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

UNIT III: MOTION IN THE OCEAN ENTRY

WORKKL 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

• HTTPS://YOUTU.BE/DT_XJP77-MK

• HTTPS://YOUTU.BE/_SAYCU1TNYG

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

https://youtu.be/dt_XJp77-mk

https://youtu.be/dt_XJp77-mk

https://youtu.be/_sayCU1TNyg

https://youtu.be/_sayCU1TNyg

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:


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

Hadle

y

Polar

Hadle

y

Ferr

al

Polar

Trade W

inds

Trade W

inds

Trad

e

Win

dsW

este

rlies

Wes

terli

es

Wes

terli

es

Westerli

es

Westerlie

s

Westerlie

s

o°

30°

30°

60°

60°

90°

East

erl

ies

East

erl

ies

Easterlies

Easterlies

ITCZ(Intertropical Convergence Zone)

Horse Latitudes

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:


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


• CONVECTION CELL


• ANGLE OF INCIDENCE

• ORBITAL INCLINATION

• CORIOLIS EFFECT

LEARNING TARGET:


SUCCESS CRITERIA:


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


• CONVECTION CELL


• ANGLE OF INCIDENCE

• ORBITAL INCLINATION

• CORIOLIS EFFECT

LEARNING TARGET:


SUCCESS CRITERIA:

• I CAN DESCRIBE THE CHARACTERISTICS OF THE ATMOSPHERE


• COMPLETE 8-3 Q 1-8 AND 8-15 Q 1-2 FOR STAMP BY END OF CLASS

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

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