Guest essay by Eric Worrall
Who could have imagined that islands which survived rapid sea level rise at the end of the last ice age have no problem coping with changes in sea level?
From: University of Auckland
Pacific atolls can adapt to rising seas and extreme storms – new study
Low-lying Pacific islands in atoll archipelagos such as Tuvalu, Tokelau and Kiribati are likely to adapt to the effects of climate change rather than simply sink beneath the waves, a new study shows.
Tuvalu, Tokelau and Kiribati are widely considered under threat from rising seas and severe storms due to climate change with their residents becoming ‘climate refugees’.
Researchers from the University of Auckland’s School of Environment recreated a scale model of tiny Fatato Island on the southeast rim of Funafuti Atoll in Tuvalu to test the ability of the real island to withstand predicted climate affects.
The study simulated higher sea levels and storm-generated waves up to 4m in a 20m-long water chute or ‘flume’ to replicate real-world sea levels of 0.5m and 1m in a purpose built laboratory at the University of Plymouth in the United Kingdom.
The team chose uninhabited Fatato as a model because they were able to create an accurate 1:50 scale replica using data collected from previous field surveys and research. In the real world, the tiny island is just 90m at its widest point and 860m long. The scale replica created for the laboratory tests was 0.6m wide, 2.6m long with a highest point of 10cm.
Using lasers to closely monitor changes in the model, and translating those to a real-world scenario, the researchers found the crest of the island – its highest ground – actually increased 1.13m height as higher sea levels and strong wave action washed sand and gravel toward it.
While that elevation was achieved at the expense of lower-lying areas, simultaneously reducing the amount of low-lying land as the crest got higher. But that might not happen in the real world where islands are continually replenished by sediment from the surrounding reef.
Importantly, the island also moved laterally, migrating across the coral reef as sand and gravel shifted position with the action of waves and higher water levels.
Lead author and University of Auckland doctoral candidate Megan Tuck says the findings, along with previous research, has profound implications for understanding the physical vulnerability of reef islands and challenges the assumption that they will simply drown.
“Atoll islands do not sit inert on the reef, instead the gravel and sand they are made up of shifts on the reef itself so that the land changes in response to environmental conditions. Interestingly, the elevation of the atoll crest – the highest ground – mirrored the rise in sea levels which suggests sea level may be an important controlling factor on island elevation.”
Co-researcher Dr Murray Ford, also from the University of Auckland, says the study shows islands are more resilient than previously thought, able to change shape or physically adjust to higher sea levels and more severe storms.
“While the effect on particular islands of climate-induced changes will vary, there is plenty of evidence to suggest these islands are more resilient than commonly thought,” he says.
“The effects on individual islands will vary so that while some areas may become uninhabitable, while areas will keep pace with rising seas. It will be up to governments and communities to decide how to respond over time but we think this study highlights the fact that nature provides a template for adaptation and island communities may need to adapt too.”
Previous research by the team, which used aerial photos going back as far as 1943 to track changes to the 101 islands that make up the Tuvalu archipelago, found that overall there was a net gain in land area of 2.9 percent or 73.5ha over the past 40 years.
Professor Paul Kench, formerly of the University of Auckland, now at Simon Fraser University in Canada, and Professor Gerd Masselink from the University of Plymouth were co-researchers in the study, published by the Geological Society of America in Geology.Read more: https://www.scimex.org/newsfeed/sea-level-rise-may-not-spell-the-end-for-low-lying-pacific-atolls
The abstract of the study;
RESEARCH ARTICLE|JULY 05, 2019Read more: https://pubs.geoscienceworld.org/gsa/geology/article-abstract/572047/physical-modelling-of-the-response-of-reef-islands?redirectedFrom=fulltext
Physical modelling of the response of reef islands to sea-level rise
Megan E. Tuck; Paul S. Kench; Murray R. Ford; Gerd Masselink
Sea-level rise and increased storminess are expected to destabilize low-lying reef islands formed on coral reef platforms, and increased flooding is expected to render them uninhabitable within the coming decades. Such projections are founded on the assumption that islands are geologically static landforms that will simply drown as sea-level rises. Here, we present evidence from physical model experiments of a reef island that demonstrates islands have the capability to morphodynamically respond to rising sea level through island accretion. Challenging outputs from existing models based on the assumption that islands are geomorphologically inert, results demonstrate that islands not only move laterally on reef platforms, but overwash processes provide a mechanism to build and maintain the freeboard of islands above sea level. Implications of island building are profound, as it will offset existing scenarios of dramatic increases in island flooding. Future predictive models must include the morphodynamic behavior of islands to better resolve flood impacts and future island vulnerability.
The alleged global warming threat to coral systems and Pacific islands has got to rank amongst the most implausible of the climate community’s claims. It is encouraging that more scientists are plucking up the courage to point out the obvious.
Update (EW): Dr K A Rodgers points out that Charles Darwin proposed coral reefs are dynamic structures in 1842. You would think almost 200 years would be long enough for the climate community to catch on.