Prediction of future urban surface temperatures using medium resolution satellite data in Harare metropolitan city, Zimbabwe

被引:70
|
作者
Mushore, Terence Darlington [1 ,3 ]
Odindi, John [1 ]
Dube, Timothy [2 ]
Mutanga, Onisimo [1 ]
机构
[1] Univ KwaZulu Natal, Sch Agr Earth & Environm Sci, Discipline Geog, P Bag X01, ZA-3209 Pietermaritzburg, South Africa
[2] Univ Limpopo, Dept Geog & Environm Studies, Private Bag X1106, ZA-0727 Sovenga, South Africa
[3] Univ Zimbabwe, Phys Dept, POB MP197, Harare, Zimbabwe
关键词
Land surface temperature; Cellular automata markov; Markov chain analysis; Urban growth; Vegetation indices; Harare; USE/LAND COVER CHANGE; WATER INDEX NDWI; HEAT-ISLAND; LAND-COVER; CLIMATE-CHANGE; BUILT-UP; IMPERVIOUS SURFACE; VEGETATION INDEX; MULTISENSOR DATA; CHANGE IMPACT;
D O I
10.1016/j.buildenv.2017.06.033
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The objective of the study was to determine the impact of urban growth on future micro-climate of Harare by predicting future distribution of land use and land cover, as well as land surface temperature using Cellular Automata Markov Chain analysis. Landsat series data was used to map Land Use and Land Cover (LULC) and land surface temperature distribution during the month of October for the year 1984, 1993, 2001 and 2015. The Cellular Automata Markov Chain analysis was used to determine long term landscape transformation at 10-year time steps from 2015 to 2045. We further tested the potential of a variety of vegetation and non-vegetation indices to predict land surface temperature. Results show that the Urban Index (UI), non-vegetation index was the best predictor of surface temperature, since it had the highest correlation with retrieved surface temperature (r = 0.9831). When tested against temperature derived from thermal band in October 2015, the mean absolute percentage error of the UI derived temperature was 5.27%. Based on changes which occurred between 1984 and 2015, the Cellular Automata Markov Chain analysis predicted that high density built-up areas will increase monotonically from 470.02 in 2015 to 490.36 km(2) in 2045. Green spaces were predicted as decreasing from 57.42 to 27.85 km(2), while croplands also decrease from 30.27 to 16.93 km(2) between 2015 and 2040. Using UI as predictor of land surface temperature, we predicted that the 18-28 degrees C class will decrease in coverage between 2015 and 2040, while the 36-45 degrees C category will increase in proportion covered from 42.5 to 58% of city. We concluded that continued urban growth will increase warming and result in high future temperatures unless mitigation efforts are strengthened. The findings of this study are important in informing future development of cities to consider growth implications on future temperatures and thermal comfort of urban residents. (C) 2017 Elsevier Ltd. All rights reserved.
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页码:397 / 410
页数:14
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