How marsh grass could help protect us from climate change

Photo by Steve Adams on Unsplash
Marshland in Holden Beach, USA, likely to have prevented storms and surges from having a worse impact in North Carolina. Photo by Steve Adams on Unsplash

By David L. Chandler, World Economic Forum (Public License).

  • Coastal marsh plants provide significant protection from surges and devastating storms.

  • Research in MIT’s Parson’s lab can help coastal planners to take important details into account when planning projects.

  • Countries must take advantage of this modeling in order to restore marshland with specific plants in certain areas.

Marsh plants, which are ubiquitous along the world’s shorelines, can play a major role in mitigating the damage to coastlines as sea levels rise and storm surges increase. Now, a new MIT study provides greater detail about how these protective benefits work under real-world conditions shaped by waves and currents.

The study combined laboratory experiments using simulated plants in a large wave tank along with mathematical modeling. It appears in the journal Physical Review — Fluids, in a paper by former MIT visiting doctoral student Xiaoxia Zhang, now a postdoc at Dalian University of Technology, and professor of civil and environmental engineering Heidi Nepf.

“After a few years, the marsh grasses start to trap and hold the sediment, and the elevation gets higher and higher, which might keep up with sea level rise.”

—Xiaoxia Zhang, now a postdoc at Dalian University of Technology, and professor of civil and environmental engineering Heidi Nepf
A new MIT study provides greater detail about how thes protective benefits of marsh plants work under real-world conditions shaped by waves and currents. The simulated plants used in lab experiments were designed based on Spartina alterniflora, which is a common coastal marsh plant. Credit: Xiaoxia Zhang.
A new MIT study provides greater detail about how thes protective benefits of marsh plants work under real-world conditions shaped by waves and currents. The simulated plants used in lab experiments were designed based on Spartina alterniflora, which is a common coastal marsh plant. Credit: Xiaoxia Zhang.

It’s already clear that coastal marsh plants provide significant protection from surges and devastating storms. For example, it has been estimated that the damage caused by Hurricane Sandy was reduced by $625 million thanks to the damping of wave energy provided by extensive areas of marsh along the affected coasts. But the new MIT analysis incorporates details of plant morphology, such as the number and spacing of flexible leaves versus stiffer stems, and the complex interactions of currents and waves that may be coming from different directions.

This level of detail could enable coastal restoration planners to determine the area of marsh needed to mitigate expected amounts of storm surge or sea-level rise, and to decide which types of plants to introduce to maximize protection.

“When you go to a marsh, you often will see that the plants are arranged in zones,” says Nepf, who is the Donald and Martha Harleman Professor of Civil and Environmental Engineering. “Along the edge, you tend to have plants that are more flexible, because they are using their flexibility to reduce the wave forces they feel. In the next zone, the plants are a little more rigid and have a bit more leaves.”

As the zones progress, the plants become stiffer, leafier, and more effective at absorbing wave energy thanks to their greater leaf area. The new modeling done in this research, which incorporated work with simulated plants in the 24-meter-long wave tank at MIT’s Parsons Lab, can enable coastal planners to take these kinds of details into account when planning protection, mitigation, or restoration projects.

“If you put the stiffest plants at the edge, they might not survive, because they’re feeling very high wave forces. By describing why Mother Nature organizes plants in this way, we can hopefully design a more sustainable restoration,” Nepf says.

Once established, the marsh plants provide a positive feedback cycle that helps to not only stabilize but also build up these delicate coastal lands, Zhang says. “After a few years, the marsh grasses start to trap and hold the sediment, and the elevation gets higher and higher, which might keep up with sea level rise,” she says.

Awareness of the protective effects of marshland has been growing, Nepf says. For example, the Netherlands has been restoring lost marshland outside the dikes that surround much of the nation’s agricultural land, finding that the marsh can protect the dikes from erosion; the marsh and dikes work together much more effectively than the dikes alone at preventing flooding.

But most such efforts so far have been largely empirical, trial-and-error plans, Nepf says. Now, they could take advantage of this modeling to know just how much marshland with what types of plants would be needed to provide the desired level of protection.

It also provides a more quantitative way to estimate the value provided by marshes, she says. “It could allow you to more accurately say, ‘40 meters of marsh will reduce waves this much and therefore will reduce overtopping of your levee by this much.’ Someone could use that to say, ‘I’m going to save this much money over the next 10 years if I reduce flooding by maintaining this marsh.’ It might help generate some political motivation for restoration efforts.”

