South pole warming three times faster than rest of the world, our research shows | Kyle Clem for the Conversation

Climate scientists long thought Antarctica’s interior may not be very sensitive to warming, but our research, published this week, shows a dramatic change.

Over the past 30 years, the south pole has been one of the fastest-changing places on Earth, warming more than three times more rapidly than the rest of the world.

My colleagues and I argue these warming trends are unlikely the result of natural climate variability alone. The effects of human-made climate change appear to have worked in tandem with the significant influence natural variability in the tropics has on Antarctica’s climate. Together they make the south pole warming one of the strongest warming trends on Earth.

The Amundsen-Scott South Pole station is the Earth's southern-most weather observatory.

The south pole is not immune to warming

The south pole lies within the coldest region on Earth: the Antarctic plateau. Average temperatures range from -60? during winter to just -20? during summer.

Antarctica’s climate generally has a huge range in temperature over the course of a year, with strong regional contrasts. Most of West Antarctica and the Antarctic Peninsula were warming during the late 20th century. But the south pole – in the remote and high-altitude continental interior – cooled until the 1980s.

Scientists have been tracking temperature at the Amundsen-Scott south pole Station, Earth’s southernmost weather observatory, since 1957. It is one of the longest-running complete temperature records on the Antarctic continent.

Our analysis of weather station data from the south pole shows it has warmed by 1.8? between 1989 and 2018, changing more rapidly since the start of the 2000s. Over the same period, the warming in West Antarctica suddenly stopped and the Antarctic Peninsula began cooling.

One of the reasons for the south pole warming was stronger low-pressure systems and stormier weather east of the Antarctic Peninsula in the Weddell Sea. With clockwise flow around the low-pressure systems, this has been transporting warm, moist air on to the Antarctic plateau.

South pole warming linked to the tropics

Our study also shows the ocean in the western tropical Pacific started warming rapidly at the same time as the south pole. We found nearly 20% of the year-to-year temperature variations at the south pole were linked to ocean temperatures in the tropical Pacific, and several of the warmest years at the south pole in the past two decades happened when the western tropical Pacific ocean was also unusually warm.

To investigate this possible mechanism, we performed a climate model experiment and found this ocean warming produces an atmospheric wave pattern that extends across the South Pacific to Antarctica. This results in a stronger low-pressure system in the Weddell Sea.

Map of the Antarctic continent

We know from earlier studies that strong regional variations in temperature trends are partly due to Antarctica’s shape.

The East Antarctic ice sheet, bordered by the South Atlantic and Indian oceans, extends further north than the West Antarctic ice sheet, in the South Pacific. This causes two distinctly different weather patterns with different climate impacts.

More steady, westerly winds around East Antarctica keep the local climate relatively stable, while frequent intense storms in the high-latitude South Pacific transport warm, moist air to parts of West Antarctica.

Scientists have suggested these two different weather patterns, and the mechanisms driving their variability, are the likely reason for strong regional variability in Antarctica’s temperature trends.

[embedded content]

What this means for the south pole

Our analysis reveals extreme variations in south pole temperatures can be explained in part by natural tropical variability.

To estimate the influence of human-induced climate change, we analysed more than 200 climate model simulations with observed greenhouse gas concentrations over the period between 1989 and 2018. These climate models show recent increases in greenhouse gases have possibly contributed around 1? of the total 1.8? of warming at the south pole.

We also used the models to compare the recent warming rate to all possible 30-year south pole temperature trends that would occur naturally without human influence. The observed warming exceeds 99.9% of all possible trends without human influence – and this means the recent warming is extremely unlikely under natural conditions, albeit not impossible. It appears the effects from tropical variability have worked together with increasing greenhouse gases, and the end result is one of the strongest warming trends on the planet.

The temperature variability at the South Pole is so extreme it masks anthropogenic effects.

These climate model simulations reveal the remarkable nature of south pole temperature variations. The observed south pole temperature, with measurements dating back to 1957, shows 30-year temperature swings ranging from more than 1? of cooling during the 20th century to more than 1.8? of warming in the past 30 years.

This means multi-decadal temperature swings are three times stronger than the estimated warming from human-caused climate change of around 1?.

The temperature variability at the south pole is so extreme it currently masks human-caused effects. The Antarctic interior is one of the few places left on Earth where human-caused warming cannot be precisely determined, which means it is a challenge to say whether, or for how long, the warming will continue.

But our study reveals extreme and abrupt climate shifts are part of the climate of Antarctica’s interior. These will likely continue into the future, working to either hide human-induced warming or intensify it when natural warming processes and the human greenhouse effect work in tandem.

  • Kyle Clem is a research fellow in climate science, Te Herenga Waka, Victoria University of Wellington

[embedded content]
[embedded content]

Leave a Reply

Your email address will not be published. Required fields are marked *

Close