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Ross Gyre variability modulates oceanic heat supply toward the West Antarctic continental shelf - Communications Earth & Environment

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Ross Gyre variability modulates oceanic heat supply toward the West Antarctic continental shelf - Communications Earth & Environment

West Antarctic Ice Sheet mass loss is a major source of uncertainty in sea level projections. The primary driver of this melting is oceanic heat from Circumpolar Deep Water originating offshore in the Antarctic Circumpolar Current. Yet, in assessing melt variability,

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Ross Gyre variability modulates oceanic heat supply toward the West Antarctic continental shelf - Communications Earth & Environment

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Ross Gyre variability modulates oceanic heat supply toward the West Antarctic continental shelf - Communications Earth & Environment

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