Tuesday, September 09, 2025

 

Targeted snow monitoring at hotspots outperforms basin-wide surveys in predicting water supply





Oregon State University
Snow coring tube 

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A student field assistant measuring the water content of snow manually with a coring tube called a "federal sampler" in the Cascade Mountains in Oregon.
 

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Credit: Mark Raleigh





CORVALLIS, Ore. – Measuring mountain snowpack at strategically selected hotspots consistently outperforms broader basin-wide mapping in predicting water supply in the western United States, a new study found.

Researchers analyzed more than 20 years of snow estimates and streamflow data across 390 snow-fed basins in 11 western states to evaluate two potential strategies for expanded snow monitoring. This analysis revealed locations the researchers are calling hotspots — localized areas where snowpack is not yet measured but is especially predictive of water supply — and their importance

They found that hotspot monitoring can improve water supply predictions in most basins, with typical gains of 11-14% compared to 4% from basin-wide mapping of snow.

“Measuring snow in the right places can benefit forecasts more than measuring it everywhere,” said lead author Mark Raleigh, a snow hydrologist at Oregon State University. “This could guide our thinking about how snow monitoring might evolve to become more optimal for water forecasting.”

Snowmelt is a key water source for about two billion people globally, including in many agricultural regions, such as the western United States. On average, about half of the water in western streams is driven by snowmelt, Raleigh said.

“Our findings can help water agencies make informed decisions for more efficient water monitoring,” Raleigh said.

For about 100 years, statistical water supply forecasting in the west has relied on snow measurements at ground-based stations. The researchers analyzed data from these snow stations and found that they accurately predict year-to-year shifts in water supply, but the stations are sparsely located and sample a small area.

As a result, there is untapped potential to improve forecasts through expanded snow monitoring across a basin, though the predictive value of each location is not usually known in advance. The study provides a framework to assess a basin’s potential for improvements and identify where the greatest and smallest gains might be found.

Basin-wide surveys are the most comprehensive method to quantify the total amount of snow in a basin. This total snow volume over a basin is most accurately measured from airplanes. Satellite data can also support snow estimates over large areas. However, deploying these types of large-scale mapping technologies can be costly compared to the sort of localized monitoring included in this study.

In the new study, published in Communications Earth & Environment, the team compared the water supply predictive ability of the basin-wide surveys versus the hotspot approach. The researchers found that although both strategies can enhance water supply predictions, the hotspot approach typically yields better or similar improvements, despite measuring snow over a much smaller portion of the basin.

“Focusing new snow measurements at hotspots is a cost-effective alternative to basin-wide surveys, with potential for more accurate water forecasts,” Raleigh said. “This efficiency is critical as we move into a time when budgets are tightening and the demand for reliable water information remains high.”

Co-authors of the paper are Eric Small and Karl Rittger, University of Colorado Boulder; Edward (Ned) Bair, Leidos Inc., a national security and health company; and Cameron Wobus, CK Blueshift, a consulting group focused on the intersection of climate and water.

WOTD WORD OF THE DAY

Alkali waste dumped in the Pacific Ocean created alkalophilic ecosystems




PNAS Nexus
Pushcore sampling 

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Pushcore sampling from the white halo close to a barrel using the ROV manipulator arm.

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Credit: Schmidt Ocean Institute




Barrels filled with industrial waste that were dumped in the sea near Los Angeles more than 50 years ago are creating new microbial ecosystems adapted to highly alkaline conditions. It has been estimated that hundreds of thousands of barrels of waste were dumped off the coast of California in the mid 20th century. Previous investigations suggested that the barrels once contained dichlorodiphenyltrichloroethane (DDT)—an insecticide known for its broad toxicity that was banned for agricultural use in 1972. 


Another study suggested the barrels once contained low-level radioactive waste. In addition, some barrels were noted to have concrete-like encrustations around their bases or to have been encircled by white “halos” on the sea floor. Paul R. Jensen and colleagues used a remotely operated vehicle to dive around 900 meters and collect cores of sediment around corroding steel barrels on the San Pedro Basin seafloor. The concentration of DDT and its breakdown products was elevated in the area, but there was no gradient with increasing concentrations as the cores approached the barrels, so the DDT likely came from a different source—possibly bulk liquid dumping. The authors found the concretions to be magnesium hydroxide precipitation and the white haloes to be calcium carbonate. Both mineral artifacts were likely caused by leakage of alkaline waste. Microbial communities around these barrels were low diversity and dominated by alkalophilic bacteria, not unlike those observed at hydrothermal vents. According to the authors, it will likely take thousands years for the ecological effects of caustic alkaline waste dumping in the San Pedro Basin to cease. 


An alkalophilic organism, or alkaliphile, is a microorganism that thrives in extremely alkaline environments, typically with a pH above 8.5 or 9, and often cannot grow well in neutral conditionsThese organisms use specialized biological mechanisms, like proton transfer strategies and sodium-hydrogen exchangers, to maintain a functional internal pH despite the harsh external conditions. 


 

Bacterial ink to restore coral reefs




PNAS Nexus

BRINK schematic 

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Schematic representation of Brink as a functional living coating designed to enhance coral settlement. A) Harvest and isolation of lipopolysaccharide-producing bacteria from the tissues of the coral Montipora capitata (Thalassotalea euphylliae H1) and marine biofilm (Cellulophaga lytica HI1). B) Optimization of biopolymer mixture for microbial cell viability and mechanical properties. Rapid light-assisted cross-linking of Brink on calcium carbonate (CaCO3) plugs, a common restoration material. C) Brink sustains living bacteria that act as biofactories, producing lipopolysaccharides to attract coral larvae from the surrounding environment.

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Credit: Levy et al.





A living ink containing bacteria attracts coral larvae and could help rebuild reefs. Corals are struggling with water pollution, as well as warming and acidification caused by climate change. One way to support coral reef persistence is to encourage coral recruitment onto the reef. Coral larvae are free-swimming animals that eventually settle onto a surface and transform into a polyp with a hard, durable body. Certain bacteria secrete chemical cues that stimulate settlement and metamorphosis. Settled polyps may then reproduce asexually, expanding the size of the reef. Daniel Wangpraseurt and colleagues created a living material that encourages coral larvae to attach and settle down. Bacterial Reef Ink (BRINK) is a photopolymerized hydrogel hosting two native Hawaiian settlement-inducing bacterial strains, Cellulophaga lytica and Thalassotalea euphylliae. In test tanks, coral settlement on surfaces coated with BRINK was fivefold higher than on surfaces without ink for one coral species and fourfold higher for a different coral species. According to the authors, the ink could be customized to support a range of settlement-inducing bacteria tailored to specific coral reef environments worldwide.