Hi! I'm Haleigh and I build island worlds like this one to see if they could host an origin of life.

NSF Graduate Research Fellow · Zonta Amelia Earhart Fellow

Haleigh Nyberg

PhD Candidate · Computational Astrobiology · Purdue

Hi! I'm Haleigh and I build island worlds like this one to see if they could host an origin of life.

NSF Graduate Research Fellow working with Dr. Stephanie Olson. I run ExoPlaSim simulations across obliquity, rotation rate, and stellar type to track wet-dry cycling in warm little ponds (conditions thought to let RNA precursors accumulate).

About

Haleigh Nyberg

Liquid water is the usual test for habitability. It tells you a planet could keep life alive, not that life could ever have started there. That second question is what my doctoral work is for: which planetary conditions actually favor an origin of life, and how to inform target prioritization for direct-imaging missions like NASA's Habitable Worlds Observatory.

In Dr. Stephanie Olson's PHAB Lab at Purdue, I use ExoPlaSim and a custom post-processing pipeline to simulate volcanic island worlds across obliquity, rotation rate, and stellar host, tracking the wet-dry cycling and prebiotic-organic accumulation that this route to an origin of life depends on. The deliverable is an Origin of Life Index, ranking exoplanet targets by their potential for wet-dry cycling, one of the leading proposed routes to an origin of life, rather than by whether they could merely sustain it.

  • NSF Graduate Research Fellow
  • Zonta Amelia Earhart Fellow
  • Ross Fellowship
  • Summa Cum Laude
  • NASA Space Grant (INSGC)
  • AGU Invited Speaker (2025)
  • Session Co-convener, Goldschmidt 2025 and 2026
Gateway visualization team - Spring 2025 cohort at Purdue
Artemis Gateway visualization team at the Purdue Data Mine, Spring 2025 (with Barrios Technology & NASA Johnson)
Haleigh beside an ISS module mockup and mission-patch wall at NASA's Johnson Space Center in Houston
ISS module mockup & mission-patch wall, NASA Johnson Space Center (Houston)
Haleigh presenting at AGU 2025
AGU 2025: "Planetary Obliquity and Origin of Life Potential" (invited)
Haleigh presenting the PALLAS poster at AGU 2025
PALLAS poster at AGU 2025
Haleigh presenting the PALLAS poster at AbSciCon 2026
PALLAS poster at AbSciCon 2026

As an NSF Graduate Research Fellow, I have served as Executive Secretary on NASA review panels for Habitable Worlds and the Exoplanets Research Program, I peer-review for the Planetary Science Journal, and I coach incoming GRFP applicants through Purdue's OGSPS fellowships office after winning my own.

Selected Projects

Research

Computational Astrobiology · ExoPlaSim

Habitability asks whether a planet could keep life alive. I ask the prior question: could life have started there in the first place? I run ExoPlaSim (a 3D general circulation model) across a parameter space of obliquity, rotation rate, star type, and surface configuration to figure out which planets allow wet-dry cycling in warm little ponds. The pond model then tracks whether precipitation, evaporation, and haze deposition let RNA precursors actually accumulate.

Chapter 1 (in prep for PNAS): where a planet cycles wet and dry follows where its star puts the light — and high obliquity opens that cycling up across the whole globe. Whether the organics survive is a separate fight: haze has to deliver them, and the ponds have to hold them through the wet phase.

Warm little pond in wet phase: rain, HCN aqueous chemistry, meteorite delivery, seepage
Wet phase (precipitation delivers organics)
Warm little pond in dry phase: UV photolysis, evaporative concentration
Dry phase (UV drives polymerization)
Dissertation overview: C1 Obliquity, C2 Rotation, C3 Host Star
Fig. 1: Dissertation overview of obliquity, rotation, and host star effects on wet-dry cycling
Hadley cell circulation and wet-dry zone distribution across latitudes for 24hr modern Earth rotation
Fig. 2: Atmospheric circulation drives precipitation patterns that control pond wet-dry cycling
Two surface-temperature maps of the same Earth-like world: a 0-degree-tilt planet warm in an equatorial band, a 90-degree-tilt planet warm at its summer pole
Axial tilt rewrites a planet's climate. Two ExoPlaSim runs of the same Earth-like world (no tilt on the left, a steep 90° tilt on the right, at northern summer). A flat planet warms in a band at the equator, but a tilted one turns its summer pole into the hottest place on the map, and that seasonal swing is what drives warm little ponds to fill and dry.

The island you see here is what I simulate (a volcanic hotspot where sea-land breeze circulation drives evaporation and precipitation through warm little ponds).

Full CV (PDF) · Google Scholar · ORCID · Olson Lab →

Supported by the National Science Foundation Graduate Research Fellowship Program under Grant No. DGE-2444108.

Resume / CV

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