Climate change: 70% of king penguins could ‘abruptly relocate or disappear’ by 2100
The arduous journey that king penguins must make in order to hunt fish to bring back to their young could become even longer as the climate warms, research suggests.
The study finds that future ocean warming in Antarctica could drive the penguins’ primary hunting grounds further poleward – away from their favoured breeding spots.
If little is done to tackle climate change, up to 70% of king penguins could be forced to find new places to breed by 2100, the lead authors tell Carbon Brief.
However, if these animals cannot find anywhere suitable to move to, they could be at risk of “disappearing” by the end of the century, the authors add.
§ Penguin pilgrimage
King penguins are well attuned to life in harsh Antarctic conditions. Breeding pairs raise their chicks on sub-Antarctic islands, including the Falklands and the Crozet Islands. In these spots, temperatures stay above freezing and predators, such as leopard seals, are kept at bay.
However, to find food for their chicks, adult penguins must venture to an ocean boundary known as the Antarctic Polar Front, where cold Antarctic waters meet and sink beneath warmer waters from mid-latitude regions. In these less frigid waters, a number of Antarctic fish species gather in large numbers.
A typical journey to this ocean boundary, which is currently situated in between the penguins’ most northern and southern breeding islands, takes seven to ten days and stretches over 300-500km.
However, future ocean warming could drive the Antarctic Polar Front to move polewards – further away from penguin breeding sites, according to Dr Robin Cristofari from the University of Turku, Finland, Dr Celine Le Bohec from the National Scientific Research Centre in France and Dr Emiliano Trucchi from the University of Ferrara, Italy, who jointly led the study published in Nature Climate Change.
If climate change continues unabated, the journey to find food could become impossible from some breeding islands, they tell Carbon Brief in a joint interview:
“The Antarctic Polar Front is moving poleward as temperatures increase due to climate change.”
Adult king penguin (Aptenodytes patagonicus) and chick Salisbury Plain South Georgia. Credit: Renato Granieri/Alamy Stock Photo.
§ Crumbling kingdom
RCP2.6: The RCPs (Representative Concentration Pathways) are scenarios of future concentrations of greenhouse gases and other forcings. RCP2.6 (also sometimes referred to as “RCP3-PD”) is a “peak and decline” scenario where stringent mitigation and carbon dioxide removal technologies mean atmospheric CO2 concentration peaks and then falls during this century. By 2100, CO2 levels increase to around 420ppm – around 20ppm above current levels – equivalent to 475ppm once other forcings are included (in CO2e). By 2100, global temperatures are likely to rise by 1.3-1.9C above pre-industrial levels.
For the study, the researchers used a set of global climate models to simulate changes to future sea temperatures and, therefore, the potential foraging distance from each penguin breeding island.
The models used three different future scenarios of greenhouse gas emissions, ranging from a scenario where global warming is limited to 2C above pre-industrial levels (RCP2.6) to a “business as usual” scenario where future climate change continues to rise unchecked (RCP8.5).
Based on their research, the scientists determined that 700km was the maximum distance that penguins could travel to hunt fish.
The maps below show the location of the penguins’ breeding islands (numbered) and the foraging area (dashed red line) during 1981-2005 (left) and under a future high emissions scenario in 2100 (right). The shaded blue areas show the extent of Antarctic sea ice.
RCP8.5: The RCPs (Representative Concentration Pathways) are scenarios of future concentrations of greenhouse gases and other forcings. RCP8.5 is a “very high baseline” emission scenario brought about by rapid population growth, high energy demand, fossil fuel dominance and an absence of climate change policies. This scenario is the highest of the RCPs and sees atmospheric CO2 rise to around 935ppm by 2100, equivalent to 1,370ppm once other forcings are included (in CO2e). The likely range of global temperatures by 2100 for RCP8.5 is 4.0-6.1C above pre-industrial levels. The release of the Shared Socioeconomic Pathways (SSPs) has introduced a number of additional “no-new-policy” scenarios, meaning RCP8.5 is no longer the sole option available to researchers as a high-end no-mitigation pathway.
For each island, orange shows the presence of a breeding colony; grey indicates that the island is too far away from a foraging site; white shows that the island that has never been occupied by penguins and blue shows that the island is covered in ice and, therefore, too cold for penguins to establish a breeding colony.
