Definition of Weather: Weather refers to short-term atmospheric conditions, including temperature, humidity, precipitation, and wind, occurring at a particular time and place.
Definition of Climate: Climate is the long-term average of weather patterns over extended periods (typically 30 years or more). It encompasses variations and trends in weather phenomena across seasons, years, and geographical areas.
Key Differences:
Duration: Weather is short-term; climate is long-term.
Variability: Weather can change rapidly; climate changes gradually over decades.
What is the Atmosphere?: The atmosphere is a layer of gases surrounding the planet, held in place by gravity.
How does Earth have an Atmosphere?: Earth's atmosphere is maintained by gravitational attraction, allowing gases to be held close to the surface.
Contribution to Weather and Climate:
The atmosphere plays a crucial role in weather patterns, as it contains water vapor that forms clouds and precipitation.
It regulates climate by distributing solar energy across the planet through convection currents, influencing temperature and weather systems.
Incoming Solar Radiation: The Earth receives varying amounts of solar energy, approximately 343 Watts/m², which is partially reflected by the atmosphere and Earth's surface.
Outgoing Solar Radiation: After absorption, the Earth emits infrared radiation, averaging about 210 Watts/m², some of which escapes into space.
Greenhouse Gases:
Some infrared radiation is absorbed and re-emitted by greenhouse gases, resulting in warming of the Earth's surface and troposphere.
This mechanism is essential for maintaining a habitable temperature on Earth.
Bottom Two Layers of the Atmosphere:
Troposphere: The lowest layer, where weather occurs and temperature decreases with altitude.
Stratosphere: Above the troposphere, contains the ozone layer, which absorbs and scatters ultraviolet solar radiation.
Greenhouse Gases and Temperature Regulation:
Greenhouse gases trap heat, preventing extreme temperature fluctuations between day and night.
Seasons:
Caused by Earth's tilt and orbit around the sun, leading to varying sunlight distribution throughout the year.
Role of Convection Currents: Convection currents move energy through the atmosphere via warm air rising and cooler air descending, creating wind.
Impact of Axis Tilt:
If Earth were not tilted, there would be minimal seasonal variation, impacting climate patterns.
Objective: To explore how the angle of insolation affects energy per unit area:
Insolation: Refers to solar radiation energy received on a given surface area during a specific time.
Definition: Convection currents are fluid movements caused by temperature differences, resulting in warm, moist air rising from the equator and cooler, denser air sinking toward the poles.
Temperature Imbalance: Heating leads to a movement of warmer air, contributing to global wind patterns.
Temperature vs. Heat: Temperature measures how hot or cold something is; heat refers to the transfer of thermal energy.
Heat Distribution: Heat moves throughout the Earth system via conduction, convection, and radiation processes.
Key Water Flows: Discusses the Atlantic Meridional Overturning Circulation:
Factors Involved: Sea ice, Gulf Stream, and varying water temperatures contribute to this flow and overall climate.
Reflectivity: Different surfaces absorb or reflect solar energy differently:
Thick clouds: 70-80%
Grass: 5-25%
Dark roof: 10-15%
Snow: 50-90%
This absorption affects local temperatures and climate.
Convection Cell Diagram: Diagrams should show the cycle of warm air rising and cool air sinking.
Latitudinal Air Motion: Expect rising air near the equator (tropics) and sinking air near poles (subtropics) due to temperature differences.
High-Pressure areas: Regions where descending dry air creates desert conditions.
Connection: This pattern explains arid zones found in these transitions.
Mechanism: Ocean and air currents are critical in distributing heat.
Matter's Role: Water plays a significant role in energy transfer due to its heat capacity and movement.
El Niño: Characterized by warmer ocean currents, leading to increased rainfall in certain regions.
La Niña: Features cooler ocean currents, often resulting in drought conditions.
Impact of Rising Air: Affects the size of the polar vortex and climate patterns in the U.S., potentially leading to diverse weather phenomena.
Jet Stream Effects: El Niño and La Niña cause significant shifts in the jet stream patterns, influencing weather conditions across continents.
Niño Index values: Analysis of temperature changes provides insights into the health of ocean systems and predictions for climatic events.
Correlation Analysis: Evaluating the relationship between El Niño conditions and temperature changes on a global scale.
Core Questions:
What is climate change?
What evidence indicates climate change?
What causes these changes and possible implications for the future?
Definition: Climate change refers to significant changes in temperature and weather patterns over extended periods, specifically the recent rise in Earth's average temperature.
Projection Models: Data indicates expected changes in global temperatures based on various scenarios, showcasing the impact of both observed and modeled changes.
Various Models: Present data on anticipated temperature variations through different greenhouse gas emission scenarios.
Representation: Indicates fluctuations in temperature over decades, showing clear trends toward warming.
Data Analysis: Comparing surface temperature records aids in understanding historical climate patterns.
Indicators of Change: Use of colored scales to visualize warming and cooling trends over time.
Interpreting Data: The blue line represents average temperatures, while red bars represent anomalies, indicating significant temperature increases.
Key Concepts:
The importance of accurately defining climate change versus global warming.
