Volcano Watch — "Move your paddle silently through the water"

The voyage also has a mission to bring awareness of the alarming changes in the Pacific that endanger the health of our ocean and the resources it provides to millions of people who depend on it.

By this weekend, the voyagers will have reached O‘ahu. While there, they will participate in a conference that seeks to address the impact of stresses, such as climate change, overfishing and pollution.

Some of the effects of climate change on the marine environment are easily observed and understood, for example, the warming of sea waters and the rising of sea level as more and more glacial ice melts.

Another effect related to climate change is more subtle, but has devastating consequences for marine life: ocean acidification.

Ocean acidification refers to the lowered pH of the oceans due to the reaction of carbon dioxide (CO₂) with seawater to form carbonic acid. CO₂ is the most prevalent greenhouse gas in the Earth's atmosphere.

Since the beginning of the industrial revolution about 200 years ago, the oceans have absorbed 525 billion tons of CO₂ from the atmosphere, nearly half of the fossil fuel carbon emissions over this period. This natural process of absorption has benefited us by reducing the greenhouse gas levels in the atmosphere, thus minimizing some impacts of global warming. The ocean's daily uptake of 22 million tons of carbon dioxide, however, is taking a toll on the chemistry of seawater.

The drop in seawater pH wreaks havoc on the chemical equilibrium of calcium carbonate, a mineral used by marine organisms like corals, lobsters, and crabs to build shells and skeletons. As the oceans become more acidic, these organisms will grow more slowly, and corals may be unable to build reefs fast enough to keep up with the rising sea level. The impacts will propagate throughout the marine food chain, affecting species diversity, commercial fisheries, and tourist economies.

There are still some skeptics who remain unconvinced that human activities are the major contributors to global climate change, and they often direct the blame at volcanoes.

There is no doubt that volcanic eruptions add CO₂ to the atmosphere, but compared to the quantity produced by human activities, their impact is almost trivial: CO₂ output of the Earth's degassing subaerial and submarine volcanoes is about 150-260 million tonnes per year, whereas human activities contribute more than 100 times that quantity (about 35,000 million tonnes in 2010). Every 2.7 days, human activities emit an amount of CO₂ comparable to the annual global volcanic CO₂ emissions.

During the ongoing Kīlauea eruption, the average annual CO₂ emission rate is about three million tonnes.

Even the Mount Pinatubo eruption on 15 June 1991—one of the three largest eruptions of the twentieth century—released only about 50 million tonnes of CO₂, or about 6 million tonnes per hour. The human CO₂ emission rate of 4 million tonnes per hour is similar. So, for a few hours during large eruptions, individual volcanoes may emit about as much or more CO₂ than human activities. But volcanic paroxysms are infrequent, while anthropogenic CO₂ is emitted continuously.

The U.S. is the single largest contributor to global warming, responsible for nearly one-quarter of global human emissions.

Modifying our habits to curb CO₂ emissions can slow the rate of change for critical ocean ecosystems. There is a lot of information on the Web about how to lower your carbon footprint and make a positive impact on our oceans. For example, go to http://epa.gov/climatechange.

The Web site of the Pacific Voyagers, also has suggestions and lots of inspiration. The motto of the current voyaging project seems especially apt for us island residents: "Move your paddle silently through the water."

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Volcano Activity Update

A small lava lake was present deep within the Halema‘uma‘u Overlook vent during the past week. Cycles of rise and fall were prevalent, causing the lava lake level—and the size of the gas plume—to fluctuate abruptly.

Lava also erupted continuously within Pu‘u ‘Ō‘ō over the past week, feeding a lava lake perched above the crater floor. Small overflows topped the rim of the perched pond occasionally, sending lava spilling onto the surrounding crater floor. Volcanic gas emissions from both vents remain elevated, resulting in relatively high concentrations of sulfur dioxide downwind.

No earthquakes beneath Hawai‘i Island were reported felt this past week.