Assessment of land use/land cover changes and its effect on land surface temperature using remote sensing techniques in Southern Punjab, Pakistan

被引:28
|
作者
Hussain, Sajjad [1 ]
Mubeen, Muhammad [1 ]
Ahmad, Ashfaq [2 ]
Majeed, Hamid [1 ]
Qaisrani, Saeed Ahmad [1 ]
Hammad, Hafiz Mohkum [3 ]
Amjad, Muhammad [1 ]
Ahmad, Iftikhar [1 ]
Fahad, Shah [4 ,5 ]
Ahmad, Naveed [6 ]
Nasim, Wajid [7 ]
机构
[1] COMSATS Univ Islamabad, Dept Environm Sci, Vehari Campus, Islamabad 61100, Pakistan
[2] Asian Disaster Preparedness Ctr ADPC, Bangkok, Thailand
[3] Muhammad Nawaz Sharif Univ Agr, Dept Agron, Multan 66000, Pakistan
[4] Hainan Univ, Coll Trop Crops, Hainan Key Lab Sustainable Utilizat Trop Bioresou, Haikou 570228, Hainan, Peoples R China
[5] Univ Haripur, Dept Agron, Khyber Pakhtunkhwa, Pakistan
[6] Univ Educ, Dept Zool, Vehari Campus, Lahore, Pakistan
[7] Islamia Univ Bahawalpur IUB, Fac Agr & Environm, Dept Agron, Bahawalpur, Punjab, Pakistan
关键词
Normalized difference vegetation index; Normalized difference water index; Normalized difference built-up index; Land surface temperature; SIMCLIM CLIMATE MODEL; NDVI; CLASSIFICATION; IMPACTS; RUNOFF; CITY;
D O I
10.1007/s11356-022-21650-8
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Land surface temperature (LST) is defined as a phenomenon which shows that microclimate of an urban system gets heated much faster than its surrounding rural climates. The expansion of buildings has a noteworthy influence on land use/land cover (LULC) due to conversion of vegetation land into commercial and residential areas and their associated infrastructure by which LST is accelerated. The objective of the research was to study the impact of changes in LULC on LST of Southern Punjab (Pakistan) through remote sensing (RS) data. Landsat images of 30-year duration (1987, 1997, 2007 and 2017) were employed for identifying vegetation indices and LST in the study region. These images also helped to work out normalized difference water index (NDWI) and normalized difference built-up index (NDBI) maps. There was an increase from 29620 (3.63 %) to 88038 ha (10.8 %) in built-up area over the 30 years. LST values were found in the range 12-42 degrees C, 11-44 degrees C, 11-45 degrees C and 11-47 degrees C in the years 1987, 1997, 2007 and 2017, respectively. Regression coefficients (R-2) 0.81, 0.78, 0.84 and 0.76 were observed between NDVI and LST in the corresponding years respectively. Our study showed that NDVI and NDWI were negatively correlated with less LST; however, NDBI showed positive correlation with high LST. Our study gives critical information of LULC and LST and will be a helpful tool for policy makers for developing effective policies in managing land resources.
引用
收藏
页码:99202 / 99218
页数:17
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