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South Pacific Sea Level and Climate Monitoring Project Workshop Round Four

Location
TONGA
Author(s)
Aung, Dr T H.
Publisher
AusAid
Publication Year:
1995
Publication Place
Australia
Physical Description:
31p,;29cm
Call Number
CLI
Language
English
Record ID:
20651
Legacy PEIN ID:
60574
General Notes
The waters of the ocean are continually moving. This motion ranges from powerful currents like the Gulf Stream, down to small swirls and eddies. What drives all this motion? The short answer is energy from the sun, and the rotation of the Earth. The most obvious way in which the Sun drives the oceanic circulation of the atmosphere that is, winds. Energy is transferred from winds to the upper layers of the ocean through frictional coupling between the ocean and the atmosphere at the sea surface. Another way is by causing variations in the temperature and salinity of seawater which in turn control its density.
Location
TONGA
Author(s)
Aung, Dr T H.
Publisher
AusAid
Publication Year:
1995
Publication Place
Australia
Physical Description:
31p,;29cm
Call Number
CLI
Language
English
Record ID:
20651
Legacy PEIN ID:
60574
General Notes
The waters of the ocean are continually moving. This motion ranges from powerful currents like the Gulf Stream, down to small swirls and eddies. What drives all this motion? The short answer is energy from the sun, and the rotation of the Earth. The most obvious way in which the Sun drives the oceanic circulation of the atmosphere that is, winds. Energy is transferred from winds to the upper layers of the ocean through frictional coupling between the ocean and the atmosphere at the sea surface. Another way is by causing variations in the temperature and salinity of seawater which in turn control its density.
Record Created: 05-Dec-2002
Record Modified: 18-Dec-2020