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Friday, November 22, 2024

Tulane PhD candidate part of study on river avulsions

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Avulsions are natural but rare phenomena that occur when a river  abruptly jumps course and forges a new river channel. Sometimes caused  by large floods, avulsions can have devastating effects on communities  while, at the same time, creating fertile deltas that have nurtured  others.

To gain a better understanding of what controls avulsion location in  the context of climate and land use changes, a team of scientists,  including a Tulane University PhD candidate, has analyzed 50 years of  satellite imagery and generated the first global database of river  avulsions.

"Avulsions are catastrophic events that can potentially displace large populations and cause massive infrastructural damage."

José Silvestre, Tulane PhD candidate

Led by researchers at the University of California at Santa Barbara (UCSB), the study was published recently in the journal Science.  The study corroborates about 10 years of experimental work by the group, which called avulsions an “understudied curiosity.”

“This dataset provides the first unambiguous test of the theory,  which demonstrates that there are three distinct regimes of avulsions on  fans and deltas,” said co-author Vamsi Ganti, an assistant professor in  the UCSB Department of Geography. “This is a long way from where we  started. A decade ago, avulsions were thought to be these chaotic and  stochastic events that were not very predictable.”

José Silvestre,  a PhD candidate in the Tulane Department of Earth and Environmental  Sciences, used satellite imagery to track how river paths have changed  through time to identify river avulsions.

Locations of avulsions include some of the world’s largest waterways,  including the Orinoco, Yellow, Nile and Mississippi rivers. A recent  example occurred in 2008, when the Kosi River in India shifted its course by over 60 miles, displacing more than 3 million people.

“We leveraged a half-century of satellite observations and coupled  these with theory and water and sediment discharge models to  characterize avulsions on alluvial fans and deltas,” Silvestre said.  “Our database revealed the existence of three distinct regimes of  avulsions on fans and deltas, which allow a predictive framework to  assess where rivers will shift course in response to land use and  climate change.”

He said that while river avulsions are natural land-building  processes that distribute sediment, water and nutrients on alluvial fans  and deltas, “they are catastrophic events that can potentially displace  large populations and cause massive infrastructural damage.”

Although interest in river avulsions has increased in recent years,  research has been limited to laboratory experiments, numerical studies  and limited field data, Silvestre said. Until now, there has been a lack  of understanding as to where avulsions occur.

The team documented 113 avulsions across the globe and found that  they were often tied to changes in channel slope or sedimentation just  upstream of the river. In some cases, avulsions were farther upstream  than expected and likely due to erosion.

Researchers are now looking at the global satellite record to develop  new metrics for characterizing the factors that drive other types of  river mobility, in addition to avulsions.

“The question that we’ve answered here is ‘where’ avulsions occur,  but we haven’t really dug into ‘when,’” Ganti said, adding that both are  equally important.

Source: https://news.tulane.edu/pr/tulane-phd-candidate-part-study-river-avulsions

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