{"id":1684,"date":"2018-04-13T18:25:45","date_gmt":"2018-04-13T18:25:45","guid":{"rendered":"https:\/\/nau.edu\/astronomy-and-planetary-science\/?page_id=1684"},"modified":"2024-05-28T08:54:19","modified_gmt":"2024-05-28T15:54:19","slug":"research","status":"publish","type":"page","link":"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/research\/","title":{"rendered":"Research"},"content":{"rendered":"<!-- shortcode-right-column-below -->\n<div class=\"shortcode-right-column\" >\n    <div class=\"shortcode-right-column__container\">\n<!-- shortcode-contact -->\n<div class=\"shortcode-contact\">\n    <div class=\"contact-header\">\n        <h3>Contact Us<\/h3>\n    <\/div>\n    <div class=\"contact-body\">\n                <a href=\"mailto:astro@nau.edu\" aria-label=\"Contact Us: Email Address\" title=\"Email Address\">\n            <div class=\"contact-icon-container\">\n                <i class=\"fas fa-envelope\" aria-hidden=\"true\"><\/i>\n                <span class=\"sr-only\">Email:<\/span>\n            <\/div>\n            <div class=\"contact-email\">astro&#8203;@nau.edu<\/div>\n        <\/a>\n                        <a href=\"tel:928-523-2661\" aria-label=\"Contact Us: Telephone Number\" title=\"Telephone Number\">\n            <div class=\"contact-icon-container\">\n                <i class=\"fas fa-phone\" aria-hidden=\"true\"><\/i>\n                <span class=\"sr-only\">Call:<\/span>\n            <\/div>\n            <div class=\"contact-phone\">928-523-2661<\/div>\n        <\/a>\n            <\/div>\n<\/div>\n\n\n<!-- shortcode-button -->\n<div class=\"shortcode-button shortcode-button--center\">\n      <a class=\"main-button\" href=\"https:\/\/www.yumpu.com\/en\/embed\/view\/aOGH7RyYIu2j4Qnl\" target=\"_blank\">View NAU\u2019s most recent brochure highlighting our world-class research faculty!<\/a>\n  <\/div>\n\n<\/div>\n<\/div>\n\n<h1>Research<\/h1>\n<p>The Department of Astronomy and Planetary Science at NAU is home to active faculty research programs in several exciting areas in the lab, at the telescope, and participating in NASA Solar System Exploration missions.<\/p>\n<h3>Current research projects:<\/h3>\n<!-- shortcode-accordion -->\n<div class=\"shortcode-accordion shortcode-accordion--closed\" style=\"position: relative;\" >\n        <a class=\"shortcode-accordion__trigger\" data-header=\"Astrobiology_0\" href=\"#\">\n      <div class=\"shortcode-accordion__header\">\n          <h4>Astrobiology <span class=\"screen-reader-text\">Accordion Closed<\/span><\/h4>\n          <span class=\"shortcode-accordion__header__arrow\"><\/span>\n      <\/div>\n    <\/a>\n    <div class=\"shortcode-accordion__body\">\n        <!DOCTYPE html PUBLIC \"-\/\/W3C\/\/DTD HTML 4.0 Transitional\/\/EN\" \"http:\/\/www.w3.org\/TR\/REC-html40\/loose.dtd\">\n<html><body>\n<h5>Relevant faculty:<\/h5>\n<table>\n<tbody>\n<tr>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/MarkSalvatore.jpg\" alt=\"Portrait Photo of Mark Salvatore\" width=\"135\">Mark<br>\nSalvatore<\/td>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/DavidTrilling.jpg\" alt=\"Portrait Photo of David Trilling\" width=\"135\">David<br>\nTrilling<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<h5>Active research:<\/h5>\n<h6>Antarctic Studies<\/h6>\n<p>What controls the distribution and activity of life in the coldest and driest locations on Earth? <strong>Dr. Salvatore&rsquo;s<\/strong> work is revolutionizing how we search for life on Earth and other planets. His research team conducts field work in the McMurdo Dry Valleys of Antarctica to study the activity of photosynthetic microbial communities and to compare these observations with orbital measurements. The goal is to be able to model the distribution, activity, health, and biochemical properties of these systems remotely to further understand the conditions required for life to thrive.<\/p>\n<figure id=\"attachment_3062\" aria-describedby=\"caption-attachment-3062\" style=\"width: 464px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-3062 size-landscape-image\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/Salvatore_Microbes-464x348.jpg\" alt=\"\" width=\"464\" height=\"348\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Salvatore_Microbes-464x348.jpg 464w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Salvatore_Microbes-800x600.jpg 800w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Salvatore_Microbes-232x174.jpg 232w\" sizes=\"auto, (max-width: 464px) 100vw, 464px\" \/><figcaption id=\"caption-attachment-3062\" class=\"wp-caption-text\">Prof. Salvatore surveying an ephemeral glacial melt stream with abundant microbial mats in Taylor Valley, Antarctica.<\/figcaption><\/figure>\n<h6>Experimental Astrobiology<\/h6>\n<p><strong>Dr. Trilling<\/strong> is carrying out several projects in experimental astrobiology in collaboration with faculty in NAU&rsquo;s Biological Sciences department. In the first, he is measuring to what degree microbial life can survive in increasingly Mars-like conditions through a series of experiments with sealed containers using both local soil from Northern Arizona and Mars analog soils. In the second, his team is carrying out physiology experiments on laboratory mice to determine the short-term and long-term effects of exposure to lunar and asteroidal dust. They are using reverse-transcriptase quantitative PCR and histology and studying airway microbiome composition to identify and quantify pulmonary epithelial inflammation, tissue remodeling, and pulmonary function pathology resulting from exposure to dust simulants. Finally, in the third, Trilling and colleagues are studying remediation techniques for perchlorates, which are present on Mars at lethal concentrations that would prevent food production (farming) there.<\/p>\n<figure id=\"attachment_3115\" aria-describedby=\"caption-attachment-3115\" style=\"width: 464px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-3115 size-landscape-image\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/Trilling-microbial-loads-464x348.png\" alt=\"\" width=\"464\" height=\"348\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Trilling-microbial-loads-464x348.png 464w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Trilling-microbial-loads-300x226.png 300w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Trilling-microbial-loads-768x578.png 768w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Trilling-microbial-loads-1024x771.png 1024w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Trilling-microbial-loads-800x600.png 800w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Trilling-microbial-loads-232x174.png 232w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Trilling-microbial-loads.png 1318w\" sizes=\"auto, (max-width: 464px) 100vw, 464px\" \/><figcaption id=\"caption-attachment-3115\" class=\"wp-caption-text\">Ari Koeppel, a PhD student working with Trilling, has found that soils with different microbial loads (insert) have different temperature profiles (data) after wetting and heating, suggesting that infrared thermography may be a sensitive astrobiology detection technique.