key: cord-0052773-864evg7g authors: Sahani, Nemai; Goswami, Sudipto Kumar; Saha, Arghya title: The impact of COVID-19 induced lockdown on the changes of air quality and land surface temperature in Kolkata city, India date: 2020-11-13 journal: Spat DOI: 10.1007/s41324-020-00372-4 sha: 0a265ce1ecf2f35d7cfdea44a3b39e88dbf26c32 doc_id: 52773 cord_uid: 864evg7g The COVID-19 pandemic and related lockdown reduced the pollution level in the major megacities worldwide. The air pollution level of the city directly influences the air temperature and also land surface temperature (LST). In this paper, authors analyzed the impact of lockdown due to COVID-19 pandemic on the pollution level of the city and resulted LST. Single channel algorithm has been used to retrieve LST from Landsat Thematic Mapper satellite data. Pre-lockdown and post-lockdown satellite data has been used to show the changes in LST due to lockdown. The air quality index of pre-lockdown and post-lockdown period of the city estimated based on seven pollutants such as PM(2.5), PM(10), NO(2), NH(3), SO(2), CO and Ozone. The pollution level of the city and LST significantly decreased after lockdown is enforced. The pollution level of the major portion of the city before lockdown is moderately polluted (95–153 µm) and after lockdown the satisfactory level of pollution level observed (33–45 µm). The mean LST before lockdown is 28.76 °C (13 March, 2020) and it decreased down to 26.56 °C after lockdown (30 April, 2020). There is a sharp decrease of low value of LST observed (23.6–17.35 °C) in the city. The increase of pollution level in the city and pollution induced local climate change is became an important issue for the municipal authorities. At that time, individual cities and transnational municipal networks started to take actions for reducing emissions of greenhouse gases and other atmospheric pollutants [1] . The release of atmospheric pollution and rapid urbanization alter the heat balance of the earth surface and atmosphere. The increase of atmospheric pollution level in the city raised the temperature in both atmosphere and surface and this leads towards urban climate change. National governments and the emerging international regime for governing urban pollution and climate change showed little attention in these activities at that stage [2] . At first, municipal action on climate change was seen in a few pioneer cities, predominantly in North America and Europe, focusing on the challenge of climate change mitigation [3, 4] . Later the number of transnational municipal networks have grown and multiplied and more number of cities have become involved in addressing this issue. The earliest work on local climate policy in urban environment and governance was conducted in the mid-1990s [5, 6] and a large body of research work has been accumulated. Most of the research was focused on mitigation and individual case studies [7, 8] , although there has been the initiation of work on urban climate adaptation in the global south [9] . In climatological and environmental studies, LST is a key variable. The reason is LST control the physical, chemical and biological processes on Earth [10] . It is related to surface energy balance and the integrated thermal state of the atmosphere within the planetary boundary layer [11] . Traditionally, LST was obtained from standard surface-air temperature by using sheltered thermometer 1.5-3.5 m above a flat, grassy, well ventilated surface. Many studies use LST as fundamental data in the study of environment and resources. Globally Satellite based surface temperature (LST) also known as skin temperature [12] . Satellite based LST products provide an estimate of the kinetic temperature of the earth's surface skin [13] which is the aggregate surface medium viewed by the sensor to a depth of about 12 lm. Skin temperature is the thermal emission of the earth surface and average effective radiative temperatures of various canopy and soil surfaces [14] . LST is called a key parameter in land surface processes because it is an indicator of climate change, controls the upward terrestrial radiation, surface sensible and latent heat flux exchange with the atmosphere [15] . On the other hand, surface heat fluxes can induce local convection in the boundary layer and produce changes in air temperature, surface winds, cloudiness and precipitation [15] . The LSTs acquired by satellite borne sensors and used for heat balance, climate modeling and global change monitoring studies [16] . The brightness temperature is calculated by Plank's law from the atmospheric