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OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul [email protected] / X 7453

OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul [email protected] / X 7453

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Page 1: OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

OCN 5401

Chapter 1

Overview

Instructor: Dr. George A. Maul

[email protected] / X 7453

Page 2: OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

Hypsographic Data

Page 3: OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

How big is 1400 million cubic kilometers? What if we made a giant cube of the ocean? How big would it be?

The average ocean volume is

1.4 x 1021 liters, or 1.4 x 1018 m3, or 1.4 x 109 km3

The average depth for the oceans is approximately 4 km.

How big is the ocean?

How big is that compared to a 12″diameter globe?1000 km/6400 km = x cm/16 cm, x = 2.5cm or about 1 inch

The cube root of 1.4 x 109 km3 is approximately 1000 km.

So we have a 1000 km3 cube.

Page 4: OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

How big is the ocean?

How big is the atmosphere?

Page 5: OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

Earth is an oblate spheroid due to rotation, and best represented mathematically by an ellipsoid.

What is the size and shape of Earth?

Equatorial radius = 6,378,137 m

Polar radius = 6,356,752 m

Satellite Altimeter

Page 6: OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

Geoid Surface TopographyThe geoid is a surface of equal potential energy (PE); a.k.a. an equipotential surface; a.k.a. a “level” surface.

Departures of the geoid from the ellipsoid

PE=m·g·h

Page 7: OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

Seafloor TopographyWhere is Earth’s longest mountain range?

Page 8: OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

Bathymetry – the process of determining seafloor

topography

Page 9: OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

Deepsea Sediment TypesWhy are they different?

Page 10: OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

How deep is the Ocean?

• Mariana Trench Z = - 11,022 m• If pressure is hydrostatic, how many atmospheres did

the bathyscaphe Trieste have on its hull?

Hydrostatic Equation

p = - g z

 

where is seawater density

g is gravity

z is water depth

p is pressure (1 Nm-2 = 1 Pa)

Page 11: OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

Perpetual Ocean Video

Ocean Surface Currents

Page 12: OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

Ocean Data Collection

Note that many areas of the ocean have no in situ observations.

Page 13: OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

Pilot Charts provide general information – US Navy Publication

Page 15: OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

RV Operations

Page 16: OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

Historical Instruments

Page 17: OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

What we measure

• Temperature

• Conductivity

• Pressure

• Velocity

• Sound speed

• Position

• Time

• Transparency

Page 18: OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

What we calculate

• Density

• Salinity

• Depth

• Heat Flux

• Volume Transport

• Dynamic Height

• Geostrophic Currents

Page 19: OCN 5401 Chapter 1 Overview Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453

OCN 5401

Questions?

Chapter 1