWP of up to 1000 times that of CO₂.
Concerns Regarding Global Warming Terminology
Importance of terminology in climate discussions:
"Global warming" reflects only temperature increases and doesn’t encompass all effects of climate change.
Examples of unintended consequences of global warming:
Melting glaciers leading to rising sea levels.
Changes in pH levels of oceans and extreme weather events.
Broader effects of climate change beyond just temperature rise.
Historical Temperature Records
Continuous monitoring of temperatures began in the 1870s with thermometers.
Limitations of historical data:
Only 150+ years of direct temperature measurements.
Other methods, like ice core analysis, can provide data spanning hundreds of thousands of years.
Ice Core Analysis
Methodology:
Ice cores extracted from glaciers in places like Antarctica.
Capture air bubbles from different periods (up to 600,000 years ago).
Purpose:
Provide indirect temperature records based on trapped gases within air bubbles.
Use of isotopic analysis to determine age of samples by comparing layers.
Glaciers vs. Ice Caps
Glacier: Terrestrial (land-based) ice which can form rivers or sheets.
Ice Cap: Floating ice formation, partially above water.
Locations of glaciers:
Significant glaciers in regions such as Greenland, Canada, and Montana (Glacier National Park).
Mount Kilimanjaro in Africa also has glaciers, but they are rapidly disappearing.
Impacts of Climate Change on Biodiversity
Current impact on species and biodiversity:
Extinction risk of many species due to changing climate.
Overall biodiversity is at risk, affecting ecosystems.
Critical to save biodiversity to maintain natural balance.
Climate Change Patterns and Trends
Rapid temperature increase is unprecedented compared to past natural fluctuations.
Potential for human-made factors (anthropogenic causes) driving climate change.
Feedback Loops and Albedo Effect
Positive feedback loops due to melting ice:
Loss of reflective snow and ice increases heat absorption, leading to further warming.
Albedo effect:
Surfaces covered in ice reflect sunlight, while darker surfaces increase heat absorption.
Discussion about Ocean Currents
Importance of ocean currents like the Gulf Stream:
Moderates climate in Western Europe.
Impact of melting glaciers on salinity and temperature of ocean currents.
Misrepresentation in media:
Movies like "The Day After Tomorrow" suggest rapid climate shifts that are scientifically implausible.
Climate and Precipitation Patterns
Climate change alters precipitation patterns:
Regions that are inherently wet become wetter, while dry regions become drier.
Water scarcity is becoming a profound issue:
Example: Great Lakes coalition to prevent water diversion due to climate concerns.
Increasing conflict in regions experiencing drought due to competition for limited water resources.
Conclusion
Reinforcement of the idea that while ecosystems may shift, the planet itself will endure.
Importance of biodiversity and human survival in the context of climate change.
Encouragement to study environmental science for deeper understanding of these issues.