radiances obtained from thermal infrared sensors [17] . The brightness temperature is then converted into LST using ground surface emissivity considering vegetation density, the roughness and thermal properties of the ground surface and water content of the soil [18] . Cities are specifically built up urban part is majorly experienced such effects of temperature rise [19, 20] and conversion of earthy materials to concrete materials, change of vegetation cover area to built up land, dumping of water in the urban area are the principal vectors of LST rise in the urban area. This phenomena gave birth to urban heat island effects [21] . World Bank [22] projected that by 2020 megacities will be increased significantly in the developing countries. Rise of LST or Urban heat island effect is one of the major consequences of urban growth and enhanced energy emission [23, 24] . Growing energy footprint is another issue because it possesses enough potentiality to discharge extra heat to the atmosphere triggering heat residues in heat balance [25] . This type of heat is generated by anthropogenic effects. The coronavirus disease 2019 (COVID-19) outbreak, which started in the Hubei province of China in 2019, has now spread to 212 countries and 2 international conveyances by May 5, 2020. WHO declaring Europe as the epicenter of the disease on March 13 [26] . Warmer temperatures will slow the spread of the COVID-19 virus has been a point of much speculation. This hypothesis has led some European countries to take policies regarding on decreased transmission rates during the summer months and India will face smaller epidemics than American or European counterparts. However, no strong evidences support such claims, SARS-CoV-2 arrived later in warmer countries. The first case of the COVID-19 pandemic in India was reported on 30 January 2020 which was originating from China. As of May 5 2020, the Ministry of Health and Family Welfare have confirmed a total of 46,711 cases, 13,161 recoveries and 1583 deaths in the country [27] . The outbreak is declared as an epidemic in states and union territories and provisions of the Epidemic Diseases Act, 1897 have been invoked. For this reason, educational institutions and many commercial establishments have been shut down in all of the country. [29] . Since the lockdown, every activity needs special permission from various administration units and almost all the domestic and international travels have been either banned or monitored closely. This type of situation limits economic activities which is very much dependent on transport network. This long time nationwide lockdown is stranded the economic pace for a long time in near future. But there are more positive issues of this period which are truly important for the environment and people. During this lockdown period, air and noise pollution were reduced by 50-70% in Kolkata, according to data released by the Central Pollution Control Board (CPCB). The less commercial activity (only essential goods and healthcare) during the lockdown period improved the air quality in different parts of the city. The air quality monitoring station at Ballygunje in south Kolkata represent an AQI of 33 on 30 April, 2020, which is good in environmental parlance. At the same time, readings at the AQI stations of Bidhannagar, Jadavpur, Rabindra Sarobar and Victoria Memorial were 28, 29, 36 and 33 respectively. According to WBPCB, the average air quality reading across Kolkata was 20 on 29 April 2020, which indicates good sign. An AQI between 0 and 50 is considered good, 51-100 satisfactory, 101-200 moderately polluted, 201-300 poor, 301-400 very poor, 401-500 severe and AQI above 500 falls in the severe plus category. LST depends upon the character of land surface area. Different methods has been used to detect LST in different areas by scientific community such as Single channel method [30] , Multi-channel method [31] , multi angle method [32] , Split window algorithm [33] and Artificial neural network [15] . In the present situation, Covid -19 pandemic and associated worldwide lockdown improved degraded environmental quality and reduce pollution level. Urban areas around the globe has been affected by heat island phenomenon, resulting from air pollution and concretized surface. Kolkata is an important metropolitan city of India trying to cope with the current situation like other parts of India. The present study attempt to explore the difference of LST of the city before and after total lockdown. In addition, authors are trying to find out the significant relationship