土壤覆盖对三宝垄城市热岛现象的影响

Rizal Mubarok, Bintang Septiarani, Reny Yesiana, Pangi Pangi
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引用次数: 1

摘要

三宝垄是中爪哇省的首府,是一个位于爪哇岛北部的大都市。1990年,三宝垄市的人口为1,249,230人,到2020年增加到1,653,524人,增幅为32.4%。至于住宅面积,1990年为12,355公顷,2020年为17,070公顷,占38.2%。数据显示,三宝垄市的人口增长与土地覆盖面积,特别是住宅面积成正比。本研究旨在探讨三宝垄市土地覆盖对城市热岛现象的影响。本研究采用的研究方法是土地覆盖分析(监督分类)、归一化植被指数(NDVI)、地表温度(LST)、覆盖和描述性分析。该方法用于获取土地覆被、温度以及土地覆被对城市热岛的影响等数据。根据分析结果可知,三宝垄市从植被用地到居住用地发生了明显的土地变化。1989年植被面积为27,055 Ha,到2020年为16,316.4 Ha。居住用地和建设用地面积由1989年的6349.2 Ha增加到2020年的18015.4 Ha。三宝垄市的温度分类以III类为主,为260 -300摄氏度。I类温度面积减小,V类温度面积增大。在建成区和居民点,ⅲ类温度在2020年的用地面积值为7.9 Ha,而在1989年、1999年和2009年的用地面积值均小于2 Ha。根据已经进行的研究,可以得出结论,三宝垄市土地覆盖的变化,特别是从植被到住区的变化,也会引起温度的变化,从而导致三宝垄市的热岛现象。
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PENGARUH TUTUPAN LAHAN TERHADAP FENOMENA URBAN HEAT ISLAND DI KOTA SEMARANG
Semarang is the capital city of Central Java Province which is a metropolitan city that is located in the north of Java Island. Semarang City had a population of 1,249,230 people in 1990 and increased to 1,653,524 people in 2020 or 32.4%. As for residential area in 1990 it was 12,355 Ha and in 2020 it was 17,070 Ha or 38.2%. The data shows that population growth in Semarang City is directly proportional to the area of land cover, especially residential area. This study aims to determine the effect of land cover on the urban heat island (UHI) phenomenon in Semarang City. The research method used in this research is land cover analysis (supervised classification), Normalized Difference Vegetation Index (NDVI), Land Surface Temperature (LST), overlay, and descriptive analysis. This method is used to obtain data on land cover, temperature, and the effect of land cover on the urban heat island. Based on the results of the analysis, it is known that the city of Semarang has a significant land change from vegetation land to residential land. Vegetation land in 1989 was 27,055 Ha, changed to 16,316.4 Ha in 2020. The area of residential land and built-up land changed from 6,349.2 Ha in 1989 to 18,015.4 Ha in 2020. The temperature classification in Semarang City is dominated by by class III, which is 260 -300 Celsius. The temperature area in class I decreases and in class V increases. In built-up land and settlements, class III temperature has a land area value of 7.9 Ha in 2020, while in 1989, 1999, and 2009 it has an area of less than 2 Ha. Based on the studies that have been carried out, it can be concluded that changes in land cover in Semarang City, especially from vegetation to settlements, also cause changes in temperature which cause the UHI phenomenon in Semarang City. 
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