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The sub-Antarctic islands are increasingly warming in the 21st century

Published online by Cambridge University Press:  24 April 2023

Werner Nel*
Affiliation:
Department of Geography and Environmental Science, University of Fort Hare, 1 King Williamstown Road, Alice, 5700, South Africa
David W. Hedding
Affiliation:
Department of Geography, University of South Africa, Pioneer Avenue, Florida, 1710, South Africa
Elizabeth M. Rudolph
Affiliation:
Afromontane Research Unit, Department of Geography, University of the Free State, 205 Nelson Mandela Avenue, Bloemfontein, 9300, South Africa
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Abstract

Type
Short Note
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.
Copyright
Copyright © The Author(s), 2023. Published by Cambridge University Press on behalf of Antarctic Science Ltd

This paper presents the rate of warming in the sub-Antarctic region in the 21st century and summarizes the landscape and ecosystem responses to the increased warming. The islands that constitute the ‘core’ of the sub-Antarctic region are South Georgia, Marion and Prince Edward islands, the archipelagos of Crozet and Kerguelen, Heard and McDonald islands and Macquarie Island (Convey Reference Convey, Goldstein and Dellasala2020). These islands are located close to the Antarctic Polar Front, with air temperatures that are consistently cool and with annual and seasonal variability buffered by the surrounding cold ocean (Convey Reference Convey, Goldstein and Dellasala2020). Climatic records from these sub-Antarctic islands have shown a warming air temperature trend throughout most of the mid- to late 20th century (Bergstrom & Chown Reference Bergstrom and Chown1999, Jacka et al. Reference Jacka, Budd and Holder2004, Pendlebury & Barnes-Keoghan Reference Pendlebury and Barnes-Keoghan2007), and reports on the landscape and ecological impacts due to the warming climate during this period are numerous (see Bergstrom & Chown Reference Bergstrom and Chown1999). Generally, the main cause of ocean and atmospheric warming is the anthropogenic forcing of the trend towards the positive phase of the Southern Annular Mode (Pohl et al. Reference Pohl, Saucède, Pergaud, Féral, Richard and Favier2021) and the associated intensification and poleward migration of the Southern Hemisphere westerly winds (Perren Reference Perren, Hodgson, Roberts, Sime and Van Nieuwenhuyze2020). It is predicted that the sub-Antarctic region will continue to warm during the 21st century (Meehl et al. Reference Meehl, Stocker, Collins, Friedlingstein, Gaye, Gregory, Solomon, Qin, Manning, Chen, Marquis and Averyt2007). Given that we have entered the third decade of the 21st century, it is now possible to assess the recent warming trends over the core sub-Antarctic islands and to hypothesize as to what impacts the future air temperatures will have on landscape and ecosystem processes during the rest of the century.

Air temperature data for Marion Island (latitude: −46.883, longitude: 37.867), the Crozet Islands (Alfred Faure; latitude: −46.433, longitude: 51.850) the Kerguelen Islands (Port Aux Francais; latitude: −49.350, longitude: 70.250), Macquarie Island (latitude: −54.499, longitude: 158.937) and South Georgia (Grytviken; latitude: −54.283, longitude: −36.500) were downloaded from the GISTEMP v4 station data database (https://data.giss.nasa.gov/gistemp/). Mean annual air temperatures (MAATs) were analysed using the monthly means in the dataset, and if any monthly mean was missing in a specific year then that year was omitted from the analysis. For comparison, the MAATs for the New Zealand-associated ‘sub-Antarctic’ islands of Campbell (latitude: −52.550, longitude: 169.167) and Auckland (Enderby; latitude: −50.483; 166.300) were also analysed. Pearson's correlation coefficients showed that the MAATs of the core sub-Antarctic islands are positively correlated with their nearest neighbours (Table Ia). The temperature data from the two New Zealand islands are also strongly correlated. Of all the islands, the MAATs at Campbell Island appear most representative of the entire sub-Antarctic region based on the significant correlations with the other islands (> 95–99% confidence).

Table I. a. Pearson's correlation coefficients (R 2) for mean annual temperature trends between stations and b. summary of linear regression statistics and rates of change of mean annual air temperature for sub-Antarctic stations.

* Significant at the 95% confidence level.

