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!
Differentiate between High tide and Spring Tide
Differentiate between Spring tide and Neap tide
Explain the relationship between the “Tidal Bulge”, High tide, and the Moon’s position with respect to Earth
Why are there TWO tidal bulges that are opposite one another?
Why is there a relationship between moon phases and tides?
OBJECTIVES: OCEANOGRAPHY
GIZMOS: TIDEs
REVIEW the Gizmos activity
Short Quiz – you may use your gizmos
Review of the February 22 Activities
Bill Nye: Oceanography
HOMEWORK:
Be sure you completed your Meteorology TEST CORRECTIONS
Read the Information on the Global Ocean Conveyor Belt (deep ocean circulation)
Look through the NEW OCEANOGRAPHY LABS (there are 2)
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 Belt, NOS Education
Ocean Conveyor Belt, NOAA Science on A Sphere
NOAA Sites
National Oceanic and Atmospheric Administration
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