Abstract
Munk and Forbes have proposed to detect greenhouse gas-induced climate changes in the World Ocean with an array of long-range acoustic transmissions from Heard Island in the southern Indian Ocean. We estimated - assuming a continuously monitorable simplified axial ray propagation - the signal-to-noise ratio for such an experiment in an environment of slow fluctuations of the thermohaline circulation on a decadal time scale. The signal and noise are obtained from two coarse-resolution ocean general circulation model simulations. An array with an acoustic source near Heard Island would monitor primarily temperature changes in the near-surface layers of the Southern Ocean rather than in low-latitude intermediate depths. The trend detection probability for any single path came out to be weak, at least for a one-decade measuring interval. But using information from at least a two-decade interval and an array of receivers improved the detection probabilities substantially. -from Authors
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CITATION STYLE
Mikolajewicz, U., Maier-Reimer, E., & Barnett, T. P. (1993). Acoustic detection of greenhouse-induced climate changes in the presence of slow fluctuations of the thermohaline circulation. Journal of Physical Oceanography, 23(6), 1099–1109. https://doi.org/10.1175/1520-0485(1993)023<1099:ADOGIC>2.0.CO;2
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