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Natural Mechanisms of Climate Change. How do we know about past climates?. Paleoclimatology - the study of the history of the earth’s climate Using: ice cores, tree rings, and lake bottom sediment. External Forces – beyond earth. Solar Energy- changes in 3 ways:
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How do we know about past climates? • Paleoclimatology- the study of the history of the earth’s climate • Using: ice cores, tree rings, and lake bottom sediment
External Forces – beyond earth • Solar Energy- changes in 3 ways: • 1. Shape of earth’s orbit – sometimes circular, sometimes elliptical • 2. Changes in earth’s tilt – currently at 23.5 degrees • Varies from 22-25 degrees over 41,00 yr cycle • Smaller the tilt means less seasonal variation.
Ocean Causes Changes • Change climates along the coasts theyu flow • Change in temp • Change in the Great Ocean Conveyor
Volcanic Activity • Releases SO2 which forms sulfic acid and reflects sunlight • Releases huge amounts of ash and dust -blocks the sun • Short tem
Atmospheric Albedo • The reflective property of the atmosphere (amount of sunlight atmosphere reflects) • An ↑ in clouds means an ↑ in reflection • A ↓ in clouds means a ↓ in reflection • The more sunlight that reaches Earth the temp ↑
Surface Albedo • Earth’s reflective capacity • Includes land, snow, water, and ice • Ice and snow reflect, land absorbs • As ice and snow melt, less sunlight is reflected, more is absorbed, temp ↑
Asteroids and Meteoroids • If huge ones impact Earth, large amounts of dust and debris in atmosphere • May block out the sun • Leading theory on what killed the dinosaurs
Plate tectonics • Changes where glaciers can form • Changes the flow of currents • Changes the climates on different continents • Redistributes the areas of absorption of solar radiation