The two climate variables which are mainly determined
by dynamical process, SLP and SW - CLR (determined by the distribution of water vapour), do not cover sufficiently wide ranges in any of the SMEs.
The vulnerability of the ice sheets to warming could be increased
by dynamical processes related to ice flow (not included in current models but suggested by recent observations) thereby increasing future sea level rise.
Not exact matches
At any given instant it can be argued that the cell is in a «state» defined
by its components — their concentrations and locations, the interactions between components — that are modulated in space and time, and the complex circuitry — that involves a large number of interacting networks and a snapshot of the
dynamical processes — such as gene expression, cell cycle, transport of components, etc..
•
Dynamical processes related to ice flow not included in current models but suggested
by recent observations could increase the vulnerability of the ice sheets to warming, increasing future sea level rise.
Such possible large - scale
dynamical feedbacks are also influenced
by small - scale
processes within the climate system.
Dynamical processes related to ice flow — which are not included in current models but suggested
by recent observations — could increase the vulnerability of the ice sheets to warming, increasing future sea level rise.
Such accelerated flow leads to increased ice discharge into the ocean, but the relevant
dynamical processes are not properly understood nor included in continental ice - sheet models, the main difficulty being the treatment of grounding - line migration in response to increased melting of ice
by the ocean.
The research areas covered
by division extend from the large - scale
dynamical / meteorological
processes and systems in the atmosphere (like cyclones and global atmosphere circulation) to the small scale turbulent mixing, they cover the time frame from centuries to seconds.