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Module 4 Earth’s Dynamics

Module 4 Earth’s Dynamics

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Page 1: Module 4 Earth’s Dynamics

Module 4 Earth’s Dynamics

Page 2: Module 4 Earth’s Dynamics

BUMI DALAM TATASURYA

• Matahari dan planet-planetnya • Anatomi bumi • Dinamika bumi

Page 3: Module 4 Earth’s Dynamics

EARTH DYNAMICS

• Rotation and revolution of planets • Heat (from solar and Earth’s mantle) • Gravity force • Electro-magnet

Page 4: Module 4 Earth’s Dynamics

EARTH’S orbit around the Sun

Page 5: Module 4 Earth’s Dynamics
Page 6: Module 4 Earth’s Dynamics

Distributian of day and night; and climate along year

Solstice: Titik balik matahari Equinox: Waktu siang dan malam sama lama

Page 7: Module 4 Earth’s Dynamics

Energy budget

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mW m-2

Heat Flow (Internal Source)

0 40 60 85 120 180 240 350

Page 9: Module 4 Earth’s Dynamics

(Hamblin & Christiansen, 2009)

The Sun’s energy on Earth

Page 10: Module 4 Earth’s Dynamics

Winds circulation

(Hamblin & Christiansen, 2009)

Page 11: Module 4 Earth’s Dynamics

Winds circulation

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The Formation of Syclones dan anticyclones

A. Jet stream begins to undulate

B. Rossby waves begin to form

C. Waves strongly developed

D. Cells of cold and warm air bodies are formed

Page 13: Module 4 Earth’s Dynamics

Spiral clouds

Page 14: Module 4 Earth’s Dynamics

Water Cycle

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How does water move among reservoirs?

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Ocean Currents• Redistribute heat across planet

(Hamblin & Christiansen, 2009)

Page 17: Module 4 Earth’s Dynamics

Deep ocean currents

(Hamblin & Christiansen, 2009)

Page 18: Module 4 Earth’s Dynamics

Weather and Climate

What is weather? What is climate? How do they differ?

• Weather is the short-term state of the atmosphere at a particular place at any given time

• Climate is a long-term composite of weather conditions at a particular place

• Short term versus long term---that is how they differ

Page 19: Module 4 Earth’s Dynamics

World Climate

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PLATE MOTIONMantle convection provides

the primary drive for plate tectonics

What drives plate motions?

MODELS: A. Layering at 660 kilometers Model B. Whole Mantle Convection Model C. Deep-layer Model

Whole Mantle

Deep Layer

Layering

Page 21: Module 4 Earth’s Dynamics

What drives plate motions

• Forces that drive plate motion

SLAB PULL Cold, dense slabs of subducted oceanic lithosphere pull the plate towards the subduction zone

MANTLE DRAG and PLATE RESISTANCE Can act to increase or decrease plate motion

RIDGE-PUSH • The higher elevation of spreading centers result in oceanic

lithosphere wanting to move “downhill”, away from the ridge • Far less important than slab-pull

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3 plate interactions: Divergent

Convergent Transform

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Morphology of the ocean (oceanic basins)

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Landforms & Surface Processes

• Glaciers • Mass Wasting

• Streams

• Shorelines

• Deserts

• Groundwaterhttp://www.berann.com

H.C. Berann (1915-1999) Yosemite National Park, 1987