The islands on the charts are: (1) Tierra del Fuego, (2) Falklands, (3) South Georgia, (4) South Sandwich, (5) Gough, (6) Bouvet, (7) Marion and Prince Edward, (8) Crozet, (9) Kerguelen, (10) Heard and McDonald, (11) Amsterdam, (12) Macquarie, (13) Auckland, (14) Campbell and (15) Chatham.
The location of the penguins’ breeding islands (numbered and coloured; see text above) and foraging area (dashed-red line) in a historical period from 1981-2005 to a future high emissions scenario in 2100. Shaded blue shows the extent of Antarctic sea ice. Source: Cristofari et al. (2018)
The right-hand map shows that the foraging area is expected to move out of reach of some islands by 2100, including Tierra del Fuego, the Falklands, Marion and Prince Edward and Crozet.
RCP4.5: The RCPs (Representative Concentration Pathways) are scenarios of future concentrations of greenhouse gases and other forcings. RCP4.5 is a “stabilisation scenario” where policies are put in place so atmospheric CO2 concentration levels off around the middle of the century, though temperatures do not stabilise before 2100. These policies include a shift to low-carbon energy technologies and the deployment of carbon capture and storage. In RCP4.5, atmospheric CO2 sits at 540ppm by 2100 – roughly 140ppm higher than now – equivalent to 630ppm once other forcings are included (in CO2e). By 2100, global temperatures are likely to rise by 2-3C above pre-industrial levels.
Together, these islands are home to roughly 70% of the total breeding population of king penguins, the research finds.
However, some southern islands are expected to become closer to the foraging boundary as it moves polewards. These include South Sandwich and Bouvet.
Changes in foraging distance on each island are shown in more detail on the charts below, which highlight results for the low emissions scenario (RCP2.6; green), the intermediate emissions scenario (RCP4.5; orange) and the high emissions scenario (RCP8.5; red).
On the charts, the red-dashed line shows the upper limit for foraging distance, beyond which penguins cannot successfully rear their chicks.
Changes in foraging distance expected on each breeding colony under a low emissions scenario (RCP2.6; green), a moderate emissions scenario (RCP4.5; orange) and a high emissions scenario (RCP8.5; red). Red line shows the upper limit for foraging distance. Source: Cristofari et al. (2018)
Under the high emissions scenario, 49% of the total population are expected to lose their breeding grounds completely by 2100, while a further 21% could “see their habitat strongly altered,” the researchers say.
The results also show that, even under low and intermediate scenarios, the Crozet and Falkland Islands are likely to become unworkable breeding grounds, the researchers say:
“The largest colonies on Crozet will still be in trouble under RCP4.5 and RCP2.6, which corresponds to around 1m breeding pairs.”
§ Island hopping?
The results show that a large proportion of king penguins could be forced to leave their breeding islands as the climate warms. However, it is not yet clear whether these animals will be able to successfully relocate to more southerly islands, which could become closer to the foraging grounds, the researchers say:
“King penguins move a lot among islands and, if a new suitable island becomes available, they will likely colonise it. The problem is that the new islands have to become available before the old one is not suitable anymore.”
Although the southern islands are expected to become closer to the Arctic Polar Front, the islands may be covered by sea ice and, therefore, be too cold for penguins to rear their chicks successfully, the researchers say:
“Southern islands may be still too cold for the king penguin to breed when northern islands get too far from the food.”
If no suitable breeding spots emerge in time, a large proportion of king penguins could “disappear” by the end of the century, the researchers say. In their paper, they conclude:
“Under the ‘business-as-usual RCP8.5 scenario, 70% of the present-day 1.6m king penguin breeding pairs are expected to abruptly relocate or disappear before the end of the century.”
§ Cutting global emissions
The new study provides an “interesting and well executed” first look at how climate change could threaten king penguins, says Dr Norman Ratcliffe, a seabird ecologist from the British Antarctic Survey (BAS), who was not involved in the research. He tells Carbon Brief:
“It’s quite a crude habitat model, I’m sure there’s a lot more to it – what king penguins need from life – than these two variables [breeding spaces and foraging distance].”
The research shows that some breeding colonies could be protected if the world were to limit the amount of future climate change, he adds:
“It’s a matter of cutting global emissions. There’s not very much compensatory habitat management you could do, you can’t create islands in the ocean.”