Vidhya Ganesh RangarajanThe University of Western Ontario | UWO · Institute for Earth and Space Exploration
Vidhya Ganesh Rangarajan
Doctor of Philosophy
About
19
Publications
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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
Education
August 2019 - August 2023
July 2015 - May 2017
July 2011 - June 2015
Publications
Publications (19)
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...
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...
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...
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...
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...
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...
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...
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...
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...
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...
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...
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...
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...
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...
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)
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?
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?
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?
This is essential as the coordinates of the image boundary pixels are not known because of lack of .lbl file in PDS Geosciences node.
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?