Introduction to Climate Change - Climate Change And Natural Resources | Lecture Notes - YNetStudyHub
Climate Change And Natural Resources

Introduction to Climate Change

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This topic will cover the basic concepts of climate change, including the greenhouse effect, global warming, and the impact of human activities on the Earth's climate system.

Introduction to Climate Change
(A concise, easy‑to‑read overview for students and anyone new to the topic)


1. What Is Climate Change?

Term Definition
Climate Long‑term patterns of temperature, precipitation, wind, and other atmospheric variables (typically averaged over 30 + years).
Weather Short‑term atmospheric conditions (hours to days).
Climate Change A measurable shift in the average state of the climate system, or its variability, over periods ranging from decades to millions of years.
Global Warming The specific aspect of climate change that refers to the rise in Earth’s average surface temperature, primarily due to human activities.

2. Why Is the Climate Changing Now?

2.1 Natural Drivers (historical background)

  • Solar variability – changes in the Sun’s output.
  • Volcanic eruptions – inject aerosols that temporarily cool the planet.
  • Orbital cycles (Milankovitch cycles) – affect the distribution of sunlight.
  • Land‑use changes – natural shifts in vegetation and surface albedo.

2.2 Anthropogenic (human‑caused) Drivers

Source Main Greenhouse Gases (GHGs) Typical Emissions
Fossil‑fuel combustion CO₂, CH₄, N₂O Power plants, transport, industry
Agriculture & livestock CH₄, N₂O Enteric fermentation, rice paddies, fertilizer use
Deforestation & land‑use change CO₂ Forest clearing, soil disturbance
Industrial processes HFCs, PFCs, SF₆ Refrigerants, electronics, metal production

Result: Concentrations of CO₂ have risen from ~280 ppm pre‑industrial to >420 ppm today, trapping more infrared radiation and warming the planet.


3. The Greenhouse Effect – How It Works

  1. Solar radiation (short‑wave) reaches Earth’s surface and is absorbed.
  2. The surface re‑emits energy as long‑wave infrared radiation.
  3. Greenhouse gases absorb and re‑emit part of this infrared radiation, sending some back toward the surface → warming.

Key gases: CO₂, CH₄, N₂O, water vapor (feedback), and synthetic gases (HFCs, etc.).


4. Observed Impacts (What the Data Show)

Indicator Recent Trend (≈ last 50 yr) Typical Consequence
Global mean surface temperature +1.2 °C relative to 1850‑1900 Heatwaves, altered ecosystems
Sea level +20 cm (global average) Coastal flooding, saltwater intrusion
Arctic sea‑ice extent ~‑13 % per decade Habitat loss, albedo feedback
Ocean heat content ↑ ~ 30 % in upper 200 m Coral bleaching, marine species shift
Extreme weather events ↑ frequency/intensity of heatwaves, heavy precipitation, droughts Economic losses, human health risks
Phenology (timing of biological events) Earlier flowering, migration Mismatch in food webs

5. Climate Feedbacks

| Feedback Type | Positive (amplifying) | Negative (dampening) | |---------------

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Unit Syllabus 8 Topics
Introduction to Climate Change
Natural Resources and Climate Change
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Mitigation Strategies for Climate Change
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Adaptation to Climate Change
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Climate Change and Food Security
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The Role of Policy and Governance in Addressing Climate Change
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Case Studies on Climate Change and Natural Resources
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The Economics of Climate Change
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