Quantification of Evening and Morning Twilight Angle in Malaysia: A Suburban-Rural Areas Comparison - sersc
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International Journal of Advanced Science and Technology Vol. 29, No. 3, (2020), pp. 14995 – 15001 Quantification of Evening and Morning Twilight Angle in Malaysia: A Suburban-Rural Areas Comparison Ngadiman, N.F.1,2,3*, Shariff, N.N.M.1,2,3 and Hamidi, Z.S.1,3,4 1 Islamic Astronomy & Solar Astrophysics (IASA) Universiti Teknologi MARA, Shah Alam, Malaysia 2 Academy of Contemporary Islamic Studies (ACIS) Universiti Teknologi MARA, Shah Alam, Malaysia 3 Institute of Science (IOS) Universiti Teknologi MARA, Shah Alam, Malaysia 4 Faculty of Applied Sciences, Universiti Teknologi MARA, Shah Alam, Malaysia 1 nfn132@gmail.com, 2nnmsza@uitm.edu.my, 3zetysh@uitm.edu.my Abstract Studies on the effects of sunlight scattering during twilight phenomena yield information about solar altitude or twilight angle value for determination of Isha and Subh prayer times. This study set out to a quantify the evening and morning twilight angle based on long time observation and compare the similarities as well as dissimilarities of results obtained between suburban and rural areas. Hence, data acquisition was performed in selected areas throughout Malaysia from April 2018 to September 2019 by recording sky brightness readings during twilight every day, utilizing Sky Quality Meter Data Logger (SQM-LU-DL). Good data visualization criterion and third-degree polynomial models have been applied to the collected data to obtain the best data. This study has found that the tendency values acquired from observation data appear to be in the range -18o for evening twilight angle and -17o to -18o for morning twilight angle. Besides, there is no specific pattern that distinguished between twilight angle variations in suburban and rural areas. The only discernable difference is that suburban area with higher population density has given a wider range and variability in twilight angle values. Keywords: twilight angle, Sky Quality Meter, polynomial measurement 1. Introduction The existence of the atmosphere surrounding the solid Earth prevents the sky from completely dark or bright during the transition of sunrise and sunset. This is due to the atmospheric molecules that scatter the sunlight, inducing illumination, or a faint glow at the sky. This phenomenon called twilight which directly associated with Muslim prayer times determination, Isha and Subh whereby shafaq (the afterglow of sunset at a certain angle) and fajr (first light before sunrise) both are astronomical phenomena part of evening and morning twilight stage respectively [1]. As stated by U.S. Naval Observatory, twilight is classified into three perceptible phases in proportion to a solar altitude below the horizon or named as twilight angle, i.e., a) civil twilight (-6o
International Journal of Advanced Science and Technology Vol. 29, No. 3, (2020), pp. 14995 – 15001 definitive as the disperse and intensity of light on the horizon incrementally changes over time, resulting in the pinpoint phenomena determination open to interpretation (ijtihad). Hence, various twilight angle values that have been used for both prayers throughout the world. The variation of this parameter value is also attributable to the different duration of twilight depending on the latitude of a location in which the parallactic angle for the diurnal path of the Sun relative to the horizon will vary at different locations [3]. Consequently, it affects how quickly or slowly the Sun’s movement below the horizon. For equatorial regions such as Malaysia, the Sun’s path nearly parallel to vertical to the horizon caused the twilight period in this country shorter than higher latitude regions. Natural phenomena such as twilight have their dynamism, which requires continuous study to observe the consistency of its pattern over time. In Malaysia, we can see few quantitative types of research utilizing various equipment besides using naked eyes, such as Sky Quality Meter photometer [4], [5], [6], [7], [8], [9], [10], [11], [12], handmade photometer [13] and DSLR [14] in measuring the morning and evening twilight angle. In some way, all these studies indicate the different value and wide-ranging of twilight angle, ranged from -17 o to -20o . Thus far, there are no satisfactory studies of the observational and data collection to justify the twilight angle values in the context of Malaysia. This study, therefore, set out to a quantify the evening and morning twilight angle based on long time observation and compare the similarities as well as dissimilarities of result s obtained between suburban and rural areas. Besides, this study also serves as a scientific document for quantitative review of evening and morning twilight in Malaysia. 