In seismology and ocean acoustics, the interface with the atmosphere is typically represented as ...
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Future sea surface temperature and sea-ice concentration from coupled ocean–atmosphere general ci...
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The estimation of high quantiles for very low probabilities of exceedance pn much smaller than 1/...
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The receiver-to-source backazimuth of atmospheric infrasound signals is biased when cross-winds a...
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Science benefits tremendously from mutual exchanges of information and pooling of effort and reso...
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