The ␣-helical antifreeze protein (AFP) from winter flounder inhibits ice growth by binding to a specific set of pyramidal surface planes that are not otherwise macroscopically expressed. The 37-residue AFP contains three 11-amino acid repeats that make a stereo-specific fit to the ice lattice along the ͗01-12͘ direction of the {20 -21} and equivalent binding planes. When the AFP was shortened to delete two of the three 11-amino acid ice-binding repeats, the resulting 15-residue peptide and its variants were less helical and showed no antifreeze activity. However, when the helicity of the peptide was reinforced by an internal lactam bridge between Glu-7 and Lys-11, the minimized AFP was able to stably express the pyramidal plane {20 -21} on the surface of growing ice crystals. This dynamic shaping of the ice surface by a single ice-binding repeat provides evidence that AFP adsorption to the ice lattice is not an "all-or-nothing" interaction. Instead, a partial interaction can help develop the binding site on ice to which the remainder of the AFP (or other AFP molecules) can orient and bind.Type I AFP 1 from winter flounder, represented by the abundant serum isoform HPLC-6 (1) is a remarkably long freestanding ␣-helix (2). Its helicity can be attributed to several structural features, which include an abundance of alanine, an extensive capping network at both termini (3), and an internal salt bridge (1, 4). From ice etching studies, it was shown that this AFP binds to the {20 -21} hexagonal bipyramidal planes of ice along the ͗01-12͘ direction (5). It has been suggested that the critical connection between structure and function in this protein is that putative ice-binding residues (Thr, Asx, and Leu) are aligned and regularly spaced along one face of the helix (5, 6). Each residue (e.g. Thr-2, Thr-13, Thr-24, and Thr-35) is spaced 11 amino acids apart (16.5 Å), which closely matches the 16.7-Å distance between repeating features of the ridge and valley topology along the ͗01-12͘ direction of the {20 -12} binding plane. Adsorption of type I AFP to these lattice binding sites through a precise distance and geometry match involving H-bonding and van der Waals interactions (5, 7) leads to inhibition of ice growth by the Kelvin effect (8, 9). In the process, seed ice crystals are constrained to form hexagonal bipyramids with a c:a axial ratio of 3.3:1, which matches the ratio predicted from the adsorption planes revealed by ice etching studies (5, 6).Several attempts have been made to model the helix in contact with the ice surface (3, 7, 10, 11). As a result, a common concern is that the number and strength of the potential interactions between ice and AFP are barely sufficient for tight binding (3, 7). One solution proposed is that all four ice-binding threonines share the same rotamer configuration and bind to ice in a "zipper-like fashion" (11). A similar hypothesis, stemming directly from the x-ray structure, is that tight binding relies on the simultaneous docking of similarly aligned and constrained ice-binding...