2025 Internship Project Overview
Black carbon (BC) exerts a strong influence on the hydrological cycle by perturbing atmospheric circulation. Yet the pathways through which BC alters precipitation remain poorly understood. Using GFDL-AM2.5 experiments, we disentangle how radiative anomalies from BC reshape static stability, humidity and circulation compared to sulfate aerosols and CO2 doubling. We find that BC-induced shortwave heating enhances upper-tropospheric stability and reduces clear-sky radiative cooling, which drives large-scale circulation changes. These circulation adjustments redistribute humidity, weakening ascent and moistening patterns that normally support precipitation while simultaneously reducing anvil cloud fraction. Our results show that precipitation changes under absorbing aerosols emerge primarily from circulation-driven humidity adjustments rather than direct thermodynamic scaling. This highlights the dominant role of circulation in mediating the hydrological impacts of BC and underscores the need to account for its distinct dynamical fingerprint when evaluating aerosol–climate interactions.
ORGANIZATION/RESEARCH GROUP
The Vecchi Research Group, Department of Geosciences, Princeton University
LOCATION
Princeton, New Jersey
Interns

Click to view the end-of-project presentation
Principal Investigator

Mentors
- Haozhe He, Postdoctoral Research Associate, High Meadows Environmental Institute


