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Century-old Deep-sea Expeditions Provide New Climate Change Insights

UMD Scientists' Analysis Shows Rapid Rate of Recent Warming in Indian Ocean

By Emily C. Nunez

Ship SMS Planet in a 1905 image

The German Navy's SMS Planet was one of three ships used by German scientists in the late 19th and early 20th centuries on global voyages to study deep-sea life. They also gathered data that present day researchers at UMD are using to develop a deeper understanding of warming caused by human activities in the Indian Ocean.

In the late 19th and early 20th centuries, German scientists and surveyors crossed choppy waters and braved dangerous conditions on arduous expeditions, one of which circumnavigated the globe. They yielded several discoveries of interest to scientists of the day—and left in their wake important clues for later generations.

­Though these early researchers were mostly interested in marine biology at a time when little was known about life in the deep sea (documenting among other things the first vampire squid sighting), some of their “cruise reports” also contained measurements of subsurface temperatures in the Indian Ocean.

A team led by atmospheric and oceanic scientists at the University of Maryland studied the long-overlooked water temperature data from these three expeditions from 1874 to 1907, digitizing the information and putting it in a modern context to offer a new perspective on ocean warming.

Their analysis, published online on June 25 in the journal Geophysical Research Letters, determined that undersea temperature changes in the Indian Ocean were limited in the late 19th and early 20th centuries. These findings are consistent with other global records, which show that ocean warming began to accelerate only in the last half of the 20th century, largely due to human-caused climate change.

Jacob Wenegrat, the paper’s lead author, said these historical measurements fill holes in the research community’s understanding of how much and how deep the Indian Ocean warmed throughout history.

“The modern observational record of subsurface ocean temperatures only goes back to about 1960,” said Wenegrat, an assistant professor in atmospheric and oceanic science at UMD. “We’ve had this gap in century-timescale observations for the Indian Ocean. At the same time, particularly in the last decade or two, the role that the Indian Ocean plays in global climate systems has become even clearer.”

Of all the heat the global ocean has taken on since 1990, the Indian Ocean has absorbed a quarter of it, helping to slow the rate of global surface air-temperature increases and mitigate climate change. This has come at a cost, though. It is one of the fastest-warming oceans, which in many cases leads to the loss of biodiversity and rising sea levels.

The region is also home to a third of the global population, with millions of people relying on fisheries and rain-fed agriculture for food. Monsoons, floods, droughts and weather patterns like El Niño are also heavily affected by warming patterns in the Indian Ocean, leading to natural disasters in many parts of the world.

“The Indian Ocean has taken up a significant amount of heat in the climate system, so even though it’s a pretty small basin, it seems to have this outsized impact on global climate,” Wenegrat said.

For these reasons and more, the researchers set out to uncover how subsurface temperatures in the Indian Ocean—measured by German crews over a century ago—fit into global records of ocean warming.

In the process, they encountered some unique challenges. They first needed to translate the cruise logs from their original German into English. Co-author and historian Ursula Rack from the University of Canterbury in New Zealand helped contextualize the translated text, explaining what types of measuring tools and equipment were used throughout the expeditions.

UMD atmospheric and oceanic science major Emma Bonanno ’21 and oceanographer Geoffrey Gebbie from the Woods Hole Oceanographic Institution co-authored the paper.

The researchers accounted for any temperature readings that could be inaccurate due to equipment limitations. This included mercury thermometers that were vulnerable to errors from the compression of the mercury at greater depths, as well as hemp lines that were easily stretched by heavy equipment and swayed by currents, potentially affecting the depth at which measurements were recorded.

Wenegrat said this study gave him a greater appreciation of the challenge—and value—of making data accessible to current and future scientists.

“There’s a lot of focus right now in ocean sciences on data reproducibility and data sharing, but it’s often thought of in relatively short time scales—you want someone to be able to reproduce your work five years or a decade from now,” Wenegrat said. “It’s incredible that we were able to pick up this data a century after it was taken and use it for purposes that were certainly not anticipated by the scientists who collected it.”



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