Location: Water Management and Systems Research
Title: Variogram time series analysis applied to the spatial structure of snow accumulationAuthor
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FASSNACHT, STEVEN - Colorado State University |
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LOPEZ-MORENO, JUAN - The Geological And Mining Institute Of Spain |
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Barnard, David |
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MORAN-TEJEDA, ENRIQUE - Universitat De Les Illes Balears |
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WEBB, RYAN - University Of Wyoming |
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VON THADEN, BENJAMIN - Colorado State University |
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PFOHL, ANNA - National Oceanic & Atmospheric Administration (NOAA) |
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COLLADOS-LARA, ANTONIO-JUAN - Universidad De Granada |
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MACDONALD, MARIN - Colorado State University |
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FLYNN, HELEN - Colorado State University |
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TEDESCHE, MOLLY - University Of Alaska |
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Submitted to: Water Resources Research
Publication Type: Peer Reviewed Journal Publication Acceptance Date: 2/23/2026 Publication Date: 3/8/2026 Citation: Fassnacht, S., Lopez-Moreno, J.I., Barnard, D.M., Moran-Tejeda, E., Webb, R., Von Thaden, B.C., Pfohl, A., Collados-Lara, A., MacDonald, M.S., Flynn, H., Tedesche, M.E. 2026. Variogram time series analysis applied to the spatial structure of snow accumulation. Water Resources Research. 62(3). Article e2025WR040065. https://doi.org/10.1029/2025WR040065. DOI: https://doi.org/10.1029/2025WR040065 Interpretive Summary: This study looked at how snowpack accumulation patterns change across different areas in the Southern Rocky Mountains. Spatial patterns are similar within about 100 kilometers (62 miles) of each other. However, the similarity decreases as distance among sites increases. The study also found that the similarity of snowpack patterns can change depending on the season and whether the ocean is warm or cold (El Niño or La Niña). In the spring and summer, patterns are similar within about 60 kilometers, while in the winter, they can be similar for up to 300 kilometers. Technical Abstract: The correlation of earth system properties is important for assessing monitoring strategies, scales of modeling, and improving the accuracy of forecasting. We present a new method to examine the scale of similar inter-annual patterns. It is applied to the snowpack accumulation using a time series of daily snow water equivalent data, here applied to the Southern Rocky Mountains of Wyoming, Colorado and New Mexico, USA. We examined sub-sets of the data to explore the differences in geographic location, land cover type, and climate patterns (Oceanic Niño Index; ONI). Results indicate that snow accumulation patterns in the Southern Rocky Mountains are consistent up to 100 kilometers, and lesser correlated up to about 380 km. The 100-km consistency is observed regardless of how the data are sub-set. However, the spatial patterns of precipitation vary by season; the summer consistency is about 60 km while the winter consistency is more than 300 km with some variance based on ONI phase. |