with pollution level (AQI) and LST in the city. Kolkata, geographically stretches from 88°17 0 20.0796 00 E to 88°27 0 33.8508 00 E longitude and 22°27 0 1.224 00 N to 22°37 0 58.461 00 N latitude. It is located on the eastern bank of river Hooghly and at 128 km north of Bay of Bengal. Kolkata city is administrated under the jurisdiction of Kolkata Municipal Corporation covering the area about 185 km. The city is now subdivided in 144 wards due to the administrative reason. The city itself is a district (smallest district of West Bengal) as well as capital of the state (Fig. 1) . Kolkata is the capital of the state of West Bengal in India was first started as a British settlement, is located on a flat terrain and tide dominated drainage outfalls. It is one of World's largest urban centers, which is Kolkata urban agglomeration or Kolkata Metropolitan Area (KMA). KMA has continuously expanded over the years and presently extends over 1851 square km. Kolkata Municipal Corporation has an area of 185 square kilometer and is divided into 144 wards [34] . The region around KMA is experienced high intensity precipitation during the monsoon months. Sometimes heavy rainfall results in high tide which is the usual source of urban flooding. Kolkata has a tropical wet and dry climate with an annual mean temperature of 26.8°C and monthly mean temperatures in the range of 19-30°C. A study in comparison of air quality data among four metropolitan areas in India indicates a higher pollution level in Kolkata in comparison to Mumbai and Chennai and close to Delhi [35] . The worst polluted traffic intersections double the city's average pollutants during busy hours [36] . The area receives most of its rainfall from the South West monsoon between June and September. Annual rainfall is about 1600 mm and highest rainfall usually occurs during the monsoon in the month of August. The study on storm patterns [37] shows peak rainfall intensities occur anywhere between 15 and 180 min after the start of rainfall which often occur two or more times in a day during the monsoon. A joint occurrence of high tide and high rainfall can bring the city to a decline, as occurred in 1978, 1999 and 2007 [38] . Kolkata is located in a coastal area and influenced by strong sea based disturbances, this city experiences an average wind speed of 7 km/h throughout the year. The wind direction is mainly southeast and southwest [39] and average value of solar radiation recorded is 1428 W/m 2 [40] . Today most of the city's planned infrastructure has met only handful of people because large number of populations living in informal settlements without access to essential infrastructure. Kolkata is experiencing slower population growth rates than other cities in India, though demographic pressures remain high [41] . Satellite data of Landsat 7 (ETM) of two periods such as before lockdown (13th March, 2020) and after lockdown (30th April, 2020) were collected from USGS Earth explorer official website (https://earthexplorer.usgs.gov/). These satellite imageries were pre-georeferenced to UTM zone 45 north projection with WGS 84 datum. Atmospheric and radiometric correction of satellite imageries were carried out by Erdas Imagine software. Boundary map of KMC was prepared from the data based on Census of India (2011) report. The estimation of LST based on single channel algorithm is completed with the help of Saga GIS software. The atmospheric air quality data are obtained from Central Pollution Control Board (CPCB) official website from Kolkata city and surrounding air quality monitoring stations (https://app.cpcbccr.com/ccr/#/caaqmdashboard-all/caaqm-landing). The hourly data on suspended air particles such as particulate matter (PM2.5 and PM10), Nitrogen di-oxide (NO 2 ), ammonia (NH 3 ), Sulphur di-oxide (SO 2 ), Carbon monoxide (CO) and Ozone (O 3 ) were collected and used to measure air quality index (AQI). Different method are used to retrieve LST from satellite imagery. In this present study, single channel algorithm used to retrieve LST in Kolkata city. Single channel algorithm had advantages over other method and widely used to extract LST using single thermal band [42] . Single channel algorithm uses estimated atmospheric parameters to correct the atmospheric effect in a single channel to retrieve LST [43] . This method also called as model emissivity method [44] and it uses the radiance measure by the satellite in a single channel from an atmospheric window [45] . This method involves a simple inversion of radiometric transfer equation (RTE) and a theoretically accurate