Nepf herself is already trying to get some of these findings included in coastal planning processes. She serves on a practitioner panel led by Chris Esposito of the Water Institute of the Gulf, which serves the storm-battered Louisiana coastline. “We’d like to get this work into the coatal simulations that are used for large-scale restoration and coastal planning,” she says.

This photo shows examples of Spartina alterniflora in China. Credit: Xiaoxia Zhang.
This photo shows examples of Spartina alterniflora in China. Credit: Xiaoxia Zhang.

“Understanding the wave damping process in real vegetation wetlands is of critical value, as it is needed in the assessment of the coastal defense value of these wetlands,” says Zhan Hu, an associate professor of marine sciences at Sun Yat-Sen University, who was not associated with this work. “The challenge, however, lies in the quantitative representation of the wave damping process, in which many factors are at play, such as plant flexibility, morphology, and coexisting currents.”

The new study, Hu says, “neatly combines experimental findings and analytical modeling to reveal the impact of each factor in the wave damping process. … Overall, this work is a solid step forward toward a more accurate assessment of wave damping capacity of real coastal wetlands, which is needed for science-based design and management of nature-based coastal protection.”

The work was partly supported by the National Science Foundation and the China Scholarship Council.

‘Momentous’ Moratorium on Deep Sea Mining Adopted at Global Biodiversity Summit

A pair of fish swim near the ocean floor off the coast of Mauritius. A motion calling for an end to deep sea mining of minerals was adopted at the world congress of the International Union for the Conservation of Nature this week. (Photo: Roman Furrer/Flickr/cc)
A pair of fish swim near the ocean floor off the coast of Mauritius. A motion calling for an end to deep sea mining of minerals was adopted at the world congress of the International Union for the Conservation of Nature this week. (Photo: Roman Furrer/Flickr/cc)

“Deep seabed mining is an avoidable environmental disaster,” said one expert on global ocean policy.

By Julia Conley, Common Dreams (CC BY-ND 3.0).

A vote overwhelmingly in favor of placing a moratorium on deep sea mineral mining at a global biodiversity summit this week has put urgent pressure on the International Seabed Authority to strictly regulate the practice. 

The vast majority of governments, NGOs, and civil society groups voted in favor of the moratorium at the world congress of the International Union for the Conservation of Nature (IUCN) on Wednesday, after several conservation groups lobbied in favor of the measure.

Eighty-one government and government agencies voted for the moratorium, while 18 opposed it and 28, including the United Kingdom, abstained from voting. Among NGOs and other organizations, 577 supported the motion while fewer than three dozen opposed it or abstained. 

Deep sea mining for deposits of copper, nickel, lithium, and other metals can lead to the swift loss of entire species that live only on the ocean floor, as well as disturbing ecosystems and food sources and putting marine life at risk for toxic spills and leaks. 

Fauna and Flora International, which sponsored the moratorium along with other groups including the Natural Resources Defense Council and Synchronicity Earth, called the vote “a momentous outcome for ocean conservation.” 

The motion called for a moratorium on mining for minerals and metals near the ocean floor until environmental impact assessments are completed and stakeholders can ensure the protection of marine life, as well as calling for reforms to the International Seabed Authority (ISA)—the regulatory body made up of 167 nations and the European Union, tasked with overseeing “all mineral-related activities in the international seabed area for the benefit of mankind as a whole.” 

In June, a two-year deadline was set for the ISA to begin licensing commercial deep sea mining and to finalize regulations for the industry by 2023. 

“Member countries of the ISA, including France which hosted this Congress, need to wake up and act on behalf of civil society and the environment now, and take action in support of a moratorium.”

—Matthew Gianni, Deep Sea Conservation Coalition

The World Wide Fund for Nature, another cosponsor of the motion, called on the ISA to reject the deep sea mining industry’s claims that mining for metals on the ocean floor is a partial solution to the climate crisis. 

“The pro-deep seabed mining lobby is… selling a story that companies need deep seabed minerals in order to produce electric cars, batteries and other items that reduce carbon emissions,” said Jessica Battle, a senior expert on global ocean policy and governance at the organization. “Deep seabed mining is an avoidable environmental disaster. We can decarbonize through innovation, redesigning, reducing, reusing, and recycling.”

