Global Ocean Conveyor Belt, A Cold Salty Deep

Slides:



Advertisements
Similar presentations
OCEAN CURRENTS AND WEATHER. Oceans currents are created by: surface wind, corliolis effect, land shape, and salt content and temperature of the water.
Advertisements

Deep Ocean Circulation
Oceans, Currents, and Weather Dynamics
Notes on “Ocean Currents”
Ocean Currents Objective:
Surface Currents and Deep Currents
Currents and Wind. The Earth is Spinning… Because Earth spins, winds and water appear to be deflected in a curved motion This is called the Coriolis Effect.
Ocean Currents and Climate. Do the Earth’s Oceans Affect Climate?
 In an inquiry classroom, teachers facilitate the construction of new knowledge by activating and then pursuing the inquisitive nature of each learner.
Phenology: Step Together Step ELF Activity: Biosphere 4A
Albedo. 3/30 WHOT Teaching Point:  Objective: Collect data on the albedo of various surfaces on Earth.  Responsibilities: Albedo Lab Due Wednesday.
Monday 10/30/2007 Ocean Currents.
Subsurface Currents The Oceans in Motion. Subsurface Currents 1.Mechanics 2.Deep water formation 3.The Importance of the Global Conveyer Belt.
Starter: What influences ocean currents? 10/23/ Convection and Ocean Currents 10/23/14 Practice : Glue notes here Application: Glue activity here.
Ocean and Climate.  Our global climate has changed over our planet's lifetime. A lot!!!  Some global climate fluctuations are on a human-time scale.
Deep Ocean Currents 90% of the ocean’s water!. Depend on Density which is affected by Density which is affected by – temperature Colder water is more.
Currents are produced by forces acting upon the water. Surface ocean currents are formed by winds that cause the water to move in the direction that the.
 In an inquiry classroom, teachers facilitate the construction of new knowledge by activating and then pursuing the inquisitive nature of each learner.
Plates and Gates ELF Activity: Geosphere 2A As.
Composition and Movement of Ocean Water. Salinity Seawater is a solution containing a variety of salts dissolved in water Expressed in grams of salt per.
DO NOW From what you learned and observed in the density investigation, hypothesize what you think happens in the red areas on the map shown, and why you.
Ocean Acidification, Life in an Acid Bath ELF Activity: Biosphere 4B
Surface Currents Movement of water that flow in the upper part of the ocean’s surface.
Ocean Currents What Are Currents? Current: a large stream of moving water that flows through the oceans. Currents carry water over very long distances.
ThermoHaline Circulation
Carbon Journey ELF Activity: Energy 1C As part of NOAA Environmental Literacy Grant #NA09SEC
Stacking up the Atmosphere ELF Activity: Atmosphere 5A.
Flashlights on Earth ELF Activity: Energy 1A As.
Ocean Circulation – Ch Ag Earth Science – Chapter 15.2.
Currents microsite.smithsonianmag.com -.
Deep Ocean Circulation. Significant vertical movement ▫Accounts for the thorough mixing of deep- water masses.
Lesson 8: Currents Physical Oceanography
What forces cause the ocean to move? Gravitational pull of the Moon and Sun Wind (friction between air and water) Coriolis Effect (spin of Earth) Differences.
The Conveyer Belt EEn  Ocean circulation travels from the Atlantic Ocean through the Indian & Pacific oceans & back again  Warm water in upper.
Ocean Currents p. 36 Ocean waters are constantly on the move. How they move influences climate and living conditions for plants and animals, even on land.
Art or Science?. Explain the thermal transfers of energy within oceans and the importance of oceanic conveyor belts.
Deep Ocean Currents (Great Ocean Conveyer Belt). Differential Solar Heating.
 In an inquiry classroom, teachers facilitate the construction of new knowledge by activating and then pursuing the inquisitive nature of each learner.
Ocean Movements Rotating Earth influences basic motion of ocean and atmospheric currents (Coriolis Effect)
Ocean Circulation Lindsay Innes and Charity Sonier.
Lesson 8: Currents Physical Oceanography
8.8 Energy Transfer within the Climate System
Waves, Currents, and Tides
Chapter 16.1 Ocean Circulation.
Ocean Currents & Climate
Temperature Differences of Land & Water
Ocean Circulation 16.1.
OCEAN CURRENTS.
Oceans and Climate Visual Vocabulary.
Global Ocean Conveyor Belt
OCEAN CURRENTS.
Ocean Currents and Energy Distribution
15.3 Global Winds and Local Winds
“Keeping It Current”.
Ocean Currents.
Surface water circulation
Wind circulation through the atmosphere
IN: How does temperate affect ocean currents?
Ocean Currents Streamlike movements of water that occur at or near the surface of the ocean are called surface currents. Surface currents are wind driven.
Key vocab 07, words 1, 2 1. Salinity(n) Saltiness or dissolved salt content of a body of water 2. Distribution (n) The action of sharing something out.
Ocean Currents.
Lesson 8: Currents Physical Oceanography
Currents.
Ocean Currents Science 8.
Ocean Currents Streamlike movements of water that occur at or near the surface of the ocean are called surface currents. Surface currents are wind driven.
Interactions between the Oceans and the Atmosphere
This material is based upon work supported by the National Science Foundation under Grant #XXXXXX. Any opinions, findings, and conclusions or recommendations.
The Oceans in Motion Subsurface Currents.
Presentation transcript:

