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Snow Albedo

SCHOOL OF ICE

ALDEN ADOLPH, MICHIGAN TECHNOLOGICAL UNIVERSITY

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Hello! I am…

  • A snow scientist
  • An engineer
  • A professor
  • A partner and parent
  • A cat lover
  • A jogger and skier
  • An unabashed “Swiftie”

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Modeling global climate is complex!

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Climate Feedbacks

    • Water vapor and temperature
    • Methane and permafrost
    • Snow and ice albedo and temperature
    • Increased precipitation and temperature

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Temperature Rises

Atmosphere holds more water vapor

Water vapor is a GHG

More heat is trapped

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Temperature Rises

Arctic permafrost thaws

Methane and CO2 are released

More heat is trapped

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Grass

0.2

Open ocean

0.06

Sea ice

0.6

Fresh snow

0.9

Forests

0.1-0.15

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Temperature Rises

Snow and ice melt

Darker, more absorbing surfaces exposed

More sunlight is absorbed by surfaces

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Temperature Rises

The atmosphere holds more water vapor

Warm: it RAINS on the ice sheets

Albedo decreases

Positive Climate Feedback

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Temperature Rises

The atmosphere holds more water vapor

Cold: it SNOWS on the ice sheet

Fresh snow makes albedo higher

Temperature Decreases

Negative Climate Feedback

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Climate Feedbacks

    • Water vapor and temperature
    • Methane and permafrost
    • Snow and ice albedo and temperature
    • Increased precipitation and temperature

Understanding and being able to model these feedbacks is critical for accurately predicting the effects of increased greenhouse gas emissions

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https://nature.desktopnexus.com/wallpaper/1276478/

NASA Satellite Image

Snow: Microscale to Macroscale

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  • α is the surface albedo
  • SW↓ is the incoming shortwave radiation
  • LW↓ and LW↑ are the incoming and outgoing longwave radiation, respectively
  • HS and HL are the sensible and latent heat fluxes from the surface
  • G is heat flux from underlying surface

Energy Available for Temperature or Phase Change

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Snow albedo is relevant in the UV, Visible and NIR parts of the electromagnetic spectrum

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Albedo is measured in the parts of the spectrum with the most incoming solar radiation

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http://lumenistics.com/what-is-full-spectrum-lighting/

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Snow albedo is affected by many factors!

  • Snow grain shape and size
  • Impurities in the snow
  • Lighting conditions
  • Surface roughness
  • Wetness

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Larger grains lead to lower albedo

LACHAPELLE, 1969, http://www.metafysica.nl/ontology/general_ontology_29m1aa.html

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Impurities in snow also reduce albedo

Black Carbon

Dust

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https://commons.wikimedia.org/w/index.php?curid=9336928

https://www.wilmaslawnandgarden.com/en_gb/service/blog/growing-plants-in-soil-substrate/

https://travelola.org/2012/07/16/dust-desert-uyuni-bolivia/

Organic Carbon

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  • Impurities like dust, black carbon, organic carbon, and algae affect visible range
  • Grain size and shape affect near infrared range more
  • Snow depth, liquid water, lighting conditions, surface roughness, and terrain slope also play a role

Snow albedo is affected by many properties�

Model results using SNICAR (Flanner et al, 2021)

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Field Observations

  • Albedo
  • Grain Size
  • Impurity Content
  • Liquid Water Content
  • Stratigraphy
  • Density

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Photos: Creator, Copyright: Kaden Staley, Michigan Technological University

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Albedo Measurement

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  • Use portable field spectral radiometer
  • Measure downwelling and upwelling solar irradiance to calculate ratio

Photo Creator, Copyright: Kaden Staley, Michigan Technological University

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Spectrometer

Control

Laptop

Integrating

Sphere

Sandwich

Light

Source

Impurity Measurement

  • Developed system to measure black carbon equivalent impurity concentration based on Grenfell et al. 2011
  • Relies on reduction in transmission of light through a filter with impurities compared to standards

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Grain Size Measurement

  • Developed system to measure snow grain size based on work by Gallet et al. 2009
  • Reflectance of snow at 1310nm and 1550 nm is sensitive to grain size and shape, but not other factors

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Liquid Water Content (LWC) Measurements

  • Microwave resonator
  • Calculates LWC from measured shift in frequency and attenuation

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Seasonal Overview:��Measurements from Minnesota show albedo evolution through a winter season

Vis

NIR

%

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Case Study: Dust and Rain on Snow

3/15/2025

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3/13

Pre Dust Event

3/15

During Dust Event

3/17

Post Dust Event

Case Study: Dust and Rain on Snow

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  • 3/13 – limited surface melting
  • 3/15 – extensive surface melting, wet and dry deposition of dust
  • 3/17 – limited surface melting, visibly dusty surface

Case Study: Dust and Rain on Snow

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Dust on Snow – April 11, 2019 in Northfield, MN

https://cimss.ssec.wisc.edu/goes/blog/wp-content/uploads/2019/04/190410_190411_goes16_splitWindow_Central_US_blowing_dust_anim.gif

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As the Western US becomes drier, these types of events could become more common.

“The map built with data from the Drought Monitor, depicts areas of drought in progressive shades of orange to red on December 8, 2020.”

NASA Earth Observatory

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Sneak Peek!

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Sneak Peek!

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Sneak Peek!

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Studying snow in the Midwest!

Measuring snow albedo

Measuring

snow depth

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Measuring

grain size

Measuring

snow density

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Collecting snow samples for impurity analysis

Measuring

snow liquid water content

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Research in Greenland

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Jobs in Polar Science

  • Researchers (Students, Professors, National Lab Scientists)
  • Engineers
  • Science Techs
  • Logistics Coordinators
  • Program Managers
  • IT Specialists
  • Communicators (Writers, Artists)
  • Policy Makers
  • Santa Claus

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There are many ways to be involved in studying climate change or developing solutions!

The more people we have involved in addressing this complex challenge, the better!

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Questions?

THANKS FOR COMING!

ALDEN ADOLPH, MICHIGAN TECHNOLOGICAL UNIVERSITY

ACADOLPH@MTU.EDU

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Teaching about albedo!

  • Ice Drilling Program (https://icedrill-education.org/) Activity

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Teaching about albedo!

  • Virtual Field Lab in the works!
  • Coming in 2025