<\/figcaption><\/figure>\n<\/body><\/html>\n\n    <\/div>\n<\/div>\n\n<!-- shortcode-accordion -->\n<div class=\"shortcode-accordion shortcode-accordion--closed\" style=\"position: relative;\" >\n        <a class=\"shortcode-accordion__trigger\" data-header=\"Astroinformatics_0\" href=\"#\">\n      <div class=\"shortcode-accordion__header\">\n          <h4>Astroinformatics <span class=\"screen-reader-text\">Accordion Closed<\/span><\/h4>\n          <span class=\"shortcode-accordion__header__arrow\"><\/span>\n      <\/div>\n    <\/a>\n    <div class=\"shortcode-accordion__body\">\n        <!DOCTYPE html PUBLIC \"-\/\/W3C\/\/DTD HTML 4.0 Transitional\/\/EN\" \"http:\/\/www.w3.org\/TR\/REC-html40\/loose.dtd\">\n<html><body>\n<h5>Relevant faculty:<\/h5>\n<table>\n<tbody>\n<tr>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/DavidTrilling.jpg\" alt=\"Portrait Photo of David Trilling\" width=\"135\">David Trilling<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p>Astroinformatics is the application of &ldquo;big data&rdquo; techniques to problems in astronomy. <strong>Dr. Trilling<\/strong> leads the Solar System Notification Alert Processing System (SNAPS) broker, which ingests data from all-sky telescopic surveys. We derive the physical properties for hundreds of thousands of asteroids, and use various computational and data science approaches to identify unusual asteroids. The science goal is to use these derived global properties of asteroids, together with the incidence rates of unusual asteroids, to help constrain how our Solar System formed and evolved. In the next few years our project will undergo a tenfold increase in scale with the LSST survey begins.<br>\n<\/p><\/body><\/html>\n\n    <\/div>\n<\/div>\n\n<!-- shortcode-accordion -->\n<div class=\"shortcode-accordion shortcode-accordion--closed\" style=\"position: relative;\" >\n        <a class=\"shortcode-accordion__trigger\" data-header=\"Exoplanets & Planetary Formation_0\" href=\"#\">\n      <div class=\"shortcode-accordion__header\">\n          <h4>Exoplanets & Planetary Formation <span class=\"screen-reader-text\">Accordion Closed<\/span><\/h4>\n          <span class=\"shortcode-accordion__header__arrow\"><\/span>\n      <\/div>\n    <\/a>\n    <div class=\"shortcode-accordion__body\">\n        <!DOCTYPE html PUBLIC \"-\/\/W3C\/\/DTD HTML 4.0 Transitional\/\/EN\" \"http:\/\/www.w3.org\/TR\/REC-html40\/loose.dtd\">\n<html><body>\n<h5>Relevant faculty:<\/h5>\n<table>\n<tbody>\n<tr>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/DavidTrilling.jpg\" alt=\"Portrait Photo of David Trilling\" width=\"135\">David Trilling<\/td>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/DiegoMunoz.jpg\" alt=\"Portrait Photo of Diego Munoz\" width=\"135\">Diego Munoz<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<h5>Active research:<\/h5>\n<h6>Formation &amp; Evolution of Planetary Systems<\/h6>\n<p><strong>Dr. Trilling<\/strong> is using the Hubble Space Telescope to discover very faint Kuiper Belt Objects. The orbits and physical properties of these distant objects will help constrain the origin of the Solar System.<\/p>\n<figure id=\"attachment_1602\" aria-describedby=\"caption-attachment-1602\" style=\"width: 232px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1602 size-landscape-image-sm\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/HST-232x174.jpg\" alt=\"Hubble Space Telescope\" width=\"232\" height=\"174\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/HST-232x174.jpg 232w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/HST-1024x762.jpg 1024w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/HST-800x600.jpg 800w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/HST-464x348.jpg 464w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/HST.jpg 1280w\" sizes=\"auto, (max-width: 232px) 100vw, 232px\" \/><figcaption id=\"caption-attachment-1602\" class=\"wp-caption-text\">Hubble Space Telescope. Image Credit: NASA<\/figcaption><\/figure>\n<p><strong>Dr. Munoz<\/strong> works on diverse topics of theoretical astrophysics, using super-computing simulations and pencil-and-paper calculations. His research interests include protoplanetary disk dynamics and evolution, exoplanets, astrophysical fluid dynamics, stellar and planetary tidal interactions, theoretical orbital dynamics, super-massive black hole binaries, and exoplanets. His work also includes the development of numerical methods for compressible gas dynamics and their implementation on massively parallel astrophysical software.<\/p>\n<\/body><\/html>\n\n    <\/div>\n<\/div>\n\n<!-- shortcode-accordion -->\n<div class=\"shortcode-accordion shortcode-accordion--closed\" style=\"position: relative;\" >\n        <a class=\"shortcode-accordion__trigger\" data-header=\"Laboratory Studies of Planetary Materials_0\" href=\"#\">\n      <div class=\"shortcode-accordion__header\">\n          <h4>Laboratory Studies of Planetary Materials <span class=\"screen-reader-text\">Accordion Closed<\/span><\/h4>\n          <span class=\"shortcode-accordion__header__arrow\"><\/span>\n      <\/div>\n    <\/a>\n    <div class=\"shortcode-accordion__body\">\n        <!DOCTYPE html PUBLIC \"-\/\/W3C\/\/DTD HTML 4.0 Transitional\/\/EN\" \"http:\/\/www.w3.org\/TR\/REC-html40\/loose.dtd\">\n<html><body>\n<h5>Relevant faculty:<\/h5>\n<table style=\"border-style: none;\">\n<tbody>\n<tr>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/ChristopherEdwards.jpg\" alt=\"Portrait Photo of Christopher Edwards\" width=\"135\">Christopher Edwards<\/td>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/JoshuaEmery.jpg\" alt=\"Portrait Photo of Josh Emery\" width=\"135\">Josh Emery<\/td>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/MarkLoeffler.jpg\" alt=\"Portrait Photo of Mark Loeffler\" width=\"135\">Mark Loeffler<\/td>\n<\/tr>\n<tr>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/MarkSalvatore.jpg\" alt=\"Portrait Photo of Mark Salvatore\" width=\"135\">Mark Salvatore<\/td>\n<td><\/td>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/StephenTegler.jpg\" alt=\"Portrait Photo of Stephen Tegler\" width=\"135\">Stephen Tegler<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<h5>Active research:<\/h5>\n<h6>Asteroidal Analogs<\/h6>\n<p><strong>Dr. Emery<\/strong> measures laboratory spectra of analogs to materials found on asteroid surfaces in order to facilitate interpretation of telescopic observations. The materials include terrestrial minerals as well as meteorites. Investigations generally include petrologic and mineralogic characterization of the samples to ground the spectral data. We typically attempt to simulate different environmental conditions on asteroid surfaces to investigate the effects on measured spectra.