Pippa Howard of Fauna and Flora International wrote ahead of the IUCN summit that “we need to shatter the myth that deep seabed mining is the solution to the climate crisis.” 

“Far from being the answer to our dreams, deep seabed mining could well turn out to be the stuff of nightmares,” she wrote. “Deep seabed mining—at least as it is currently conceived—would be an utterly irresponsible and short-sighted idea. In the absence of any suitable mitigation techniques… deep-sea mining should be avoided entirely until that situation changes.”

End of Arctic Sea Ice by 2035 Possible, Study Finds

August 11th, 2020, by Alex Kirby (CC BY-ND 4.0)

How soon will the northern polar ocean be ice-free? New research expects the end of Arctic sea ice by 2035.

LONDON, 11 August, 2020 − The temperature of the Arctic matters to the entire world: it helps to keep the global climate fairly cool. Scientists now say that by 2035 there could be an end to Arctic sea ice.

Photo by Willian Justen de Vasconcellos on Unsplash
Photo by Willian Justen de Vasconcellos on Unsplash

The northern polar ocean’s sea ice is a crucial element in the Earth system: because it is highly reflective, it sends solar radiation back out into space. Once it’s melted, there’s no longer any protection for the darker water and rock beneath, and nothing to prevent them absorbing the incoming heat.

High temperatures in the Arctic during the last interglacial – the warm period around 127,000 years ago – have puzzled scientists for decades.

Now the UK Met Office’s Hadley Centre climate model has enabled an international research team to compare Arctic sea ice conditions during the last interglacial with the present day. Their findings are important for improving predictions of future sea ice change.

What is striking about the latest research is the date it suggests for a possible total melt − 2035. Many studies have thought a mid-century crisis likely, with another even carefully specifying 2044 as the year to watch. So a breathing space of only 15 years may surprise some experts.

“The prospect of loss of sea ice by 2035 should really be focussing all our minds on achieving a low-carbon world as soon as humanly feasible”

During spring and early summer shallow pools of water form on the surface of the Arctic sea ice. These “melt ponds” help to determine how much sunlight is absorbed by the ice and how much is reflected back into space. The new Hadley Centre model is the UK’s most advanced physical representation of the Earth’s climate and a critical tool for climate research, and it incorporates sea ice and melt ponds.

The researchers report their findings in the journal Nature Climate Change. Using the model to look at Arctic sea ice during the last interglacial, they concluded that the impact of intense springtime sunshine created many melt ponds, which played a crucial role in sea ice melt. A simulation of the future using the same model indicates that the Arctic may become sea ice-free by 2035.

The joint lead author of the team is Dr Maria Vittoria Guarino, an earth system modeller at the British Antarctic Survey (BAS) in Cambridge. She says: “High temperatures in the Arctic have puzzled scientists for decades. Unravelling this mystery was technically and scientifically challenging. For the first time, we can begin to see how the Arctic became sea ice-free during the last interglacial.

“The advances made in climate modelling mean that we can create a more accurate simulation of the Earth’s past climate which, in turn, gives us greater confidence in model predictions for the future.”

Dr Louise Sime, the group head of the palaeoclimate group and joint lead author at BAS, says: “We know the Arctic is undergoing significant changes as our planet warms. By understanding what happened during Earth’s last warm period we are in a better position to understand what will happen in the future.

Melt ponds crucial

“The prospect of loss of sea ice by 2035 should really be focussing all our minds on achieving a low-carbon world as soon as humanly feasible.”

Dr David Schroeder from the University of Reading, UK, who co-led the implementation of the melt pond scheme in the climate model, says: “This shows just how important sea ice processes like melt ponds are in the Arctic, and why it is crucial that they are incorporated into climate models.”

The extent of the areas sea ice covers varies between summer and winter. If more solar energy is absorbed at the surface, and temperatures rise further, a cycle of warming and melting occurs during summer months.

When the ice forms, the ocean water beneath becomes saltier and denser than the surrounding ocean. Saltier water sinks and moves along the ocean bottom towards the equator, while warm water from mid-depths to the surface travels from the equator towards the poles.

Scientists refer to this process as the ocean’s global “conveyor-belt”. Changes to the volume of sea ice can disrupt normal ocean circulation, with consequences for global climate. Climate News Network