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thought of as hot spots . The relationship of LST between p.c impervious surface area (%ISA) and elevation has been investigated in the current study. Parameter like %ISA which represents the extent of urbanization has been used for the UHI analysis and its relationship with LST has been discovered to be season impartial. Positive relationship has been discovered between LST and %ISA with a consistent rising development. In the imply LST and %ISA relationship, it has been observed that the coefficient of correlation of winter season is 0.eighty one which is slightly higher compared to monsoon and summer time seasons. Normally the temperature falls with increase in altitude. But on this examine, as the elevation increases, rising development of LST could be observed. Negative relationship between LST and Elevation scatterplots has been observed in excessive altitude areas throughout monsoon season in comparison with summer season and winter seasons. Besides other factors elevation additionally performs a significant position in LST dynamics and spatial distribution of LST. Seasonal vegetation phenology can significantly alter surface albedo which in flip impacts the global vitality stability and the albedo warming/cooling feedbacks that influence climate change. To monitor and quantify the surface dynamics of heterogeneous landscapes, excessive temporal and spatial decision synthetic time collection of albedo and the improved vegetation index had been generated from the five hundred m Moderate Resolution Imaging Spectroradiometer operational Collection V006 every day BRDF/NBAR/albedo merchandise and 30 m Landsat 5 albedo and near-nadir reflectance data through using the Spatial and Temporal Adaptive Reflectance Fusion Model . The traditional Landsat Albedo (Shuai et al., 2011) makes use of the MODIS BRDF/Albedo products by assigning appropriate BRDFs from coincident MODIS products to every Landsat picture to generate a 30 m

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