Global Ocean Conveyor Belt, A Cold Salty Deep This material is based on work supported by an Environmental Literacy Grant from the National Oceanic and Atmospheric Administration's Office of Education (NA0909SEC4690009) and prior work supported by the National Science Foundation under Grants ANT-0342484 and ESI-0632175. Any opinions, findings, and conclusions or recommendations expressed in these materials are those of the authors and do not necessarily reflect the views of the NOAA or the NSF. Global Ocean Conveyor Belt, A Cold Salty Deep ELF Activity: Hydrosphere 3A http://andrill.org/education/elf_activities_3A.html As part of NOAA Environmental Literacy Grant #NA09SEC490009 to the University of Nebraska–Lincoln's, ANDRILL Science Management Office.

There is only one ocean and the waters are not still. Give your students an outline of the world and have them draw a continuous line through all the oceans, touching all 7 continents. This will demonstrate that the oceans are all connected. www.noaa.gov In the above picture notice how the waters of all the oceans are connected.

Due to winds and surface currents, the waters continually move and mix. Scientists use buoys floating in the ocean equipped with tracking devices to create these maps. The surface water currents are different from the deep water currents driven by temperature and density. www.noaa.gov This map shows the movement of surface water due to the action of the winds.

Cold, salty, dense water sinks under warmer fresher water. The sinking of cold water at the poles and its replacement by warmer water from the equator creates a current. This is called a thermohaline circulation because it is based on temperature and water density due to salt content. As ocean water freezes to ice, the salt is left behind making the liquid water more salty and dense. As it sinks, warm surface water moving from the equator replaces it. This causes a current to form. Have your students follow the formation of this current cycle in the diagram here. thermo = temperature haline = salt Image: national academy of sciences

The Great Ocean Conveyor Belt This large current of the global ocean water moves heat away from the equator and brings nutrient-rich bottom waters to areas where life thrives. Notice the current along the eastern side of the U.S. This current takes warm water to Europe and is responsible for Europe’s mild winter temperatures. www.noaa.gov Red = warm surface water Blue = cold salty deep water

Warm water carried north away from the Equator provides Europe with mild winters. You can see satellite images of the ocean’s water temperatures at noaa.gov. Satellite image showing water temperatures along the eastern U.S. Images: www.noaa.gov

A Polar View of the Global Ocean Conveyor Belt An interesting map showing the same current from a polar angle. Here you can see the cold water which completely circles Antarctica. This is one reason Antarctica is much colder than the Arctic. www.wikipedia.com

In these two activities (Cold Salty Deep and Global Ocean Conveyer Belt), students create models of ocean currents to demonstrate the thermohaline circulation of water throughout the Earth’s system.

This material is based on work supported by an Environmental Literacy Grant from the National Oceanic and Atmospheric Administration’s Office of Education (NA09SEC4690009) and prior work supported by the National Science Foundation under Grants ANT-0342484 and ESI-0632175. Any opinions, findings, and conclusions or recommendations expressed in these materials are those of the authors and do not necessarily reflect the views of the National Oceanic and Atmospheric Administration or the National Science Foundation. http://andrill.org/education/elf/activities