| description abstract | Up to forty neutrally buoyant floats (20 at 700 m, 20 at 1300 m) were used in the POLYMODE Local Dynamics Experiment (LDE) to provide a quasi-Lagrangian description of the structure and evolution of the mesoscale eddy field in a limited region characterized by higher kinetic energy levels than those obtained in MODE. This paper is an overview and summary of the data collected. The temporal development of the two-level float array is presented in a sequence of maps, each spanning five days. In these one readily notices an ?oscillation? of floats at 1300 m in a NE-SW direction before the cluster breaks apart. At 700 m the float cluster subdivides much more rapidly. The first setting of 700-m floats drifts to the west; the second group, launched two months later, goes far to the east. Ensemble averages as a function of time of the floats at 1300 m reveal great sensitivity to the ?oscillatory? velocity field while the array is ?tight? or coherent the corresponding 700-in averages, although noisy, show clearly the westward and eastward motion of the first and second clusters respectively. Grand averages for ?, ? (cm s?1), and kinetic energy (ergs gm?1) are (?1.8, 0., 80) and (?1.6, 0., 34) for the shallow and deep floats. The spatial correlation functions show 1arge scales of coherence. The zero-crossing of the transverse-velocity correlation function is about 100 km for both the 700- and 1300-m floats compared to 55 km for the 1500-m goats in MODE. The longitudinal correlation scale is also much larger. | |
