LIFE SCIENCES

Daniele Canzio, PhD, University of California, San Francisco (Neuroscience)

Kaiyu Guan, University of Illinois Urbana-Champaign (Agriculture & Animal Sciences)

Philip J. Kranzusch, PhD, Dana-Farber Cancer Institute; Harvard Medical School (Microbiology)

Elizabeth Nance, PhD, University of Washington (Biomedical Engineering & Biotechnology)

Tomasz Nowakowski, PhD, University of California, San Francisco (Neuroscience)

Samuel H. Sternberg, PhD, Columbia University/Howard Hughes Medical Institute (Molecular & Cellular Biology)

CHEMICAL SCIENCES

Song Lin, PhD, Cornell University (Organic Chemistry)

Joseph Cotruvo, Jr., PhD, The Pennsylvania State University (Biochemistry & Structural Biology)

Frank Leibfarth, PhD, The University of North Carolina at Chapel Hill (Polymer Chemistry)

Ryan Lively, PhD, Georgia Institute of Technology (Chemical Engineering)

Leslie M. Schoop, PhD, Princeton University (Inorganic & Solid-State Chemistry)

Yogesh Surendranath, PhD, Massachusetts Institute of Technology (Inorganic & Solid-State Chemistry)

PHYSICAL SCIENCES & ENGINEERING

Charlie Conroy, PhD, Harvard University (Astrophysics & Cosmology)

Nathaniel Craig, PhD, University of California, Santa Barbara (Theoretical Physics)

Matthew McDowell, PhD, Georgia Institute of Technology (Materials Science & Nanotechnology)

Prateek Mittal, PhD, Princeton University (Computer Science)

Elaina J. Sutley, PhD, University of Kansas (Civil Engineering)

Zhongwen Zhan, PhD, California Institute of Technology (Physical Earth Sciences)

Precipitation δ¹⁸O provides important insights into the decadal variability of the East Asian monsoon. Using both isotope-enabled climate simulations and reconstructions, this study found a quasi-11-year cycle in precipitation δ¹⁸O (δ¹⁸O_p) across the monsoon region. The cycle was driven by enhanced solar activity, which strengthens the Walker circulation and increases moisture transport from the equatorial Pacific. The results have suggested that the quasi-11-year δ18O_p cycle primarily reflects shifts in moisture sources driven by solar activity. The findings were recently published in SCIENCE CHINA Earth Sciences.