<\/p>\n<figure id=\"attachment_4000\" aria-describedby=\"caption-attachment-4000\" style=\"width: 600px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-4000 size-uncropped-large\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/Emery-AsteroidalAnalogResearch-600x439.png\" alt=\"\" width=\"600\" height=\"439\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Emery-AsteroidalAnalogResearch-600x439.png 600w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Emery-AsteroidalAnalogResearch-300x220.png 300w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Emery-AsteroidalAnalogResearch-1024x750.png 1024w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Emery-AsteroidalAnalogResearch-768x562.png 768w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Emery-AsteroidalAnalogResearch.png 1535w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><figcaption id=\"caption-attachment-4000\" class=\"wp-caption-text\">Left image is a meteorite ground to powder. The red color in the top frame shows the effects of weathering from the Earth&rsquo;s atmosphere, and the bottom frame shows the same meteorite after appropriate chemical processing to remove the weathered components. The plots on the right show spectra of this meteorite and other similar meteorites (from Lucas et al. 2019).<\/figcaption><\/figure>\n<h6>Evolution of Planetary Surfaces<\/h6>\n<p><strong>Dr. Loeffler<\/strong> runs the <a href=\"http:\/\/www.astro.nau.edu\/~loeffler\/\" target=\"_blank\" rel=\"noopener noreferrer\">Processes, Environments, and Astrochemistry on Extraterrestrial Surfaces (PEAXS) Laboratory<\/a> at NAU, which studies the physical, chemical, and structural evolution of planetary surfaces.<\/p>\n<figure id=\"attachment_1900\" aria-describedby=\"caption-attachment-1900\" style=\"width: 595px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1900\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/\/LabStudies-1.jpg\" alt=\"Loeffler's Lab\" width=\"595\" height=\"291\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/LabStudies-1.jpg 595w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/LabStudies-1-300x147.jpg 300w\" sizes=\"auto, (max-width: 595px) 100vw, 595px\" \/><figcaption id=\"caption-attachment-1900\" class=\"wp-caption-text\">The ultra-high vacuum system used to laser irradiate minerals relevant to asteroids and the Moon. Spectral analyses of samples can be performed in situ. Not shown are the pulsed laser, low-energy ion gun, or the catcher plate.<\/figcaption><\/figure>\n<p><!--\n<strong><a href=\"https:\/\/planetgeomorph.nau.edu\" target=\"_blank\" rel=\"noopener\">Dr. Burr<\/a><\/strong> conducts experiments in the high-pressure Titan Wind Tunnel at the NASA Ames Research Center to determine the minimum wind speed needed to form the vast dunes seen on Titan.\n\n&#091;caption id=\"attachment_2981\" align=\"aligncenter\" width=\"960\"&#093;<img loading=\"lazy\" decoding=\"async\" class=\"wp-image-2981 size-tall-banner-image\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/Burr-Titan-Wind-Tunnel-960x384.jpg\" alt=\"\" width=\"960\" height=\"384\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Burr-Titan-Wind-Tunnel-960x384.jpg 960w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Burr-Titan-Wind-Tunnel-465x186.jpg 465w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Burr-Titan-Wind-Tunnel-1440x576.jpg 1440w\" sizes=\"auto, (max-width: 960px) 100vw, 960px\" \/> Titan Wind Tunnel at the NASA Ames Research Center.&#091;\/caption&#093;\n--><\/p>\n<h6>Instrument Development<\/h6>\n<p><strong>Dr. Edwards<\/strong> designs and builds prototype instruments for use in the laboratory, the field, and ultimately space. Specifically, he works with novel thermal infrared techniques designed to maximize scientific output while minimizing size, weight, and power.<\/p>\n<figure id=\"attachment_1902\" aria-describedby=\"caption-attachment-1902\" style=\"width: 401px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1902\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/LabStudies-4.jpg\" alt=\"Simulated IR map of the Moon\" width=\"401\" height=\"401\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/LabStudies-4.jpg 401w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/LabStudies-4-150x150.jpg 150w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/LabStudies-4-300x300.jpg 300w\" sizes=\"auto, (max-width: 401px) 100vw, 401px\" \/><figcaption id=\"caption-attachment-1902\" class=\"wp-caption-text\">Simulated infrared data of the Moon from a thermal infrared imager proposed by Dr. Edwards and colleagues.<\/figcaption><\/figure>\n<h6>Planetary Ices<\/h6>\n<p><strong>Dr. Tegler<\/strong> studies ices relevant to the surfaces of Kuiper Belt Objects in the Astrophysical Ice Laboratory using transmission and Raman spectroscopy.<\/p>\n<figure id=\"attachment_1901\" aria-describedby=\"caption-attachment-1901\" style=\"width: 553px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1901\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/\/LabStudies-2.jpg\" alt=\"Astrophysical Ices Lab\" width=\"553\" height=\"313\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/LabStudies-2.jpg 553w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/LabStudies-2-300x170.jpg 300w\" sizes=\"auto, (max-width: 553px) 100vw, 553px\" \/><figcaption id=\"caption-attachment-1901\" class=\"wp-caption-text\">An NAU student, Dr. Tegler, and Dr. Will Grundy (Lowell Observatory) working in the Astrophysical Ice Laboratory.<\/figcaption><\/figure>\n<p><!--\n<strong><a href=\"https:\/\/planetgeomorph.nau.edu\" target=\"_blank\" rel=\"noopener\">Dr. Burr<\/a><\/strong> conducts experimental studies into the effects on icy cobbles of transport in liquid nitrogen rivers on Titan. They do this research using the Titan Tumbler, developed by Dr. Joe Levy at Colgate University, to tumble icy cubes at liquid nitrogen temperatures to quantify the amount of rounding, size reduction, and resulting fine sediment production.