Vidhya Ganesh Rangarajan

Vidhya Ganesh Rangarajan
The University of Western Ontario | UWO · Institute for Earth and Space Exploration

Doctor of Philosophy

About

19
Publications
2,706
Reads
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72
Citations
Introduction
I am currently a research assistant at the Institute of Earth & Space Exploration and the Department of Earth Sciences at Western University, Canada. I am also a science team member of the Colour and Stereo Surface Imaging System (CaSSIS) instrument onboard the ExoMars TGO. My research areas focus on detecting and assessing seasonal and temporal changes on the Martian surface from high resolution imagery, with a long term goal pointed towards understanding the evolution of planetary surfaces.
Additional affiliations
November 2018 - June 2019
Indian Institute of Technology Kanpur
Position
  • Researcher
Description
  • Lunar Geology
July 2017 - November 2018
Indian Institute of Technology Guwahati
Position
  • Fellow
Description
  • Martian Geomorphology and Geochemistry
May 2016 - July 2016
National Institute of Technology Karnataka
Position
  • Summer Intern
Education
August 2019 - August 2023
The University of Western Ontario
Field of study
  • Geology and Planetary Sciences
July 2015 - May 2017
Birla Institute of Technology, Mesra
Field of study
  • Remote Sensing
July 2011 - June 2015
Bangalore University
Field of study
  • Civil Engineering

Publications

Publications (19)
Article
Full-text available
The present-day water cycle on Mars has implications for habitability and future human exploration. Water ice clouds and water vapour have been detected above the Tharsis volcanic province, suggesting the active exchange of water between regolith and atmosphere. Here we report observational evidence for extensive transient morning frost deposits on...
Article
Mars is host to a variety of active surface processes that relate to changes in seasonal ice/frost, slope activity, wind and processes potentially relating to liquid water. Regular monitoring and change detection of these phenomena is crucial to not only provide us insights into present day Martian surface conditions, but also its past geologic and...
Article
Full-text available
Water ice in the Martian mid‐latitudes has advanced and retreated in response to variations in the planet's orbit, obliquity, and climate. A 150 m‐diameter new impact crater near 35°N provides the lowest‐latitude impact exposure of subsurface ice on Mars. This is the largest known ice‐exposing crater and provides key constraints on Martian climate...
Article
Recurring Slope Lineae (RSL) are narrow, dark streaks lengthening down Martian steep slopes during warm seasons, fading during the cold ones and regularly recurring every Martian year. Their origin is still debated. Although initially interpreted as possible flows of seeping water, either coming from a subsurface aquifer or through atmospheric proc...
Article
Slope streaks are albedo features that form frequently on equatorial Martian slopes. Most slope streaks are dark relative to surrounding terrains, a minor fraction is bright, and there are rare transitioning streaks that exhibit a contrast reversal partway downslope. Their formation mechanisms and physical surface properties are not well understood...
Article
Thermal inertia has been found to play a significant role in planetary remote sensing applications, forming the basis of potentially all major lithological discriminations of the planetary surface. It has always been visualised to serve as a distinctive thermal property of the surface with its values remaining fairly constant at least for a short t...
Conference Paper
Full-text available
Thermal inertia (TI) of a planetary surface exhibits its ability for heat storage and re-radiation during day and night time respectively. Consequently, their magnitudes are closely defined by the physical and thermal properties of the surface strata and the near surface thermal environment. This has potentially paved the way for its utility as an...
Conference Paper
The study made use of aerosol optical depth (AOD) data obtained from Moderate-resolution Imaging Spectroradiometer (MODIS) sensor on board Terra satellite at 10km resolution and meteorological parameters predicted using Weather Research Forecasting (WRF) model to estimate countrywide PM2.5 concentration. PM2.5 concentration and meteorological data...
Conference Paper
The planned water structures on the Brahmaputra River have been a great source of concern for India. One such concern is the possible diversion of part of the Tibetan tributary of the river from one such operational dam, Zangmu which could cause a possible reduction of discharge to Brahmaputra. The current study focuses on estimation of discharge a...
Conference Paper
Full-text available
The surface energy budget (SEB) is a comprehensive strategy to understand the thermal behaviour of a planetary surface. Knowledge of the surface radiative transfer helps us understand near surface thermal environments. There are various methods and numerical models to partially compute energy budgets. The best methods for efficient calculation of e...
Conference Paper
Jezero, an impact crater located in NE Syrtis is home to a large diversity of alteration minerals and fluvial features. The current study aims to map the abundance of rock-bearing mafic minerals in the region and analyze them with the estimated surface thermal inertia and thereby generate a hydrated mineral potential map. It is seen that the crater...
Article
Remote sensing techniques have proved to be highly efficient in the exploration of Mars. Availability of several sensors operating across the electromagnetic spectrum on-board orbiters, landers and rovers has helped better understand the surface and atmospheric conditions on the Red planet. This article summarises the application potential of the s...
Conference Paper
Syrtis Major Planum is a major volcanic construct on Mars ridden with a large number of fluvial channels mostly draining into the adjacent Isidis basin. These channels have been attributed to have formed by lava flows from the calderas of the construct onto the basin. However, with availability of high spatial and spectral resolution remote sensing...
Conference Paper
Contrast Limited Adaptive Histogram Equalization technique (CLAHE) is a widely used form of contrast enhancement, used predominantly in enhancing medical imagery like X-rays and to enhance features in ordinary photographs. This paper aimed to understand the effectiveness of using this technique in multispectral satellite imagery and to study its ef...
Technical Report
Contrast Limited Adaptive Histogram Equalization technique (CLAHE) is a widely used form of contrast enhancement, used predominantly in enhancing medical imagery like X-rays and to enhance features in ordinary photographs. This work is aimed to understand the effectiveness of using this technique in multispectral satellite imagery and to study its...

Questions

Questions (5)
Question
I've been observing from several thermal models applied to satellite data like THEMIS/TES for Mars that they prefer using bolometric temperatures over spectral temperatures for thermal inertia estimates. Can anyone help me understand what is the major difference between the two and why bolometric temperatures are preferred?
Question
The CTX EDR data is composed of pixels displaying digital numbers. Is there any way to convert this DN value to radiance, then reflectance and subsequently generate Lambert albedo from the same?
Question
Is it possible to get both day and night datasets of the same date in order to calculate temperature difference for apparent thermal inertia? If so, how can I identify the two datasets from the entire list in Mars Orbital Data Explorer Node?
Question
This is essential as the coordinates of the image boundary pixels are not known because of lack of .lbl file in PDS Geosciences node.
Question
I have successfully computed thermal inertia on a seasonal basis using THEMIS data for a region in Mars which I found to be sinusoidally varying, peaking at Ls = 250-270 and dipping at Ls = 90-110. What may be the cause for this variation and how do I substantiate my conclusion with other data like Curiosity?

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