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Exploring the relationship between LST and land cover of Bengaluru by concentric ring approach

机译:通过同心环接近探索孟加拉堡LST和陆地覆盖关系的关系

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The present study aims at investigating the impact of land cover features in enhancing or mitigating Land Surface Temperature (LST) in a semi-arid tropical metropolitan city of Bengaluru, India. Spatial distribution of LST and land cover types of the area were examined in the circumferential direction, and the contribution of land cover classes on LST was studied over 28 years. Urban growth and LST were modelled using Landsat and MODIS data for the years 1989, 2001, 2005 and 2017 based on the concentric ring approach. The study provides an efficient methodology for modelling and parameterisation of LST and urban growth by fitting an inverse S-curve into urban density (UD) and mean LST data. In addition, multiple linear regression models which could effectively predict the LST distribution based on land cover types were developed for both day and night time. Based on the analysis of remotely sensed data for LST, it is observed that over the years, urban core area has increased circumferentially from 5 to 10 km, and the urban growth has spread towards outskirts beyond 15 km from the city centre. As urban expansion occurs, the area under the study experiences an expansive cooling effect during day time; at night, an expansive heating effect is experienced in accordance with the growth in UD in the suburban area and outskirts. The regression models that were developed have relatively high accuracy withR(2)value of more than 0.94 and could explain the relationship between LST and land cover types. The study also revealed that there exists a negative correlation between urban, vegetation, water body and LST during day time while a positive correlation is observed during night. Thus, this study could assist urban planners and policymakers in understanding the scientific basis for urban heating effect and predict LST for the future development for implementing green infrastructure. The proposed methodology could be applied to other urban areas for quantifying the distribution of LST and different land cover types and their interrelationships.
机译:本研究旨在调查土地覆盖特征在印度半干旱热带大都市城市孟加拉堡市的增强或减轻土地表面温度(LST)。在圆周方向上检查了地区LST和陆地覆盖类型的空间分布,并在28年内研究了LST上的土地覆盖类别的贡献。基于同心环方法,在1989年,2001年,2005年和2017年,使用Landsat和Modis数据进行了建模的城市成长和LST。该研究通过将逆S曲线拟合到城市密度(UD)和平均LST数据来提供LST和城市增长的建模和参数化的有效方法。此外,可以有效地预测基于陆地覆盖类型基于陆地覆盖类型的LST分布的多元线性回归模型。根据对LST的远程感测数据的分析,观察到多年来,城市核心区域从5到10公里处的周向增加,城市增长距离市中心超过15公里的郊区。由于城市扩张发生,该研究区域的区域经历了白天的膨胀冷却效果;在夜间,根据郊区和郊区的UD的增长,经历了膨胀的加热效果。开发的回归模型具有相对高的精度(2)值超过0.94,可以解释LST和陆地覆盖类型之间的关系。该研究还透露,在白天的时间内城市,植被,水体和LST之间存在负相关性,同时在夜间观察到正相关性。因此,本研究可以帮助城市规划者和政策制定者了解城市供热效果的科学依据,并预测LST为实现绿色基础设施的未来发展。拟议的方法可以应用于其他城市地区,用于量化LST和不同土地覆盖类型及其相互关系的分布。

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