Understanding deeply supercooled water is key to unraveling many of water's anomalous properties. However, developing this understanding has proven difficult due to rapid and uncontrolled crystallization. Using a pulsed-laser-heating technique, we measure the growth rate of crystalline ice, G(T), for 180 K < T < 262 K, that is, deep within water's "no man's land" in ultrahigh-vacuum conditions. Isothermal measurements of G(T) are also made for 126 K ≤ T ≤ 151 K. The self-diffusion of supercooled liquid water, D(T), is obtained from G(T) using the Wilson-Frenkel model of crystal growth. For T > 237 K and P ∼ 10 −8 Pa, G(T) and D(T) have super-Arrhenius ("fragile") temperature dependences, but both cross over to Arrhenius ("strong") behavior with a large activation energy in no man's land. The fact that G(T) and D(T) are smoothly varying rules out the hypothesis that liquid water's properties have a singularity at or near 228 K at ambient pressures. However, the results are consistent with a previous prediction for D(T) that assumed no thermodynamic transitions occur in no man's land.ater is not a typical liquid, and its unusual properties have been discussed by many authors (1-13). Anomalies are observed in thermodynamic response functions (such as the isobaric heat capacity and the isothermal compressibility) and dynamic properties (such as diffusion, viscosity, and dielectric relaxation) over a wide range of pressures, P, and temperatures, T. These anomalies become more pronounced for supercooled water, and it is generally believed that the unusual properties arise as water adopts a more ice-like structure as the temperature decreases. However, the underlying reasons are fiercely debated (5,11,(14)(15)(16)(17). At ambient pressures, many of the anomalous properties appear to diverge at a temperature, T s , around 228 K leading to the "stability-limit conjecture" in which the liquid becomes unstable below T s (2). Several other models have been proposed to explain the thermodynamic anomalies including the liquid-liquid critical point model (3), the critical-point free scenario (18), and the singularity-free hypothesis (19). However, it is noteworthy that both thermodynamic and dynamic properties apparently diverge at ∼T s (1, 2). To explain the similarities in the thermodynamics and dynamics, Adam-Gibbs theory is attractive because it connects changes in the entropy of a liquid to its dynamics (20). Using this theory, Starr et al. (6) predicted that the self-diffusion of water, D(T), undergoes a dynamic crossover from super-Arrhenius to Arrhenius behavior (often called a "fragile-to-strong" transition) at temperatures just below the homogeneous nucleation temperature, T H , at ∼235 K. However, purely dynamical explanations have also been proposed (5,21).Differentiating between various theories has proven difficult because the onset of rapid crystallization at T H has prevented experiments below this point (5, 22). Another approach involves heating low-density amorphous (LDA) ice above its glass transition tempe...