or constructed channels to accommodate the flow, water overflows the stream banks, spilling out into adjacent low lying areas. Riverine flooding occurs as a consequence. The dynamics of riverine flooding vary with terrain. In relatively flat areas, land may stay covered with shallow, slow-moving floodwater for days or even weeks. In hilly and mountainous areas, floods may come minutes after a heavy rain. The short notice, large depths and high velocities of flash floods make these types of floods
Mean global sea-level has already begun rising; over the 20th century mean sea-level rose 0.17 metres (0.12 metres – 0.22 metres). Significantly the rate of this rise was seen to accelerate towards the end of the century. What is modelled in this study is observed sea-level, which is a function of mean sea level, tidal influences and meteorological forcing of the mean sea-level. All three components of observed sea-level are subject to change. The three chief factors contributing to changes in
1.Introduction Comprehensively, we are probably aware that Mass Tourism has the accompanying attributes: (a) involvement of a huge number of people in tourism, (b) holidays are being standardized, rigidly packaged and inflexible (Karamustafa 2012), (c) it is being mass produced and mass marketed and (d) consumed by tourists that are unconcerned about the local culture or practices. This goes to say that Mass Tourism requires vast improvement in tourism and the need of the involvement of international
The rising floodwaters forced thousands of people onto their rooftops without access to potable water. The breeched levee that resulted in the destruction of the Lower Ninth Ward raised suspicions of foul play with many residents. This case study focuses on the deep distrust for the government in the Lower Ninth Ward following Hurricane Katrina. Physical Setting The Lower Ninth Ward is a neighborhood of the city of New Orleans, Louisiana. Like many areas in New Orleans, the neighborhood