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)
Tipping Thresholds (Oregon State U Press Release, One Earth Paper & Guardian article):
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