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A Neutral Density Variable for the World's Oceans


Jackett, DR and McDougall, TJ, A Neutral Density Variable for the World's Oceans, A Neutral Density Variable for the World's Oceans, 27, (2) pp. 237-263. ISSN 0022-3670 (1997) [Refereed Article]

DOI: doi:10.1175/1520-0485(1997)027<0237:ANDVFT>2.0.CO;2


The use of density surfaces in the analysis of oceanographic data and in models of the ocean circulation is widespread. The present best method of fitting these isopycnal surfaces to hydrographic data is based on a linked sequence of potential density surfaces referred to a discrete set of reference pressures. This method is both time consuming and cumbersome in its implementation. In this paper the authors introduce a new density variable, neutral density γn, which is a continuous analog of these discretely referenced potential density surfaces. The level surfaces of γn form neutral surfaces, which are the most appropriate surfaces within which an ocean model's calculations should be performed or analyzed. The authors have developed a computational algorithm for evaluating γn from a given hydrographie observation so that the formation of neutral density surfaces requires a simple call to a computational function. Neutral density is of necessity not only a function of the three state variables: salinity, temperature, and pressure, but also of longitude and latitude. The spatial dependence of γn is achieved by accurately labeling a global hydrographie dataset with neutral density. Arbitrary hydrographic data can then be labeled with reference to this global γn field. The global dataset is derived from the Levìtus climatology of the world's oceans, with minor modifications made to ensure static stability and an adequate representation of the densest seawater. An initial field of γn is obtained by solving, using a combination of numerical techniques, a system of differential equations that describe the fundamental neutral surface property. This global field of γn values is further iterated in the characteristic coordinate system of the neutral surfaces to reduce any errors incurred during this solution procedure and to distribute the inherent path-dependent error associated with the definition of neutral surfaces over the entire globe. Comparisons are made between neutral surfaces calculated from γn and the present best isopycnal surfaces along independent sections of hydrographic data. The development of this neutral density variable increases the accuracy of the best-practice isopycnal surfaces currently in use but, more importantly, provides oceanographers with a much easier method of fitting such surfaces to hydrographic data.

Item Details

Item Type:Refereed Article
Research Division:Earth Sciences
Research Group:Oceanography
Research Field:Physical oceanography
Objective Division:Environmental Management
Objective Group:Marine systems and management
Objective Field:Oceanic processes (excl. in the Antarctic and Southern Ocean)
UTAS Author:Jackett, DR (Mr Jackett)
UTAS Author:McDougall, TJ (Professor Trevor McDougall)
ID Code:12654
Year Published:1997
Web of Science® Times Cited:446
Deposited By:IASOS
Deposited On:1997-08-01
Last Modified:2011-08-15

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