Impact of land use and land cover change on land surface temperature over Lake Tana Basin

被引:0
|
作者
Arsiso, Bisrat Kifle [1 ,2 ]
Tsidu, Gizaw Mengistu [2 ]
Abegaz, Nuredin Teshome [2 ,3 ]
机构
[1] Ethiopian Civil Serv Univ, Dept Environm & Climate Change, Addis Ababa, Ethiopia
[2] Botswana Int Univ Technol & Sci, Dept Earth & Environm Sci, Priv Bag 16, Palapye, Botswana
[3] Ethiopian Space Sci & Technol Inst, Addis Ababa, Ethiopia
基金
新加坡国家研究基金会;
关键词
Remote sensing; Land surface temperature; Observed minus reanalysis (OMR); Land use land cover (LULC); MODIS remote sensing image; USE/LAND-COVER; CLIMATE-CHANGE; VEGETATION; URBANIZATION; NDVI; VALIDATION; PLATEAU; TRENDS; REGION; RANGE;
D O I
10.1016/j.jafrearsci.2023.105047
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Isolation of climate and Land Use and Land Cover (LULC) changes and their compounded effect is complicated since the two influence each other through forcing-feedback cycles. This study investigates the changes in LULC and its contribution to the change in surface and air temperature in the Lake Tana Basin using data obtained from MODIS remote sensing satellites, ground observation and reanalysis model. Observation minus reanalysis (OMR) method and various analysis tools are used to estimate the impact of LULC changes on temperature. The analysis of LULC change indicates that an increase of Savanna and other type of forest cover by about 519 km2 from year 2001 to year 2020. Wetland increased by about 83.7 km2 during the said period. During the period 2001-2020, about 56.5% baren-land areas are being converted into wetland. The conversion of water bodies and baren land to wetland is likely due to the increase of water hyacinth on both the water body and nearby baren-land whereas the increase in Savanna is linked to an on-going eucalyptus tree plantation. The negative correlation between LST and NDVI (reaching a value of -0.60) is noticed over the Basin throughout the year on inter-annual time scale. An increase in vegetation cover such as Savanna and broad leaf forest coincides with the decreasing LST with an average rate of 0.08%/decade. Also, a reduction in temperature, derived from OMR, at an average cooling rate of about 0.87%/decade is observed in the study period. However, an increase in the LST change rate over built-up and grassland is about 0.03%/decade. Therefore, we conclude that the consistent associations of the increase in areal coverage of the some LULC types with lowest LSTs, 2m-temperature and temperature trend derived from NDVI-LST and LULC-LST associations as well as OMR temperature and LST are unambiguous signatures of the effect of LULC change on temperature over Lake Tana Basin, distinct from that arising due to climate change.
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页数:16
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