Geological aspects of object localization for the cultural heritages in the territory of Kyiv are studied. The monitoring of landslides processes for the Kyiv and landslide risk assessment for the cultural heritage with using remote sensing data is provided. In this paper on example of certain areas of the Kyiv metropolitan area the application of methodological issues are considered in the analysis of cosmic material changes in the landscape and the functional structure of Kyiv are associated with intense development in the valley of the Dnieper river and within the historical part

The surface temperature distribution analysis of the condition and characteristics within one of the industrial centers of the south of Ukraine, Mykolaiv, from 1985 to 2018 was carried out on the basis of Landsat thermal infrared data processing. Temporal development of surface temperature distribution was investigated both for the entire territory of the city and for individual profiles crossing the diverse landscape and functional city areas. Significant surface temperature distribution divergences during temporal variations in different, but steady landscapes and functional conditions have been stated. Abnormally high temperatures are found within industrial zones, reaching 40–43оC. The water temperatures of the Southern Bug, Ingula and Lake Liski are the lowest and are determined by the amount of water mass. The highest temperature oscillation (up to 15oC) during the research period, was recorded on the artificially aggradated sands within floodplain of the Southern Bug, after the residential building “Namyv” was built and within the “Zhovtneve” reservoir, after its draining. The main types of residential development of the city — a medium, low-rise buildings and private cottages surrounded by trees and lawns, forming a stable temperature background. Limited distribution of impermeable surfaces, significant planting, intensive watering resulted in the formation of a negative thermal anomaly within the city, a peculiar cool oasis against a hot background of steppe agro-landscapes.

Within the urban heat island that exists over Kyiv, the temperature distribution strongly depends on the landscape-functional structure of the city, namely on the degree of heating and radiation of the land cover, their relationships, proportion and changes over time. Using the thermal ranges of the satellite data of the Landsat mission, we have considered why, and where exactly, the land surface temperature changes (LST) occur from 1986 to 2018. The spatio-temporal analysis of LST is performed using profiles that cross industrial and post-industrial territories of Kyiv. It’s been shown that such territories have higher level of land surface temperature according to artificial covering surface density increasing. The Shulyavsk and Svyatoshinsk industrial zones that historically exists in central and west part of the city have been taken, as example. The post-industrial transformation of such, territories today unfortunately, does not meet the requirements of the revitalization in spite of their transformation and a decreasing in the production load. The most intense temperature increases are recorded on the outskirts of the city through new housing construction and destruction of natural landscapes, which significantly expanded the boundaries of the urban thermal island. Analysis of the surface temperatures by seasons showed that the thermal anomalies exist over industrial areas, but the LST oscillation amplitude reaches 15оС in summer between production and forest-park areas.