Small water clusters absorb heat and catalyze pivotal
atmospheric
reactions. Yet, experiments produced conflicting results on water
cluster distribution under atmospheric conditions. Additionally, it
is unclear which “phase transitions” such clusters exhibit,
at what temperatures, and what are their underlying molecular mechanisms.
We find that logarithmically small tails in the radial probability
densities of (H2O)n clusters
(n = 2 – 6) provide direct testimony for such
transitions. Using the best available water potential (MB-pol), an
advanced thermostating algorithm (g-BAOAB), and sufficiently
long trajectories, we map the “bifurcation”, “melting”,
and (hitherto unexplored) “vaporization” transitions,
finding that both melting and vaporization proceed via a “monomer
on a ring” conformer, exhibiting huge distance fluctuations
at the vaporization temperatures (Tv). Tv may play a role in determining the atmospheric
cluster size distribution such that the dimer and tetramer, with their
exceptionally low/high Tv values, are
under/over-represented in these distributions, as indeed observed
in nondestructive mass spectrometric measurements.