NATIONAL SCIENCE EDUCATION STANDARDS CORRELATIONS

Science as Inquiry

  • Ability to do scientific inquiry (5-8, 9-12)
  • Understanding of scientific inquiry (5-8, 9-12)

    Physical Science

  • Motions and forces (5-8, 9-12)
  • Transfer of energy (5-8)

    Earth & Space Science

  • Structure of the earth system (5-8)
  • Earth in the solar system (5-8)
  • Energy in the earth system (9-12)

    Science & Technology

  • Understandings about science and technology (5-8, 9-12)

    Science in Personal & Social Perspectives

  • Natural hazards (5-8)
  • Science and technology in society (5-8)
  • Environmental quality (9-12)
  • Natural and human-induced hazards (9-12)
  • Science and technology in local, national, and global challenges (9-12)

    History and Nature of Science

  • Science as human endeavor (5-8, 9-12)
  • Nature of science knowledge (9-12)

  • tidal surge

    Written by Kevin Goff & Susan Haynes.
    Edited and updated by Carol Hopper Brill & Chris Petrone.
    Photo courtesy of NOAA.

    Coastal Storm Data Activity #5: The Gulf Stream &emdash; Storm-Maker

    Now, we come full circle to study sea surface temperatures again. This time, we'll concentrate our observations along the Atlantic coast, looking at the Gulf Stream. This famous current forms the western boundary of the North Atlantic Gyre's clockwise circulation. Flowing from south to north, the Gulf Stream moves warm water from subtropics to temperate latitudes and is the East Coast's powerful storm maker. It can carry hurricanes up the Eastern seaboard during summer and early fall, fueling the storms' strength with warm, wet air. And, since it carries some warm water year-round, the Gulf Stream also plays a role in promoting Nor'easters from fall through spring.

    Moving currents of air and ocean interact to create these dangerous storms. Nor'easters usually develop off the coast of North Carolina or Virginia when the cold Labrador Current coming down from the North meets the warm Gulf Stream coming up from the South. The contrast in the air temperatures above these currents help form a low pressure system. At the same time over Canada, winds circulate in a clockwise motion around a high pressure system. These cold winds dip deeply into the United States, colliding with the warmer air mass sitting above the sea. Since warm air is lighter, it rapidly rises over the arctic air, drawing moisture with it. The pressure then plummets and a wet, violent tempest takes shape.

    Data Activity & Discussion: Tracking the Gulf Stream

    Look for the Gulf Stream at the Cool Room website.

    Look again at the water temperatures off the Atlantic Coast.

    Now that you know how to find lows and read wind barbs: Do you see any relationship between the position and strength of a low, the wind speed and the occurrence of large waves?

    Return to the Coastal Storms DATA mainpage.

    Go to the previous Coastal Storms DATA activity.


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