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Spectral Indices Across Remote Sensing Platforms and Sensors Relating to the Three Poles
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Spectral Indices Across Remote Sensing Platforms and Sensors Relating to the Three Poles

  1. 83 Advances in Remote Sensing Technology and the Three Poles, First Edition. Edited by Manish Pandey, Prem C. Pandey, Yogesh Ray, Aman Arora, Shridhar D. Jawak, and Uma K. Shukla. © 2023 John Wiley & Sons Ltd. Published 2023 by John Wiley & Sons Ltd. 6 Spectral Indices Across Remote Sensing Platforms and Sensors Relating to the Three Poles An Overview of Applications, Challenges, and Future Prospects Mallikarjun Mishra1 , Kiran Kumari Singh2,13 , Prem C. Pandey3 , Rahul Devrani4 ,Avinash Kumar Pandey5 , KN Prudhvi Raju1 , Prabhat Ranjan6 ,Aman Arora7 , Romulus Costache8 , Saeid Janizadeh9 , Nguyen Thuy Linh10 , and Manish Pandey11,12, * 1 Department of Geography, Ravenshaw University, Cuttack, Odisha, India 2 Department of Geography, Central University of Punjab, Bathinda, Punjab, India 3 School of Natural Sciences, Shiv Nadar Institution of Eminence, Greater Noida, Uttar Pradesh, 201314, India 4 Delhi School of Climate Change & Sustainability, Institution of Eminence, University of Delhi, Delhi - 110007, India 5 Department of Chemistry, GLA University, Chaumuhan, Mathura, Uttar Pradesh, India 6 Central Pollution Control Board, Ministry of Environment, Forest, and Climate Change, Parivesh Bhawan, East Arjun Nagar, Shahdara, Delhi, India 7 Bihar Mausam Seva Kendra, Planning and Development Department, Government of Bihar, Patna, Bihar, India 8 Department of Civil Engineering, Transilvania University of Brasov, Brasov, Romania 9 Department of Watershed Management Engineering and Sciences, Faculty in Natural Resources and Marine Science, Tarbiat Modares University, Tehran, Iran 10 Institute of Applied Technology, Thu Dau Mot University, Binh Duong province, Vietnam 11 University Center for Research & Development (UCRD), Chandigarh University, Mohali, Punjab, India 12 Department of Civil Engineering, University Institute of Engineering, Chandigarh University, Mohali, Punjab, India 13 Department of Geography, Central University of South Bihar, Gaya-824236, Bihar, India * Corresponding author spectral bands are employed, keeping in view the spectral response to the ground features. Remote sensing helps to acquire spatial and temporal data and to increase our understanding of polar dynamics. It is a system that measures electromagnetic energy ema- nating from an object. However, the remotely-sensed images are the result of various interrelated processes and can provide information about the characteristics of the surface materials based on characteristics of electromag- netic radiation, atmospheric interaction, and sensor char- acteristics (Campbell and Wynne, 2011). Remote-sensing technology has advanced tremendously over the past few decades in terms of its spectral (ranging from visible to microwave), spatial (ranging from kilometer to sub- meter), radiometric, and temporal (from years to months to hours to minutes) characteristics, which have facili- tated the research community to experiment with varie- ties of remotely-sensed data (Liang and Wang, 2020). Fortunately, various satellite platforms have made multi- spectral data freely available to research community, such as the Landsat series (30 m spatial resolution) and Sentinel 2 (10 m and 20 m spatial resolution of different spectral bands). The commercially available data are available at a very fine spatial and higher spectral resolution. In recent times, the use of UAVs (Unmanned Aerial Vehicles) and LiDAR have surged forward to acquire spatial information with higher spatial and temporal resolution. 6.1 Introduction In recent years, remote-sensing technology has advanced our knowledge in polar research. Satellite-based observa- tions such as optical (Landsat series), synthetic aperture radar (SAR) satellite imagery, and very-high-resolution images have been applied through various analytical tech- niques to understand the dynamic processes operating in the lithosphere (Özkan et al., 2018), atmosphere (Yang et al., 2020), biosphere (Yang et al., 2020), hydrosphere (Cermakova, et al., 2019), in general, the cryospheric com- ponent of the hydrosphere (How et al., 2021), and anthro- posphere (DaCamara et al., 2019; Agyeman et al., 2021). Figure 6.1 illustrates the spheres of our planet, and various objects, also called “Elements of Identification (IoE),” that advances in remote-sensing technology has helped, is help- ing, and will help plan future missions by space agencies of different countries and groups of countries aiming to mon- itor and manage the betterment of our society. Remote sensing has been widely used to understand geology, geo- morphology, ice shelfs, glaciers, coastlines, and vegetation cover. The study of the polar regions is of utmost impor- tance to understand the atmospheric–oceanic process of the globe. This review paper has compiled a comprehen- sive database on remote-sensing application of polar research through various spectral indices. Several impor- tant challenges are discussed that occur when different
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