method for LST retrieval [42, 45] . The retrieval of LST from satellite imagery using single channel algorithm follows four step (Fig. 2 ) such as retrieval of TOA spectral radiance, conversion of spectral radiance to at-sensor brightness temperature, estimation of land surface emissivity and finally estimation of land surface temperature [42, 46, 47] . Top-of-Atmosphere (TOA) spectral radiance (L k ) estimated from Landsat data product with calibrated digital number (Q cal ) using radiometric rescale calibration coefficient or post-calibration dynamic ranges of spectral radiance (L min k ÀL max k ) of the bands [48] . The post calibration dynamic ranges of spectral radiance for thermal sensors (TM) was used to convert calibrated digital numbers (Q cal ) to TOA spectral radiance (L k ). The spectral radiance (L k ) is calculated using equation-1 [49] . Landsat 7 band-6 data ware converted into TOA spectral radiance (L k ) using radiometric rescaling coefficient such as band specific multiplicative rescaling factor (M L ); Q cal = digital number (DN) of each pixel; and band specific additive rescaling factor (A L ) [50] . Step 2: Transmission of spectral radiance to atsensor brightness temperature Brightness temperature (T B ) is the radiance of the incoming electromagnetic radiation which is travelling upward from the top of the earth's atmosphere (Latif 2014). TOA spectral radiance (L k ) value has been converted into brightness temperature (T) using Eq. 2 [51] . where T B = At satellite brightness temperature, L k = TOA spectral radiance, K 1 and K 2 = thermal conversion constant. Emissivity is the ability of a body to emit radiation [52] . In other word, it is radiative properties of an object [46] . Land surface emissivity (e) is a useful tool to understand the land surface energy budget from satellite data and also a fundamental element to estimate LST. The estimation of land surface emissivity (e) from brightness temperature (T B ) follows three step such as (a) calculation of NDVI, (b) estimation of proportion of vegetation (P V ) and (c) estimation of land surface emissivity (e). To calculate land surface emissivity (e) the primary task is to estimate Normalized Difference Vegetation Index (NDVI) using Red and NIR band of Landsat TM. NDVI calculated using Eq. 5 and the value ranges between -1 and 1 (Fig. 5) . (b) Estimation of proportion of vegetation (P V ) Proportion of vegetation or fractional vegetation cover can be obtained based on NDVI value. Proportion of vegetation (P V ) calculated using following equation. where P V = Proportion of vegetation, NDVI = Normalized Difference Vegetation Index, NDVI max = maximum value of NDVI and NDVI min = minimum value of NDVI. (c) Estimation of land surface emissivity (e) Land surface emissivity estimated based on Eq. 5 where e = Land surface emissivity and P V = Proportion of vegetation. LST has been calculated using at-sensor brightness temperature (T B ) and land surface emissivity (e) using Eq. 8 [47, 51] . where, LST = land surface temperature in Kelvin scale, J/K, h = Planck's constant = 6:626 Â 10 À34 Js, and c = velocity of light = 2:998 Â 10 8 m/s) and e = Land surface emissivity. The LST estimated in Kelvin scale and converted into degree Celsius scale by subtracting 273.15 from each pixel value. Air quality index (AQI) is a composite index that transforms the weighted values of individual air pollutants into a single index [53] . In India, Central Pollution Control Board (CPCB) and Ministry of Environment and Forest (MoEF), government of India initiated the project National Air Quality Index (NAQI). The measurement of NAQI follows two steps: (1) formation of sub-indices of each pollutant and (2) aggregation of sub-indices to get an overall AQI [54] . To derive National Air Quality Index (NAQI) maximum operator approach used to remove uncertainty and eclipsing [55] . Step 1: Formation of sub-indices (I 1 ; I 2 . . .I n Þ for all pollutant variables (X 1 ; X 2 ; . . .; X n Þ carried out using Eq. 7. Where I i = sub-index value, X i = pollutant concentrations. Step 2: Aggregation of sub-indices performed based on overall index (I) or AQI. 3.2.6.1 Sub-indices (Step 1) Sub-indices explains the changes of specific pollutant and related environmental consequences. Sub-indices is the relationship between pollutant concentration X i and corresponding sub-indices I i . The relationship may be linear, non-linear and segmented linear. The relationship between I and X represented as- where a = slope of line, b = intercept and X = 0. Based on 'linear segmented principle' sub-indices (I i ) for a given pollutant concentration (C p Þ calculated based on following Eq. 10. where B HI = breakpoint concentration greater or equal to given concentration, B LO = breakpoint concentration smaller or equal to given concentration, I HI = AQI value corresponding to B HI , I LO = AQI value corresponding to B LO , C P = pollutant concentration. Step 2) The subindices are combined in a simple additive form or weighted additive form. Different methods used to combine subindices and estimate Air quality index (I) such as weighted additive form (Eq. 11), non-linear aggration form (Eq. 14), root-mean-square form (Eq. 15) and Min or Max operator (Eq. 16) [53, 54] . where P w i = 1, I i ¼ sub-indices for pollutant I, n = number of pollutant variables, w i = weightage of the pollutant. where p = positive real number [ 1. Root-mean-square form Min or max operator I ¼ Min or Max I 1 ; I 2 ; I 3 ; . . .; I n ð Þ ð 14Þ Normalized difference built-up index (NDBI) is useful method to extract urban buildup area. NDBI estimated using Eq. 15. NDBI value ranges between -1 and 1. Higher value indicate build up areas and lower value means vegetation and negative value are water bodies. Normalized difference water index (NDWI) is used to detect the surface water content [56] . NDWI estimated using Eq. 16. where MIR band = mid infrared band, NIR band = Near infrared band and Green band = green band of TM. The entire Kolkata city (KMC) is covered with multiple land use/cover types ranging from water bodies (Lake and Swamps) to vegetation cover (East Kolkata Wetland) and high density high rise buildings in the city center, interspersed with large areas covered with slums. The area covered by vegetation patches increased slightly in the eastern part of Kolkata and in some scattered parts of southern Kolkata in comparison to the other parts of the study area. Across the entire study area, LST values increased from the outskirts towards the inner urban areas, where concentration of water body and green areas are relatively low. LST patterns were found as non-symmetrical and non-concentric, with high temperature zones clustered towards west of the central axis and beside the river Hooghly. There exists significant difference of LST of pre-lockdown and postlockdown period in the city (Fig. 3) . The highest and lowest LST in before lockdown is 36.6°C and 23.6°C whereas after lockdown it decreased to 35.7°C and 17.3°C respectively. Thus, the range of LST of postlockdown period decreased significantly due to the decrease in pollution level in the city (Figs. 4, 5, 6 ). To understand the relationship and correlation of determination of LST with different Landuse indices such as Normalized Difference Buildup Index (NDBI), Normalized Difference Vegetation Index (NDVI) and Normalized Difference Water Index (NDWI), correlation graph prepared (Fig. 5) . The value of NDVI varied from -0.333 to 0.518. There exists negative relationship between NDVI with LST. The R 2 value is 21.82% and it indicates lower dependency of NDVI in the determination of LST. Figure 5 shows that low NDVI values were detected at the northern and central part of the study area, corresponding to the built up areas (such as buildings, roads etc.). NDVI was used as an index of vegetation abundance. This index is related to biomass, chlorophyll content and water stress. High NDVI values were discovered in certain patch of the study area, corresponding to green vegetation. The spatial pattern of NDVI appeared to be scattered and concentric. High NDVI values formed a belt in eastern and western direction and was scattered within study area, consistent with the distribution of parks and recreation sites. Build up areas and barren land has difference reflection pattern than vegetation cover. Figure 5 shows that NDBI is ranging from -0.933 to 0.559 where the R 2 value is 50.35%. The coefficient of determination indicates that the NDVI highly controls the concentration of LST in the city. All over the city the concentration of higher NDVI value has been observed. The CBD of the city near Barabajar Region very high value of NDBI found. High value of NDBI was distributed principally in the northern part, but the areas with high NDBI expanded in the whole city, except some scattered patches. Eastern part of the city low NDBI value observed due to the existence of wetlands. In the study area, NDWI is ranging from -0.297 to 0.403 where the R 2 value is 12.43% (Fig. 5) . NDWI calculated based on Landsat 7 satellite imagery and it reflects very high NDWI observed the places where water bodies are