Sarah Dodson-Robinson | |
---|---|
Born | |
Alma mater | Rochester Institute of Technology University of California, Santa Cruz |
Known for | Astrophysics |
Awards | NSF GRFP Spitzer Fellowship ContentsNSF CAREER Award |
Scientific career | |
Thesis | Chemistry of planet formation (2008) |
Doctoral advisor | Gregory P Laughlin |
Sarah Dodson-Robinson is an American astronomer known for her work on planet formation and an associate professor of physics and astronomy at the University of Delaware. [1]
She was born in Los Angeles, California. She goes by the name “Sally.” Dodson-Robinson always had an interest for Space Science. When she was 7 or 8 years old, she joined The Planetary Society and collected the mini-posters of planets and moons that came with the magazine. [2]
Dodson-Robinson was inspired to become an astronomer by Stephen Hawking. She was later further influenced by her undergraduate and graduate advisors, Elliott Horch and Greg Laughlin, respectively. [2]
In 2002, Dodson-Robinson received her B.S. at Rochester Institute of Technology. She then began graduate study at the University of California, Santa Cruz. There, she received her M.S. in 2005 and her Ph.D. in Astronomy and Astrophysics in June of 2008. [1] [2]
Dodson-Robinson research focuses on planet formation and planetary archaeology and also includes more traditional astronomy topics such as protostellar disk chemistry, galactic chemical evolution, and brown dwarfs. [3] With the use of analytical theory and numerical simulations of the dynamical and chemical environment of planet growth, she is able to uncover the formation histories of exoplanets and solar system objects.
Dodson-Robinson joined the University of Texas as an assistant professor in 2009. [2] [3] In Spring 2014, Dodson-Robinson began work at The University of Delaware.
In 2021, Dodson-Robinson authored the textbook Origins of Giant Planets, Volume 1: Disks, dust, and planetesimals. [4]
Dodson-Robinson has received multiple honors and awards for her work and research. As a graduate student in 2002, she was awarded the National Science Foundation Graduate Research Fellowship. [5] She received the Spitzer Fellowship in 2008 and took leave from the University of Texas to use it for work at the NASA Exoplanet Science Institute. [2] [5]
While at the University of Texas, she was honored as a Charter Member into the Society for Teaching Excellence. In 2013, she received the Annie Jump Cannon Award in Astronomy from the American Astronomical Society for her work on the formation of planetary systems. [6] That year she was also awarded a National Science Foundation’s CAREER Award for her work, titled “Giant Planets in Dusty Disks.” [7]
Planetesimals are solid objects thought to exist in protoplanetary disks and debris disks. Believed to have formed in the Solar System about 4.6 billion years ago, they aid study of its formation.
The nebular hypothesis is the most widely accepted model in the field of cosmogony to explain the formation and evolution of the Solar System. It suggests the Solar System is formed from gas and dust orbiting the Sun which clumped up together to form the planets. The theory was developed by Immanuel Kant and published in his Universal Natural History and Theory of the Heavens (1755) and then modified in 1796 by Pierre Laplace. Originally applied to the Solar System, the process of planetary system formation is now thought to be at work throughout the universe. The widely accepted modern variant of the nebular theory is the solar nebular disk model (SNDM) or solar nebular model. It offered explanations for a variety of properties of the Solar System, including the nearly circular and coplanar orbits of the planets, and their motion in the same direction as the Sun's rotation. Some elements of the original nebular theory are echoed in modern theories of planetary formation, but most elements have been superseded.
A protoplanetary disk is a rotating circumstellar disc of dense gas and dust surrounding a young newly formed star, a T Tauri star, or Herbig Ae/Be star. The protoplanetary disk may also be considered an accretion disk for the star itself, because gases or other material may be falling from the inner edge of the disk onto the surface of the star. This process should not be confused with the accretion process thought to build up the planets themselves. Externally illuminated photo-evaporating protoplanetary disks are called proplyds.
A protoplanet is a large planetary embryo that originated within a protoplanetary disk and has undergone internal melting to produce a differentiated interior. Protoplanets are thought to form out of kilometer-sized planetesimals that gravitationally perturb each other's orbits and collide, gradually coalescing into the dominant planets.
David Clifford Jewitt is a British-American astronomer who studies the Solar System, especially its minor bodies. He is based at the University of California, Los Angeles, where he is a Member of the Institute for Geophysics and Planetary Physics, the Director of the Institute for Planets and Exoplanets, Professor of Astronomy in the Department of Physics and Astronomy and Professor of Astronomy in the Department of Earth, Planetary and Space Sciences. He is best known for being the first person to discover a body beyond Pluto and Charon in the Kuiper belt.
Planetary migration occurs when a planet or other body in orbit around a star interacts with a disk of gas or planetesimals, resulting in the alteration of its orbital parameters, especially its semi-major axis. Planetary migration is the most likely explanation for hot Jupiters. The generally accepted theory of planet formation from a protoplanetary disk predicts that such planets cannot form so close to their stars, as there is insufficient mass at such small radii and the temperature is too high to allow the formation of rocky or icy planetesimals.
In astrophysics, accretion is the accumulation of particles into a massive object by gravitationally attracting more matter, typically gaseous matter, into an accretion disk. Most astronomical objects, such as galaxies, stars, and planets, are formed by accretion processes.
