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(Table 1) Accumulation of opal and eaolian sediment in ODP Site 145-886
This dataset has no description
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(Table 1) Accumulation of opal and eaolian sediment in ODP Hole 145-885A
This dataset has no description
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(Table 3) Lithogenic flux data of sediment core M40/4_SL71
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(Table 3) Lithogenic flux data of sediment core M40/4_SL67
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(Table 3) Lithogenic flux data of sediment core M40/4_KL51
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Dust content in sediments of ODP Hole 108-659A in the North Atlantic
This dataset has no description
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(Table 2) Sedimentology of core V21-146 in the Northwest Pacific Ocean
This dataset has no description
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(Table 4) Dust and opal content from DSDP Hole 68-503B
This dataset has no description
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NEEM-2011-S1 ice-core aerosol record (conductivity, NH4, NO3, BC, acidity, Na...
A continuous ice core analytical system was used to analyze the ~410 m NEEM-2011-S1 ice core collected in summer 2011 near the NEEM deep drilling site in NW Greenland. The core... -
Atmospheric river dust scores for 2001 to 2018
The AR "dust score" characterizes the dustiness of the environment associated with ARs that made landfall along the west coast of the U.S. between 2001 and 2018 using... -
Back Trajectories for "Atmospheric Dust Deposition Varies by Season and Eleva...
Back trajectory runs to accompany analysis of dust at sites near Boulder, CO, USA using the Stochastic Time-Inverted Lagrangian Trajectory model (STILT) run with High Resolution... -
Dust aerosol optical depth, supplement to: Voss, Kara K; Evan, Amato T (2019)...
Dust Aerosol Optical Depth deprived from the MODIS sensor on the Terra satellite platform at 1 degree latitude x 1 degree longitude spatial resolution between 45 south and 50... -
Single-grain mineralogical data from two Antarctic ice cores (Dome B, Dome C)...
Mineral species and polymorphs identified in two antarctic ice cores by single-grain Raman spectroscopy. Data are provided for the Holocene and for the last glacial period,... -
Dust motion in snow microstructure, supplement to: Hagenmuller, Pascal; Flin,...
The deposition of light-absorbing particles (LAPs) such as mineral dust and black carbon on snow is responsible for a highly effective climate forcing, through darkening of the... -
(Table 1) Mass-accumulation rates for the non-authigenic, inorganic, crystall...
Elevated regions in the central parts of ocean basins are excellent for study of accumulation of eolian material. The mass-accumulation rates of this sediment component appear... -
(Table 1) Age, porocity, density, mass accumulation rates and grain size of t...
Eolian dust preserved in deep-sea sediments provides a record of atmospheric circulation throughout geologic time. This eolian component has been isolated to determine its mass... -
(Table T1) Sedimentation rate, bulk density and mass accumulation rate of ODP...
Ocean Drilling Program Leg 198 Site 1208 is located on the Central High of Shatsky Rise (36°7.6301'N, 158°12.0952'E) in the North Pacific Ocean at a water depth of 3346 m. A... -
(Table 3) Aeolian component of North Pacific pelagic sediments, supplement to...
Isolation and analysis of the eolian component of late Cenozoic pelagic sediments from the North Pacific provides direct information concerning changes in atmospheric... -
Linear sedimentation rates and mass accumulation rates of detritus and Kosa o...
In order to reconstruct past variations in the east Asian monsoon and to establish a direct link between terrestrial and marine climatic records, we evaluated the temporal... -
Accumulation rates of Late Cretaceous eolian sediments in DSDP Hole 62-463 in...
Eolian dust preserved in deep-sea sediment can provide a direct historical record of global atmospheric circulation. Data from a reasonably complete Upper Cretaceous section of...