present. The surrounding places of Ganga River also influences the high concentration of NDWI in the city. Water bodies in Kolkata city are very sparse, only a few pockets of water body is left. Among all of these indices, the coefficient of determination is highest in the case of NDBI, because residential land use accounts 79% of all land use category, followed by vegetation and water body. Places with more temperature than average is decreasing in number due to the closure of commercial, industrial and transport activities during lockdown. Further study of general temperature profile of the study area from the LST images indicate that the temperature decreases from North and North-West to South and South-East direction (Fig. 3) . To understand and estimate the decrease of LST in different parts of the city, the pixel wise changes of the different temperature zone pre-lockdown and post-lockdown period were estimated ( Fig. 7; Table 1 ). For this logical analysis five sequential temperature zone map prepared such as [ 30°C, [ 28°C, [ 26°C, [ 24°C and \ 24°C prepared. The decrease of pixel count of individual temperature zone significantly indicates the change of LST in pre-lockdown and post-lockdown period ( Table 1) . LST is influenced by many parameters such as solar incident radiation, angle of incidence of solar radiation, surface properties such as surface roughness, moisture content, extent of vegetation and air temperature. The spatial change is experienced not only in the case of LST, but also in the concentration of PM 2.5 , PM 10 , NO 2 , NH 3 , SO 2 , CO and Ozone pollutants in air. In this study, 10 important weather station have been selected for data collection of pollution. Sources of air pollutants can be classified as primary and secondary sources. Primary pollutants are identified (PM 2.5 , PM 10 , NO 2 , NH 3 , SO 2 , CO) from the anthropogenic interference like power generation, automobile exhausts, factories, agricultures, airplanes etc. On the other hand Ozone (03) has been considered as a (30 April, 2020) secondary sources, which is formed with interaction between primary pollutants (SEPA). The atmosphere can also be polluted by particles material other than gaseous pollutants. These particles (either in fluid, in solid state or in suspension), have a divergent size and composition and are sometimes called aerosols. They are often categorized as 'floating dust', but are best known as particulate matter (PM). Particulate matter (PM) is not a single pollutant, but rather is a mixture of many chemical components. It is a composite mixture of solids and aerosols mixture of small dry solid fragments, droplets of liquid and solid cores with liquid glazing. Most of the particles differ widely in shape, size and chemical composition, and may include inorganic ions, metallic compounds, elemental carbon, organic compounds, and compounds from the earth's crust. Particles are defined by their diameter for air quality regulatory purposes. Those with a diameter of 10 microns or less (PM 10 ) are inhalable and can persuade adverse health effects. In every urban center, these particulate matters (PM) take the most important position in all the other air pollutants. In Kolkata city, concentration of both particulate matters (PM 2.5 and PM 10 ) were intensive before lockdown. In both the cases, high intensity of suspended particles concentrated in northern and middle part of the city on 13th March. After that 30th April experimental sample shows the drastic change of particle matters in the city due total locked down. This positive change of air quality encouraged for a healthy breathing condition in the city. The other elements of air pollution like NO 2 , NH 3 , SO 2 , CO and secondary Ozone gas made a drastic down fall between these two consecutive dates of locked down (Table 2) . So, at a glance it has been very clear that peripheral eastern side of Hugli River, which has been more pollution prone due to industrial activities (Fig. 6) . As well as, central part of city especially Burrabazar, Raja Bazar, Kankurgachi, Bowbazar, Ballygunge, Taltala, Tangra, Lalbazar, Esplanade and Park Street experienced intense traffic congestion on a normal day. General trend shows that Outer skirts of the city has been less polluted than the central and northern part of the city in every pollution parameters (Fig. 6) . It can be easily rectify that outer growth of the present Kolkata city has more over residential in pattern rather than commercial or industrial. Therefore, older section of Kolkata is more congested as well as catalyst of