Ice Sheet Dynamics (Nature Editorial & 4 Studies):

Ice sheets big & small

Oligocene deep ocean oxygen isotope variations primarily driven by temperature

Spatially variable response of Antarctica’s ice sheets to orbital forcing during the Pliocene (Paywall)

Synchronous bipolar retreat of mid-latitude ice masses during Heinrich Stadials (Paywall)

Deglaciation of the Prudhoe Dome in northwestern Greenland in response to Holocene warming (Paywall)