Article Excerpt: While the world rightfully focuses on the Covid-19 pandemic, the planet is still warming. This summer’s Antarctic weather, as elsewhere in the world, was unprecedented in the observed record.
Antarctica may be isolated from the rest of the continents by the Southern Ocean, but has worldwide impacts. It drives the global ocean conveyor belt, a constant system of deep-ocean circulation which transfers oceanic heat around the planet, and its melting ice sheet adds to global sea level rise.
Antarctica represents the simple, extreme end of conditions for life. It can be seen as a “canary in the mine”, demonstrating patterns of change we can expect to see elsewhere.
This summer, Casey Research Station, in the Windmill Islands oasis, experienced its first recorded heatwave. For three days, minimum temperatures exceeded zero and daily maximums were all above 7.5C. On 24 January, its highest maximum of 9.2C was recorded, almost 7C above Casey’s 30-year mean for the month.
The arrival of warm, moist air during this weather event brought rain to Davis Research Station in the normally frigid, ice-free desert of the Vestfold Hills. The warm conditions triggered extensive meltwater pools and surface streams on local glaciers. These, together with melting snowbanks, contributed to high-flowing rivers and flooding lakes.
By February, most heat was concentrated in the Antarctic Peninsula at the northernmost part of the continent. A new Antarctic maximum temperature of 18.4C was recorded on 6 February at Argentina’s Esperanza research station on the peninsula – almost 1C above the previous record. Three days later this was eclipsed when 20.75C was reported at Brazil’s Marambio station, on Seymour Island east of the peninsula.
The pace of warming from global climate change has been generally slower in East Antarctica compared with West Antarctica and the Antarctic Peninsula. This is in part due to the ozone hole, which has occurred in spring over Antarctica since the late 1970s.
The hole has tended to strengthen jet stream winds over the Southern Ocean, promoting a generally more “positive” state of the Southern Annular Mode in summer. This means the Southern Ocean’s westerly wind belt has tended to stay close to Antarctica at that time of year creating a seasonal “shield”, reducing the transfer of warm air from the Earth’s temperate regions to Antarctica.
But during the spring of 2019 a strong warming of the stratosphere over Antarctica significantly reduced the size of the ozone hole. This helped to support a more “negative” state of the Southern Annular Mode and weakened the shield.
Other factors in late 2019 may have also helped to warm Antarctica. The Indian Ocean Dipole was in a strong “positive” state due to a late retreat of the Indian monsoon. This meant that water in the western Indian Ocean was warmer than normal. Air rising from this and other warm ocean patches in the Pacific Ocean provided energy sources that altered the path of weather systems and helped to disturb and warm the stratosphere.
Given the generally cold conditions of Antarctica, the warmth may have benefited the flora (mosses, lichens and two vascular plants) and microbes and invertebrates, but only where liquid water formed. Areas in the Vestfold Hills away from the flooding became more drought-stressed over the summer.
High temperatures may have caused heat stress in some organisms. Antarctic mosses and lichens are often dark in colour, allowing sunlight to be absorbed to create warm microclimates. This is a great strategy when temperatures are just above freezing, but heat stress can occur once 10C is exceeded.
Based on our experience from previous anomalous hot Antarctic summers, we can expect many biological impacts, positive and negative, in coming years. The most recent event highlights the connectedness of our climate systems: from the surface to the stratosphere, and from the monsoon tropics to the southernmost continent.
Under climate change, extreme events are predicted to increase in frequency and severity, and Antarctica is not immune.