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Unit 6 Climate and Global Climate Change
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Climate The LONG TERM weather patterns for an area.
Describes monthly or annual variations in: Temperature Precipitation Wind Other weather variables
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What Affects Climate? 1. Latitude:
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Equator receives more direct sunlight → Warmer Climates
North & South of equator sunlight is indirect → Cooler Climates
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Climate Zones: Tropical Zone: Equator to 23.5° N & S
Temperate zone: 23.5° ° N & S Polar zone: 66.5° to N & S poles Polar Zone Temperate Zone Tropical Zone Temperate Zone Polar Zone
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2. Topography Water heats & cools more slowly than land: Earth’s Oceans moderate coasts → coastal climates
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↑ altitude, ↓ temp Leeward side of mountains → drier air
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3. Air Masses Continental (dry) vs Maritime (wet)
Tropical (warm) vs Polar (cold)
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4. Circulation Cells Cells of air circulation are driven by solar energy & earth’s rotation These cells transport energy & heat from equator to poles
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Climate Classification
Köppen classification system Divides climates based on average temperatures, precipitation & vegetation
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Global Climate change A pattern of change that occurs over many years (NOT seasonal variations from year to year) Global warming: the increase in average global temperature that has occurred over MANY years
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Greenhouse Gases Heat trapping gases in the atmosphere: Carbon Dioxide
Methane Nitrous Oxide Water vapor Effects on the climate depend on: How much is produced How long it stays in the atmosphere How much heat it can trap
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Water Vapor Water vapor increases as the Earth’s surface warms
Water vapor leads to climate warming Climate warming leads to more evaporation of water & more water vapor – a positive feedback loop
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Natural Causes of Climate Change
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Earth’s Climate in the Past
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Earth’s Wobble: the 26,000 year precession cycle affects Earth’s seasons
Earth’s Orbit: changes from circular to elliptical over a 100,000 year cycle
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Volcanic Activity: volcanic ash in the atmosphere blocks the Sun and cools Earth’s climate
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Solar Activity: sunspot cycles affect temperatures on Earth
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Sunspots and Sunspots Cycles:
Occur ~every 11 years Dark spots up to 50,000 miles wide Move across the surface of the sun Give off more energy
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Photosynthesis Plants take in CO2 (a greenhouse gas) and put out O2. This reduces greenhouse gases
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El Nino Southern Oscillation (ENSO)
Cycles of El Nino, warmer waters, and La Nina, cooler waters, off South America. Causes cycles of wet & dry weather
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Microclimates A localized pocket with a climate different from the surrounding area. Example:
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Using ice cores, scientists found there is more CO2 in atmosphere today than in past
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The level of the greenhouse gases methane, CO2, and nitrous oxide are increasing.
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Carbon Dioxide (CO2) 55% of human produced greenhouse gas Comes from:
Fossil fuel combustion for power Cutting down or burning trees Industrial processes (making cement or chemicals) Can stay thousands of years
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Methane (CH4) 30% of human produced greenhouse gas Comes from:
Livestock (cows and sheep) Landfills Natural gas Mining coal Stays ~12 years Traps 20 times more heat than CO2
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Nitrous Oxide (N2O) 5% of human produced greenhouse gas Comes from:
Farming (fertilizer) Fossil fuel combustion Industrial processes Stays ~114 years Traps 298 times more heat than CO2
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Sources of Greenhouse Gas emissions in US
Electricity production (32%) Fuel combustion for transportation (20%) Industrial processes (20%) Agriculture(10%) Residential (10%)
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Heat Islands Cities and urban centers with many concrete buildings and asphalt have a warmer climate than surrounding rural areas
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