Representativeness of meridional hydrographic sections in the western South Atlantic
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ID: 308076
2004
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Abstract
Many studies of the oceanic circulation are based on data collected during quasi-synoptic hydrographic surveys. After spatial averaging, to e lter out the effects of mesoscale variability, it is often explicitly or implicitly assumed that the synoptic hydrographic gradients are representative of a quasi-steady “ mean” state. Climatological tracer e elds and e oat data at the depth of the North Atlantic Deep Water in the western South Atlantic (Brazil Basin) support the notion of a quasi-steady mean circulation characterized by alternating bands of primarily zonal e ow with meridional scales of several hundreds of km. Visually, the mean circulation appears to dominate three samples of the large-scale meridional-density-gradient e eld taken between 1983 and 1994. A quantitative comparison reveals, however, that the baroclinic temporal variability of the zonal velocities is of the same magnitude as the mean and is associated with similar spatial scales. The synoptic geostrophic e ow e eld is, therefore, only marginally representative of the mean state. Thus, the data do not support one of the central assumptions of reference-velocity methods, such as linear box-inverse models and the b-spiral, because baroclinic temporal variability renders the equation systems underlying these methods inconsistent. A modal decomposition of the temporally varying baroclinic zonal velocity e eld in the Brazil Basin indicates that the e rst two dynamical modes dominate, accounting for ’90% of the rms velocities. The residual e ow e eld that remains after removing the e rst two baroclinic modes from the three synoptic samples is dominated by the mean circulation. However, its magnitude is not sufe cient to account for the e oat and tracer observations. Therefore, it is necessary to determine the projection of the mean zonal velocities onto the barotropic and the e rst two baroclinic modes in order to diagnose fully the mean zonal circulation in the western South Atlantic. There is evidence that the representativeness of synoptic hydrographic sections in other regions may be similarly marginal.
| Reference Key |
openalex_W2034156307
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| Authors | Andreas M. Thurnherr, K. G. Speer |
| Journal | journal of marine research |
| Year | 2004 |
| DOI |
10.1357/00222400460744618
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| URL | |
| Keywords | Keywords not found |
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