Member Since 2014
Manar Al Asad
Student, Brown University
Professional Experience
Brown University
Student
2021 - Present
University of California Berkeley
Student
2021 - 2021
University of British Columbia
Research Scientist
2016 - 2020
University of British Columbia
Student
2009 - 2014
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Education
University of British Columbia
Bachelors
2014
Honors & Awards
Study of the Earth's Deep Interior Section Award for Graduate Research
Received December 2024
Publications
Boulder Diversity in the Nightingale Region of Asteroid (101955) Bennu and Predictions for Physical ...
The sample of asteroid (101955) Bennu was collected from the Nightingale sample site by the Origins, Spectral Interpretation, Resource Identificati...
December 06, 2023
Modes of Mantle Convection, Their Stability, and What Contro...
October 03, 2023
The Formation of Terraces on Asteroid (101955) Bennu
April 09, 2022
Bifurcated Current Sheets in Mercury's Magnetotail: Observat...
November 09, 2021
Global Patterns of Recent Mass Movement on Asteroid (101955)...
September 10, 2020
AGU Abstracts
The Co-Evolution of a Planet’s Water Budget and its Tectonic Regime
AGU 2024
study of earth's deep interior | 12 december 2024
Manar Al Asad, Harriet C. Lau, Greg Hirth
The viscosity structure of the mantle plays an important in a planets tectonic regime. In particular, Al Asad & Lau (2024)[1] found that asthenosp...
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Investigating the heterogeneity of asteroid Bennu’s parent body by linking micro- and macro-scale
EXPLORING ROCKY BODY EVOLUTION IN THE SOLAR SYSTEM AND BEYOND II ORAL
study of earth's deep interior | 15 december 2023
Erica R. Jawin, Tim McCoy, Lisette Melendez, Cathe...
The sample of near-Earth asteroid (101955) Bennu, collected by the NASA OSIRIS-REx mission, will arrive on Earth in late September, 2023. As Bennu is ...
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Sudden vs. Gradual Transitions in Earth’s Convective Regime
EXPLORING EARTH’S EVOLUTION: THE HADEAN THROUGH THE PRESENT II ORAL
study of earth's deep interior | 14 december 2023
Manar Al Asad, Harriet C. Lau
In the canonical view of convection, the style of mantle convection may be fully determined with knowledge of two physical parameters, usually the int...
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