2. Methodology 2.1. Data Collection Data acquisition was performed in four (4) different locations throughout Malaysia involving the east and west of Peninsular Malaysia and Sabah from April 2018 to September 2019. These locations represent suburban and rural areas as shown in Table 1. This classification is based on the Department of Statistics Malaysia, which defines urban areas as having a combined population of 10 000 or more at the time of the Census 2010 with at least 60% of the population were involved in non-agricultural activities. Table 1. Location of Data Collection Type of Observation Site Coordinate Elevation (m) Population of District Location Selangor Observatory 3.8192° N, 7 103153 (BCS) 100.8143° E Suburban 5.8082352° N, Kuala Besut (BST) 7 140952 102.5814666° E 4.177633° N, Kuala Lipis (LPS) 66 85341 102.08035° E Rural 6.021572° N, Kundasang (PLI) 1642 94092 116.603637° E Several methods currently exist for the twilight angle measurement. In this study, sky brightness during twilight phenomena was recorded each minute in magnitude per square arc second (MPSAS) unit every day utilizing portable photometer, Sky Quality Meter Data Logger (SQM-LU-DL). The selection of this equipment is since there is a good agreement between the photoelectric measurement and the naked eye [15]. This photometer which composed of high sensitivity TAO TSL237S sensor ISSN: 2005-4238 IJAST 14996 Copyright ⓒ 2020 SERSC
International Journal of Advanced Science and Technology Vol. 29, No. 3, (2020), pp. 14995 – 15001 was set to 10 MPSAS thresholds and oriented towards the zenith because of the least contaminated area of the sky. 2.2. Data Selection The selection of the best data is based on good data visualization and root mean square error value (RMSE). Theoretically, a graph with good data visualization will form a light curve, whereas, for evening twilight, the brightness of the sky would increase as the Sun is getting away from the horizon and would reach a point of maximum brightness which would continue to remain constant throughout the night. On the contrary for morning twilight, at nighttime, the brightness is constant because the sunlight no longer affects the sky and the night sky brightness becomes decreases as the Sun approaches the horizon. To support the criteria of good data visualization, the sky brightness data will be filtered by fitting the data to the third-degree polynomial models. The polynomial function as following: (1) where y is the recorded night sky brightness readings during twilight in MPSAS unit, x is the altitude of the Sun or twilight angle in degree unit and a, b, c, d are the polynomial parameters. We used the RMSE as standard statistical metric to select the good data, which a good light curve will produce RMSE value
International Journal of Advanced Science and Technology Vol. 29, No. 3, (2020), pp. 14995 – 15001 Figure 1. Percentage of Good Sky Brightness Data at Each Observation Site It is important to mention that Figure 2(a) and (b) are the identical pattern of night sky brightness during twilight phenomena at each observation site on the same date (note that the triangle marks in the graph represent suburban area and circle marks for rural area). It can be seen during evening twilight the sky brightness readings continue increasing as the Sunsets until reaching the maximum point and remain steady throughout the night. Similarly, the graph readings during morning twilight will portray the same pattern in which the brightness of the sky starts to decrease gradually from the constant readings as the Sun begins to move closer to the horizon. Further data visualization analysis showed that in Figure 2(a), the sky at BST reached the maximum brightness after 75 minutes of sunset (twilight angle = - 16.88o) which is earlier than two other sites, BCS and LPS, 79 minutes (twilight angle = -18.68 o) and 78 minutes after sunset respectively (twilight angle = -18.53 o). Meanwhile, Figure 2(b) indicates that LPS began to decline 75 minutes before sunrise (twilight angle = -18.77 o), followed by BST and PLI which dropped 71 minutes before sunrise (twilight angle = -17.82 o and -17.84 o respectively) What is striking about Figure 2 is no significant difference was found between obtained twilight angle at suburban and rural areas. Apparently, rural areas are less exposed to light pollution supposedly would detect the disappearance of shafaq later and recognize the appearance of fajr faster than suburban areas. This has made the acquired data do not seem to be in line with the theory. Howbeit, it is indisputable that the overall sky brightness readings in rural areas are darker than suburban areas. (a) (b) 18.9 18.6 18.3 MPSAS 18 17.7 17.4 17.1 BST BCS LPS 16.8 30 40 50 60 70 80 90 100 Time after sunset (minutes) Figure 2. Sky Brightness During Evening Twilight and Morning Twilight on 19th June 2018 and 1st May 2019 ISSN: 2005-4238 IJAST 14998 Copyright ⓒ 2020 SERSC
