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PANGAEA.
Data Publisher for Earth & Environmental Science

Clemens, Steven C (1998): Dust flux in the Arabian Sea [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.857566, Supplement to: Clemens, SC (1998): Dust response to seasonal atmospheric forcing: Proxy evaluation and calibration. Paleoceanography, 13(5), 471-490, https://doi.org/10.1029/98PA02131

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Abstract:
Eolian grain size and flux were measured on samples from 11 Arabian Sea sediment traps deployed 200-1250 km offshore. The timing of increased grain size is coincident with the onset of strong summer monsoon winds and dust storm activity over the Arabian Peninsula and Middle East. Data spanning a full annual cycle show that eolian grain size is highly correlated with barometric pressure (r=-0.91) and wind speed (r=0.84), enabling calibration of the downcore record in terms of these primary meteorological variables. Eolian flux is highly correlated with organic carbon flux (r=0.80); both increase 6–8 weeks after the grain size increase and summer monsoon onset. This lag, and the low correlation between eolian grain size and eolian flux (r=0.36), likely result from the differential sinking rates of large and small dust particles in the surface waters as well as biological scavenging associated with monsoon-induced productivity.
Related to:
Clemens, Steven C (1998): Arabian Sea Sed. Trap Dust Flux, Grain Size Data. NOAA National Centers for Environmental Information, https://doi.org/10.25921/C591-2C79
Coverage:
Median Latitude: 15.863883 * Median Longitude: 60.550667 * South-bound Latitude: 10.000000 * West-bound Longitude: 58.802000 * North-bound Latitude: 17.400000 * East-bound Longitude: 65.000000
Date/Time Start: 1994-11-13T14:00:00 * Date/Time End: 1995-12-15T23:00:00
Size:
6 datasets

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