dc.description.abstract |
Urban heat island is a phenomena occurring due to differences in warming between urban and
rural areas. The issue was known since 1818 after the release of the research work of Luke Howard
known as the climate of London. Whereas in Ethiopia in general, and in the study area in
particular, it is not common to see researches focusing on heat island. There are researches on
urban heat island causative factors but there lack studying the present and future impacts on urban
utilities. Therefore, this study was focusing on analyzing spatial and temporal variations and
future trends of heat island, prominent driver which lead to this variation, the implications of
climate change on surface urban heat intensity, and impacts of the excessive heat intensity. Data
obtained from United States Geological Survey/USGS/, and government offices include satellite
images from 1990-2020, temperature and rainfall data from 1990-2020, water consumption data
and electric consumption data from 2008-2020. These were analyzed using geospatial techniques
Mann-Kendall and homogeneity test models. Maximum likelihood algorithm, Oke’s urban heat
island (UHI) algorithm, multiple linear regression, the Likert scale, path model and Auto
Regressive Integrated Moving Average (ARIMA) Model. The findings of the study ascertained
urban heat intensity in the study area in 1990 was 3°C and in 2020 it was 4.6°C, and in 2024 it is
3.1°C and in 2040 it will be 3.04°C which implies future intensification of heat intensity but with
a lesser extent from 1990-2020. The southern, southwestern and southeastern parts of the City and
its outskirts were with highest Land Surface Temperature record in 2013 which was estimated to
be 42°C and the northern, northcentral, northwestern and northeastern parts of the City and its
outskirts were with lowest land surface temperature record in 1990 which was estimated to be
32°C. In addition to this, population density was identified as the prominent cause for urban
heating in the study area. Moreover, climate change which causes urban warming was ascertained
to be the worries of the area. The p-value and the Sens slope indicated that the air temperature
was showing an upward trend. Furthermore, water consumption was 2.378 m
3
/person/annum/1°C
while electricity consumption was 1.616 kWh/person/annum/1°C and future water and electricity
consumption will be 4 m
3
/person/annum/1°C
and 2.9 kWh /person/annum/1°C. From this it can be
concluded that urban heating has an impact on urbanites. Therefore, it is recommended that the
city administration should work on containing the incoming population from nearby satellite towns
and nearby rural areas through the development of infrastructures and introducing villagization
programs. It should also work on urban greeneries which have less LST records. Furthermore,
since it was impossible to deter the construction industries, emphasis should be given to
controlling the design, type of construction materials, and the finishing materials used. The
construction materials should be high albedo to reduce the heating effects of buildings. The city
administration should design a workable policy that can enable thermal management. |
en_US |