Warm Core Ring Project 19 April - 6 May, 1982
Warm Core Ring Project 19 April - 6 May, 1982
Date
1983-12
Authors
Phinney, David A.
Langton, Elizabeth W.
Garside, Jean C.
Langton, Elizabeth W.
Garside, Jean C.
Linked Authors
Alternative Title
Citable URI
As Published
Date Created
Location
Sargasso Sea
DOI
10.1575/1912/6975
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Keywords
Water masses
Ocean circulation
Marine biology
Chemical oceanography
Knorr (Ship : 1970-) Cruise KN93
Warm Core Rings
Ocean circulation
Marine biology
Chemical oceanography
Knorr (Ship : 1970-) Cruise KN93
Warm Core Rings
Abstract
The second cruise of the Warm Core Rings program marks the
beginning of an intensive season of field study. Again, our interests
are primarily concerned with measuring the bio-optical properties of
rings and surrounding water masses. Through our observations of the
horizontal and vertical distributions of phytoplankton and their
pigments concurrent with observations of the submarine light field, we
attempt to further our understanding of the relationship between light
and photosynthetic organisms in the sea, and our ability to remotely
sense them. Several modifications to the main objectives of the program's field
efforts, from those of October 1981, are to be noted. Studies of ring
81-D in October 1981 was the first attempt for many investigators to
make measurements in the unique environment of a warm core ring. As the
likelihood of the ring surviving until the following field season was
slim, no attempt was made to revisit the ring. Physical measurements
were made from a constantly mobile platform, R/V Endeavor, while the
biological platform, R/V Atlantis II, sat on station for days.
Biological measurements ~vere spatially divided into three sub-areas:
slope water, ring center, and the high velocity region.With our feet wet, the strategy was now to select a ring that would
be long lived, such that it could be revisited several times during the
field season. lfhile the physical measurements were being made in much
the same fashion from R/V Endeavor, biologists were split among R/V
Knorr and R/V Oceanus, with a resultant increase in mobility. Finally, measurements of the surrounding water masses grew to include the Gulf
Stream and Sargasso Sea.