\n\n&#091;caption id=\"attachment_2982\" align=\"aligncenter\" width=\"464\"&#093;<img loading=\"lazy\" decoding=\"async\" class=\"size-landscape-image wp-image-2982\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/TitanTumbler.gif\" alt=\"\" width=\"464\" height=\"320\" \/> Slow-motion gif of tumbling ice clasts in the Titan Tumbler, at Colgate University in Hamilton, NY, where experimental work is underway in collaboration with Professor Joe Levy and his students. The Titan Tumbler setup has now been updated to a 15-cm diameter roller mill, tumbling ice clasts at a chilly 194 K (-80 C) thanks to solid-CO2 cooling.&#091;\/caption&#093;\n--><\/p>\n<h6>Terrestrial Studies<\/h6>\n<p><strong>Dr. Salvatore<\/strong> and <strong>Dr. Edwards<\/strong> collaborate in the laboratory analysis of terrestrial samples for comparison to remotely acquired signatures on planetary surfaces.<\/p>\n<\/body><\/html>\n\n    <\/div>\n<\/div>\n\n<!-- shortcode-accordion -->\n<div class=\"shortcode-accordion shortcode-accordion--closed\" style=\"position: relative;\" >\n        <a class=\"shortcode-accordion__trigger\" data-header=\"Observational Planetary Science_0\" href=\"#\">\n      <div class=\"shortcode-accordion__header\">\n          <h4>Observational Planetary Science <span class=\"screen-reader-text\">Accordion Closed<\/span><\/h4>\n          <span class=\"shortcode-accordion__header__arrow\"><\/span>\n      <\/div>\n    <\/a>\n    <div class=\"shortcode-accordion__body\">\n        <!DOCTYPE html PUBLIC \"-\/\/W3C\/\/DTD HTML 4.0 Transitional\/\/EN\" \"http:\/\/www.w3.org\/TR\/REC-html40\/loose.dtd\">\n<html><body>\n<h5>Relevant faculty:<\/h5>\n<table style=\"border-style: none; width: 100%;\">\n<tbody>\n<tr>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/JoshuaEmery.jpg\" alt=\"Portrait Photo of Josh Emery\" width=\"135\">Josh Emery<\/td>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/StephenTegler.jpg\" alt=\"Portrait Photo of Stephen Tegler\" width=\"135\">Stephen Tegler<\/td>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/CristinaThomas.jpg\" alt=\"Portrait Photo of Cristina Thomas\" width=\"135\">Cristina Thomas<\/td>\n<\/tr>\n<tr>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/DavidTrilling.jpg\" alt=\"Portrait Photo of David Trilling\" width=\"135\">David Trilling<\/td>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/ChadTrujillo.jpg\" alt=\"Portrait Photo of Chad Trujillo\" width=\"135\">Chad Trujillo<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<h5>Active research:<\/h5>\n<h6>Characterization of Kuiper Belt Objects<\/h6>\n<p><strong>Drs. Emery, Tegler, Trilling<\/strong>, and <strong>Trujillo <\/strong> are all involved with the identification and characterization of Kuiper Belt Objects using a multitude of instruments and techniques. For example, <strong>Dr. Trujillo<\/strong> is actively searching the outer reaches of our Solar System to find extremely distant Trans-Neptunian minor planets and dwarf planets &mdash; the unusual orbits of these objects suggest that there may be an undiscovered giant planet lurking in our outer Solar System. <strong>Dr. Emery<\/strong> led a large survey of Centaurs and KBOs with the Spitzer space telescope to investigate ices and organics on their surfaces, and he looks forward to continuing those investigations with the James Webb Space Telescope.<\/p>\n<figure id=\"attachment_1612\" aria-describedby=\"caption-attachment-1612\" style=\"width: 718px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1612\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/OortCloud-2012VP113tile.jpg\" alt=\"OortCloud 2012VP113tile\" width=\"718\" height=\"204\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/OortCloud-2012VP113tile.jpg 1436w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/OortCloud-2012VP113tile-300x85.jpg 300w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/OortCloud-2012VP113tile-768x218.jpg 768w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/OortCloud-2012VP113tile-1024x291.jpg 1024w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/OortCloud-2012VP113tile-600x170.jpg 600w\" sizes=\"auto, (max-width: 718px) 100vw, 718px\" \/><figcaption id=\"caption-attachment-1612\" class=\"wp-caption-text\">These images show the discovery of the new inner Oort cloud object 2012 VP113, taken about 2 hours apart on UT November 5, 2012 with the Dark Energy Camera (DECam) on the CTIO 4-meter telescope in Chile.<br>Image credit: Scott S. Shappard\/Carnegie Institution for Science.<\/figcaption><\/figure>\n<h6>Composition of Asteroids<\/h6>\n<p><strong>Dr. Thomas<\/strong> uses visible and near-infrared spectroscopy to characterize the composition of asteroids. She recently completed a ground-based spectral survey of the Massalia, Merxia, and Agnia families of asteroids using the NASA Infrared Telescope Facility (IRTF) and SOAR telescopes.<\/p>\n<figure id=\"attachment_1907\" aria-describedby=\"caption-attachment-1907\" style=\"width: 970px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1907\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/OPS-1.jpg\" alt=\"NASA\/IRTF spectra of NEOs.\" width=\"970\" height=\"167\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/OPS-1.jpg 970w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/OPS-1-300x52.jpg 300w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/OPS-1-768x132.jpg 768w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/OPS-1-600x103.jpg 600w\" sizes=\"auto, (max-width: 970px) 100vw, 970px\" \/><figcaption id=\"caption-attachment-1907\" class=\"wp-caption-text\">Example NASA IRTF spectra of various near-Earth objects, as presented in Thomas et al. (2014).<\/figcaption><\/figure>\n<p><strong>Dr. Emery<\/strong> investigates compositions of Main Belt and Trojan asteroids with reflectance spectroscopy at visible and near-infrared wavelengths and emission spectroscopy at mid-infrared wavelengths using ground- and space-based telescopes. He has particularly focused on the 2&ndash;4 &mu;m region to study asteroidal volatiles and organics.