Analysis of Land Cover Changes to Increase Land Surface Temperature in Surabaya using Landsat Satellite

Shanas Septy Prayuda, MarithaNilam Kusuma
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Abstract

Surabaya has experienced very significant development in the last few decades. Changes in land use will cause the Urban Heat Island phenomenon. This study aims to determine how far the impact of land cover changes on the increase in surface temperature in the Surabaya. The use of Landsat satellite imagery is considered very effective in describing land cover and surface temperature because it has good spatial resolution and long data availability. During 1991 – 2020 there was a significant decrease in the amount of vegetation by 24.3%, decrease in the number of water bodies by 4.9%, and increase in the number of buildings by 29.2%. The average increase in Land Surface Temperatures was 1.40°C between decades 2 and 1, and an increase of 2.19°C between decades 3 and 2. The development of Surabaya began in the city center and then developed mainly in the west and east. The urban development model is consistent with the pattern of land surface temperature changes. Each type of land cover has special characteristics on the value of NDVI, NDBI, and surface temperature. Changes in cover from water bodies to buildings have the highest contribution to increasing the and surface temperature. There was a significant increase in hotspots in decade 3 in Surabaya which indicated an increasingly severe UHI phenomenon.
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利用大地遥感卫星分析土地覆盖变化对泗水地表温度升高的影响
在过去几十年中,泗水经历了巨大的发展。土地利用的变化将导致城市热岛现象。本研究旨在确定土地覆被变化对泗水地表温度上升的影响程度。由于 Landsat 卫星图像具有良好的空间分辨率和较长的数据可用性,因此在描述土地覆被和地表温度方面非常有效。1991-2020 年间,植被数量大幅减少了 24.3%,水体数量减少了 4.9%,建筑物数量增加了 29.2%。第二个十年与第一个十年之间,地表温度平均上升了 1.40°C,第三个十年与第二个十年之间,地表温度平均上升了 2.19°C。泗水的发展始于市中心,随后主要向西部和东部发展。城市发展模式与地表温度变化规律一致。每种类型的土地覆被对 NDVI 值、NDBI 值和地表温度都有特殊的影响。从水体到建筑物的覆盖变化对地表温度和地表温度的增加贡献最大。在第 3 个十年中,泗水的热点明显增加,这表明局地温差影响现象日益严重。
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