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50 Years of Ocean Discovery: National Science Foundation 1950-2000 (2000)
Commission on Geosciences, Environment and Resources (CGER)
Ocean Studies Board (OSB)

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. "Major Physical Oceanography Programs at NSF: IDOE Through Global Change." 50 Years of Ocean Discovery: National Science Foundation 1950-2000. Washington, DC: The National Academies Press, 2000.

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50 Years of Ocean Discovery: National Science Foundation 1950—2000

gram, under the direction of the World Climate Research Program was begun. Called CLImate VARiability, (CLIVAR), it is now viewed as the next major atmosphere-ocean program, with the goal of greatly improving our ability to forecast variations in climate on very long time scales. CLIVAR field programs are expected to last at least through the next decade and perhaps provide at last scientific motivation for the long-awaited Global Ocean Observing System, perhaps even a Global Climate Observing System.

In looking back at the IDOE, recall that one of the major characteristics of programs during this time was the initiation of major programs and then their dissection into smaller but still collaborative programs for the sake, primarily, of simplifying the management required. Recall the four major components of IDOE: Environmental Forecasting (EF), Environmental Quality (EQ), Living Resources (LR), and Non-living Resources, or Sea Bed Assessment (SBA). Consider for a moment the breakdown, or dissection, of the EF program, which consisted largely of physical oceanography programs. The major examples are MODE (Mid-Ocean Dynamics Experiment), POLYMODE (the U.S.-Soviet follow-on to MODE), NORPAX (North Pacific Experiment), ISOS (International Southern Ocean Studies), CLIMAP (Climate Long-range Investigation, Mapping, and Prediction Study), and CUEA (Coastal Upwelling Ecosystems Analysis). The latter two showed the way to truly interdisciplinary work, with CLIMAP studying physical phenomena in the distant past using paleoceanographic techniques and CUEA showing the way to investigating the physical impacts on fisheries, or "living resources."

Another legacy of the IDOE was the start-up of a number of midsize programs during the last year of the decade. These were clearly multiyear projects, with a requirement that funding continue in order to maintain them. Whether they were started in order to guarantee funding continuity or whether the continuity was already planned is not clear to me. In any case, they were logical follow-ons, but also led the way into the large global programs to follow. Some examples are the Coastal Ocean Dynamics Experiment (CODE); Tropic Heat (TH), a study of the Eastern Pacific Cold Tongue; Pacific Equatorial Ocean Dynamics Experiment (PEQUOD); the Western Equatorial Pacific Ocean Circulation Study (WEPOCS); and Transient Tracers in the Ocean (TTO), which was a follow on to the Geochemical Ocean Sections (GEOSECS) study, and a precursor to the tracer work to be done in WOCE and other survey experiments. This is another example of two disciplines coming together to study common problems.

Perhaps a better way of looking at the transition is shown in Table 1. MODE, which Walter Munk describes briefly, was the first comprehensive look at the mesoscale eddy field. Followed by the joint Russian-U.S. POLYMODE, it paved the way for the World Ocean Circulation Experiment. In a similar fashion, the GEOSECS program, leading into the study of Transient Tracers, also paved the way for the high-precision tracer work during WOCE.

TABLE 1 Time Line Summary Illustrating the Development from the Coordinated Program s of IDOE Through Mid-size Programs of the Transition Period (1980-1985) into the Global Programs of the USGCRP (WOCE and TOGA)

1970-1980

1980-1985

1985-1990

IDOE

Midsize Follow-ons

Global change

MODE

POLYMODE

WOCE

 

Transient Tracers

 

NORPAX

NORPAX (cont.)

TOGA

 

(Hawaii-Tahiti Shuttle)

 

 

PEQUOD

 

 

Tropic Heat

 

 

WEPOCS

 

Similarly, NORPAX, expanding its range with the Hawaii to Tahiti Shuttle, largely a survey using expendable bathythermographs with frequent crossings of the equator, was one of many midsize programs that paved the way for TOGA. Others include Tropic Heat, PEQUOD, WEPOCS, the National Oceanic and Atmospheric Administration's EPOCS (Eastern Pacific Ocean Climate Study), and others.

Major characteristics of these midsize programs include the following:

  1. They are needed to address problems too big for one or two principal investigators (PIs).

  2. They are usually regional, not basin-wide or global.

  3. They require several, but usually a s mall number of PIs.

  4. They usually involve coordinated field work.

  5. They are usually fully collaborative.

  6. The cost averages approximately $1 million to $3 million per year.

  7. There is little need for international or interagency coordination.

Some of the parallel characteristics of global change programs are the following:

  1. The studies are usually long-term (several years) and large-scale (global or at least basin-wide).

  2. They require a large number of PIs, although funding may be accomplished through individual grants.

  3. They require a collective review process that may differ from the normal review of individual proposals.

  4. The cost may average $5 million to $10 million per year or more for any given program.

  5. They are usually fully inter-agency (national programs).

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Front Matter (R1-R6)
Keynote Lecture The Emergence of the National Science Foundation as a Supporter of Ocean Sciences in the United States (1-8)
Landmark Achievements of Ocean Sciences Achievements in Biological Oceanography (9-21)
Achievements in Chemical Oceanography (22-43)
Achievements in Physical Oceanography (44-50)
Achievements in Marine Geology and Geophysics (51-64)
Deep Submergence: The Beginnings of Alvin as a Tool of Basic Research (65-66)
The History of Woods Hole's Deep Submergence Program (67-84)
Creating Institutions to Make Scientific Discoveries Possible A Chronology of the Early Development of Ocean Sciences at NSF (85-92)
Ocean Sciences at the National Sciences Foundation: Early Revolution (93-95)
Ocean Sciences at the National Sciences Foundation: An Administrative History (96-106)
Two Years of Turbulence Leading to a Quarter Century of Cooperation: The Birth of UNOLS (107-116)
Scientific Ocean Drilling, from AMSOC to COMPOST (117-127)
Technology Development for Ocean Sciences at NSF (128-134)
Large and Small Science Programs: A Delicate Balance The Great Importance of “Small” Science Programs (135-140)
The Role of NSF in “Big” Ocean Science: 1950 to 1980 (141-148)
Major Physical Oceanography Programs at NSF: IDOE Through Global Change (149-151)
Major International Programs in Ocean Sciences: Ocean Chemistry (152-162)
Ocean Sciences Today and Tomorrow The Future of Physical Oceanography (163-168)
The Future of Ocean Chemistry in the United States (169-171)
The Future of Marine Geology and Geophysics: A Summary (172-183)
Out Far and In Deep: Shifting Perspectives in Ocean Ecology (184-191)
Global Ocean Science: Toward an Integrated Approach (192-194)
Education in Oceanography: History, Purpose, and Prognosis (195-200)
Evolving Institutional Arrangements for U.S. Ocean Sciences (201-206)
NSF's Commitment to the Deep (207-209)
Fifty Years of Ocean Discovery (210-211)
Argo to ARGO (212-213)
The Importance of Ocean Sciences to Society (214-216)
Appendix A: Symposium Program (217-222)
Appendix B: Symposium Participants (223-232)
Appendix C: Poster Session (233-234)
Appendix D: NSF Division of Ocean Sciences: Senior Science Staff, Rotators, IPAs, and Visiting Sciences (235-246)
Appendix E: Support of Ocean Sciences at NSF from 1966 to 1999 (247-249)
Appendix F: Organizational Charts (250-257)
Appendix G: NRC Project Oversight (258-258)
Appendix H: Acronyms (259-262)
Index (263-270)
Supplementary Pictures (271-278)