UNIT III: MOTION IN THE OCEAN ENTRY WORK KL OCEANOGRAPHY

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 MK MK YG 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

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

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

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

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

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

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

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