Constraining the North Atlantic Circulation with Transient Tracer Observations

• Main Author: Li, Xingwen
• Other Authors: MASSACHUSETTS INST OF TECH CAMBRIDGE
• Format: Text
• Language: English
• Published: 2003
• Subjects: Physical and Dynamic Oceanography; *OCEAN CURRENTS; *TRACER STUDIES; *CHEMICAL OCEANOGRAPHY; MATHEMATICAL MODELS; TRANSIENTS; DATA MANAGEMENT; THESES; THERMAL EXPANSION; BOUNDARY VALUE PROBLEMS; SALINITY; AIR WATER INTERACTIONS; TEMPERATURE COEFFICIENTS; NORTH ATLANTIC OCEAN; FLUORINATED HYDROCARBONS; CHLORINATED HYDROCARBONS; RADIOACTIVE DECAY; TRITIUM; *OCEAN CIRCULATION; *TRANSIENT TRACERS; CHLOROFLUOROCARBONS; DATA ASSIMILATION; NADW; North Atlantic
• Online Access: http://www.dtic.mil/docs/citations/ADA413812; http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA413812

The capability of transient tracers to constrain the ocean circulation in the North Atlantic is explored. Study of an idealized tracer shows that inferences of circulation properties from transient state distributions are impacted by uncertainties in the time-varying boundary conditions and sparse data coverage. Comparison of CFC, tritium, temperature and salinity (T-S) observations with model results in the North Atlantic shows that regions of important model-data disagreements in the transient tracer fields can also be readily identified in the T-S distributions. In the model, excessive vertical penetration of convective adjustment, leads to problematic production and outflow of the NADW, again appearing in both transient tracer and T-S fields. Sensitivities of the model fields are determined using the adjoint model. In the dual solutions, CFC-11, CFC-11/CFC-12 ratio age, and T - (Beta/alpha)S (alpha and Beta are thermal and haline expansion coefficients, respectively) exhibit the major ventilation pathways and the associated timescales, in the model. High sensitivity fields are candidates for providing the most powerful constraints in the corresponding inverse problems. Assimilation of both CFC and tritium data, with different input histories, sampling distributions, and radioactive decay constants, shows that by adjusting only initial-boundary conditions of CFCs and tritium, a 1 deg x 1 deg offline model and the transient tracer data can be brought into near-consistency, in the domain between 4.5 degrees South and 39.5 degrees North of the North Atlantic. Constraining a GCM with transient tracers is thus fully practical. However, the large uncertainties in the time-varying boundary conditions of transient tracer concentrations, and in their interior distributions, renders the transient tracers less-effective in determining the circulation than are more conventional steady tracers, and known oceanic dynamics. The original document contains color images. All DTIC reproductions will be in black and white. Sponsored in part by Grants NAG5-7857 and NAG5-11933. Prepared in cooperation with Woods Hole Oceanographic Institution, Woods Hole, MA.