February 28, Tuesday: a day Take out your ch #22 Agenda with work, and your gizmos activity



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Research Earth Science Agenda

February 28, Tuesday: A Day


  • Take out your CH #22 Agenda with work, AND your GIZMOS activity

  • Take out your test corrections.


WARM-UPS: We will go over these warm-ups from the last 2 classes!

  1. Differentiate between High tide and Spring Tide

  2. Differentiate between Spring tide and Neap tide

  3. Explain the relationship between the “Tidal Bulge”, High tide, and the Moon’s position with respect to Earth

    1. Why are there TWO tidal bulges that are opposite one another?

  4. Why is there a relationship between moon phases and tides?


OBJECTIVES: OCEANOGRAPHY

  1. GIZMOS: TIDEs

    1. REVIEW the Gizmos activity

    2. Short Quiz – you may use your gizmos

  2. Review of the February 22 Activities

  3. Bill Nye: Oceanography



HOMEWORK:

  1. Be sure you completed your Meteorology TEST CORRECTIONS

  2. Read the Information on the Global Ocean Conveyor Belt (deep ocean circulation)

  3. Look through the NEW OCEANOGRAPHY LABS (there are 2)

    1. REVIEW all the information on salinity, ocean water temperatures, and tides!



commerce.gov

noaa.gov

Top of Form

Bottom of Form

The global ocean conveyor belt is a constantly moving system of deep-ocean circulation driven by temperature and salinity

The great ocean conveyor moves water around the globe.

The ocean is not a still body of water. There is constant motion in the ocean in the form of a global ocean conveyor belt. This motion is due to thermohaline currents (thermo = temperature; haline = salinity). Cold, salty water is dense and sinks to the bottom of the ocean while warm water is less dense and rises to the surface.

The ocean conveyor gets it “start” in the Norwegian Sea, where warm water from the Gulf Stream heats the atmosphere in the cold northern latitudes. This loss of heat to the atmosphere makes the water cooler and denser, causing it to sink to the bottom of the ocean. As more warm water is transported north, the cooler water sinks and moves south to make room for the incoming warm water. This cold bottom water flows south of the equator all the way down to Antarctica. Eventually, the cold bottom waters are able to warm and rise to the surface, continuing the conveyor belt that encircles the globe.

It takes almost 1,000 years for the conveyor belt to complete one “cycle.”

For more information:


The Global Conveyor BeltNOS Education
Ocean Conveyor BeltNOAA Science on A Sphere

NOAA Sites

National Oceanic and Atmospheric Administration



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