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individual events that have a limited duration, superimposed on the background of these gradual changes. As a result, the gradual changes in time and space have to be assessed together with processes that lead to flooding and erosion events. These processes include storm surges, waves and tides or a combination of these processes and lead to ESL events see Figure 4.4. In this section, newly emerging understanding of these different episodic and gradual aspects of sea level change are assessed, within a context of sea level changes measured directly over the last century, and those inferred for longer geological time scales. This longerterm perspective is important for contextualising future projections of sea level and providing guidance for processbased models of the individual components of SLR, in particular the ice sheets. In addition, anthropogenic subsidence may affect local sea level substantially in many locations but this process is not taken into account in values reported here for projected SLR unless specifically noted. Another major issue is the effect on bearing capacity of the ground. In many coastal zones, as the ground consists of loose sediment deposition, its bearing capacity is not high by its nature. In addition to this, sealevel rise raises the water table in the aquifers, increasing the risk of liquefaction

custom name chicago bears football all over print bedding set 1
custom name chicago bears football all over print bedding set 1

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