International Journal of Advanced Science and Technology Vol. 29, No. 3, (2020), pp. 14995 – 15001 As for the statistical comparison of evening and morning twilight angle value from each observation site. The results obtained from this measurement are summarized in Tables 3 and 4. For overall 529 observations days, the mean values of evening twilight angle measured in suburban areas were -18.22 o (SD=0.67) and - 18.3 o (SD=0.8) for BCS and BST, showing 0.1 o -0.4o (equivalent to 0.7-1.6 minutes) slightly faster in detecting disappearance of shafaq, compared to the rural twilight angle of -18.63o (SD=0.74) and -18.47 o (SD=0.81) at LPS and PLI. The pattern shown during the morning twilight was unalike, with all suburban and rural sites detecting the decrease in sky brightness at an average value of -18.1 o (equivalent to about 72 minutes before sunrise), except for BST, which averaged -17.92o (SD=1.23), slightly late in detecting the appearance of fajr. Considering the acquired mean values, the tendency for evening and morning twilight angle distribution is likely to be around -17 o to -18o . Nevertheless, based on the observational data, the values of both twilight angles were seen ranged from -20o to -14 o. There is no specific pattern that distinguished between twilight angle variations in suburban and rural areas. What can be deduced is that BST is the site with the widest range for both twilight angles. This is likely due to the highest population density compared to other sites which resulting the variability in twilight angle values. Table 2. Descriptive Analysis of Measured Evening Twilight (o) at Each Observation Site Results BCS BST LPS PLI Minimum -20.2172 -20.5527 -20.5647 -20.5269 Maximum -16.88 -15.2487 -16.0698 -16.6441 Range 3.3372 5.304 4.4949 3.8828 Mean -18.2296 -18.3097 -18.6327 -18.4652 Standard Deviation (SD) 0.667227 0.815565 0.737193 0.809961 Standard Error 0.108239 0.081967 0.074468 0.120742 Table 3. Descriptive Analysis of Measured Morning Twilight (o) at Each Observation Site Results BCS BST LPS PLI Minimum -19.3598 -20.0157 -19.23 -19.7093 Maximum -16.9563 -14.5302 -16.5184 -16.2637 Range 2.4035 5.4855 2.7116 3.4456 Mean -18.176 -17.92391493 -18.10213188 -18.16737105 Standard Deviation (SD) 0.727426485 1.227708058 0.666131588 0.741452055 Standard Error 0.181856621 0.149988411 0.08019282 0.085050384 Besides, the pattern of measured data is further strengthened in Figure 3, which represents the distribution of 0.5° width bars as the frequency of 529 evening and morning twilight observations from all sites. While the concentration of the measured twilight angle was delineated in the box-whisker plots graphs. It can be seen in Figure 3(a) that - 18o is the most commonly evening twilight angle observed at each site. The values of - 15o, -16o and -20o at each location had a frequency of less than 3%, except for the frequency value of the -16o angle at BST which equals 8%. Morning twilight also exhibits the same twilight angle pattern as depicted in Figure 3(b). The -14o, -15o, -16o and -20o angles have frequencies less than 7%, not including -16o at BST with a frequency of 10%. ISSN: 2005-4238 IJAST 14999 Copyright ⓒ 2020 SERSC
International Journal of Advanced Science and Technology Vol. 29, No. 3, (2020), pp. 14995 – 15001 Therefore, these clustered bars provide important insight into twilight angle patterns in suburban and rural areas where values of -15o, -16o and -20o may be measured during observation, but the frequency is extremely small and sporadic. (a) (b) Figure 3. Frequency Distribution of Measured Evening and Morning Twilight Angle 4. Conclusion In conclusion, this study has identified that the acquired mean of evening twilight angle from all sites is within the range of -18 o, while the range for the mean of morning twilight angle is slightly wider at -17o to -18o . These findings are in accord with most of the twilight angle values in previous studies. Additionally, there is no definite pattern that discerned between twilight angle variations in the suburban and rural areas as indicated by the collected data. What can be inferred is that one of suburban site, BST, has the widest range for both twilight angles. This is likely attributable to the highest population density compared to other sit es, inducing the variability in twilight angle values. Long