Introduction to Climate Change - Climate Change Adaptation And Mitigation | Lecture Notes - YNetStudyHub
Climate Change Adaptation And Mitigation

Introduction to Climate Change

2 mins read 373 words Topic 1 of 8
Study with AI Tutor Learn 2× faster Instant Q&A Quiz practice
Launch AI Lesson
Text Size:
PDF Save

This topic introduces the concept of climate change, its causes, and the potential impacts it has on the environment and society.

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


1. What Is Climate Change?

Term Meaning
Climate The long‑term (30‑year+) average of temperature, precipitation, wind, etc., for a region.
Weather Short‑term atmospheric conditions (hours‑days).
Climate Change A statistically significant shift in the average state of the climate or its variability over periods of decades to millennia.
Global Warming The observed rise in Earth’s average surface temperature, primarily caused by increased greenhouse gases (GHGs).

Key point: Global warming is a driver of broader climate change, which includes changes in precipitation patterns, sea‑level rise, and extreme‑event frequency.


2. The Science Behind Climate Change

2.1 The Greenhouse Effect

  1. Solar radiation reaches Earth → some is reflected, most is absorbed.
  2. The surface re‑emits infrared (IR) radiation.
  3. Greenhouse gases (GHGs) such as CO₂, CH₄, N₂O, and water vapor absorb IR and re‑radiate it back, warming the lower atmosphere.
Greenhouse Gas Primary Sources Atmospheric Lifetime
CO₂ (Carbon Dioxide) Fossil‑fuel combustion, cement production, deforestation Decades to centuries
CH₄ (Methane) Agriculture (ruminants), landfills, natural gas systems ~12 years
N₂O (Nitrous Oxide) Fertilizer use, industrial processes ~114 years
Fluorinated gases (e.g., HFCs) Refrigerants, electronics 10–10,000 years

2.2 Radiative Forcing

  • Definition: The net change in Earth’s energy balance (incoming vs. outgoing radiation) caused by a factor (e.g., GHG concentration).
  • Positive forcing → warming; negative forcing → cooling.

The Intergovernmental Panel on Climate Change (IPCC) estimates that human activities have produced a +2.3 W m⁻² radiative forcing (2021 data), driving the observed warming.

2.3 Feedback Mechanisms

Feedback Effect on Climate Example
Water‑vapor feedback Positive Warmer air holds more vapor → more greenhouse effect.
Ice‑albedo feedback Positive Melting ice reduces reflectivity → more solar absorption.
Carbon‑cycle feedback Mixed Permafrost thaw releases CO₂/CH₄ (positive).
Cloud feedback Uncertain (both) Changes in cloud type/altitude affect radiation.

3. Evidence of Climate Change

Indicator Observed Trend (1900‑2020) Data Source
Global mean surface temperature +1.1 °C ↑ NASA GISS, NOAA
Ocean heat content ↑ ~30 % in upper 200 m ARGO floats
Sea‑level rise 3.3 mm yr⁻¹ (average) Satellite altimetry
Arctic sea‑ice extent (Sept) ↓ ~13 % per decade NSIDC
Glacial mass loss Millions of gigatonnes lost GRACE satellites
Extreme weather frequency
Topic Concept Map
Ask AI Tutor 24/7 Live

Click any prompt to explore this topic interactively with your AI Tutor:

Explain in simple terms Give me 3 practice exam questions Summarize key principles in 5 points
Unit Syllabus 8 Topics
Introduction to Climate Change
Climate Change Adaptation Strategies
Upgrade
Mitigation Techniques for Climate Change
Upgrade
Policy and Governance in Climate Change
Upgrade
Climate Resilience and Vulnerability Assessment
Upgrade
Economic Implications of Climate Change
Upgrade
Community Engagement and Climate Action
Upgrade
Climate Change Communication and Education
Upgrade