<\/p>\n<figure id=\"attachment_3991\" aria-describedby=\"caption-attachment-3991\" style=\"width: 600px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-3991 size-uncropped-large\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/Emery-AsteroidResearch-600x233.png\" alt=\"\" width=\"600\" height=\"233\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Emery-AsteroidResearch-600x233.png 600w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Emery-AsteroidResearch-300x117.png 300w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Emery-AsteroidResearch-1024x398.png 1024w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Emery-AsteroidResearch-768x298.png 768w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Emery-AsteroidResearch.png 1460w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><figcaption id=\"caption-attachment-3991\" class=\"wp-caption-text\">Left: Plot showing the orbital and size distribution of different 3-&mu;m spectral types (from Takir and Emery 2012). Right: Mid-infrared emissivity spectra of four asteroids of different spectral types (from Emery et al. 2019).<\/figcaption><\/figure>\n<h6>Icy Moons \/ Ocean Worlds<\/h6>\n<p><strong>Dr. Emery<\/strong> studies the surface compositions of the moons of the giant planets to understand the compositions of ices and structures of the near surface layer.<\/p>\n<figure id=\"attachment_3997\" aria-describedby=\"caption-attachment-3997\" style=\"width: 600px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-3997 size-uncropped-large\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/Emery-IceOceanMoonslResearch-600x288.png\" alt=\"\" width=\"600\" height=\"288\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Emery-IceOceanMoonslResearch-600x288.png 600w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Emery-IceOceanMoonslResearch-300x144.png 300w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Emery-IceOceanMoonslResearch-1024x492.png 1024w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Emery-IceOceanMoonslResearch-768x369.png 768w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Emery-IceOceanMoonslResearch.png 1329w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><figcaption id=\"caption-attachment-3997\" class=\"wp-caption-text\">NIR spectrum (black with yellow error bars; 1-2.5 &mu;m) and spectrophotometry (3.6-5.8 &mu;m, diamonds) of Ariel, one of the regular moons of Uranus, showing the presence of H&not;2O and CO2 ice. The different model fits at short and longer wavelengths indicate stratification within the near-surface layers (modified from Cartwright et al. 2015).<\/figcaption><\/figure>\n<h6>Investigation of Near-Earth Asteroids<\/h6>\n<figure id=\"attachment_1419\" aria-describedby=\"caption-attachment-1419\" style=\"width: 300px\" class=\"wp-caption alignright\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1419 size-square-image\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/dct_6x9-300x300.jpg\" alt=\"DCT-MilkyWay\" width=\"300\" height=\"300\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/dct_6x9-300x300.jpg 300w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/dct_6x9-150x150.jpg 150w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/dct_6x9-600x600.jpg 600w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><figcaption id=\"caption-attachment-1419\" class=\"wp-caption-text\">Northern Arizona University is a formal scientific partner with the Discovery Channel Telescope (DCT), a 4.3-meter observatory located forty miles southeast of NAU in Happy Jack, Arizona. The DCT is owned and operated by the Lowell Observatory, which is also closely partnered with NAU in the advising of graduate students, the National Undergraduate Research Observatory (NURO), and the instruction of NAU astronomy courses. Photo credit: Stephen Tegler<\/figcaption><\/figure>\n<p><strong>Dr. Trilling<\/strong> uses telescopes all over the world and in space to study the physical properties of Near-Earth Asteroids. He leads two projects to develop and enhance instrumentation to support this&nbsp; research. <strong>Dr. Thomas<\/strong> is a co-investigator on the Mission Accessible Near-Earth Object Survey (MANOS), which observes small, newly discovered NEOs. She also led the investigation of the observability of NEOs with the upcoming James Webb Space Telescope (JWST). <strong>Dr. Emery<\/strong> uses the same techniques to study silicate mineralogy and volatile compositions of near-Earth asteroids as described above for Main Belt and Trojan asteroids.<\/p>\n<h6>Thermophysical Characterization of Planetary Surfaces<\/h6>\n<p><strong>Dr. Emery<\/strong> observes small bodies across the Solar System in the thermal infrared (i.e., the heat emitted by the surfaces). These observations enable determination of sizes and albedos (a technique called radiometry). Detailed thermal observations also enable thermophysical characterization of the surfaces, which, in turn, provide a window into the physical structure of the surface (e.g., is it covered in fine regolith like the Moon, or more bouldery, such as the NEAs Bennu and Itokawa).<\/p>\n<figure id=\"attachment_3995\" aria-describedby=\"caption-attachment-3995\" style=\"width: 464px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"size-landscape-image wp-image-3995\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/Emery-ThermoPhysicalResearch-464x348.png\" alt=\"\" width=\"464\" height=\"348\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Emery-ThermoPhysicalResearch-464x348.png 464w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Emery-ThermoPhysicalResearch-800x600.png 800w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Emery-ThermoPhysicalResearch-232x174.png 232w\" sizes=\"auto, (max-width: 464px) 100vw, 464px\" \/><figcaption id=\"caption-attachment-3995\" class=\"wp-caption-text\">Modeled (a) Temperature, (b) 4-5 &mu;m flux, and (c) 22-&mu;m flux of NEA 101955 Bennu. These models were computed to analyze thermal observations of Bennu with the Spitzer space telescope and characterize the surface before the launch of OSIRIS-REx (from Emery et al. 2014).<\/figcaption><\/figure>\n<\/body><\/html>\n\n    <\/div>\n<\/div>\n\n<!-- shortcode-accordion -->\n<div class=\"shortcode-accordion shortcode-accordion--closed\" style=\"position: relative;\" >\n        <a class=\"shortcode-accordion__trigger\" data-header=\"Planetary and Solar System Dynamics_0\" href=\"#\">\n      <div class=\"shortcode-accordion__header\">\n          <h4>Planetary and Solar System Dynamics <span class=\"screen-reader-text\">Accordion Closed<\/span><\/h4>\n          <span class=\"shortcode-accordion__header__arrow\"><\/span>\n      <\/div>\n    <\/a>\n    <div class=\"shortcode-accordion__body\">\n        <!DOCTYPE html PUBLIC \"-\/\/W3C\/\/DTD HTML 4.0 Transitional\/\/EN\" \"http:\/\/www.w3.org\/TR\/REC-html40\/loose.dtd\">\n<html><body>\n<p>At the Astronomy and Planetary Science Department, researchers are extending our understanding of orbital dynamics in the Solar System and beyond, seeking to decipher the past and understand the future or planetary systems. We dissect the implications of Newton&rsquo;s Universal Law of Gravitation to comprehend their impact on the solar system&rsquo;s structure and history, and to further out understand ing of the complex nature of orbital dynamics in general. Our research spans a broad range of subjects, including exoplanets, active asteroids, and Kuiper Belt objects, providing insights into their unique roles and behaviors.