BE_2024v14n4

Bioscience Evidence 2024, Vol.14, No.4, 161-171 http://bioscipublisher.com/index.php/be 169 8.4 Potential technological and methodological advancements Technological advancements such as the combination of ground-penetrating radar with terrestrial LiDAR scanning offer promising methods to estimate the spatial distribution of liquid water content in snowpacks non-destructively and at high resolutions (Webb et al., 2018). The use of process-based snow modeling combined with high-resolution LiDAR data can improve predictions of the effects of forest management on snowpack (Krogh et al., 2020). Additionally, the development of decision support tools using machine learning can help synthesize complex snow-forest interactions and inform water management practices (Krogh et al., 2020). Enhanced global observations, both in situ and remotely sensed, will be crucial for evaluating and improving climate models, thereby reducing uncertainties in snowpack predictions (Simpkins et al., 2018). By addressing these challenges and gaps, and leveraging technological advancements, we can improve our understanding and management of snowpack resources, which are critical for sustaining ecosystems and human water needs in the face of climate change. 9 Concluding Remarks Winter snowpack plays a crucial role in water resource management and ecosystem function. As a natural reservoir, it stores water during the winter and gradually releases it in the spring and summer, which is vital for maintaining river flows, supporting agricultural production, and supplying urban water needs. However, climate change is significantly impacting snowpack dynamics, leading to reduced snow accumulation, earlier snowmelt, and changes in the timing and availability of water. These changes pose new challenges for water resource management, as traditional practices and infrastructure often struggle to adapt to these shifts. Snowpack is not only a key component of water resources, particularly in regions that rely on snowmelt for their water supply, such as the western United States, but it also supports ecosystem health by regulating soil moisture, recharging groundwater, and maintaining stream flows. However, changes in snowpack dynamics can disrupt these critical processes, leading to negative impacts on ecosystems and biodiversity. In light of these challenges, there is an urgent need for integrated management approaches, improved observation networks, and predictive models to better understand and respond to the impacts of snowpack changes on water resources and ecosystems. Further research into the interactions between snowpack, atmospheric conditions, and ecosystem processes will aid in developing more effective management strategies to address the complex effects of climate change. Acknowledgments The authors acknowledge the two anonymous peer reviewers for their careful evaluation and valuable feedback on this manuscript. Conflict of Interest Disclosure The authors affirm that this research was conducted without any commercial or financial relationships that could be construed as a potential conflict of interest. References Beria H., Larsen J., Ceperley N., Michelon A., Vennemann T., and Schaefli B., 2018, Understanding snow hydrological processes through the lens of stable water isotopes, Wiley Interdisciplinary Reviews: Water, 5(6): e1311. https://doi.org/10.1002/wat2.1311 Bilish S., Callow J., McGrath G., and McGowan H., 2019, Spatial controls on the distribution and dynamics of a marginal snowpack in the Australian Alps, Hydrological Processes, 33: 1739-1755. https://doi.org/10.1002/hyp.13435 Chen X., Gong L., and Liu Y., 2018, The ecological stoichiometry and interrelationship between litter and soil under seasonal snowfall in Tianshan Mountain, Ecosphere, 9(11): e02520. https://doi.org/10.1002/ecs2.2520 Clifton C., Day K., Luce C., Grant G., Safeeq M., Halofsky J., and Staab B., 2018, Effects of climate change on hydrology and water resources in the Blue Mountains Oregon USA, Climate Services, 10: 9-19. https://doi.org/10.1016/j.cliser.2018.03.001

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