Patterns of Ocean Circulation

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Presentation transcript:

Patterns of Ocean Circulation Prevailing winds produce ocean currents and generate gyres Example: the North Atlantic Ocean Trade winds blow west Westerlies blow east Creates a clockwise gyre in the North Atlantic Circular pattern influenced by coriolis effect

Patterns of Ocean Circulation Westerlies Trade winds

Position of Landmasses Large landmasses in the Northern Hemisphere help to dictate ocean currents and flow Very little land in the Southern Hemisphere

Vertical Mixing of Ocean

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 off South America

ENSO Climate Patterns

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

Rain Shadows Mountains force humid air to rise Air cools with altitude, clouds form, and precipitation occurs (windward side) Dry air mass moves leeward side of mountain

Tornadoes Powerful funnel of air associated with a severe thunderstorm Formation Strong updraft of spinning air forms as mass of cool dry air collides with warm humid air Spinning funnel becomes tornado when it descends from cloud Wind velocity = up to 300 mph Width ranges from 1m to 3.2 km

Tropical 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 Spin causes upward spiral of clouds Many names: Hurricane (Atlantic), typhoon (Pacific), cyclone (Indian Ocean)

Internal Planetary Processes Layers of the earth Lithosphere Outermost rigid rock layer composed of plates Asthenosphere Lower mantle comprised of hot soft rock

Internal Planetary Processes Plate Tectonics- study of the processes by which the lithospheric plates move over the asthenosphere Plate Boundary - where 2 plates meet Divergent Convergent Transform

Plates and Plate Boundaries

Earthquakes Caused by the release of accumulated energy as rocks in the lithosphere suddenly shift or break Occur along faults Energy released as seismic wave

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 Magnitude 9.3 earthquake in Indian Ocean Triggered tsunami that killed over 230,000 people in South Asia and Africa