As noted by Reager (2016) in A Decade of Sea Level Rise Slowed by Climate -
Driven Hydrology, researchers had determined the seasonal delay in the return of precipitation to the oceans causes sea levels to oscillate by 17 ± 4 mm [~ 0.7 inches] per year.
«A Decade of Sea Level Rise Slowed by Climate -
Driven Hydrology.»
Working from a set of projections from eight different global climate models being driven by three different emissions scenarios, the authors used statistical downscaling to
drive a hydrology model to determine what changes could be seen to the hydrology of these regions.
Not exact matches
Climate projections were statistically downscaled and used to
drive a macro-scale
hydrology model at high spatial resolution.
These Coupled Model Intercomparison Project Phase 3 (CMIP3) simulations were statistically downscaled and used to
drive the Variable Infiltration Capacity (VIC)
hydrology model over several watersheds.
The piece about the Greenland ice sheet had not a peep about the effect of geothermal activity under the ice sheet and the basal melting that is occurring
driving the vigorous subglacial
hydrology as outlined in Rogozhina et al, 2016.