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The relationship between land cover and the urban heat island in northeastern Puerto Rico

机译:波多黎各东北部土地覆盖与城市热岛的关系

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Throughout the tropics, population movements, urban growth, and industrialization are causing conditions that result in elevated temperatures within urban areas when compared with that in surrounding rural areas, a phenomenon known as the urban heat island (UHI). One such example is the city of San Juan, Puerto Rico. Our objective in this study was to quantify the UHI created by the San Juan Metropolitan Area over space and time using temperature data collected by mobile- and fixed-station measurements. We also used the fixed-station measurements to examine the relationship between average temperature at a given location and the density of remotely sensed vegetation located upwind. We then regressed temperatures against regional upwind land cover to predict future temperature with projected urbanization. Our data from the fixed stations show that the average nighttime UHI calculated between the urban reference and rural stations (ΔT_(CBD-rural)) was 2.15 °C during the usually wet season and 1.78 °C during the usually dry season. The maximum UHI value for San Juan was calculated as 4.7 °C between the urban and forest sites and 3.9 °C between the urban and an open, rural site. Comparisons of diurnal temperature trends at urban, grassland, and forested sites indicate that canopy cover reduced daytime warming. Temperature was predicted best (r~2 = 0.94) by vegetation in upwind easterly directions, especially that within 180 m of the sensor. Results from the mobile measurements show that the UHI has reached the base of the Luquillo Mountains. Predictions of future development and temperatures suggest that if the present pattern of development continues, over 140 km~2 of land that showed no signs of UHI in 2000 will have an average annual UHI between + 0.4 and + 1.55 °C by 2050. Furthermore, more than 130 km~2 of land area with a current UHI between + 0.4 and + 1.4 °C in 2000 will have an average UHI greater than + 1.55 °C by 2050.
机译:在整个热带地区,与周围的农村地区相比,造成人口流动,城市增长和工业化的状况导致城市地区的温度升高,这种现象被称为城市热岛(UHI)。这样的例子之一就是波多黎各的圣胡安市。我们在这项研究中的目的是使用移动站和固定站测量收集的温度数据来量化圣胡安都会区在空间和时间上创建的UHI。我们还使用固定站测量来检查给定位置的平均温度与位于上风的遥感植被密度之间的关系。然后,我们将温度与区域上风向的土地覆盖量进行了回归,以预测未来城市化预计的温度。我们从固定站获得的数据表明,在通常的雨季中,城市参考站和农村站之间的平均夜间UHI(ΔT_(CBD-农村))为2.15°C,而在通常的旱季为1.78°C。在城市和森林站点之间,圣胡安的最大UHI值经计算为4.7°C,在城市和开放的农村站点之间为3.9°C。在城市,草地和森林地区的昼夜温度趋势比较表明,树冠覆盖减少了白天的变暖。植被在上风向东的方向上最好地预测温度(r〜2 = 0.94),尤其是在传感器180 m以内的温度。流动测量的结果表明,UHI已到达卢基洛山脉的底部。对未来发展和气温的预测表明,如果继续以目前的发展模式发展,到2050年,超过140 km〜2的土地没有UHI迹象,那么到2050年,年平均UHI将在+ 0.4至+ 1.55°C之间。到2000年,当前UHI在+ 0.4至+ 1.4°C之间的土地面积超过130 km〜2,到2050年平均UHI将超过+ 1.55°C。

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