<\/p>\n<h5>Relevant faculty:<\/h5>\n<table>\n<tbody>\n<tr>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/DiegoMunoz.jpg\" alt=\"Portrait Photo of Diego Munoz\" width=\"135\">Diego Munoz<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<h5>Active research:<\/h5>\n<p><strong>Dr. Munoz<\/strong> works on diverse topics of theoretical astrophysics, using super-computing simulations and pencil-and-paper calculations. His research interests include protoplanetary disk dynamics and evolution, exoplanets, astrophysical fluid dynamics, stellar and planetary tidal interactions, theoretical orbital dynamics, super-massive black hole binaries, and exoplanets. His work also includes the development of numerical methods for compressible gas dynamics and their implementation on massively parallel astrophysical software.<br>\n<\/p><\/body><\/html>\n\n    <\/div>\n<\/div>\n\n<!-- shortcode-accordion -->\n<div class=\"shortcode-accordion shortcode-accordion--closed\" style=\"position: relative;\" >\n        <a class=\"shortcode-accordion__trigger\" data-header=\"Planetary Surface Processes_0\" href=\"#\">\n      <div class=\"shortcode-accordion__header\">\n          <h4>Planetary Surface Processes <span class=\"screen-reader-text\">Accordion Closed<\/span><\/h4>\n          <span class=\"shortcode-accordion__header__arrow\"><\/span>\n      <\/div>\n    <\/a>\n    <div class=\"shortcode-accordion__body\">\n        <!DOCTYPE html PUBLIC \"-\/\/W3C\/\/DTD HTML 4.0 Transitional\/\/EN\" \"http:\/\/www.w3.org\/TR\/REC-html40\/loose.dtd\">\n<html><body>\n<h5>Relevant faculty:<\/h5>\n<table>\n<tbody>\n<tr>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/ChristopherEdwards.jpg\" alt=\"Portrait Photo of ChristopherEdwards\" width=\"135\">Christopher Edwards<\/td>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/MarkSalvatore.jpg\" alt=\"Portrait Photo of Mark Salvatore\" width=\"135\">Mark Salvatore<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<h5>Active research:<\/h5>\n<p><!--\n\n\n<h6>Fluvial and Aeolian Geomorphology<\/h6>\n\n\nRivers leave tell-tails signs on landscapes and are important indicators of volatile flow, sediment transport, and habitability. <strong><a href=\"https:\/\/planetgeomorph.nau.edu\" target=\"_blank\" rel=\"noopener\">Dr. Burr<\/a><\/strong> studies the deposits left by ancient rivers on Mars. These deposits now form positive-relief ridges, due to erosion of the surrounding landscape by wind, and help us understand ancient Martian climate.\n\n&#091;caption id=\"attachment_2968\" align=\"aligncenter\" width=\"464\"&#093;<img loading=\"lazy\" decoding=\"async\" class=\"size-landscape-image wp-image-2968\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/Burr-ancient-river-deposits-on-Mars-464x348.jpg\" alt=\"\" width=\"464\" height=\"348\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Burr-ancient-river-deposits-on-Mars-464x348.jpg 464w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Burr-ancient-river-deposits-on-Mars-232x174.jpg 232w\" sizes=\"auto, (max-width: 464px) 100vw, 464px\" \/> Ancient river deposits on Mars.&#091;\/caption&#093;\n\n<strong><a href=\"https:\/\/planetgeomorph.nau.edu\" target=\"_blank\" rel=\"noopener\">Dr. Burr<\/a><\/strong> also studies present day rivers on Titan, the largest satellites of Saturn. At 10 times Earth's distance from the Sun, Titan has a very frigid surface, so that water exists only as ice. However, liquid nitrogen and methane --which are gases at Earth temperatures -- flow as liquid on Titan, forming both rivers and lakes.\n\n&#091;caption id=\"attachment_2969\" align=\"aligncenter\" width=\"439\"&#093;<img loading=\"lazy\" decoding=\"async\" class=\"size-landscape-image wp-image-2969\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/Burr-Rivers-into-a-northern-lake-on-Titan-439x348.jpg\" alt=\"\" width=\"439\" height=\"348\" \/> Rivers into a northern lake on Titan.&#091;\/caption&#093;\n--><\/p>\n<h6>Mars Surface Investigations<\/h6>\n<p>Both <strong>Dr. Edwards<\/strong> and <strong>Dr. Salvatore<\/strong> are Participating Scientists on the Mars Science Laboratory Curiosity rover mission, where they are active in both surface investigations and rover operations. In addition, their work focuses on understanding martian surface composition and thermophysical properties using reflectance and emission spectroscopy.<\/p>\n<figure id=\"attachment_1597\" aria-describedby=\"caption-attachment-1597\" style=\"width: 960px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1597 size-tall-banner-image\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/MarsCuriosity-IresonHill-960x384.jpg\" alt=\"MarsCuriosity-IresonHill\" width=\"960\" height=\"384\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/MarsCuriosity-IresonHill-960x384.jpg 960w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/MarsCuriosity-IresonHill-465x186.jpg 465w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/MarsCuriosity-IresonHill-1440x576.jpg 1440w\" sizes=\"auto, (max-width: 960px) 100vw, 960px\" \/><figcaption id=\"caption-attachment-1597\" class=\"wp-caption-text\">Ireson Hill, a layered sedimentary outcrop, as imaged by the Curiosity rover in Gale crater.<br>Image Credit: NASA\/JPL\/Caltech\/MSSS<\/figcaption><\/figure>\n<h6>Planetary Analogs<\/h6>\n<p><strong>Dr. Salvatore<\/strong> uses analog environments and landscapes on Earth to understand how the martian surface has evolved over geologic time. Specifically, his work in the Transantarctic Mountains has demonstrated how the martian surface has geochemically evolved even under cold and dry conditions.<\/p>\n<figure id=\"attachment_1893\" aria-describedby=\"caption-attachment-1893\" style=\"width: 628px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1893\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/PlanetarySurfaces-2.png\" alt=\"Earth-Mars surface comparison\" width=\"628\" height=\"287\"><figcaption id=\"caption-attachment-1893\" class=\"wp-caption-text\">Surfaces throughout the Transantarctic Mountains resemble those on modern Mars thanks to the prevalence of cold, dry, and stable climatic and geologic environments.