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UNIT III: MOTION IN THE OCEAN ENTRY WORK KL OCEANOGRAPHY.

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Presentation on theme: "UNIT III: MOTION IN THE OCEAN ENTRY WORK KL OCEANOGRAPHY."— Presentation transcript:

1 UNIT III: MOTION IN THE OCEAN ENTRY WORK KL OCEANOGRAPHY

2 KL OCEAN WK 35 M 5/18 DO NOW EXPLAIN WHAT THE CORIOLIS EFFECT IS. WHAT CAUSES IT? KEY VOCAB CORIOLIS EFFECT ATMOSPHERIC CIRCULATION CELLS HTTPS://YOUTU.BE/DT_XJP77- MK HTTPS://YOUTU.BE/DT_XJP77- MK HTTPS://YOUTU.BE/_SAYCU1TN YG HTTPS://YOUTU.BE/_SAYCU1TN YG LEARNING TARGET: I CAN EXPLAIN HOW INTERACTIONS BETWEEN THE ATMOSPHERE AND OCEAN GENERATE EARTH’S WEATHER AND CLIMATE SUCCESS CRITERIA: I CAN EXPLAIN THE RELATIONSHIP BETWEEN RADIANT ENERGY AND HEAT BALANCE AND HOW THEY IMPACT WEATHER AND CLIMATE DESCRIBE THE CORIOLIS EFFECT COMPLETE 8-3 Q 1-8 AND 8-15 Q 1- 2 FOR STAMP BY END OF CLASS

3 KL OCEAN WK 35 T 5/19 DO NOW WHAT ARE ATMOSPHERIC CIRCULATION CELLS? WHAT DO THE GENERATE? KEY VOCAB CORIOLIS EFFECT ATMOSPHERIC CIRCULATION CELLS EASTERLIES WESTERLIES TRADE WINDS FERRELL CELL HADLEY CELL POLAR CELL LEARNING TARGET: I CAN EXPLAIN HOW INTERACTIONS BETWEEN THE ATMOSPHERE AND OCEAN GENERATE EARTH’S WEATHER AND CLIMATE SUCCESS CRITERIA: DESCRIBE HOW THE CORIOLIS EFFECT INFLUENCES THE FORMATION OF ATMOSPHERIC CIRCULATION CELLS I CAN IDENTIFY THREE ATMOSPHERIC CIRCULATION CELLS AND THE PREVAILING WINDS THEY PRODUCE

4 GLOBAL AIR CIRCULATION Ferral Hadley Polar Hadley Ferral Polar Trade Winds Westerlies Easterlies ITCZ (Intertropical Convergence Zone) Horse Latitudes

5 KL OCEAN WK 35 W 5/20 DO NOW HOW DOES THE GREENHOUSE EFFECT WORK? KEY VOCAB GREENHOUSE EFFECT INFRARED RADIATION SOLAR/RADIANT ENERGY CORIOLIS EFFECT CFCS LEARNING TARGET: I CAN EXPLAIN HOW INTERACTIONS BETWEEN THE ATMOSPHERE AND OCEAN GENERATE EARTH’S WEATHER AND CLIMATE SUCCESS CRITERIA: I CAN DESCRIBE HOW THE GREENHOUSE EFFECT HEATS THE PLANET TO MAKE IT HABITABLE FOR ORGANISMS SKETCH, COLOR AND LABEL GREENHOUSE EFFECT DIAGRAM

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7 KL OCEAN WK 35 TH 5/20 DO NOW DO WE GET AS MUCH RADIANT ENERGY AS THEY DO AT THE EQUATOR? WHY? KEY VOCAB ATMOSPHERE HEAT BALANCE GREENHOUSE EFFECT CONVECTION CELL SOLAR/RADIANT ENERGY ANGLE OF INCIDENCE ORBITAL INCLINATION CORIOLIS EFFECT LEARNING TARGET: I CAN EXPLAIN HOW INTERACTIONS BETWEEN THE ATMOSPHERE AND OCEAN GENERATE EARTH’S WEATHER AND CLIMATE SUCCESS CRITERIA: I CAN EXPLAIN THE RELATIONSHIP BETWEEN RADIANT ENERGY AND HEAT BALANCE AND HOW THEY IMPACT WEATHER AND CLIMATE

8 KL OCEAN WK 35 TH 5/21 DO NOW HOW ARE WAVES GENERATED? KEY VOCAB CREST, TROUGH PERIOD WAVE SPEED WAVE HEIGHT SWELL TIDES DIURNAL SEMIDIURNAL MIXED SHOAL LEARNING TARGET: IDENTIFY THE BASIC CHARACTERISTICS OF DIFFERENT TYPES OF WAVES AND IDENTIFY SOURCES OF ENERGY THAT CAUSE THESE WAVES SUCCESS CRITERIA: IDENTIFY 3 TYPES OF WAVES IDENTIFY THE SOURCE(S) OF ENERGY THAT CAUSE THREE TYPES OF WAVES IDENTIFY PARTS OF A WAVE CALCULATE WAVE SPEED DESCRIBE THE CHANGES A WAVE GOES THROUGH AS IT APPROACHES THE CONTINENTAL MARGIN AND TRAVELS ACROSS THE CONTINENTAL SHELF

9 KL OCEAN WK 35 TGIF 5/22 DO NOW IF A RESEARCHER MEASURED THE PERIOD OF A WAVE AT 6 SECONDS AND THE WAVE SPEED AT 10 M/S, WHAT IS THE LENGTH OF THIS WAVE? KEY VOCAB PERIOD WAVE SPEED WAVELENGTH SHOAL REFLECTION REFRACTION DISTURBING FORCE LEARNING TARGET: I CAN DESCRIBE THE BASIC CHARACTERISTICS OF A WAVE. SUCCESS CRITERIA: I CAN DESCRIBE WHAT CAUSES WAVES I CAN CALCULATE WAVE SPEED I CAN DESCRIBE THE CHANGES THE CHANGES WAVES GO THROUGH AS THE SHOAL

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12 KL OCEAN WK 35 M 5/18 DO NOW WHICH GAS MAKES UP THE MAJORITY OF OUR ATMOSPHERE? KEY VOCAB ATMOSPHERE GREENHOUSE EFFECT CONVECTION CELL SOLAR/RADIANT ENERGY ANGLE OF INCIDENCE ORBITAL INCLINATION CORIOLIS EFFECT LEARNING TARGET: I CAN EXPLAIN HOW INTERACTIONS BETWEEN THE ATMOSPHERE AND OCEAN GENERATE EARTH’S WEATHER AND CLIMATE SUCCESS CRITERIA: I CAN DESCRIBE THE CHARACTERISTICS OF THE ATMOSPHERE I CAN EXPLAIN THE RELATIONSHIP BETWEEN RADIANT ENERGY AND HEAT BALANCE AND HOW THEY IMPACT WEATHER AND CLIMATE COMPLETE 8-3 Q 1-8 AND 8-15 Q 1-2 FOR STAMP BY END OF CLASS


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