** Significant at the 99% confidence level.

Macquarie, Kerguelen and Marion islands have warmed by between 0.8°C and 1.7°C since air temperature recordings started during the mid-20th century. These trends are significant at the 95–99% confidence level, except at the Crozet Islands (2006–2021) because of missing data (Table Ib). As expected, the warming trend established during the 20th century is continuing into the 21st century, but the recent (2000–2021) trend of warming (°C/100 years) is in all respects higher than the long-term trend (Table Ib, column 5). Since the turn of the century, the core sub-Antarctic islands (plus Campbell Island) show a warming trend of between 2.3 and 2.9°C/100 years, while the Auckland Islands (Enderby) shows a warming trend of 4.7°C/100 years. From linear extrapolation of the long-term trends up to 2000, the predicted temperature in 2050 is 5.3°C at Macquarie Island, 5.9°C at the Kerguelen Islands and 6.7°C at Marion Island. However, from the rate measured since 2000, MAATs in the middle of the century (2050) are predicted to be 6.0°C at Macquarie Island, 6.3°C at the Kerguelen Islands and 7.2°C at Marion Island. Under current warming trends (2000–2021), the MAATs in 2050 at Campbell Island and the Auckland Islands could be as high as 8.2°C and 10.0°C, respectively. The current warming trend (since 2000) of between 2.3 and 2.9°C/100 years measured at the sub-Antarctic islands is already in line with the 2–3°C warming predicted for this region under the A2 emissions scenario by 2080–2099 (relative to 1980–1999; Meehl et al. Reference Meehl, Stocker, Collins, Friedlingstein, Gaye, Gregory, Solomon, Qin, Manning, Chen, Marquis and Averyt2007, fig. 10.8) and is within the projected change in surface air temperature (2–3°C) for the sub-Antarctic region at the end of the century (2081–2100) under the highest baseline emissions scenario of RCP8.5 (IPCC 2014, fig. SPM.7).

These measured (and extrapolated) warming trends in air temperature at the sub-Antarctic islands are impacting landscape and ecosystem processes. The further (accelerated) demise of glacial ice (from those islands that still have it), due to either the increase in air temperature (Sumner et al. Reference Sumner, Meiklejohn, Boelhouwers and Hedding2004) and/or the decrease in snow accumulation (Favier et al. Reference Favier, Verfaillie, Berthier, Menegoz M, Jomelli and Kay2016), means that the cryosphere is fast approaching an irreversible tipping point in the sub-Antarctic, as predicted by Bakke et al. (Reference Bakke, Paasche, Schaefer and Timmermann2021). Warmer air temperatures will also modify ground thermal dynamics, which could impact the frequency and magnitude of needle ice growth, the freezing depths of both diurnal and seasonal frost and sediment movement and cycling. Needle ice formation is a very important diurnal soil frost process across most islands (Nel et al. Reference Nel, Boelhouwers, Borg, Cotrina, Hansen and Haussmann2021), impacting several keystone species and small-scale geomorphic processes in the fellfield habitat (Nel & Boelhouwers Reference Nel and Boelhouwers2014). Transported propagules of invasive plant species have been shown to have increased rates of establishment and range expansion in the terrestrial habitats of the sub-Antarctic (Convey Reference Convey, Goldstein and Dellasala2020). Invasive vertebrates pose a significant risk to the ecology of sub-Antarctic islands, as shown by the impacts of the mice currently existing on Marion Island on ecosystem structure and functioning (Greve et al. Reference Greve, Mathakutha, Steyn and Chown2017) and on the predation on seabirds (Dilley et al. Reference Dilley, Schoombie, Schoombie and Ryan2016; see also mousefreemarion.org). Under an increasingly warming climate, the risk posed by invasive species to the ecology of the sub-Antarctic islands is predicted to intensify. The effective implementation of biosecurity measures for the sub-Antarctic islands is becoming progressively more crucial (Convey Reference Convey, Goldstein and Dellasala2020).

Acknowledgements

Jan Boelhouwers is thanked for original insights into the regionality of air temperature trends. The reviewer is thanked for valuable inputs regarding the original manuscript.

Financial support

Our research in the sub-Antarctic is conducted through the financial support of the South African National Research Foundation (grant under SANAP-NRF: 129235).

Author contributions

All of the authors have made substantial contributions to this paper and approved the final version of the manuscript. The authors' contributions appear below as per CRediT guidelines: WN: Conceptualization, Methodology, Validation, Formal analysis, Writing - Original Draft. DWH: Validation, Writing - Review & Editing. EMR: Validation, Writing - Review & Editing.

