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The geographic location of Hangzhou.

The geographic location of Hangzhou.

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Article
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There are many indications that Urban Heat Island (UHI) is a significant contributor to the increased emission of greenhouse gases due to the increase in energy consumption for cooling during summer. Hangzhou is currently the second hottest city in China, and this paper investigates how the West Lake and the Xixi Wetland areas in the city act as pa...

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Context 1
... the capital of Zhejiang Province, lies 180 km south- west of Shanghai (Figure 1). It has a total area of 16 596 km 2 and forms part of Yangtze River Delta region, one of the most dy- namically developed, densely populated and concentrated urba- nized areas situated on the east coast of China [5]. ...
Context 2
... the cooler air from the Qiantang River also cannot be blown to the urban area either, because the buildings on the northeast side of the river are highest and block the cool wind into the urban area. Figure 10a and b shows the case where the wind direction changes to southwest and the comparison with the prime case. It is clear that the shape of UHI changes. ...
Context 3
... the gap between buildings also relates to another variable, the SVF, which is an important indicator of the magni- tude of urbanization of a city. Figure 11 shows that an area with low SVF can be normally recognized as urban area where UHI effect is significant. Nevertheless, the impact of SVF on UHI is quite complicated. ...
Context 4
... reference weather data file of Hangzhou is downloaded from Energy Plus webpage. Figure 12 shows the appearance of the urban building model designed in Ecotect. Table 2 displays the material descriptions of the simulated urban building and Table 3 lists the average monthly temperature value in reference and the modified weather data files. ...
Context 5
... this case study, cooling demand of urban building in summer is simulated to evaluate the impact of the temperature increase of 0.58C on the cooling energy consumption of the designed urban building, as Figure 13 illustrates. If the ambient temperature increases 0.58C, the total cooling demand of the urban building is 41 KWh=m 2 , which is 10.8% higher than the value that is based on the reference weather data file. ...

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Citations

... For example, Ryu and Baik (2013) demonstrated that urban breeze could transport high-reactivity precursors and O 3 -rich air to Seoul, leading to about 15-ppb increase in O 3 concentrations. Some research on the impacts of land cover and their distributions to UHI in HMA has been carried out (Shen et al., 2013;Chen et al., 2014;Li et al., 2015). None of the previous work, however, focused on the role of UHIC on O 3 in HMA. ...
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... Previous studies have focused on the impact of urban geometry on outdoor thermal comfort, such as the aspect ratio (Ali-Toudert & Mayer, 2006;Emmanuel et al., 2007), SVF (Ali-Toudert & Mayer, 2006;Andrade & Alcoforado, 2008;Kakon et al., 2009;Krüger et al., 2011;Shen et al., 2013), street orientation (Ali-Toudert & Mayer, 2007;Emmanuel et al., 2007;Fahmy & Sharples, 2009;Hedquist & Brazel, 2014;Ketterer & Matzarakis, 2014), building density (Hedquist & Brazel, 2014;Perini & Magliocco, 2014;Shen et al., 2013), and building forms (Fig. 9 and Table B1). The interaction between aspect ratio, orientation, and vegetation inside a street canyon is required to determine the level of thermal stress at the pedestrian level (Yahia & Johansson, 2013). ...
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... [24,45]. UHI mitigation strategies have also been studied, including park induced cool islands [18,37]; passive cooling systems [52,53]; urban canyon orientation and aspect ratio [33]; and material properties [63]. It has been validated against field measurements [59], showing that it can reasonably simulate air T, as well as building surface radiative T and energy balance components [68]. ...
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An obstacle to the modeling of strategies to mitigate extreme urban temperatures is frequently the lack of on-site meteorological data. The current study thus reports on a method that used the Weather Research and Forecasting (WRF) model to generate inputs for the ENVI-met model to produce building-scale canyon temperatures within a 300 m square near downtown San Jose. A land use distribution was generated for WRF by a WUDAPT classification, and the days of inter-est were the then hottest day in California history and a typical summer day. The source of met-eorological data for ENVI-met, run with a 1.5 m cubic grid, was either an urbanized version of WRF; its default version; or observations at the closest NWS site. All WRF simulations were run on a 1 km grid, and output at its grid closest to the study area provided ENVI-met with lateral boundary conditions. The mitigation strategy was comprised of three parts, which either in-creased vegetation, rooftop albedo, or architectural shade elements. Results showed all strategies with only negligible impacts on ENVI-met nighttime 1 m level temperatures. Increased vegeta-tion, however, was the most effective daytime strategy on both days, as it effected the largest area. The maximum vegetative cooling on the extreme and average days was −3.5 and −3.3 °C, respectively. While increased rooftop albedos produced near negligible impacts, increased architectural shading produced corresponding values of −1.6 and −1.7 °C, respectively.