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      <image:title>News - MOSH Lab Media Interviews: Snow Situation in Northeast B.C. - Make it stand out</image:title>
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      <image:title>News - Real-time weather and snow data in Valemount!</image:title>
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      <image:title>News - Real-time weather and snow data in Valemount!</image:title>
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      <image:title>News - Real-time weather and snow data in Valemount!</image:title>
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      <image:title>News - Real-time weather and snow data in Valemount!</image:title>
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      <image:title>News - Real-time weather and snow data in Valemount!</image:title>
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      <image:caption>Head of the Robson Valley near Valemount, British Columbia.</image:caption>
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      <image:caption>The team, posing for a truck-bumper photo.</image:caption>
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      <image:caption>Community dinner in Centennial Park, Valemount.</image:caption>
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      <image:title>News - MA/MSc Student: Community Adaptation to Changing Mountain Snowpacks and Geohazards - Make it stand out</image:title>
      <image:caption>Robson Valley flooding, 1 July 2021. Credit: Sandra James</image:caption>
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      <image:caption>Observed (top left) and modelled snow depths in the Kananaskis study area, Alberta. The full model (top right) includes wind downscaling and accounts for recirculation and gravitational and blowing-snow redistribution. Absent these processes (bottom panels), the model can’t capture the magnitude or complex distribution of observed snow depths.</image:caption>
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      <image:caption>Testing the slope monitor above University Way.</image:caption>
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      <image:caption>Testing the real-time device on UNBC campus.</image:caption>
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      <image:caption>UNBC students heading towards the toe of the Athabasca Glacier during the 2024 Physical Geography Field School (photo: J. Shea).</image:caption>
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      <image:title>Blog - BC Snow Pillows - Make it stand out</image:title>
      <image:caption>Snow pillow (on the ground) and snow depth sensor (mounted off the tower) somewhere in the woods. From Engel et al. (2022; http://dx.doi.org/10.21079/11681/44122)</image:caption>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/5cef5be5f96d9700014f04af/5e5576fe-fefa-48f5-879f-0a8c947fa0aa/1B01PPC-demo.png</image:loc>
      <image:title>Blog - BC Snow Pillows - Make it stand out</image:title>
      <image:caption>Example of historical SWE data from snow pillow 1B01P (Mount Wells) showing the seasonal patterns of snow accumulation and melt. Each individual SWE year is given as a gray trace, and the percentiles of SWE by day of year are given in blue (25th), orange (50th), and green (75th).</image:caption>
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      <image:title>Blog - BC Snow Pillows - Make it stand out</image:title>
      <image:caption>Left: Historical SWE (25th and 75th percentiles are dashed blue, median is solid blue) and current year’s SWE (orange points). Right: Daily change in SWE for historical median values (blue) and current year (orange).</image:caption>
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      <image:title>Blog - BC Snow Pillows - Make it stand out</image:title>
      <image:caption>Map of current “percent of normal” for BC’s snow pillow network, and inset histogram with overall mean (vertical black line).</image:caption>
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      <image:caption>Whatever it is, the way you tell your story online can make all the difference.</image:caption>
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      <image:caption>Peyto Glacier in 2017 (photo: J. Shea)</image:caption>
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      <image:caption>Figure 1: Fifty shades of basin hypsometry, clustered into three main categories: top-heavy (purple), middle (green), and bottom heavy (yellow).</image:caption>
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      <image:caption>Figure 2: Snowpack volume responses for the three different hypsometry types and two warming scenarios.</image:caption>
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      <image:caption>Figure 3: Average daily snowmelt rates for three different basin geometries (purple = top-heavy, yellow = bottom-heavy) and temperature increases.</image:caption>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/5cef5be5f96d9700014f04af/1618026579437-48EICILGCC2WN005IJYH/Figure1revised.jpg</image:loc>
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      <image:caption>Figure 4: Study area map, with the location of top-heavy (purple), intermediate (green), and bottom-heavy (yellow) mountain basins.</image:caption>
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      <image:title>Blog - Field Work: Alpine Ground Temperature Observations</image:title>
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      <image:caption>Snow pillow locations in the Upper Fraser River Basin.</image:caption>
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