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To rectify this, beginning in May 2012 we measured the salinity of water from freshwater ponds and rice paddies on Polder 32 in areas that experienced long-term inundation with brackish tidal channel water and in control areas that were not inundated.
Much of the story was drawn from the legend of Gilgamesh, the ancient Mesopotamian hero, which recounts the tale of a great inundation with details strikingly similar to those in Genesis.
According to the interview (13 in Fig. 3), inundation with PDCs ended before 12 15.
Long-term inundation with brackish water from the surrounding tidal channels and deposition of salt-rich sediments may lead to salinization of surface water bodies in polders.
Furthermore, inundation with cool water decreased skin temperatures more quickly than the clothing insulating case and led to a modest decrease in the burn extent.
There was also substantial diagenetic enrichment of poorly crystalline Fe-oxides near the soil surface following tidal inundation, with reactive Fe spanning 400 1800 µmol g− 1.
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Two main habitats are differentiated (Wittmann et al., 2002): (i) low-várzea forests, influenced by mean inundations with heights between 3.0 and 7.5 m (corresponding to a mean inundation period of 50 230 days year−1) and (ii) high-várzea forests, influenced by mean inundations with heights of <3.0 m (<50 days year−1).
Social resilience of the region has been tested with both terrorist attacks and the widespread inundation associated with Superstorm Sandy.
According to a worst scenario, the potential tsunami might hit the coast of Painan about 26 minutes after the rupture and the entire city could be inundated with a maximum inundation depth of about 7 m.
The dominant effect of bottom resistance is to reduce the range of inundation, particularly with larger resistance coefficients.
Fig. 5 Tsunami inundation associated with a modeled megathrust and b upper-plate fault ruptures along the Manila Trench forearc region.
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