Chapter 15: Air, Weather, and Climate

1. Chapter 15: Air, Weather, and Climate

2. 15.1 The Atmosphere Is A Complex System • Absorbed solar energy warms our world • Mostly Stored in the Oceans • The greenhouse effect is energy capture by gases in the atmosphere • “A Little Greenhouse Effect is a Good Thing” • Evaporated water stores energy, and winds redistribute it

4. Atmospheric Circulation

5. Climate Versus Weather

6. Climate is what you expect and weather is what you get

7. 15.2 Weather Events Follow General Patterns • Why does it rain? • The Coriolis effect explains why winds curve • Ocean currents modify our weather • Billions of people rely on seasonal rain • Frontal systems create local weather • Cyclonic storms can cause extensive damage

8. Why It Rains • Water Evaporates Out of Oceans • Minor Contribution from Lakes, Rivers, Land • About 13,000 km3 of water in atmosphere (> Lake Superior) • Only 1 ppm of total surface water • Condenses as Clouds • A 1 km3 cloud contains a few million kg of water • Collision of Cloud Droplets is too Slow • Bergeron Process • Water Evaporates off Ice Crystals and Condenses on Water Droplets

9. The Coriolis Effect

28. Not a Manifestation of the Coriolis Effect! • Too small scale for the Coriolis Effect to be significant

29. 15.2 Weather Events Follow General Patterns • Why does it rain? • The Coriolis effect explains why winds curve • Ocean currents modify our weather • Billions of people rely on seasonal rain • Frontal systems create local weather • Cyclonic storms can cause extensive damage

30. Fronts and Low Pressure Systems

31. World Hurricane Tracks 1995-2003

32. 15.3 Natural Climate Variability • Climates have changed dramatically throughout history • Earth’s movement explains some cycles • El Nifio is an ocean-atmosphere cycle • Recent changes are unusually rapid • The IPCC assesses data for policymakers

33. Post Ice-Age Climate • 11,000 Younger Dryas Cooling • 9,000-6,000 Mid-Holocene Warm Period (“Climatic Optimum”) • 900-1300 AD – Medieval Warm Period • 1300-1450 Little Ice Age I • 1450-1550 Partial Recovery • 1550-1800 Little Ice Age II

34. 15.4 How Do We Know Recent Climate Change Is Human-caused? • The IPCC finds overwhelming evidence of anthropogenic climate change • Argument from Authority • Read the Scientific Literature • CO2is the most important of many factors • Most Important Greenhouse Gas is Water Vapor • Explain How Increasing Greenhouse Gases Will Not Cause Warming

35. 15.5 What Are The Effects Of Climate Change, And Should We Care? • Global warming will be costly; preventing it might not be • Flooding, drought, storms, and disease are key risks • Some People Argue for Benefits • Longer Growing Seasons • More Habitable Land • Reduced Energy Costs

36. Possible Effects of Global Warming • More Heat Extremes • Drought • Rise in Sea Level • Temporary Severe Cold Spell? • Rapid Migration of Ecological Zones • More Biomass but Lower Nutritional Value

37. 15.6 Envisioning Solutions • The Kyoto Protocol called for a 5 percent reduction in carbon emissions • Stabilization wedges could work now • Alternative practices can be important • Regional initiatives are emerging • What Can You Do? Reducing Carbon Dioxide Emissions

38. What We Know and Don’t Know • Certain: Carbon Dioxide Increase • Nearly Certain: Climate is Warming • Debatable (Legitimately) • How much is of human origin? • Permanent or temporary warming? • Uncertain: • Can we do anything? • Will benefits exceed costs? • Risks of premature policy decisions?

39. The Spectrum of Skepticism