<\/figcaption><\/figure>\n<\/body><\/html>\n\n    <\/div>\n<\/div>\n\n<!-- shortcode-accordion -->\n<div class=\"shortcode-accordion shortcode-accordion--closed\" style=\"position: relative;\" >\n        <a class=\"shortcode-accordion__trigger\" data-header=\"Spacecraft Missions_0\" href=\"#\">\n      <div class=\"shortcode-accordion__header\">\n          <h4>Spacecraft Missions <span class=\"screen-reader-text\">Accordion Closed<\/span><\/h4>\n          <span class=\"shortcode-accordion__header__arrow\"><\/span>\n      <\/div>\n    <\/a>\n    <div class=\"shortcode-accordion__body\">\n        <!DOCTYPE html PUBLIC \"-\/\/W3C\/\/DTD HTML 4.0 Transitional\/\/EN\" \"http:\/\/www.w3.org\/TR\/REC-html40\/loose.dtd\">\n<html><body>\n<h5>Relevant faculty:<\/h5>\n<table style=\"border-style: none;\">\n<tbody>\n<tr>\n<td style=\"text-align: center;\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/JoshuaEmery.jpg\" alt=\"Portrait Photo of Josh Emery\" width=\"135\">Josh Emery<\/td>\n<td style=\"text-align: center;\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/ChristopherEdwards.jpg\" alt=\"Portrait Photo of ChristopherEdwards\" width=\"135\">Christopher Edwards<\/td>\n<td style=\"text-align: center;\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/CristinaThomas.jpg\" alt=\"\" width=\"135\" height=\"163\">Cristina<br>\nThomas<\/td>\n<td style=\"text-align: center;\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/MarkSalvatore.jpg\" alt=\"\" width=\"135\" height=\"163\">Mark<br>\nSalvatore<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<h5>DART<\/h5>\n<p><a href=\"https:\/\/www.nasa.gov\/planetarydefense\/dart\" target=\"_blank\" rel=\"noopener noreferrer\">NASA&rsquo;s DART (Double Asteroid Redirection Test)<\/a> will impact the moon of the near-Earth binary asteroid Didymos. The mission is an important test of asteroid deflection through kinetic impact and is NASA&rsquo;s first planetary defense mission. <strong>Dr. Thomas<\/strong> leads the DART observations working group. This group focuses on using ground-based telescopes to obtain more information about the Didymos binary system and the orbit of the moon in particular. This information is critical to the mission because the observations will be used to note the change in the orbit of the asteroid moon after the impact of DART. We need to have a very firm understanding of the pre-impact orbit to understand how much we&rsquo;ve changed the orbit. The DART mission is being developed and led for NASA by the Johns Hopkins University Applied Physics Laboratory.<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"size-landscape-image wp-image-3013 aligncenter\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/Thomas-DART-464x348.jpg\" alt=\"\" width=\"464\" height=\"348\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Thomas-DART-464x348.jpg 464w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Thomas-DART-800x600.jpg 800w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Thomas-DART-232x174.jpg 232w\" sizes=\"auto, (max-width: 464px) 100vw, 464px\" \/><\/p>\n<h5>Lucy<\/h5>\n<p><strong>Dr. Emery<\/strong> leads the surface composition working group on <a href=\"http:\/\/lucy.swri.edu\/\" target=\"_blank\" rel=\"noopener noreferrer\">NASA&rsquo;s Lucy mission<\/a> to explore the Trojan asteroids. The nature and origin of the Trojan asteroids, which share Jupiter&rsquo;s orbit around the sun, remain elusive. Lucy will provide the first close-up view of this large population of primitive objects.<\/p>\n<figure id=\"attachment_3008\" aria-describedby=\"caption-attachment-3008\" style=\"width: 464px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-3008 size-landscape-image\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/Emery-lucy_trajectory.gif\" alt=\"\" width=\"464\" height=\"348\"><figcaption id=\"caption-attachment-3008\" class=\"wp-caption-text\">Animation of the trajectory of the Lucy spacecraft during its mission to the Trojans.<\/figcaption><\/figure>\n<h5>Mars Odyssey Thermal Emission Imaging System<\/h5>\n<p><strong>Drs. Edwards<\/strong> and <strong>Salvatore<\/strong> use thermal infrared imaging data from the Mars Odyssey Thermal Emission Imaging System (THEMIS) to reveal the compositional and physical properties of the martian surface. These high resolution thermal infrared data reveal key information about Mars&rsquo; volcanic, weathering and alteration processes.<\/p>\n<figure id=\"attachment_3017\" aria-describedby=\"caption-attachment-3017\" style=\"width: 464px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"size-landscape-image wp-image-3017\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/Edwards-Meridiani_4K-464x348.jpg\" alt=\"\" width=\"464\" height=\"348\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Edwards-Meridiani_4K-464x348.jpg 464w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Edwards-Meridiani_4K-800x600.jpg 800w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Edwards-Meridiani_4K-232x174.jpg 232w\" sizes=\"auto, (max-width: 464px) 100vw, 464px\" \/><figcaption id=\"caption-attachment-3017\" class=\"wp-caption-text\">False color nighttime temperature Thermal Emission Imaging System mosaic of Meridiani Planum highlighting the surface physical property differences.<\/figcaption><\/figure>\n<h5>Mars Science Laboratory<\/h5>\n<p><strong>Drs. Edwards<\/strong> and <strong>Salvatore<\/strong> use Mars Science Laboratory (Curiosity) rover data to help constrain past and present environments on Mars in unprecedented detail. In addition to helping plan the rover activities, scientific investigations include studies that link orbital data to ground truth, detailed geochemical and mineralogical comparisons as well as earth analog studies.<\/p>\n<figure id=\"attachment_3018\" aria-describedby=\"caption-attachment-3018\" style=\"width: 464px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"size-landscape-image wp-image-3018\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/Edward-PIA20316-464x348.jpg\" alt=\"\" width=\"464\" height=\"348\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Edward-PIA20316-464x348.jpg 464w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Edward-PIA20316-800x600.jpg 800w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/373\/Edward-PIA20316-232x174.jpg 232w\" sizes=\"auto, (max-width: 464px) 100vw, 464px\" \/><figcaption id=\"caption-attachment-3018\" class=\"wp-caption-text\">Mars Science Laboratory &ldquo;selfie&rdquo; taken using the Mars Hand Lens Imager (MAHLI) instrument at &ldquo;Namib Dune&rdquo; in the Bagnold dune field.