Geomorphological map** is a well-established method for examining earth surface
processes and landscape evolution in a range of environmental contexts. In glacial …

We synthesize the current understanding of glacier activity on Svalbard from the end of the
Late Pleistocene (12,000 yrs. before present) to the end of the Little Ice Age (c. 1920 AD) …

Rates of ice mass loss at the calving margins of tidewater glaciers (frontal ablation rates) are
a key uncertainty in sea level rise projections. Measurements are difficult because mass lost …

Consistent and continuous data on glacier surface velocity are important inputs to time
series analyses, numerical ice dynamic modelling and glacier mass flux computations …

Glacimarine processes affect about 20% of the global ocean today, and this area expanded
considerably under cyclical full-glacial conditions during the Quaternary (Fig. 1)(Dowdeswell …

It is commonly asserted that there are two distinct classes of glacier surges: slow, long-
duration 'Svalbard-type'surges, triggered by a transition from cold-to warm-based conditions …

Identifying glaciers that exhibit surge-type behavior is important when using evidence of ice
front fluctuations as a proxy for reconstructing past climate oscillations. This study identifies …

Switches between cold‐and warm‐based conditions have long been invoked to explain
surges of High Arctic glaciers. Here we compile existing and new data on the thermal regime …

We present a highly detailed study of calving dynamics at Tunabreen, a tidewater glacier in
Svalbard. A time-lapse camera was trained on the terminus and programmed to capture …

Fjord-terminating glaciers in Svalbard lose mass through submarine melt and calving
(collectively: frontal ablation), and surface melt. With the recently observed Atlantification of …