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Footprints of the Nature in Cities; Urban Heat Island Effects
                       and the Role of Afforestation Efforts in Reduction of These Effects

            Table 2: The Effects of Urban Heat Island on Water Resources


                            The demand for water increases along with the increasing temperatures
                             of the urban heat island. Especially during the summer months, when
              Increased Water
               Consumption    temperatures rise excessively, the use of cooling systems, landscape
                             irrigation, and personal water consumption increase. This situation in-
                            creases pressure on regional water resources (Oke, 1982) In arid regions,
                                 this effect can lead water resources to decline more rapidly.



                             The urban heat island can alter local climate characteristics, affecting
                              precipitation patterns. Rising temperatures accelerate evaporation,
                Rainfall and    leading to disruptions in the water cycle. It can also lead to more intense
               Water Cycle   rainfall in urban areas. Intense rainfall can lead to sudden flood events
                             and cause damage to urban infrastructure (Grimmond, 2007). This pro-
                              cess makes it more difficult to manage water resources effectively.




                            High temperatures in urban areas can cause surface waters to warm up.
                             Since warm water has a reduced capacity to hold oxygen, ecosystem
               The Negative
             Impacts on Water   disturbances can be observed in surface water sources such as rivers and
                             lakes. High temperatures also increase water pollution by negatively af-
                 Quality
                            fecting water quality (Kaushal et al., 2010). (24) Additionally, temperature
                                    increase can lead to algal blooms in water sources.


                             Rising temperatures, combined with the urban heat island effect, place
                Pressure on    additional strain on water distribution infrastructure in cities. Especially
               Infrastructure  old pipe systems may be damaged due to expansion and contraction,
                             leading to water leaks and losses (Rosenfeld et al., 1995). Additionally,
                             high temperatures can increase the rate of evaporation, causing water
                                          reserves to deplete more quickly.


               UHE raises temperatures within cities, accelerating evaporation, which can
            lead to the drying up of surface waters and a decline in lake and river levels.
            Increased temperatures also affect the natural water cycle, raising water
            temperature and reducing water quality. The increase in water temperature,
            especially in ponds and rivers within cities, reduces oxygen levels, making it
            more difficult for plant and animal species in aquatic ecosystems to survive.
            The  UHE  effect  increases  water  consumption  and  dependence  on  cooling
            systems like air conditioners in cities, thereby raising the demand for water
            resources. This can threaten urban water security, particularly during dry
            periods. For these reasons, managing the impact of UHE on water resources is
            crucial for a sustainable water policy and the long-term water security of cities.



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