When analyzing the resulting spatiotemporal profiles of substrate cleavage by effector caspases, the spatial anisotropies of the model input were translated into a homogeneous response across the modelled distance (Fig. 3A, C).
The analyses involving buildings presented here are preliminary, as the number of OSM buildings across our modelled permafrost domain was obviously much less than the actual number.
This was achieved with the OSM places map feature, which includes ca. 10 times more populated settlements than analogous open datasets (e.g., the Global Rural Urban Mapping Project, Naturalearthdata.com Populated places) across the modelled permafrost region.
R&D priority should be given to those less-policy-sensitive technologies that are in any case deployed rapidly across the modelled time horizon (e.g. PV), but also to those deployed up to their technical potentials and typically less sensitive to exogenous policy routes.
The results presented here consider many different possible configurations across the modelled networks.
The model developed was validated with empirical data and showed that the dilution effect was strongly sensitive to a combination of factors related to HSR, the perception of habitat by hosts and their movement across the modelled lattices.
Other locations showed a similar pattern across the events modelled, although with different depth range values.
Both locations showed similar patterns in flow velocities across the scenarios modelled (Fig. 4b,c).
This distribution pattern is consistent across the events modelled, with the smaller events showing lower absolute maximum water level values but similar overall spatial trends.
Design adaptability to orientation change was modelled across two scenarios; current building energy efficiency standards and pending improved energy efficiency standards.
