2025 Internship Project Overview
Arctic amplification (AA), the amplified surface temperature response in the Arctic relative to the global average, emerges under both CO2 increase and removal. Here, we investigate AA in a collection of CESM1 simulations subjected to various instantaneous CO2 increases (2x, 3x, 4x, 5x, 6x, 7x, 8x CO2) and, subsequently, instantaneous CO2 removal back to preindustrial levels. We find that AA is weaker following CO2 removal (cooling) compared to CO2 increase (warming). A feedback decomposition using radiative kernels reveals that the weaker AA during CO2 removal is primarily driven by changes in the albedo feedback, lapse rate, cloud feedbacks and atmospheric heat transport. Notably, our results contrast with previous findings showing stronger AA when CO2 is decreased below pre-industrial values. Together, these results indicate a state-dependent AA response to CO2 removal: AA is weaker when returning to preindustrial values but stronger when CO2 falls below preindustrial values. This state dependence suggests the potential for a delayed cooling response in the Arctic should CO2 removal occur in the current or future warmer climate.
ORGANIZATION/RESEARCH GROUP
The Vecchi Research Group, Department of Geosciences, Princeton University
LOCATION
Princeton, New Jersey
Interns

Minor(s): Engineering Physics, Robotics
Click to view the end-of-project presentation
Principal Investigator

Mentors
- Ivan Mitevski, Postdoctoral Research Associate, Geosciences

