Dissolved Gaseous Tracers in the South Atlantic Ventilation Experiment:  Chlorofluoromethanes
{'Code': '06040302', 'Directorate': {'Abbreviation': 'GEO', 'LongName': 'Directorate For Geosciences'}, 'Division': {'Abbreviation': 'OCE', 'LongName': 'Division Of Ocean Sciences'}}
{'SignBlockName': 'Donald L. Rice', 'PO_EMAI': None, 'PO_PHON': None}
Two campaigns to measure transient tracers in the Atlantic              Ocean (TTO/NAS and TTO/Equatorial) were funded by NSF during the                period from 1980 to 1985.  A complete data base for modelling                   this ocean basin would include a South Atlantic Study to:                               1.Determine CO2 transports and their influence on world                 climate,                                                                        2.Constrain models of major ocean currents in this area,                        and                                                                             3.Confirm an observed 5-fold increase in the addition                           rate of new carbon to the thermocline.                                                  Eight components of such a study (SAVE) will be performed by            investigators from LDGO, Princeton, University of Washington,                   WHOI, and SIO.  The track record of these scientists is well                    established by successful completion of previous studies in the                 Equatorial and North Atlantic.  They will provide physical and                  chemical expertise which will be directed toward a cooperative                  effort to reach the goals of the geochemical study.                                     This component is aimed at using dissolved gaseous tracers              to determine rates of thermocline ventilation, rates and pathways               of spreading Antarctic Intermediate Water, rates and paths of                   Deep and Bottom Water spreading, and rates of cross-equatorial                  exchange.  From a knowledge of the extent of equilibration of                   dissolved gases in the formation area with the atmosphere, the                  spreading rates can be determined from a simple box model.
{'FirstName': 'Ray', 'LastName': 'Weiss', 'PI_MID_INIT': 'F', 'PI_SUFX_NAME': None, 'PI_FULL_NAME': 'Ray F Weiss', 'EmailAddress': 'rfweiss@ucsd.edu', 'NSF_ID': '000449795', 'StartDate': '05/01/1987', 'EndDate': None, 'RoleCode': 'Principal Investigator'}
{'Name': 'University of California-San Diego Scripps Inst of Oceanography', 'CityName': 'LA JOLLA', 'ZipCode': '920931500', 'PhoneNumber': '8585341293', 'StreetAddress': '8622 DISCOVERY WAY # 116', 'StreetAddress2': None, 'CountryName': 'United States', 'StateName': 'California', 'StateCode': 'CA', 'CONGRESSDISTRICT': '50', 'CONGRESS_DISTRICT_ORG': 'CA50', 'ORG_UEI_NUM': 'QJ8HMDK7MRM3', 'ORG_LGL_BUS_NAME': 'UNIVERSITY OF CALIFORNIA SAN DIEGO', 'ORG_PRNT_UEI_NUM': 'QJ8HMDK7MRM3'}
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[{'Code': '1610', 'Text': 'PHYSICAL OCEANOGRAPHY'}, {'Code': '1670', 'Text': 'Chemical Oceanography'}, {'Code': '3772', 'Text': None}, {'Code': '5419', 'Text': 'INTERNATIONAL SUPPORT'}]
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