Climate Change and Its Effects

Overview of Course Structure

  • First homework due this weekend.

    • Worth approximately 10 points.

    • Content is manageable, with three homework assignments throughout the semester.

  • Homework submission will be done via HuskyCT.

  • The first assignment will be released tomorrow at 9 AM.

    • The assignment will consist of a worksheet based on a video watched.

  • Deadline for completion: Monday at 9 AM.

  • Deadlines are strict; extensions are not typically granted except for technical issues.

    • Students should contact the instructor via email if submission issues arise.

  • Submissions must be in .doc or .pdf format.

    • Links to documents will not be accepted.

  • Multiple options for completing homework:

    1. Handwriting, scanning via phone (most modern phones can scan documents).

    2. Typing responses directly in a document editor.

  • Emphasis on personal input over AI-generated responses:

    • Students are encouraged to reflect on their learning without relying on AI tools like ChatGPT.

    • If AI usage is suspected, students may receive a zero.

    • Students can discuss any discrepancies if they believe they did not use AI.

Introduction to Climate Change

  • Today's lecture will cover the scientific aspects of climate change, connected to global change concepts.

  • Objective of the course:

    • To build an understanding of climate change causes, consequences, and impacts.

    • To simplify scientific concepts so all students can understand.

Distinction between Weather and Climate

  • Definitions:

    • Weather: Refers to short-term atmospheric conditions.

    • Example: Snow one day and sun the next in Connecticut.

    • Climate: Describes long-term average weather patterns in a specific area.

    • Climate includes statistical properties like average temperature and variance over long periods (years).

  • Importance of distinguishing weather from climate:

    • Weather represents immediate atmospheric conditions and is difficult to predict accurately.

    • Climate is easier to model due to the long-term data available.

Climate System Elements

Atmosphere

  • The atmosphere's thickness:

    • Measures approximately 100 kilometers (60 miles) from Earth's surface.

  • Dense with various gases that contribute to climate dynamics.

Oceans

  • Oceans cover 71% of Earth's surface and significantly influence climate.

    • Average depth of the oceans: 2.3 miles.

    • Ocean conditions affect global climate through water vapor and temperature exchanges.

Land

  • Land accounts for approximately 29% of Earth's surface, influencing weather and climate through its absorption and reflection properties.

  • Freshwater is less than 1% and is critical in land ecosystems.

Solar Influence

  • The sun's role is significant:

    • Its energy drives atmospheric circulation and weather patterns.

    • Solar variations and Earth's position also affect climate conditions over time.

Atmospheric Circulation

  • Air circulation is crucial in climate regulation:

    • Warm air is less dense and rises.

    • Cold air is denser and sinks.

  • Hadley Cells: Air movement around the equator creates large-scale air circulation patterns termed Hadley cells.

  • Trade winds are produced by the interaction of these air cells with Earth's rotation.

  • Circulation impacts weather and climatic conditions worldwide.

    • At the equator, warm air creates a lot of precipitation due to its rise and cooling.

Greenhouse Gas Effect

  • The greenhouse gas effect explains how certain gases warm the Earth's atmosphere:

    • Solar radiation hits Earth, with some energy reflected back into space.

    • Greenhouse gases absorb and radiate heat back towards Earth's surface, maintaining temperate conditions for life.

  • Key greenhouse gases include:

    • Carbon dioxide (CO$_2$)

    • Methane (CH$_4$)

    • Nitrous oxide (N$_2$O)

  • Increased concentrations of these gases enhance the greenhouse effect, leading to global warming.

Cloud Effects on Climate

  • Clouds can cool Earth's surface by reflecting solar radiation.

    • Albedo Effect: Measurement of reflectivity of different surfaces.

    • Lower clouds reflect about 90% of sunlight, cooling the surface.

  • Day vs. Night Effects:

    • During the day, clouds tend to cool the surface; at night, they trap heat and keep the surface warmer.

Ocean Dynamics

Ocean's Role

  • Oceans are essential for:

    • Providing water vapor, a major greenhouse gas.

    • Absorbing and storing carbon dioxide, impacting atmospheric levels.

  • Evaporation from oceans contributes significantly to greenhouse gas concentrations.

Nutrient Upwellings

  • Upwellings bring nutrients to the ocean surface, promoting marine biodiversity:

    • Nutrient-rich areas lead to higher biological productivity.

Carbon Cycles

  • Two carbon cycles influence climate regulation:

Slow Carbon Cycle

  • Involves geological processes and long-term weathering of rocks.

  • Operates over millions of years, balancing CO$_2$ levels through sedimentation and volcanic activity.

Fast Carbon Cycle

  • Driven by biological processes like photosynthesis and respiration.

  • Carbon moves rapidly through ecosystems and the atmosphere; significantly faster than the slow cycle.

Climate Variability: El Niño and La Niña

  • El Niño Southern Oscillation (ENSO) significantly affects global climate variability:

    • Characterized by fluctuations in wind patterns and sea temperatures.

    • Alters weather scenarios, causing extremes like droughts and heavy rainfall events.

Historical Climate Changes

  • Volcanic eruptions, plate tectonics, and carbon cycling have historically altered climates:

    • Different periods of icehouse (cold) and greenhouse (warm) phases.

    • Current climate is warming in an icehouse phase, driven by anthropogenic emissions.

  • Scientific records show an increase in global temperatures and CO$_2$ concentrations since the 1800s, significantly correlating with human activities.

  • Historical data from the Mid-Miocene reflects potential consequences of current temperature increases.

Conclusion and Next Steps

  • Homework assignment #1 involves analyzing changes impacting food systems in the context of climate change and will dive deeper into the Anthropocene.

  • Assignment reference: Video “In Solving the Maze: A Big History of Food Complexity.”