英译汉 高手帮忙 5
Chia(1970)alsoconductedasimilarstudyasNiewoltandconsideredtheeffectofvariationsinclou...
Chia (1970) also conducted a similar study as Niewolt and considered the effect of variations in cloud patterns on the microclimate. Chia found out that a combination of low solar radiation receipts and low wind speed together with a low cloud ceiling reduced the city rural temperature and relative humidity differences.
Nichol (1994) presented UHI in Singapore through the remote sensing technology. Roughly over 4 1C difference was observed from the satellite image of Singapore. The observation of UHI in Singapore provides evidence that the local buildings do have the great impact on the local climate. The most recent study done in Singapore is the exploration conducted by Roth (2002), which explores the UHI dynamics in Singapore. Preliminary results based on traverse observations conducted in spring and summer of year 2001 have shown that night time heat island magnitudes of up to 4 1C with lowest temperatures observed in densely vegetated areas.
Wong and Chen (2003) investigated the severity and impact of UHI on the environmental conditions and identified the possible causes by using thermal satellite image and mobile survey. He also explored the various potential measures that could be implemented to minimize the impact.
Satellite images and geographical information system (GIS) are also used for UHI study besides using field measurement method. One of the examples is UHI study in Rhode Island (Brown University, 2004). The study focused on Providence city. By analyzing thermal data obtained with ETM+ onboard Landsat 7 on July 2001 and the land use/land cover classification from Rhode island GIS, the spatial distribution of land uses, vegetative cover, and the daytime land surface temperature in Providence was identified. The densely populated residential districts, commercial and industrial areas represent urban heat islands, with the surface temperature as high as 43 1C in summer days. On an average, the summertime land surface temperature is
20 1C higher than in the surrounding suburban areas and 13 1C higher than in treed neighborhoods. The highest level of mean land surface temperature of 32.5 1C is observed in mixed industrial areas, followed by industrial area and commercial with the range of 31–32 1C. The maximum mean land surface temperature in high-density residential areas amounts to 28 1C. 展开
Nichol (1994) presented UHI in Singapore through the remote sensing technology. Roughly over 4 1C difference was observed from the satellite image of Singapore. The observation of UHI in Singapore provides evidence that the local buildings do have the great impact on the local climate. The most recent study done in Singapore is the exploration conducted by Roth (2002), which explores the UHI dynamics in Singapore. Preliminary results based on traverse observations conducted in spring and summer of year 2001 have shown that night time heat island magnitudes of up to 4 1C with lowest temperatures observed in densely vegetated areas.
Wong and Chen (2003) investigated the severity and impact of UHI on the environmental conditions and identified the possible causes by using thermal satellite image and mobile survey. He also explored the various potential measures that could be implemented to minimize the impact.
Satellite images and geographical information system (GIS) are also used for UHI study besides using field measurement method. One of the examples is UHI study in Rhode Island (Brown University, 2004). The study focused on Providence city. By analyzing thermal data obtained with ETM+ onboard Landsat 7 on July 2001 and the land use/land cover classification from Rhode island GIS, the spatial distribution of land uses, vegetative cover, and the daytime land surface temperature in Providence was identified. The densely populated residential districts, commercial and industrial areas represent urban heat islands, with the surface temperature as high as 43 1C in summer days. On an average, the summertime land surface temperature is
20 1C higher than in the surrounding suburban areas and 13 1C higher than in treed neighborhoods. The highest level of mean land surface temperature of 32.5 1C is observed in mixed industrial areas, followed by industrial area and commercial with the range of 31–32 1C. The maximum mean land surface temperature in high-density residential areas amounts to 28 1C. 展开
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嘉（ 1970 ）还进行了一项类似的研究，并认为作为Niewolt的影响云层的变化模式的小气候。吴家发现，低相结合的太阳辐射的收益和低风速一起低云上限降低了城市农村温度和相对湿度的差异。
尼科尔（ 1994 ）提出了城市热岛在新加坡通过遥感技术。大约超过4 1C号不同的是观察到的卫星图像的新加坡。城市热岛的观察在新加坡提供的证据表明，当地的建筑确实有很大的影响当地的气候。最近的研究工作是在新加坡进行的勘探罗斯（ 2002年） ，其中探讨了城市热岛动力在新加坡举行。初步结果的意见的基础上进行遍历春季和夏季的2001年已经表明，夜间热岛强度高达4 1C号观察与最低气温在草木茂密的地区。
黄，陈（ 2003 ）调查的严重性和影响的城市热岛的环境条件，并确定了可能的原因使用热卫星图像和移动调查。他还探讨了各种可能采取的措施可以实施，以尽量减少影响。
卫星图像和地理信息系统（ GIS ）也用于城市热岛研究除了利用领域的测量方法。其中一个例子是城市热岛研究，罗得岛（布朗大学， 2004年） 。研究的重心集中在普罗维登斯市。通过分析获得的数据与热血症+板载Landsat 7号关于2001年7月和土地利用/土地覆盖分类从罗得岛地理信息系统，空间分布的土地利用，植被覆盖，并且白天地表温度在普罗维登斯确定。人口密集的住宅区，商业和工业领域的代表城市热岛，在地表温度高达43 1C号夏季天。平均，夏季地表温度是
20 1C号高于周边郊区和13 1C号高于绿树社区。最高级别的平均地表温度32.5 1C号是观察混合工业区，其次是工业和商业领域的一系列31-32 1C号。最高平均地表温度在高密度住宅区达28 1C号。
尼科尔（ 1994 ）提出了城市热岛在新加坡通过遥感技术。大约超过4 1C号不同的是观察到的卫星图像的新加坡。城市热岛的观察在新加坡提供的证据表明，当地的建筑确实有很大的影响当地的气候。最近的研究工作是在新加坡进行的勘探罗斯（ 2002年） ，其中探讨了城市热岛动力在新加坡举行。初步结果的意见的基础上进行遍历春季和夏季的2001年已经表明，夜间热岛强度高达4 1C号观察与最低气温在草木茂密的地区。
黄，陈（ 2003 ）调查的严重性和影响的城市热岛的环境条件，并确定了可能的原因使用热卫星图像和移动调查。他还探讨了各种可能采取的措施可以实施，以尽量减少影响。
卫星图像和地理信息系统（ GIS ）也用于城市热岛研究除了利用领域的测量方法。其中一个例子是城市热岛研究，罗得岛（布朗大学， 2004年） 。研究的重心集中在普罗维登斯市。通过分析获得的数据与热血症+板载Landsat 7号关于2001年7月和土地利用/土地覆盖分类从罗得岛地理信息系统，空间分布的土地利用，植被覆盖，并且白天地表温度在普罗维登斯确定。人口密集的住宅区，商业和工业领域的代表城市热岛，在地表温度高达43 1C号夏季天。平均，夏季地表温度是
20 1C号高于周边郊区和13 1C号高于绿树社区。最高级别的平均地表温度32.5 1C号是观察混合工业区，其次是工业和商业领域的一系列31-32 1C号。最高平均地表温度在高密度住宅区达28 1C号。
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