Biological station integral to climate change study
UM’s Flathead Lake Biological Station aquatic ecologist Shawn Devlin oversees the Flathead Monitoring Program, which maintains one of the strongest long-term ecological and water quality records in the world.
Over the last few decades, water scientists have noticed a rapid and consistent warming of surface temperatures. Changes beneath the water surface, however, have been subtler, but could still have significant consequences for lake ecosystems.
In a study recently published in Nature’s Scientific Reports, Shawn Devlin, an aquatic ecologist at the University of Montana Flathead Lake Biological Station, and a global team of researchers provide the most comprehensive data set to date of long-term summertime vertical temperature profiles in more than 100 lakes across the world. Led by Rachel Pilla and Craig Williamson of the University of Miami-Ohio, researchers analyzed summer temperature trends, not only in the surface-water layers of the lakes, but also in deep-water layers and vertical thermal structures.
“One thing that made this study so remarkable is the scope,” said Devlin, who oversees FLBS’s Flathead Monitoring Program, one of the oldest lake monitoring programs in the world. “We were able to track the long-term surface and deep-water temperature trends of each individual lake and insert that information into a much larger picture to uncover patterns that help us understand what’s happening.”
After examining the data, which spanned nearly four decades beginning in 1970, researchers found consistent, significant increases in surface temperatures – an average of nearly 0.4 degrees Celsius per decade – across the lakes studied. Additionally, researchers were able to use lake models to predict the temperature changes in surface layers on a fairly consistent basis.
But when it came to the deep-water layers, a surprising development emerged. While the temperature trends showed little change on average – an increase of 0.06 degrees Celsius per decade – there was high variability across the lakes. The deep-water temperature of one of the lakes increased by nearly 0.7 degrees Celsius per decade, while the deep-water temperature of another lake actually decreased by the same amount.
This variability couldn’t be explained by trends in surface water temperatures or any other external drivers examined in the study. As a result, lake models were only able to predict deep-water temperature trends in 8.4% of the lakes studied.
“It’s a very interesting phenomenon,” Devlin said. “It’s something we see right here at Flathead Lake, which has a unique ability to mask the impacts of climate change. Even though the surface temperatures have increased quite a bit here in the past couple decades, the average temperature has remained essentially the same.”
According to Devlin, Flathead Lake on the whole is able to offset its rise in surface layer temperatures with a large deep-water layer that is bolstered by a steady inflow of snow melt and glacial runoff. As a result, Flathead Lake’s deep-water layer is actually cooling slightly.
While it may at first seem positive that Flathead Lake and others like it aren’t experiencing the dramatic temperature changes in their deep-water layers as they are on the surface, the implications can potentially be quite dire.
Larger temperature differences between the deep-water and surface-water layers make for stronger stratification. The stronger the stratification, the stronger and more robust the thermocline (the transition layer, or barrier, between waters of different temperatures) becomes, which can prevent the movement of materials and organisms between surface and deeper waters. This can greatly impact the ecology of a lake by creating nutrient imbalances, modifying critical oxygen levels throughout the lake and altering fish communities and production.
To fully understand what the future holds for our lake ecosystems, however, additional research will need to be done.
“Flathead Lake is now part of our global understanding of one of the biggest threats to our freshwater ecosystems, which is climate change,” Devlin said. “This is an important first step toward a better scientific understanding, and it wouldn’t be possible without the decades of extensive monitoring and modeling efforts of the Flathead Monitoring Program and those who support our work.”
For Devlin, incorporating Flathead Lake’s extensive data into the global research on lakes and working with lake experts from all over the world makes for more powerful science.
“Flathead Lake is a great template of how lakes could work when not greatly influenced by human impacts. We were able to show that our lake is a treasure trove of scientific merit and study, which makes this an important moment scientifically for the Flathead Monitoring Project, the Bio Station and UM.”
This study was made possible through the support of the Global Lake Ecological Observatory Network, in addition to numerous foundations and grants.
PHOTO 1: UM’s Flathead Lake Biological Station aquatic ecologist Shawn Devlin oversees the Flathead Monitoring Program, which maintains one of the strongest long-term ecological and water quality records in the world.
PHOTO 2: Flathead Lake was one of 102 lakes across the globe that were subjects in a four-decade study of surface and deep-layer water temperatures.