Climate change and its effects on Rocky Mountain alpine lakes

Climate change and its effects on Rocky Mountain alpine lakes
Credit: Canadian Light Source

Alpine lakes in the Rocky Mountains are important biological hot spots of that ecosystem. These lakes do not have enough nutrients to support large amounts of aquatic life because of the cold climate in the surrounding watershed. Rather, the lakes are home to oligotrophs, organisms that grow slowly and can survive in harsh aquatic environments. The lakes also host a variety of cold-water fish, such as trout, that are preyed upon by birds, including osprey and bald eagles.

Researchers from University of Wyoming, U.S. Geological Survey, and the Canadian Light Source conducted experiments at the CLS on the that is deposited to the Rocky Mountains to learn more about how the alpine lakes could be affected by climate change. They looked specifically at in dust and how it is made available to the organisms in the cold lakes and streams, because phosphorus is one of the major limiting nutrients, and its availability could affect the functions and properties of alpine lake ecosystems.

Phosphorus is an essential nutrient for all life forms and the lack of it is one of the reasons the of these alpine lakes is limited. Because phosphorus is not readily available from surrounding watersheds, aeolian dust (dust that is blown by the wind) becomes an important source of phosphorus to alpine lakes and can substantially affect aquatic ecosystems. Much of the dust deposited to the Rockies is generated from the Colorado Plateau Desert, where high aridity and recent land-use changes promote wind erosion of soils to produce dust. Dust emission is expected to increase from the warming and drying deserts and plains of the American West. Such additional dust will likely deliver to mountain ecosystems beyond amounts documented for recent decades.

Climate change and its effects on Rocky Mountain alpine lakes
Moderate resolution imaging spectroradiometer (MODIS) satellite image showing a major dust event originating in the Four Corners region of the southern Colorado Plateau on April 16, 2013.  Red lines outline the extent of dust emission visible on this image. Dust trajectory is towards the dust on snow sites (yellow circles) to the northeast. Other potential dust source areas in eastern Utah are obscured by clouds. Credit: Canadian Light Source

Using the SXRMB beamline at the CLS, the researchers were able to characterize the type of phosphorus in the dust and dust-source soils on the Colorado Plateau. Their work showed that the phosphorus in the dust is mainly bound to calcium. This form of phosphorus is unstable and will dissolve in acidified lakes. Considering the increasing input due to changes in the climate and land use and the acidification of these alpine lakes, this study suggests that the alpine lakes may not be limited in phosphorus in the future. An accumulation of phosphorous could result in more algal growth in alpine lakes. Such growth can decrease available oxygen for fish. This would adversely impact population of alpine lake fish, such as trout that require cold, well-oxygenated water, environmental conditions maintained only in oligotrophic lakes.

Climate change and its effects on Rocky Mountain alpine lakes
DOS Layers:  Dust events are recorded as discrete dust layers (D6 – D8) visible in the snow pit face. Credit: Center for Snow and Avalanche Studies.

More information: Zhuojun Zhang et al. Phosphorus Speciation and Solubility in Aeolian Dust Deposited in the Interior American West, Environmental Science & Technology (2018). DOI: 10.1021/acs.est.7b04729

Citation: Climate change and its effects on Rocky Mountain alpine lakes (2018, April 9) retrieved 3 December 2022 from
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