basal water layer thickness W i,j , hydraulic potential P i,j , normal- ization N i,j , water flux φ i,j (for coupling to an A-grid ice model), at the grid cell edges: water transport
The major regional ozone depletion events that were visible at all coastal stations, and discussed above, can also be seen in Fig. The August event is clearly evident in Site C as
Fresh water hosing experiments, in which the Atlantic Meridional Overturning Circulation (AMOC) is perturbed by imposing a fresh water flux, usually in the North Atlantic, are
The model ensemble mean annual mean temperature change, LIG minus pre-industrial (Fig. 6a), is characterised by maximum warming at high latitudes, especially in the Arctic..
From this observation, one could conclude that thermodynamic growth conditions can vary substantially within the surveyed region, such that a 1-D ther- modynamic growth model for
Records of XRF Si/Al log-ratios reflecting changes in biogenic opal concentrations (marine productivity), XRF records of Fe (in cps) reflecting relative changes in terrigenous
Detailed sediment descriptions of the drill cores 5011-1A, 1B and 1C from central Lake El’gygytgyn, along with mea- surements of magnetic susceptibility and gamma-ray density,
Measured vertical profiles of ozone mixing ratio with the DIAL along the inbound flight track, and in situ measurements (gray line) along the outbound flight track (position B1 in
