Introduction to Physical
Oceanography
Copyright
I hereby grant any user right to download and print a copy of
the book for personal use. I also grant all teachers, lecturers, and
professors the right to download the book and to make multiple copies
for use by their students. The multiple copies may be made by copy centers. Students
may be charged the cost of reproducing the book.
I do not grant rights to the text for commercial purposes.
Download the Book
These files are the latest version, August 13, 2008. The files
are in Adobe Portable Document Format. This version has hyperlinked Table of
Contents and Index for easier navigation of the document in Adobe Acrobat Reader.
I thanks Andrew Kiss of the University of New South Wales in Canberra Australia
for his help in using the \hyperref package to produce the links.
Book |
Complete book in a 9.6 Mbyte file with index. |
Cover |
Color cover for your book. |
If you don't have an Acrobat Reader, you can download one for
free from Adobe.
Introduction
This is a new textbook describing physical-oceanographic
processes, theories, data, and measurements. In addition to the
classical topics, I have included discussions of heat fluxes, the
role of the ocean in climate, the deep circulation, equatorial
processes including El Nino, data bases used by oceanographers, the
role of satellites and data from space, ship-based measurements, and
the importance of vorticity in understanding oceanic flows.
I have used the text to teach upper-division undergraduates and
graduate students in oceanography, meteorology, and ocean
engineering. Because many students have already taken courses that emphasize
math, I have minimized the math and emphasized processes. Still, students should
have studied differential equations and introductory college physics.
The text is typeset and it has high-resolution figures produced
by Adobe Illustrator CS2. The book was produced in LATEX2ε using TeXShop
2.14 on an Intel dual-processor
iMac running OS-X 10.4.11. The resulting typeset, 345 page,
book.pdf file is only 9.5 Megabytes. If you make multiple copies I recommend
you use a copy center that can make copies directly from the book.pdf file.
These copies will be much better
than copies made from printed pages.
If you have problems, please contact me at stewart@ocean.tamu.edu
Web Version
A web-based
version the book is also
available..
What's New!! Fall 2008 Revisions
This edition has a few minor and more important changes:
- Corrected a few minor errors. There are less and less thanks
to the many readers who have found errors in the past.
- Added information about the new Reference Salinity scale in
Section 6.1.
- Corrected an important error in my discussion of potential
temperature in Section 6.5.
- Added information about MODIS and Jason-2.
- Removed references to controversy about vertical mixing in
the ocean in Section 8.4. The controversy has been resolved.
- Added more information about abrupt climate at end of the
last ice age in Section 13.1.
- Added more information about mixing driving the deep circulation
in Section 13.3 and , and the role of Ekman pumping in the Antarctic and
its influence on the deep circulation in Section 13.5
- Added information about measured variability of the North
Atlantic meridional overturning circulation in Section 13.4.
- Removed information about solitons in Section 16.2. It is
not that important in an introductory text that is alreay too long.
The table below links to the latest version of Introduction
to Physical Oceanography in Adobe Acrobat Portable Document Format (pdf
files). The files may be downloaded and printed if you wish a nice printed
copy of the book. Altogether, there are viii + 345 pages in the book.
Fall 2007 Revisions
This edition has several changes from the previous edition. The
changes include:
- Mostly many small changes and corrections of minor errors.
I thank all of you who have emailed comments to me this year.
- COADS has been changed to the new ICOADS.
- Revised section on definition of salinity to separate definition
from extensions of definition to typical temperatures found in the ocean.
- Revised section on temperature to refer to the new Smith and
Reynolds Improved Optimal Interpolation scheme.
- Added information on Prandtl's discovery of the boundary layer
and its importance to oceanography
- Revised paragraphs on altimeter errors to include more accurate
values now being achieved for Jasin and Topex/Poseidon.
- Revised figure 12.7 to show western intensification.
- Clarified importance of equatorial heating for atmospheric
circulation, and role of el Nino.
- Added information on the Advanced Circulation Model for coastal
processes and storm surges.
Fall 2006 Revisions
This edition has several changes from the previous edition. The
changes include:
- Updated information on maps of seafloor features and global
bathymetric maps.
- Revised section on measurements of winds to better describe
satellite measurements of winds.
- Revised section on measurements of currents to state more
clearly the important techniques and drop less important information.
