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Southern Globec: Snow and Ice Studies
photo D. Costa D. Martinson, R. Smith, D. Perovich, B. Elder, S. Stammerjohn, K. Claffey Chris Fritsen, Jeramie Memmot, Sarah Marshal, Angela Gibson, Shonna Dovel
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Snow and Ice measurements
Snow and ice varies spatially and evolves temporally Interested in ice cover as a habitant barrier Snow and ice physical properties Snow and ice optical properties Time series - buoys
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Physical properties: bridge watch
Hourly observations ASPECT protocol Ice type,thickness,fraction Mean thickness = 46 cm Mean concentration ~ 0.8
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Physical properties: surveys
Measured every meter snow depth ice thickness freeboard flooded layer interface temperature Selected sites snowpits ice cores Robert 6 August 2001 Snow depth Mean = 23 cm Standard deviation = 9 Range = cm Ice thickness Mean = 71 cm Standard deviation = 50 Range = cm 67 % flooded
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Physical properties: surveys
6 August 9 August
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Physical properties: surveys
Summary of 400+ holes Snow depth Mean / median = 16 / 11 Standard deviation = 11 Ice thickness Mean / median = 62 / 44 Standard deviation = 44 Freeboard Mean/median = -0.9/ 0.0 Standard deviation = 9.5
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Physical properties: snowpits
Selected snowpits Vertical profiles of temperature density grain size grain type Mean density = .25 g cm-3
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Physical properties: ice cores
Profiles of - T,S, nb - structure - crystallography - d O18 About 30 sites Date: 28 July Event 21 Lat. 66o 21'.6 S Long. 70o 43'.1 W Thickness: 33 cm Granular: 58% Columnar: 42%
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Optical properties “Fernando” 11 August (1300) Snow depth = 28 cm
8 cm of new snow 20 cm of slush. Ice thickness = 44 cm Peak ~ 490 nm Ice is “clean”
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Optical properties TR-6 Robert 6 August 2001 Mean transmittance
- PAR: - UV-B:
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Time series: buoys 4 buoys 2 simple barometric pressure position
air temperature 2 complex, have in addition snow depth ice thickness ice temperature ocean temperature spectral irradiance Enlarged Area August 2001 November 2001
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Time series: buoys Robert 6 August 2001 Latitude = 68o 04
Longitude = 70o 13 20oC changes common Major snowfall Little change at ice bottom Air Snow Water
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Time series: ice growth
Lots of snow, 130 cm Little change at bottom What if? Negative freeboard => flooding => ice growth Air Snow Ice Ocean
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Time series: light levels
3 irradiance sensors Above ice, below ice, in ocean Each sensor had 4 wavelengths (412, 442, 491, and 555 nm) Steady increase in incident Peaks, valleys => sunny, cloudy Decrease in transmittance => increase in snowdepth
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Summary Ice is a mess! Granular ice common Flooding and freezeback
Surface growth of ice Mean snow depth = 16 cm Mean ice thickness = 62 cm Light transmittance < 1% Peak of 2-5% at ~ 490 nm Time series 1 m of snowfall 60 cm of snow-ice? Steady increase in incident Not in transmittance
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