increasing air pollution. At the end, over all air quality index (AQI) has been made from the database of ten sample zones on different pollutant parameters. Significantly over all city reflect moderately polluted (100.01-152.99) on the date before locked down (13th march). In 30th April air quality index (AQI) has been show very good result (33.00-44.99). This upgraded quality has positively regenerate pure inhalable air in the city. There is significant change in LST between 13th March and 30th April has been found. In the Fig. 3 , Spatial variation of the temperature between local pockets are significantly low than it was on 13th March. The average temperature of Kolkata city is 28°C on both dates. Figure 3 shows stronger LST intensity in 13th March than in 30th April. The figure also shows that larger areas that were affected by high LST was on 13th March, before lockdown was initiated. The spatiotemporal change between these to pre-lockdown and post-lockdown period is not only obvious in the changing pattern of LST, but also witnessed substantial downfall of the pollutants. Especially, during the study period PM 2.5 , PM 10 3 and SO 2 the reduction have counted are low in comparison to the others. In urban areas, NO 2 and CO is mainly emitted from combustion practice from road traffic, particularly diesel and smaller concentration of gasoline, vehicles, manufacturing industry and power plants. The concentration of SO 2 in Kolkata city is also high because of its activity as river port. Majority of SO 2 starts off from shipping emissions (large cargo ships, cruises and ferries). On the other hand, NH 3 originated mainly from agricultural sources [58] . So concentration of this particular gas is much below the acceptable limit. However, the concentration of NH 3 is significantly decreased during the lockdown phase because petrol engine vehicles comprise most of the Urban NH 3 [59, 60] . 8 h. average daily maximum concentration of O 3 (38.587 from 40.069) in the study period shows negligible decrease. The concentration of Ozone (O 3 ) increases especially in the industrial and transport dominated locations which are out of operation during lockdown period. Overall, AQI (Air Quality Index) has been changed significantly from moderately polluted (100.01-152.99) to Good (33.00-44.99) air quality. This is a clear indication that substantial improvement of the air quality is due to the implementation of air quality control measures in lockdown period. There exists the differentiation in changes of LST behaviour in different functional region of the KMC. The landuse pattern of the city also determines the nature of LST. Thus for the detailed explanation micro level study carried out based on different landuse and functional zone within study area such as residential area, industrial area, commercial area (CBD), traffic congestion area and wetlands areas. Thus six functional zone selected for further explanation (Fig. 8) . Zone 1 located in the northern corner of the city and it comprising ward no. 5 to ward no. 57 (Fig. 9a) . Most of the land use classification in this part is dominated by commercial, residential and mixed residential land use. There are also a few green area and dispersed industrial land use is found. Mixed residential area included administrative and commercial activities along with residential land use. North Kolkata is the oldest part of the city and for this reason, residential density is very high. There are a number of slums sheltering large number of people also. In most cases, slums and developed residential areas are overlaps. The vertical development of residential land use in recent years led to mixed land use phenomena. Central Business District (CBD) of Dalhousie, Chowringhee and commercial center of Burrabazar are part of zone 1 where higher LST observed. There is significant decrease of LST observed in this zone due changes of atmospheric pollution level. Zone 2 is located in South west part of the city (Fig. 9b) and industrial landuse is common in this area. The two main neighborhoods of this zone are Garden Reach and Behala. These two are comprising ward no. 80; 133-141 and 118-132 respectively. These are the two oldest neighborhoods of Kolkata and home of several major industries. Other major land use category is residential land use. The average decrease of LST in this zone is highest in comparison to other zones. Waterbody and public parks generally showing lower temperature than industrial land use. Zone 3 of Kolkata Municipality is the part of south Kolkata and expanded from ward no. 65 to