References

Bakke, J., Paasche, Ø., Schaefer, J.M. & Timmermann, A. 2021. Long-term demise of sub-Antarctic glaciers modulated by the Southern Hemisphere westerlies. Scientific Reports, 11, 10.1038/s41598-021-87317-5.CrossRefGoogle ScholarPubMed
Bergstrom, D.M. & Chown, S.L. 1999. Life at the front: history, ecology and change on Southern Ocean islands. Trends in Ecology and Evolution, 14, 10.1016/S0169-5347(99)01688-2.CrossRefGoogle ScholarPubMed
Convey, P. 2020. Current changes in Antarctic ecosystems. In Goldstein, M.I. & Dellasala, D.A., eds, Encyclopedia of the world's biomes, vol. 2. Amsterdam: Elsevier, 666685.CrossRefGoogle Scholar
Dilley, B.J., Schoombie, S., Schoombie, J. & Ryan, P.G. 2016. 'Scalping' of albatross fledglings by introduced mice spreads rapidly at Marion Island. Antarctic Science, 28, 10.1017/S0954102015000486.CrossRefGoogle Scholar
Favier, V., Verfaillie, D., Berthier, E. Menegoz M, ., Jomelli, V., Kay, J.E., et al. 2016. Atmospheric drying as the main driver of dramatic glacier wastage in the southern Indian Ocean. Scientific Reports, 6, 10.1038/srep32396.CrossRefGoogle ScholarPubMed
Greve, M., Mathakutha, R., Steyn, C. & Chown, S.L. 2017. Terrestrial invasions on sub-Antarctic Marion and Prince Edward islands. Bothalia, 47, 10.4102/abc.v47i2.2143.CrossRefGoogle Scholar
IPCC. 2014. Climate change 2014: synthesis report. Contribution of Working Groups I, II and III to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Geneva: IPCC, 151 pp.Google Scholar
Jacka, T.H., Budd, W.H. & Holder, A. 2004. A further assessment of surface temperature changes at stations in the Antarctic and Southern Ocean, 1949–2002. Annals of Glaciology, 39, 10.3189/172756404781813907.CrossRefGoogle Scholar
Meehl, G.A., Stocker, T.F., Collins, W.D., Friedlingstein, P., Gaye, A.T., Gregory, J.M., et al. 2007. Global climate projections. In Solomon, S., Qin, D., Manning, M., Chen, Z., Marquis, M., Averyt, K.B., et al. eds, Climate change 2007: the physical science basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge: Cambridge University Press, 749844.Google Scholar
Nel, W. & Boelhouwers, J.C. 2014. First observations of needle ice initiation in the sub-Antarctic. Antarctic Science, 26, 10.1017/S0954102013000722.CrossRefGoogle Scholar
Nel, W., Boelhouwers, J.C., Borg, C.-J., Cotrina, J.H., Hansen, C.D., Haussmann, N.S., et al. 2021. Earth science research on Marion Island (1996–2020): a synthesis and new findings. South African Geographical Journal, 103, 10.1080/03736245.2020.1786445.CrossRefGoogle Scholar
Pendlebury, S.E. & Barnes-Keoghan, I.P. 2007. Climate and climate change in the sub-Antarctic. Papers and Proceedings of the Royal Society of Tasmania, 141, 10.26749/rstpp.141.1.67.Google Scholar
Perren, B.B., Hodgson, D.A., Roberts, S.J., Sime, L., Van Nieuwenhuyze, W., et al. 2020. Southward migration of the Southern Hemisphere westerly winds corresponds with warming climate over centennial timescales. Communications Earth and Environment, 1, 10.1038/s43247-020-00059-6.CrossRefGoogle Scholar
Pohl, B., Saucède, T., Pergaud, J., Féral, J.-C., Richard, Y., Favier, V., et al. 2021. Recent climate variability around the Kerguelen Islands (Southern Ocean) seen through weather regimes. Journal of Applied Meteorology and Climatology, 60, 10.1175/JAMC-D-20-0255.1.Google Scholar
Sumner, P.D., Meiklejohn, K.I., Boelhouwers, J.C. & Hedding, D.W. 2004. Climate change melts Marion Island's snow and ice. South African Journal of Science, 100, 395398.Google Scholar
Figure 0

Table I. a. Pearson's correlation coefficients (R2) for mean annual temperature trends between stations and b. summary of linear regression statistics and rates of change of mean annual air temperature for sub-Antarctic stations.