Emperor Penguins thrive in harsh conditions, but a new study shows that their fate depends on human action to slow global warming and associated loss of sea ice.
A polar bear wandering on melting pack ice in Canada, north of the Arctic Circle, during the summer 2017. Scientists say the last interglacial offers lessons for future sea level rise.
Florian Ledoux/The Nature Conservancy
Antarctica is no longer the sleeping giant of sea level rise. New research delved into the past and found when the Earth warms, its ice sheets can melt extremely quickly.
Indonesian residents wade through flood water near the Ciliwung river in Jakarta in February 2018. Our emissions in the near future will lock in sea level rise over centuries.
Bill Hare, Potsdam Institute for Climate Impact Research
New research confirms that what the world pumps into the atmosphere today has grave long-term consequences. Governments - especially Australia's - must urgently ramp up efforts to reduce emissions.
Evening light on a Heard Island icescape. The island is part of the Kerguelen Plateau, which is being jointly studied by France and Australia.
Matt Curnock
New research shows that warming by more than 2°C could be a tipping point for Antarctica's ice sheets, resulting in widespread meltdown and changes to the world's shorelines for centuries to come.
Meltwater on the ice shelf near the McMurdo research station, Antarctica.
Nicholas Bayou / UNAVCO
The IPCC report says extreme sea level events that used to hit once a century will occur once a year in many places by 2050. This situation is inevitable, even if emissions are dramatically curbed.
Antarctic winds have a huge effect on weather in other places.
NASA Goddard Space Flight Center/Flickr
‘Dual use’ technology – technology used for both peaceful and military purposes – is allowed in Antarctica, according to the treaty.
Since the last ice age, the ice sheet retreated over a thousand kilometres in the Ross Sea region, more than any other region on the continent.
Rich Jones
Dan Lowry, Te Herenga Waka — Victoria University of Wellington
New research shows that ocean and air temperatures both contributed to the melting of Antarctica's Ross Ice Shelf in the past, but melting from below by a warming ocean became more important over time.
A wild leopard seal on South Georgia.
James Robbins
Jennifer Walsh, National Oceanic and Atmospheric Administration
Sending autonomous vehicles to the Southern Ocean can be fraught with anxiety, especially if one of them doesn't make radio contact when it's supposed to.
Scientists measured the thickness and basal melt of the Ross Ice Shelf.
Supplied
Emperor penguins have a few hidden tricks to stay warm, like blood vessels in the nose arranged so they can regain most of the heat that would be lost by breathing.
A small boat in the Illulissat Icefjord is dwarfed by the icebergs that have calved from the floating tongue of Greenland’s largest glacier, Jacobshavn Isbrae.
Michael Bamber
A paleooceanographer describes her ninth sea expedition, this time retrieving cylindrical 'cores' of the sediment and rock that's as much as two miles down at the ocean floor.
The Casey Station is part of Australia’s permanent outpost in Antarctica.
Shaun Brooks
Nick Golledge, Te Herenga Waka — Victoria University of Wellington
Climate scientist predict that the combined effect of ice loss in Greenland and Antarctica will be more extreme weather, with impacts on agriculture, infrastructure and human life itself.
Sea ice responds to changes in winds and ocean currents, sometimes with origins thousands of kilometres away.
NASA/Nathan Kurtz
Antarctic sea ice cover fell to an all-time low recently and hasn't yet recovered. Why? The initial answers could lie in an unlikely place – the tropics.
The Antarctic Circumpolar Current keeps Antarctica cold.
Shutterstock
The Antarctic Circumpolar Current provides a barrier to heat that keeps warm subtropical waters away from Antarctica. Yet, there are a few places where the heat gets through.
Professor of Earth Science and Climate Change, Director of PANGEA Research Centre, Director of Chronos 14Carbon-Cycle Facility, and UNSW Director of ARC Centre for Excellence in Australian Biodiversity and Heritage, UNSW