This review paper is the first to collect and synthesise the available knowledge, across
various disciplines, on the importance of wintertime freshwater inflow from tidewater glaciers …

The sudden propagation of a major preexisting rift (full-thickness crack) in late 2016 on the
Larsen C Ice Shelf, Antarctica led to the calving of tabular iceberg A68 in July 2017, one of …

Fjords are conduits for heat and mass exchange between tidewater glaciers and the coastal
ocean, and thus regulate near‐glacier water properties and submarine melting of glaciers …

At tidewater glacier termini, ocean‐glacier interactions hinge on two sources of freshwater—
submarine melt and subglacial discharge—yet these freshwater fluxes are often …

Fjord dynamics influence oceanic heat flux to the Greenland ice sheet. Submarine iceberg
melting releases large volumes of freshwater within Greenland's fjords, yet its impact on fjord …

A wealth of research has focused on elucidating the key controls on mass loss from the
Greenland and Antarctic ice sheets in response to climate forcing, specifically in relation to …

Frontal ablation, the combination of submarine melting and iceberg calving, changes the
geometry of a glacier's terminus, influencing glacier dynamics, the fate of upwelling plumes …

The rate of ocean-driven retreat of Greenland's tidewater glaciers remains highly uncertain
in predictions of future sea level rise, in part due to poorly constrained glacier-adjacent water …

Tidewater glaciers calve icebergs into the marine environment which serve as pupping,
molting, and resting habitat for some of the largest seasonal aggregations of harbor seals …

Tidewater glaciers are an important and difficult part of the cryosphere to study owing to their
complex nature and often inaccessible and physically challenging environments. The …