<\/figcaption><\/figure>\n<h5>Near Earth Object Surveyor Mission<\/h5>\n<p><strong>Dr. Emery<\/strong> is on the investigation team of the <a href=\"https:\/\/neocam.ipac.caltech.edu\/\" target=\"_blank\" rel=\"noopener noreferrer\">NEO Surveyor Mission<\/a>, a planned thermal infrared space telescope designed to discover and characterize near-Earth objects.<\/p>\n<figure id=\"attachment_3009\" aria-describedby=\"caption-attachment-3009\" style=\"width: 464px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-3009 size-landscape-image\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/Emery-neocam-464x348.jpg\" alt=\"\" width=\"464\" height=\"348\"><figcaption id=\"caption-attachment-3009\" class=\"wp-caption-text\">The NEO Surveyor space telescope will survey the regions of space closest to the Earth&rsquo;s orbit, where potentially hazardous asteroids are most likely to be found. NEO Surveyor will use infrared light to characterize their physical properties such as their diameters. (Image credit: NASA\/JPL-Caltech)<\/figcaption><\/figure>\n<h5>OSIRIS-REx<\/h5>\n<p><strong>Drs. Emery<\/strong>, <strong>Thomas<\/strong>, and <strong>Edwards<\/strong> work on <a href=\"https:\/\/www.asteroidmission.org\/\" target=\"_blank\" rel=\"noopener noreferrer\">NASA&rsquo;s OSIRIS-REx mission<\/a> to return samples from the near-Earth asteroid Bennu. Characterizing the geology, geophysics, composition, and thermal properties of the surface with spacecraft data enables sample site selection, establishes context for laboratory analyses of returned samples, and provides the first detailed picture of the nature of small asteroids. Dr. Emery leads the thermal analysis working group, which is responsible for analysis of thermal data returned by the two spectrometers.<\/p>\n<figure id=\"attachment_3007\" aria-describedby=\"caption-attachment-3007\" style=\"width: 464px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-3007 size-landscape-image\" src=\"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-content\/uploads\/sites\/373\/\/Emery-3_Asteroid-Bennu-Rotation_SM.gif\" alt=\"\" width=\"464\" height=\"348\"><figcaption id=\"caption-attachment-3007\" class=\"wp-caption-text\">Rotation movie of NEA Bennu&rsquo;s rocky surface, as viewed by OSIRIS-REx during approach to the asteroid.<\/figcaption><\/figure>\n<\/body><\/html>\n\n    <\/div>\n<\/div>\n\n<!-- shortcode-accordion -->\n<div class=\"shortcode-accordion shortcode-accordion--closed\" style=\"position: relative;\" >\n        <a class=\"shortcode-accordion__trigger\" data-header=\"Theoretical and Computational Astrophysics_0\" href=\"#\">\n      <div class=\"shortcode-accordion__header\">\n          <h4>Theoretical and Computational Astrophysics <span class=\"screen-reader-text\">Accordion Closed<\/span><\/h4>\n          <span class=\"shortcode-accordion__header__arrow\"><\/span>\n      <\/div>\n    <\/a>\n    <div class=\"shortcode-accordion__body\">\n        <!DOCTYPE html PUBLIC \"-\/\/W3C\/\/DTD HTML 4.0 Transitional\/\/EN\" \"http:\/\/www.w3.org\/TR\/REC-html40\/loose.dtd\">\n<html><body>\n<p>Theoretical astrophysics involves formulating mathematical models and hypothesis to describe how physical processes operate in the cosmos. With the aid of the cutting-edge super-computing facility MONSOON, our work in theoretical and computational astrophysics allows us to develop and test physical theories, predict astronomical phenomena, interpret observations, simulate cosmic events and even guide future experimental design. At the Astronomy and Planetary Science Department at NAU, we implement the tools of theoretical astrophysics to model the origin and evolution of planetary systems, the interaction of planets and stars, the intricate orbits of multiple-body systems, and the gravitational coupling between super-massive black holes and their gaseous surroundings<\/p>\n<h5>Relevant faculty:<\/h5>\n<table>\n<tbody>\n<tr>\n<td style=\"text-align: center;\" width=\"20%\"><img decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/www.astro.nau.edu\/PEOPLE\/photos\/DiegoMunoz.jpg\" alt=\"Portrait Photo of Diego Munoz\" width=\"135\">Diego Munoz<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<h5>Active research:<\/h5>\n<p><strong>Dr. Munoz<\/strong> works on diverse topics of theoretical astrophysics, using super-computing simulations and pencil-and-paper calculations. His research interests include protoplanetary disk dynamics and evolution, exoplanets, astrophysical fluid dynamics, stellar and planetary tidal interactions, theoretical orbital dynamics, super-massive black hole binaries, and exoplanets. His work also includes the development of numerical methods for compressible gas dynamics and their implementation on massively parallel astrophysical software.<br>\n<\/p><\/body><\/html>\n\n    <\/div>\n<\/div>\n\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Research The Department of Astronomy and Planetary Science at NAU is home to active faculty research programs in several exciting areas in the lab, at the telescope, and participating in NASA Solar System Exploration missions. Current research projects: &nbsp;<\/p>\n","protected":false},"author":84,"featured_media":3522,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_relevanssi_hide_post":"","_relevanssi_hide_content":"","_relevanssi_pin_for_all":"","_relevanssi_pin_keywords":"","_relevanssi_unpin_keywords":"","_relevanssi_related_keywords":"","_relevanssi_related_include_ids":"","_relevanssi_related_exclude_ids":"","_relevanssi_related_no_append":"","_relevanssi_related_not_related":"","_relevanssi_related_posts":"","_relevanssi_noindex_reason":"","ring_central_script_selection":"","footnotes":""},"class_list":["post-1684","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-json\/wp\/v2\/pages\/1684","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-json\/wp\/v2\/users\/84"}],"replies":[{"embeddable":true,"href":"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-json\/wp\/v2\/comments?post=1684"}],"version-history":[{"count":65,"href":"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-json\/wp\/v2\/pages\/1684\/revisions"}],"predecessor-version":[{"id":5440,"href":"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-json\/wp\/v2\/pages\/1684\/revisions\/5440"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-json\/wp\/v2\/media\/3522"}],"wp:attachment":[{"href":"https:\/\/in.nau.edu\/department-astronomy-planetary-science\/wp-json\/wp\/v2\/media?parent=1684"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}