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Published byAmie Goodman Modified over 9 years ago
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Chapter 4 Ecosystems and the Physical Environment
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Cycling of Materials Matter moves between ecosystems, environments, and organisms 5 major cycles: Carbon, Nitrogen, Phosphorus, Sulfur and Water (hydrologic)
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The Carbon Cycle
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The Nitrogen Cycle
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The Phosphorus Cycle
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The Sulfur Cycle
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The Water (Hydrologic) Cycle
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Solar Radiation
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Temperature Changes with Latitude
Solar energy does not hit earth uniformly Due to earth’s spherical shape and tilt Equator (a) High concentration High Temperature Closer to Poles (c) Low concentration Low Temperature From (a) to (c) In diagram below
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Temperature Changes with Season
Seasons determined by earth’s tilt
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The Atmosphere 21% O 78% N 1% Ar, CO2, Ne and He
Shields earth from high energy radiation
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Atmospheric Layers
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Atmospheric Circulation
Near Equator Warm air rises, cools and splits to flow towards the poles ~30° N & S sinks back to surface Air moves along surface back towards equator Moves heat from equator to the poles
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Surface Winds Large winds due in part to pressures caused by global circulation of air High Low High Low High Winds blow from high to low pressure Regional differences in surface warming is the start of global air circulation patterns Warm air rises and holds more moisture (areas of high rainfall) Cool air sinks and is drier (areas where deserts form, 30°latitude north and south) Low High
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Coriolis Effect Coriolis Effect
Influence of the earth’s rotation on movement of air and fluids (water) Turns them Right in the Northern Hemisphere Turns them Left in the Southern Hemisphere Earth rotates from East to West Deflects wind from straight-line path
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Coriolis Effect
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Patterns of Ocean Circulation
Prevailing winds produce ocean currents and generate gyres Pacific Gyre Circular pattern influenced by Coriolis effect Trade winds blow west Westerlies blow east This becomes important later when we talk about plastics in the ocean.
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Patterns of Ocean Circulation
Westerlies Trade winds
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Vertical Mixing of Ocean
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Surfers, Seals, and the Sea
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Ocean Interaction with Atmosphere - ENSO
El Niño-Southern Oscillation (ENSO) Periodic large scale warming of surface waters of tropical E. Pacific Ocean Normal conditions westward blowing tradewinds keep warmest water in western Pacific ENSO conditions trade winds weaken and warm water expands eastward to South America Big effect on fishing industry and wildlife off South America
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ENSO Climate Patterns
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Weather and Climate Weather Climate
The conditions in the atmosphere at a given place and time Temperature, precipitation, cloudiness, etc. Climate The average weather conditions that occur in a place over a period of years 2 most important factors: temperature and precipitation
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Rain Shadows
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Tropical Cyclone aka: hurricane, typhoon, cyclone
Giant rotating tropical storms Wind > 119 km per hour Formation Strong winds pick up moisture over warm surface waters and starts to spin due to Earth’s rotation
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Tsunami Giant undersea wave caused by an earthquake, volcanic eruption or landslide Travel > 450 mph Tsunami wave may be 1m deep in ocean Becomes 30.5m high on shore
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