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Not just frozen water: Measuring snow’s nitrogen pulse Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

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Page 1: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

Not just frozen water:

Measuring snow’s nitrogen pulse

Sarah J. Nelson, University of MaineHannah Webber, SERC Institute

Ivan Fernandez, University of Maine

Page 2: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

“Snow on the ground is a dynamic medium.”

- Mark Williams, UC Boulder

See: http://snobear.colorado.edu/Markw/Intro/Snow/MtnSnowpack/snowpack.html

Page 3: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

Snowfall:

• Freshly fallen snow. • For example, 2.5 inches of snow fell

in Bangor on Feb. 27, 2010.

Page 4: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

Snowfall: Protocol 9

Page 5: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

Snowpack:

• Accumulated snow on the ground. • E.g., Snowpack

was 36 inches on Feb. 26, 2010.

www.arts.monash.edu.au

Page 6: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

Snowpack: Protocol 9

Page 7: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

Snow Water Equivalent (SWE):

• “the amount of water contained within the snowpack.

• It can be thought of as the depth of water that would theoretically result if you melted the entire snowpack instantaneously.”

www.or.nrcs.usda.gov/Snow/about/swe.html

Page 8: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

Snow water equivalent: Protocol 10

Page 9: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

Snow Density:

• the ratio of the volume of meltwater that can be derived from a sample of snow to the original volume of the sample.

• E.g., 1.2" water equivalent divided by 15" of snow = .08 density (= 8%).

Page 10: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

We will measure snow melt:Surface runoff produced from melting snow

Page 11: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

How much water?

Page 12: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

Stream stage: Protocol 8

ga.water.usgs.gov/edu/measureflow.html

Page 13: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

How much nitrogen through the snowmelt period?

Page 14: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

Nitrogen in stream water: Protocol 7

Page 15: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

Snowmelt is surface runoff, but

• By the time it’s in the stream, was are also measuring what has moved through the watershed (some soil signal, existing water in the stream)

• Other protocols deal with soils and watershed characteristics – these give students’ questions some dimension!

Page 16: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

Acadia Learning is a joint effort of the Schoodic Education and Research Center (SERC) Institute at Acadia National Park, the University of Maine, and Maine Sea Grant.

It is supported by:

• National Science Foundation (DEB 1056692)

• Maine Department of Education

• National Oceanic and Atmospheric Administration

• Private donors

Page 17: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

Watershed scale: snow cover

• Which places have snow, and how patchy is it?

www.nohrsc.nws.gov/interactive/html/map.html

Page 18: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

Density & SWE math

• Snow Density = Snow Depth / SWE Density must be in decimal form. For

example:  25% = 0.25 Density is usually specified in kilogram

per cubic meter (kg/m3). • The density of water is 1000 kg/m3 and snow

density is usually measured as a ratio to this. • So snow which is 100 kg/m3 is specified as

100/1000, or 10% (of the density of water). www.avalanche-center.org/Education/glossary

Page 19: Sarah J. Nelson, University of Maine Hannah Webber, SERC Institute Ivan Fernandez, University of Maine

What’s in that snow?

• Like rain, needs a condensation nucleus to form

• Then particles and gases can glom on as snow forms, grows, travels Snow crystal photos – check out:

http://www.its.caltech.edu/~atomic/snowcrystals/class/class.htm