- Dropped the description of fresh-water transports. I think
the topic is beyond the scope of the book.
- Made a few minor changes in wording and corrected a very small
number of typographical errors. I thank all of you who have found almost
all errors in previous years.
- As a result, the book is one page shorter this year.
Fall 2005 Revisions
The files below are the latest version, August 10, 2005.
This edition has only minor changes from the previous edition.
The changes include:
- Clarified the discussion of important forces in Chapter 7.
- Dropped all statements that a derivation is simple. It may
be simple to some, but not to many students.
- Added a new figure on Ekman flow in Chapter 9.
- Revised the discussion of flow into and out of the Mediterranean
Sea in Chapter 7.
- Made a few minor changes in wording and corrected a few typographical
errors.
Fall 2004 Revisions
This edition has only minor changes from the previous edition.
The changes include:
- Deleted all references to the practical salinity unit (psu).
It doesn't exist. Salinity is a dimensionless ratio of masses.
- Clarified the derivation of Margules' equation on page 171.
- Made a few minor changes in wording and corrected a few typographical
errors.
Spring 2004 Revisions
This edition has only minor changes from the previous edition. The changes
include:
- Revision of discussion of using vorticity to explain western boundary currents
on page 204-205.
- Changed explanation of tide generating forces on page 301.
- Corrected error in equations describing the Ekman layer on page 139.
- Corrected errors in figure 3.2.
- Clarified differences between a surface analysis and reanalyzed
weather data on pages 47.
- Made a few minor changes in wording and corrected a few typographical errors.
Fall
2003 Revisions
The important changes include:
- Many figures have been redrawn, some have been replaced.
- The index is much improved.
- Many references have been deleted or added. The
calls to references in the text now agree with references at the end of
the book.
- Chapter 13 on the deep circulation has been revised
to include recent advances in our understanding of the deep mass flow.
Out is any reference to the thermohaline circulation (it is used in too
many conflicting ways). In is the information that the deep flow is driven
by
wind and tidal mixing.
- Hundreds of minor revisions throughout the book.
Fall 2002 Revisions
The important changes include:
- We have an index! Trey Morris, a
student, spent the summer tagging all the LaTeX files used to make
the book. From these we produced an index and the pdf files
below.
- Don Johnson, another student, spent months redrawing many
figures.
- I simplified some of the discussions of errors. I found that
students jumped to the conclusion that if there were several
sources of error, no matter how small, the data were essentially
worthless. This shortened the book by seven pages.
- I made hundreds of small changes to the text.
Spring 2002 Revisions
The important changes include:
- Gradually replacing poor scanned images with newly redrawn
figures.
- Corrected some significant errors in Chapter 10: tables had
wrong values in one column, and text describing how currents are
calculated from measurements of density was confusing
- Many minor changes in all chapters.
- The book is one page longer.
- Adobe index file added.
Fall 2001 Revisions
The important changes include:
- A beautiful cover.
- Clarified the values for vertical diffusivity removing the
conflict between Munk's value and measurements.
- Revised the discussion of Ekman pumping and the role of
vorticity in section 12.3.
- Revised section 6.5 on density.
- Added a description of neutral density.
- Revised or redrew many figures.
- Corrected many, many typos and other minor irritating
errors.
- The book is a few pages shorter.
- Plus, I learned more about Adobe Illustrator 9 and Distiller 5
than I ever wanted to know. My testing leads me to believe the pdf
files will print correctly.
Fall 2000 Revisions
I have revised many sections of the book, added new figures
illustrating key concepts, and corrected many small errors. The
important changes include:
- More information on double diffusion.
- Much revised section on Ekman currents.
- Added description of the North Atlantic circulation in chapter
10, including discussion of the Gulf Stream and negative
viscosity.
- Clarified that vertical mixing drives the deep circulation,
and added a description of the Antarctic Circumpolar Current in
Chapter 13.
- Revised discussion of El Nino/La Nina.
- Dropped the old Chapter 15 on the observed circulation of the
ocean and added the information to other chapters.
Department
of Oceanography, Texas A&M University
Robert H. Stewart, stewart@ocean.tamu.edu
All contents copyright © 2008 Robert H. Stewart, All rights
reserved
Updated
June 3, 2009
URL:
http://oceanworld.tamu.edu/resources/ocng_textbook/PDF_files/book_PDF_files.html