Method: begin of core to 69.749m = CFA Bern layer counting; 69.837m - end of core = densification model by Schwander et al. (1993)
Institute of Oceanographic Sciences Deacon Laboratory (now National Oceanography Centre, Southampton). Authorship was originally "BODC" and was changed by request of the BODC.
The salinity profiles have been checked for spurious points as well as sensor drift. The drift correction has not been applied to each profile so ther is still a use at your own risk warning on them. Some original files had data thrown away and so filled the data with null values. These profiles have been removed from the data included here. Also if a temperature or salinity was missing, the pressure level has been...
Species PCOB; No of rings 175; Begin 1817; End 1991
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
Processing method: splined, velocity algorithm: splined. Data have been checked by the WOCE Subsurface Float Data Assembly Center. See hdl:10013/epic.32931.d001 for further information.
Bongo net frame diameter: 60 cm; mesh size: 335 µm; towing speed 2-3 knots in a circular path
Actual Evapotranspiration (AET) consists of evaporation from rainwater intercepted by the canopy before it reaches the ground, from wet and moist soil, and the transpiration through stomata on plant stems and leaves. Evapotranspiration claimed 61% of all rainwater that falls on land. Using the satellite remote sensing data, evapotranspiration from earth land surface have been collected by NASA. Zhang, Kimball et al. (2009) spatially aggregated the global 8-km NASA dataset and published the global monthly...
Historical reanalysis climate data (TMAX, TMIN, PCP) at 0.5o resolution from Climate Research Unit East Anglia (CRU TS 3.1) is reformatted for use in SWAT models. The daily data covers the period of (1970-2005). This data can serve as observed data in regions where observed data is sparse or not available. For future data, we used the ISI-MIP data (Hempel et al., 2013, doi:10.5194/esd-4-219-2013). These were created using five GCM archives as input: HadGEM2-ES, IPSL-CM5A-LR,...
(Table 13) Distribution of Oligocene to Miocene radiolarians in DSDP Hole 33-317B from the Central Pacific OceanAnnika Sanfilippo & Catherine A Nigrini
Species abundance: C = common, F = few, R = rare, + = single specimen, ? = dubious identification, - = searched for and not found
For definition of quality flags see hdl:10013/epic.31518.d001
Species LASI; No of rings 205; Begin 1786; End 1990
Species ABAL; No of rings 46; Begin 1638; End 1683
Data derive from coulometer, CHNS analyzer, and pyrolysis oven (rock eval)
Location: Arosa, Switzerland; Distance from radiation site: 200 km
Species PCAB; No of rings 44; Begin 1454; End 1497