ward no. 105 (Fig. 9c ). There are neighborhoods namely Tiljala, Bhowanipore, Ballygaunge, Park Circus etc. Shortage of residential lands forced people to move in these swamp areas. Recently, land shortage in Kolkata attracts people in these areas which was upgraded and now became the prime plots for high-rise expansion, commercial as well as residential complexes. There are a number of healthcare facilities are available in Mukundapur, Ruby and adjacent areas and became a medical hub. Changing transport and communication system as well as government planning is changed the entire area. In the lockdown period, there are a drastic change in LST composition is found in this region (Fig. 9c) . The changes of LST is prominent in landuse with water bodies and vegetation cover Zone 4 is located in South Kolkata and expanded from ward no. 94 to ward no. 114 (Fig. 9d) . Neighborhoods of this area are Tollygunge, Bansdroni, Jadavpur, Garia etc. These areas are famous for residential, commercial and educational land use. Tollygunge and Garia are wellknown for commercial centers, restaurants, daily markets etc. During lockdown period, commercial and transportation activities were shut down which is the main reason behind the decrease in LST. Zone 5 is a part of East Kolkata, which is distributed between two wards, ward no. 58 and ward no. 108 (Fig. 9e) . This is the location of famous East Kolkata Wetland which is located in ward no. 58. This wetland is a complex of natural and manmade wetlands and cover 125 square kilometers including salt marshes and salt meadows, as well as sewage farms and settling ponds. This is designated a ''wetland of international importance'' under the Ramsar Convention on 19th August, 2002. The other important neighborhoods are Tangra, Dhapa and Bantala. Tangra is located upon marshy and reclaimed low-lying land, is the home of over 350 tanneries. Dhapa is the area which consists landfill sites where the solid wastes of the city are dumped. Garbage Farming is a common practice in the landfill sites which produces 40 percent of the green vegetables in the Kolkata markets. Bantala houses Kolkata Leather Complex spread over an area of 450 hectares, along with IT SEZ. Residential areas are spread across this area, in accordance to industry, wetland and dumping ground. During lockdown period, LST ranges from 22 to 30°C observed in this area which is 24-32°C pre-lockdown period. Zone 6 is located in North Kolkata, which is the part of ward no. 1 to ward no. 12 (Fig. 9f) . The neighborhood of this area is Cossipore, Sinthee, Chitpur, Bagbazar, Hatibagan, Shyambazar, Shobhabazar etc. These are the oldest area of Kolkata city which was urbanized during East India Company rule. There are a range of land use variations in this area, which is ranging from residential, commercial, transport and industrial land use. High density of residential, transportation and commercial activities are the reason for high LST. Surface temperature is coming to an ease during lockdown, where it was ranging from 24 to 30°C with small pockets of high and low temperatures. The rise of temperature at the global city is a major environmental threat around the globe. The rapid urbanization increased the pollution level of the city and it also influences the atmospheric temperature as well as LST. The COVID-19 pandemic and related lockdown worldwide has been reduced the pollution level. The significant impact observed in the major megacities of the world. The lockdown due to COVID-19 pandemic in the country, the pollution level of the city drastically improved. The decline of pollution level influences the LST in the city. The study aimed to analyze the impact of lockdown due to COVID-19 pandemic on the LST in the city. Single-channel algorithm used to retrieve LST from Landsat TM satellite data. Pre-lockdown and postlockdown atmospheric pollutants data and satellite imageries used to investigate the impact of COVID-19 pandemic on changes of LST. Air quality index (AQI) in different parts of the city estimated based on seven air pollutants such as PM 2.5 , PM 10 , NO 2 , NH 3 , SO 2 , CO and Ozone. The result indicates that the pollution level and LST significantly declined after lockdown in different parts of the city. The reduction of LST and atmospheric pollution can improve the ecological stability and habitat in the city. Funding None. Availability of data and material Data should be made available on request. Conflict of interest The authors declares that they have no conflict of Interest. 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