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    PANGAEA
    In:  Supplement to: Rea, David K; Janecek, Thomas R (1982): Late Cenozoic changes in atmospheric circulation deduced from North Pacific eolian sediments. Marine Geology, 49(1-2), 149-167, https://doi.org/10.1016/0025-3227(82)90034-2
    Publication Date: 2023-10-19
    Description: Isolation and analysis of the eolian component of late Cenozoic pelagic sediments from the North Pacific provides direct information concerning changes in atmospheric circulation. A 50% increase in intensity of both the prevailing westerlies and the tradewinds coincides with increasing pole-to-equator temperature gradients resulting from the onset of northern hemisphere glaciation. At the same time, the mass flux of dust from continents to the North Pacific increased by a factor of 4.5, apparently reflecting significantly increased continental aridity associated with the late Cenozoic glacial ages.
    Keywords: 31-292; 32-305; 32-310; 62-463; Accumulation rate, dust; Accumulation rate, mass; AGE; Calculated after FOLK; Deep Sea Drilling Project; Density, dry bulk; DRILL; Drilling/drill rig; DSDP; Dust, aeolian; Event label; Glomar Challenger; GPC-3; Leg31; Leg32; Leg62; LL44-GPC-3; Median, grain size; North Pacific; North Pacific/CONT RISE; North Pacific/Philippine Sea/CONT RISE; North Pacific/SEAMOUNT; PC; Piston corer; Sedimentation rate
    Type: Dataset
    Format: text/tab-separated-values, 442 data points
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