Cryospheric Sciences

Enigmatic Climatic Event: Antarctic Cold Reversal

Enigmatic Climatic Event: Antarctic Cold Reversal

In this week’s blog, Levan Tielidze tells us about the insight into the response of mountain glaciers to the Antarctic Cold Reversal (ACR) event in New Zealand to better understand the climatic history of the Southern Hemisphere during the last deglaciation. The ACR was a cold period occurred in the Southern Hemisphere during the transition from the last glacial period to the current interglacial one. A kind of last glacial gasp during the warming of the southern hemisphere. Let’s discover something more!

When was Antarctic Cold Reversal

After the Last Glacial Maximum (about 21,000 years ago), the last deglaciation began worldwide. This period was characterized by global warming and sea level rise due to the massive discharge of freshwater from continental ice sheets and glaciers. The process of warming and ice melting continued globally almost until the Early Holocene (around 11,700 years). However, the warming trend during the deglaciation was interrupted by cooling episodes between ~15,000–12,000 years ago. They were not synchronous in the two hemispheres. A major cooling events was specifically recognised in the Southern Hemisphere and in mid-latitudes, including New Zealand. It is known as the Antarctic Cold Reversal and occurred between 14,500 and 12,500 years ago. Investigating climate fluctuations during the Antarctic Cold Reversal is important because they provide an example of non-linear climate change during a past period of global warming, which may have relevance for present-day climate change that will become even more acute under the projected warming. Putting such changes into perspective requires a deep understanding of past climate evolution as a possible window for the prediction of future changes of the climate. Glacier records from New Zealand situated in the southwestern Pacific provide a rare record of past Southern Hemisphere climate changes and are ideal tools for testing hypotheses about the competing drivers of the Antarctic Cold Reversal.

The new study

In a recently published study, we aimed to improve our understanding of the glacier behaviour and climate events during the Antarctic Cold Reversal in the Southern Alps of New Zealand. Using cosmogenic exposure dating and geomorphological mapping we reconstructed the geometries of former glaciers in the Ahuriri River valley. Furthermore, based on the reconstructed glacier snowline (i.e. the boundary between the zone of the glacier that accumulates snow and the one subject to ice melting) and the local temperature gradient we estimated past temperatures during the Antarctic Cold Reversal.

Our results indicate that the advance of the former glacier during the cold pulse culminated at ~14,500 years ago, while the next re-advance or stationary phase occurred at ~13,600 years ago (Figure 2). About thousand years later (~12,600 years ago), the former glacier had lowered ~140 m and built another prominent terminal moraine ridge.

Figure 2. Photo of the two clearly visible moraine ridges from the Southern Alps indicating glacier re-advance or stationary phase at ~14,500 and ~13,600 years ago. Yellow dots indicate the location of the samples. Black digits indicate sample ages, while the red numbers indicate sample names. The outlier (excluded) sample is given by red italic text. [Credit: Tielidze et al., 2023].

Our estimate of snowline reconstructions at ~14,500 years ago based on the local temperature gradient returns an air temperature estimate ~3.9 °C lower than today (1981-2010). Other two snowline reconstructions from ~13,600 and ~12,600 years ago suggesting a ~3.5 and ~2.3 °C cooler climate than today. Consequently, one of the main findings of our study is the confirmation of early glacier re-advance or stillstand at ~14,500 years ago in New Zealand, which has been previously recognised with only limited evidence (e.g. Kaplan et al., 2013; Putnam et al., 2010). On this basis, our study proposes that the early cooling and the maximum ice extent in New Zealand in the first centuries of the Antarctic Cold Reversal reflects the northward shift of the southern westerlies winds, persistent winds typical of mid-latitudes and subpolar areas. This caused lower temperatures and/or relatively higher precipitation and resulted in the re-advance or stationary phase of glaciers in the Southern Alps.

Further reading

Edited by Stefan Thiele & Giovanni Baccolo

Levan Tielidze is an early career scientist at Victoria University of Wellington, New Zealand and at Ilia State University, Georgia. His field of research is modern glaciers and glacial-geomorphological studies of the mountainous areas in the Late Quaternary. Contact email: He tweets as @LevanTielidze.

This guest post was contributed by a scientist, student or a professional in the Earth, planetary or space sciences. The EGU blogs welcome guest contributions, so if you've got a great idea for a post or fancy trying your hand at science communication, please contact the blog editor or the EGU Communications Officer to pitch your idea.

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