Understanding proxies and their usefulness in climate science.
Possible Indicators:
Glacial retreat
Changes in plant and animal habits
Ocean temperature increases
Expectations: Explanation of what these changes indicate in light of rising temperatures.
Factors:
Glacial melting, snow cover reduction, sea-level rise, and temperature changes in oceans and air.
Conclusion: The impact of climate change on ecosystems and wildlife observed in regions like Yellowstone.
Data Visualization: Interpretation of geographical temperature changes and what these suggest for regional climate impacts.
Trends: Analysis showing increased ocean heat content over decades and its implications for global weather patterns.
Predictions: Expected shifts in rainfall patterns in various months as a result of climate scenarios projected for the future.
Various Explanations:
Changes due to solar radiation
Natural variability influences
Anthropogenic causes linked to emissions.
Simulation Insights: Examination of climate models and their results regarding natural and anthropogenic factors.
Milankovitch Cycles: Explain how these cycles affect seasonal and temperature changes on Earth's surface.
Data Correlation: Understanding how graphs show the interplay between CO2 levels and temperature over time.
Assessment of Forces: Comparison of models showing natural versus human-induced climate changes.
Impact Measurement: Indicating the changes due to human activity and natural phenomena from 1750-2011.
Mechanism: Understanding how increased gas emissions contribute to climate change and the dual nature of the greenhouse effect.
Contribution: Identification of key contributors to greenhouse gas emissions and their potential effects on global warming.
Breakdown: Overview of GHG emissions broken down by economic sectors and types of gases.
Key Gases: Identifying dominant greenhouse gases affected by human activity, especially CO₂, and their impact on temperature.
Supportive Evidence: Outlining sources of evidence supporting climate change and potential global actions to mitigate its impact.
Thermal Reservoirs: Analysis of energy storage across different Earth's components – oceans, atmosphere, and land forms.
Reflection and Absorption: Discussing the implications of decreasing ice cover on heat absorption and its role in climate feedback loops.
Trends and Cities: Exploring global emissions trends from various regions and their implications for climate policy.
Future Indicators: Climate model predictions regarding CO2 emissions and their expected surface temperature rise.
Anticipated Impacts:
Rising sea levels
Increased frequency and intensity of weather events
Ecosystem disruptions
Food security issues
Loss of biodiversity.
Assessing Certainty: The reliability of climate change predictions based on varying confidence levels.
Temperature Changes Analysis: Investigating temperature predictions for regions under multiple scenarios to understand potential impacts.
Analysis of Extremes: Identifying areas most vulnerable to significant temperature changes as a result of climate change.
Long-Term Climate Changes: Examining trends showing predicted increases in temperature averages over time.
Long-Term Evaluation: Importance of reviewing comprehensive data sets for proper understanding of climate trends.
Interruptions in Trends: Discussing periods without temperature rises coinciding with increased emissions, emphasizing variability.
Understanding Fluctuations: Evaluation of global temperature anomalies and their implications for climate studies.
External Influences: Discussing how volcanic activity and El Niño events can abruptly alter temperature patterns.
Regional Effectiveness: Noting specific impacts of climate change in the Pacific Northwest, including warming temperatures and changing precipitation patterns.
Data Evaluation: Emphasizing the importance of accurate data representation and avoiding selective data interpretation.
Misconceptions: Debunking fallacies regarding periods of no warming amid increasing greenhouse gas concentrations.
Trend Stability: Analysing current trends confirming ongoing consistent warming despite temporary fluctuations.
Regional Climate Changes: Understanding how different regions respond to broader climate phenomena—including warming and alterations in precipitation.
Future Climate Impacts: Discussing potential future climate scenarios focusing on extreme weather events and ecological changes.
Long-term Observations: Analyzing shifts in weather patterns and their implications for climate science.
Significant Variations: Noting the impacts of climate change on ecosystems—including shifts in species distribution and agricultural productivity.
Understanding Long-term Trends: Use of comprehensive historical data to understand current climatic trends and future projections.
Evaluating Yearly Stabilities: Investigating long-term fluctuations and their implications for winter sports, water supplies, and ecosystems.
Climate Sensitivity: Evaluating the stability of snowpack levels over lengthy periods and identifying influencing factors.
Longitudinal Data: Evaluation of varying temperature changes, accentuating the need for comprehensive analysis to understand climate trajectory.
Impacts Across Decades: Analyzing expected impacts of warming in future decades, focusing on mid-century and late-century scenarios.
Forecasting Changes: Discussing changes in temperature expectations reaching further into the 21st century.
Temperature Changes: Continued predictions of changes throughout various timeframes and the anticipated impact on global conditions.
Weather Data Evaluation: Using hydrological data models to gauge water vapor changes and implications for weather prediction accuracy.
Global Warming Effects: Potential consequences on environment, economy, and social structures, including shifting agricultural zones and resource availabilities.
Anticipated Changes: Discussing notable impacts, including extreme weather events and agricultural shifts affecting food security.
Essential Questions: A summary of critical questions regarding atmospheric understanding, greenhouse effects, and the importance of recognizing various sources of climate change evidence.