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  1. ; ; ; ; ; ; ; ; ( , The Journal of Physical Chemistry C)
    Free, publicly-accessible full text available July 21, 2023
  2. ; ; ; ; ( , Findings of the Association for Computational Linguistics)
    Free, publicly-accessible full text available May 1, 2023
  3. ; ; ; ; ; ; ( , Faraday Discussions)
    Ultrafast excited state processes of transition metal complexes (TMCs) are governed by complicated interplays between electronic and nuclear dynamics, which demand a detailed understanding to achieve optimal functionalities of photoactive TMC-based materials for many applications. In this work, we investigated a cyclometalated platinum( ii ) dimer known to undergo a Pt–Pt bond contraction in the metal–metal-to-ligand-charge-transfer (MMLCT) excited state using femtosecond broadband transient absorption (fs-BBTA) spectroscopy in combination with geometry optimization and normal mode calculations. Using a sub-20 fs pump and broadband probe pulses in fs-BBTA spectroscopy, we were able to correlate the coherent vibrational wavepacket (CVWP) evolution with themore »stimulated emission (SE) dynamics of the 1 MMLCT state. The results demonstrated that the 145 cm −1 CVWP motions with the damping times of ∼0.9 ps and ∼2 ps originate from coherent Pt–Pt stretching vibrations in the singlet and triplet MMLCT states, respectively. On the basis of excited state potential energy surface calculations in our previous work, we rationalized that the CVWP transfer from the Franck–Condon (FC) state to the 3 MMLCT state was mediated by a triplet ligand-centered ( 3 LC) intermediate state through two step intersystem crossing (ISC) on a time scale shorter than a period of the Pt–Pt stretching wavepacket motions. Moreover, it was found that the CVWP motion had 110 cm −1 frequency decays with the damping time of ∼0.2 ps, matching the time constant of 0.253 ps, corresponding to a redshift in the SE feature at early times. This observation indicates that the Pt–Pt bond contraction changes the stretching frequency from 110 to 145 cm −1 and stabilizes the 1 MMLCT state relative to the 3 LC state with a ∼0.2 ps time scale. Thus, the ultrafast ISC from the 1 MMLCT to the 3 LC states occurs before the Pt–Pt bond shortening. The findings herein provide insight into understanding the impact of Pt–Pt bond contraction on the ultrafast branching of the 1 MMLCT population into the direct ( 1 MMLCT → 3 MMLCT) and indirect ISC pathways ( 1 MMLCT → 3 LC → 3 MMLCT) in the Pt( ii ) dimer. These results revealed intricate excited state electronic and nuclear motions that could steer the reaction pathways with a level of detail that has not been achieved before.« less
    Free, publicly-accessible full text available June 1, 2023
  4. ; ; ; ( , USENIX Security Symposium)
    Free, publicly-accessible full text available January 1, 2023
  5. ; ; ; ; ; ; ( , The Journal of Physical Chemistry A)
    Free, publicly-accessible full text available November 4, 2022
  6. ; ; ; ; ; ; ; ; ( , The Journal of Physical Chemistry A)
    Free, publicly-accessible full text available October 14, 2022
  7. ; ; ; ; ; ; ; ( , The Journal of Physical Chemistry Letters)
    Full Text Available 
  8. ; ; ; ( , IEEE Journal on Selected Areas in Communications)
    Full Text Available 
  9. ; ; ; ; ; ; ; ; ; ; et al ( , Nature Communications)
    Abstract Changes in the Atlantic Meridional Overturning Circulation, which have the potential to drive societally-important climate impacts, have traditionally been linked to the strength of deep water formation in the subpolar North Atlantic. Yet there is neither clear observational evidence nor agreement among models about how changes in deep water formation influence overturning. Here, we use data from a trans-basin mooring array (OSNAP—Overturning in the Subpolar North Atlantic Program) to show that winter convection during 2014–2018 in the interior basin had minimal impact on density changes in the deep western boundary currents in the subpolar basins. Contrary to previous modeling studies, wemore »find no discernable relationship between western boundary changes and subpolar overturning variability over the observational time scales. Our results require a reconsideration of the notion of deep western boundary changes representing overturning characteristics, with implications for constraining the source of overturning variability within and downstream of the subpolar region.« less
    Free, publicly-accessible full text available December 1, 2022
  10. ; ; ; ; ( , IEEE Transactions on Vehicular Technology)
    Full Text Available