On Ocean Transport Diagnostics: The Idealized Age Tracer and the Age SpectrumSource: Journal of Physical Oceanography:;2002:;Volume( 032 ):;issue: 006::page 1987DOI: 10.1175/1520-0485(2002)032<1987:OOTDTI>2.0.CO;2Publisher: American Meteorological Society
Abstract: The idealized age tracer is commonly used to diagnose transport in ocean models and to help interpret ocean measurements. In most studies only the steady-state distribution, the result of many centuries of model integration, has been presented and analyzed. However, in principle the transient solution provides more information about the transport. Here it is shown that this information can be readily interpreted in terms of the ventilation histories of water masses. A simple relationship is derived, valid for stationary transport, between the transient evolution, τid(r, t), of the idealized age tracer and the ?age spectrum,? G(r, t), the distribution of times t since a water mass was last ventilated. Namely, G(r, t) = ??ttτid(r, t). Implications of the relationship are discussed, and the relationship is illustrated with an idealized model.
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contributor author | Hall, Timothy M. | |
contributor author | Haine, Thomas W. N. | |
date accessioned | 2017-06-09T14:55:21Z | |
date available | 2017-06-09T14:55:21Z | |
date copyright | 2002/06/01 | |
date issued | 2002 | |
identifier issn | 0022-3670 | |
identifier other | ams-29717.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4166975 | |
description abstract | The idealized age tracer is commonly used to diagnose transport in ocean models and to help interpret ocean measurements. In most studies only the steady-state distribution, the result of many centuries of model integration, has been presented and analyzed. However, in principle the transient solution provides more information about the transport. Here it is shown that this information can be readily interpreted in terms of the ventilation histories of water masses. A simple relationship is derived, valid for stationary transport, between the transient evolution, τid(r, t), of the idealized age tracer and the ?age spectrum,? G(r, t), the distribution of times t since a water mass was last ventilated. Namely, G(r, t) = ??ttτid(r, t). Implications of the relationship are discussed, and the relationship is illustrated with an idealized model. | |
publisher | American Meteorological Society | |
title | On Ocean Transport Diagnostics: The Idealized Age Tracer and the Age Spectrum | |
type | Journal Paper | |
journal volume | 32 | |
journal issue | 6 | |
journal title | Journal of Physical Oceanography | |
identifier doi | 10.1175/1520-0485(2002)032<1987:OOTDTI>2.0.CO;2 | |
journal fristpage | 1987 | |
journal lastpage | 1991 | |
tree | Journal of Physical Oceanography:;2002:;Volume( 032 ):;issue: 006 | |
contenttype | Fulltext |