PHYSICAL OCEANOGRAPHY 11:628:451, 16:712:501
Fall 2000
Department of Marine and Coastal Sciences

INSTRUCTORS:
    Jim Miller, IMCS 111D, 932-6555 x545, miller@imcs.rutgers.edu
    Scott Glenn, IMCS 111C, 932-6555 x544, glenn@imcs.rutgers.edu
    Dale Haidvogel, IMCS 214D, 932-6555 x256, dale@ahab.rutgers.edu
    TA- Hank Statscewich, Blake Hall, 932-3299, stats@imcs.rutgers.edu

       The earth is a complex system of interacting natural and human components which can be divided into the atmosphere, biosphere, geosphere, and hydrosphere.  To understand the interrelationships among these different components, we must have some understanding of each of them.  The focus of this course is on the physical processes within the hydrosphere, with emphasis on the worldþs oceans.  The scales of these processes range through spatial scales from centimeters to global and time scales from seconds to centuries. Paleoceanographic processes extend the temporal scales to millenia and longer.  An understanding of the concepts of physical oceanography is often necessary to fully appreciate and understand processes in the other oceanographic disciplines, marine biology, chemical oceanography, and marine geology.

       Physical oceanography is important in many different ways.  Much of the worldþs human population lives near the coast where the effects of marine weather, hurricanes, waves, tides, and coastal currents are manifested.  Regional current systems, such as the Gulf Stream, are important components of the global ocean circulation.  El Nino is an example of a larger-scale phenomenon whose equatorial origin belies its global impacts on the atmosphere and ocean.  Finally, the oceans play an important role in the planetary climate system and the recent interest in climate change.

COURSE DESCRIPTION:

       This course is designed to introduce students to the important physical processes in the oceans in such a way that they will understand both the conceptual physical principles and at the larger scale how these fit into the earth as a system.  The initial focus is to develop the basic equations which describe the principles upon which physical oceanography is based.  These principles are then used to help understand waves, tides, currents, and the large-scale ocean circulation.  Homework problems are assigned to reinforce the concepts learned in class.  Throughout the course, examples will be given to show how physical oceanography affects and is affected by the biological, chemical, and geological processes in the ocean.

OBJECTIVES:

To introduce students to the basic principles underlying physical processes in the ocean. To show students that the basic physical principles can be represented with mathematical equations. To apply these basic physical principles to develop an understanding of specific ocean phenomena and processes.

To understand some of the important linkages between physical oceanography and the other oceanographic disciplines-- marine biology, chemical oceanography, and marine geology. To help understand why physical oceanography is important in the  earth system and to learn about the interactions with other components of the system, particularly the atmosphere.

GRADING:

Three exams (75%)
Homework (25%)

TEXT:

Introduction to Physical Oceanography, Second Edition, John Knauss, 1997

OTHER REFERENCES ON RESERVE:

Principles of Ocean Physics, J. Apel
Physical Oceanography of Coastal Waters, K. F. Bowden
Ocean Circulation, The Open University, J. Brown et al.
Waves, Tides and Shallow Water Processes, The Open University, J. Brown et al.
Introduction to Physical Oceanography, Second Edition, J. Knauss
Principles of Physical Oceanography, G. Neumann and W. Pierson
Descriptive Physical Oceanography, G. Pickard and W. Emery
Introductory Dynamic Oceanography, S. Pond and G. Pickard
Regional Oceanography:  An Introduction, M. Tomczak and J. Godfrey
 

Questions or comments?
send mail to the webmaster