An ice giant is a giant planet composed mainly of elements heavier than hydrogen and helium, such as oxygen, carbon, nitrogen, and sulfur. There are two ice giants in the Solar System: Uranus and Neptune.
In astronomy or planetary science, the frost line, also known as the snow line or ice line, is the minimum distance from the central protostar of a solar nebula where the temperature is low enough for volatile compounds such as water, ammonia, methane, carbon dioxide and carbon monoxide to condense into solid grains, which will allow their accretion into planetesimals. Beyond the line, otherwise gaseous compounds can be quite easily condensed to allow formation of gas and ice giants; while within it, only heavier compounds can be accreted to form the typically much smaller rocky planets.
Ray Jayawardhana is the Provost of Johns Hopkins University and a Professor of Physics and Astronomy. Until October 2023, Jayawardhana was the Harold Tanner Dean of the Cornell University College of Arts and Sciences and a Professor of Astronomy at Cornell University, effective September 1, 2018. He was formerly Dean of Science and a Professor of physics & astronomy at York University. Prior to that, he was a Professor of Astronomy & Astrophysics at the University of Toronto, and an Assistant Professor of Astronomy at the University of Michigan. In July 2023, Johns Hopkins University announced that Jayawardhana had been selected as its 16th provost. His primary research areas include the formation and early evolution of stars, brown dwarfs and planets. His current research focuses on characterizing exoplanets using telescopes on the ground and in space.
A debris disk, or debris disc, is a circumstellar disk of dust and debris in orbit around a star. Sometimes these disks contain prominent rings, as seen in the image of Fomalhaut on the right. Debris disks are found around stars with mature planetary systems, including at least one debris disk in orbit around an evolved neutron star. Debris disks can also be produced and maintained as the remnants of collisions between planetesimals, otherwise known as asteroids and comets.
The five-planet Nice model is a numerical model of the early Solar System that is a revised variation of the Nice model. It begins with five giant planets, the four that exist today plus an additional ice giant between Saturn and Uranus in a chain of mean-motion resonances.
Pebble accretion is the accumulation of particles, ranging from centimeters up to meters in diameter, into planetesimals in a protoplanetary disk that is enhanced by aerodynamic drag from the gas present in the disk. This drag reduces the relative velocity of pebbles as they pass by larger bodies, preventing some from escaping the body's gravity. These pebbles are then accreted by the body after spiraling or settling toward its surface. This process increases the cross section over which the large bodies can accrete material, accelerating their growth. The rapid growth of the planetesimals via pebble accretion allows for the formation of giant planet cores in the outer Solar System before the dispersal of the gas disk. A reduction in the size of pebbles as they lose water ice after crossing the ice line and a declining density of gas with distance from the sun slow the rates of pebble accretion in the inner Solar System resulting in smaller terrestrial planets, a small mass of Mars and a low mass asteroid belt.
Elisa Victoria Quintana is a scientist working in the field of astronomy and planetary science at NASA Goddard Space Flight Center. Her research focuses the detection and characterization of exoplanets in addition to studying how they form. She is best known for the detection of Kepler 186f, the first Earth-sized planet found in the habitable zone of a star other than the Sun.
Heather A. Knutson is an astrophysicist and professor at California Institute of Technology in the Division of Geological and Planetary Sciences. Her research is focused on the study of exoplanets, their composition and formation. She won the American Astronomical Society's Newton Lacy Pierce Prize in Astronomy for her work in exoplanetary atmospheres.
Sarah T. Stewart-Mukhopadhyay is an American planetary scientist known for studying planet formation, planetary geology, and materials science. She is a professor at the University of California, Davis in the Earth and Planetary Sciences Department. She was a professor at Harvard University Department of Earth and Planetary Sciences from 2003 to 2014.
Anne-Marie Lagrange, born March 12, 1962 in the Rhône-Alpes region of France, is a French astrophysicist. Lagrange's work focuses on the research and study of extrasolar planetary systems. Lagrange is the holder of numerous scientific awards and honorary decorations, including Knight of the Legion of Honour and is a member of the French Academy of Sciences since 2013.
Elizabeth J. Tasker is a British astrophysicist and science writer.
Lynnae C. Quick is an American planetary geophysicist and Ocean Worlds Planetary Scientist at NASA Goddard Space Flight Center. Her research centers on theoretical modeling of cryovolcanic processes on the icy moons and dwarf planets in the Solar System as well as modeling volcanic activity on Venus and the Moon. Quick is a member of the Dawn, Europa Clipper, and Dragonfly Mission science teams. She is also a member of the NASA Solar System Exploration Research Virtual Institute (SSERVI) Toolbox for Research and Exploration (TREX) team, and serves as co-chair of the Earth and Planetary Systems Sciences section of the National Society of Black Physicists.
Paola Andrea Pinilla Ortiz is a Colombian astrophysicist whose research concerns the accretion of interplanetary dust clouds into protoplanetary disks as part of the formation of exoplanets. Educated in Colombia and Germany, she works in England as associate professor in exoplanets at the University College London Department of Space & Climate Physics, affiliated with the university's Mullard Space Science Laboratory.