term research with suitable integration of various methods and equipment as well as the use of naked eyes on twilight measurement would help us to establish a greater degree of accuracy of twiligh t angle value. Acknowledgment This work was partially supported by the grant, 600-IRMI/FRGS 5/3 (100/2019), UiTM grants and Kementerian Pengajian Tinggi Malaysia. Special thanks to the Universiti Teknologi MARA and University of Malaya for supporting this study. References [1] N. N. M. Shariff, Z. S. Hamidi, A. Mohamad, M. Z. Zainuddin, "Background Theory of Twilight in Isha and Subh Prayer Times," in Dimensi Penyelidikan Astronomi Islam, University of Malaya, 2013, pp. 121-132. [2] P. K. Seidelmann and S. Urban, Eds., Explanatory Supplement to the Astronomical Almanac, University Science Books, 2012. [3] I. Bromberg, "The Duration of Twilight," University of Toronto, Canada, 2019. [Online]. Available: http://individual.utoronto.ca/kalendis/index.html. [4] A. H. A. Aziz, M. Z. A. Yusof, and M. N. Muhamad, "Kajian Bermulanya Waktu Fajar," Jurnal Falak, no. 4, pp. 1-18, 2018. ISSN: 2005-4238 IJAST 15000 Copyright ⓒ 2020 SERSC
International Journal of Advanced Science and Technology Vol. 29, No. 3, (2020), pp. 14995 – 15001 [5] R. A. Wahab, "Kajian Waktu Terbir Fajar Bagi Menentukan Awal Waktu Subuh," in Muzakarah Falak Peringkat Kebangsaan, 2017. [6] N. Kadir, Penilaian Semula Parameter Penentuan Awal Waktu Solat Subuh Penilaian Semula Parameter Penentuan Awal Waktu Solat Subuh Di Malaysia Dari Perspektif Astronomi Islam, 2017. [7] M. A. Niri, "Kajian Waktu Terbit Fajar Bagi Menetukan Permulaan Waktu Subuh," in Muzakarah Falak Peringkat Kebangsaan, 2017. [8] M. S. Shukor and M. Z. Zainuddin, "Perbandingan Metodologi Kajian Penentuan Masuknya Fajar Sadiq dan Hilangnya Syafaq Ahmar: Kajian Kecerahan Langit," Jurnal Falak, vol. 1, pp. 133-139, 2015. [9] S. A. M. Nor and M. Z. Zainuddin, "Sky Brightness for Determination of Fajr and Isha Prayer by Using Sky Quality Meter," International Journal of Scientific & Engineering Research, vol. 3, no. 8, pp. 3-5, 2012. [10] M. A. Niri, M. Z. Zainuddin, S. Man, S. A. M. Nawawi, R. A. Wahab, K. Ismail, N. H. A. Zaki and A. A. Ghani, "Astronomical Determinations for the Beginning Prayer Time of Isha'," Middle-East Journal of Scientific Research, vol. 12, no. 1, pp. 101-107, 2012. [11] H. M. Sadali, J.i Sulong and A. H. A. Aziz, Parameter Kedudukan Matahari Bawah Ufuk Bagi Penentuan Waktu Subuh dan Isyak, 2011. [12] N. N. M. Shariff, Sky Brightness at Twilight: Detectors Comparison between Human Eyes and Electronic Device For Isha' and Subh from Islamic and Astronomical Considerations, 2008. [13] N. Ahmad, M. Z. Zainuddin and M. S. Yahya, "Kajian Kecerahan Langit Di Ufuk Senja dan Fajar," Jurnal INSTUN, no. 1, pp. 49-66, 2007. [14] K. Bahali, A. L. Samian, N. Muslim and N. S. A. Hamid, "Measuring the sun depression angle of dawn with a DSLR camera," Sains Malaysiana, vol. 47, no. 11, pp. 2877-2885, 2018. [15] A. H. Hassan, Y. A. Abdel-hadi, I. A. Issa and N. Y. Hassanin, "Brightness and color variation for evening and morning twilights at Bahria of Egypt IV," NRIAG Journal of Astronomy and Geophysics, vol. 3, no. 1, pp. 37-45, 2014. Authors Nurul Fathin Ngadiman, currently pursuing her MA in Contemporary Islamic Studies besides being Islamic Astronomy & Solar Astrophysics (IASA) research assistant at Universiti Teknologi MARA, Shah Alam, Malaysia, who is working on Isha and Subh Light Curve Profile research. She obtained her BA in Shariah: Islamic Astronomy in 2018 at University of Malaya (UM). Her degree’s project is about atmospheric extinction and night sky brightness using photometry technique. Project done at Langkawi National Observatory, Malaysia. Assoc. Prof. Dr. Nur Nafhatun Md Shariff received BA in Shariah: Islamic Astronomy in 2006, MSc in Islamic Astronomy in 2009 and PhD in Science & Technology Studies in 2013 at University of Malaya. She is currently at Universiti Teknologi MARA, Shah Alam, Malaysia. Her research area includes astronomy (light pollution monitoring, Isha and Subh prayer time determination, hilal – Islamic new moon research), solar studies (solar monitoring – optical and radio) and sustainability (sustainable agriculture). Assoc. Prof. Dr. Zety Sharizat Hamidi received BSc in Physics in 2004, MSc in Physics in 2008 and PhD in Solar Astrophysics in 2014 at University of Malaya. Currently Senior Lecturer at Universiti Teknologi MARA, Shah Alam, Malaysia. Her research area includes solar astrophysics, Islamic astronomy, climate change and environment, antenna, radio and optical astronomy. ISSN: 2005-4238 IJAST 15001 Copyright ⓒ 2020 SERSC
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