Summary Microalgae adapted to near‐zero temperatures and high light levels live on snowfields and glaciers worldwide. Snow algae have red‐colored pigments that darken snow surfaces, lowering its albedo and accelerating snowmelt. Despite their importance to the cryosphere, we know little about controls on snow algal productivity and biomass.Here, we characterize photophysiology from diverse natural field‐collected populations of alpine snow algae from the North Cascades of Washington, USA, where the major red‐bloom producing generaChlainomonas,Sanguina, andRosettawere present. We tested short‐term physiological responses of snow algae to light (0–3000 μmol m−2 s−1) and CO2levels (0–1600 ppm), allowing us to determine the saturating light and CO2levels for snow algal community net photosynthesis.All snow algal communities surveyed were adapted to extremely high light levels (3000 μmol m−2 s−1). In addition, photosynthesis rates of all the snow algal communities responded strongly to increasing CO2levels. At current atmospheric CO2levels (420 ppm), snow algal net photosynthesis rates were onlyc.50% saturated.Together, these results suggest the primary productivity of important bloom‐forming snow algal communities in alpine ecosystems will likely rise as atmospheric CO2concentrations increase, regardless of potential changes in available light levels.
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Albedo change from snow algae blooms can contribute substantially to snow melt in the North Cascades, USA
Abstract Snow algae are ubiquitous in the Pacific Northwest cryosphere in the summer where snowmelt is an important contribution to regional watersheds. However, less attention has been given to biological impurities as drivers of snowmelt compared to inorganic light-absorbing particles. Here we map snow algae near Mt. Baker with a multispectral camera on an uncrewed aerial vehicle using (1) principal components and (2) spectral indexing. The two approaches are tested under differing bloom states and verified with coincident algal pigment and cell count data. During high bloom intensity we found an average instantaneous radiative forcing of 237 W m−2with a maximum of 360 W m−2. This translated to 1,508 ± 536 m3of melted snow water equivalent in the 0.1 km2basin. These results demonstrate snow algae contribute to snowmelt at mid-latitudes and the potential for uncrewed autonomous vehicles to map snow algae over expansive areas of the cryosphere.
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- Award ID(s):
- 2046240
- PAR ID:
- 10490587
- Publisher / Repository:
- Nature Communications Earth and Environment
- Date Published:
- Journal Name:
- Communications Earth & Environment
- Volume:
- 4
- Issue:
- 1
- ISSN:
- 2662-4435
- Subject(s) / Keyword(s):
- Cryosphere snow algae albedo snowmelt radiative forcing UAVs multi-spectral imagery
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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