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The image depicts a comparative side-by-side diagram of water cycle processes in forested versus urban areas. On the forested side: permeable topsoil above less permeable subsoil on rock allows for processes such as infiltration, baseflow, evaporation, transpiration, and precipitation, resulting in significant infiltration contributing to water table replenishment and runoff formation. In contrast, the urban side features reduced infiltration, reduced baseflow, reduced evaporation, reduced transpiration, increased erosion, and increased polluted runoff due to impermeable surfaces, illustrating the impacts of urbanization on water movement and distribution.
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The diagram illustrates the water process in forested areas compared with urban areas.
Overall, there are six different stages, from precipitation of water to runoff. Also, the amount of rain falling is same in two regions; however, there is significantly less water re-entering the sky and permeating through the ground in cities than in forests.
Above the ground, more water gets to the sky in forested areas compared to the urban territory; however, the amount of water falling from the sky is equal on two sides. ‘Runoff’ process has more water in urban areas, but evaropation happens similar in both areas.
There are three stages, which happen under the ground. In forests. significant amount of water soaks through the topsoil and subsoil, whereas a negligible amount filtrates through these soil layers, which leads to a reduction in the baseflow in cities. The water table is noticeably higher beneath forested regions than it is beneath in urban regions
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