collaborative research on sunlight and the arctic atmosphere-ice-ocean system ( aios )
DESCRIPTION
Collaborative Research on Sunlight and the Arctic Atmosphere-Ice-Ocean System ( AIOS ). Hajo Eicken Univ. of Alaska Fairbanks. Bonnie Light Univ. of Washington. Ron Lindsay Univ. of Washington. Rebecca Woodgate Univ. of Washington. Kay Runciman Univ. of Washington. Jeremy Harbeck UAF. - PowerPoint PPT PresentationTRANSCRIPT
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Collaborative Research on Sunlight and the Arctic Atmosphere-Ice-Ocean System (AIOS)
Hajo EickenUniv. of Alaska
Fairbanks
Ron LindsayUniv. of Washington
Bonnie LightUniv. of Washington
Rebecca WoodgateUniv. of Washington
Don PerovichCRREL
John WeatherlyCRREL
Kay RuncimanUniv. of Washington
The AIOS sunlight team
Jeremy HarbeckUAF
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Sunlight and the Arctic AIOS
Goals1. Enhance our understanding of the present role that solar radiation plays in the Arctic AIOS2. Improve our ability to predict its future role.
Objectives1. Determine the spatial and temporal variability of the partitioning of solar energy.2. Understand how changes in sea ice, snow cover, and cloudiness will affect the solar
partitioning and the resulting impacts.3. Assess the impact of seasonal, interannual, and decadal variability on absorbed sunlight.4. Establish if the variability of solar heating corresponds to the dominant modes of large-scale
variability (e.g., Arctic Oscillation). 5. Evaluate and improve the treatment in models of solar energy in the Arctic AIOS.
Where does all the sunlight go?
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Solar partitioning Determine solar energy
• Incident on surface• Reflected to atmosphere• Absorbed in snow and ice• Transmitted to ocean
Reflected
Absorbed
Transmitted
Atmosphere
Ice
Ocean
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Temporal and spatial variabilityMay
June
July August September
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Key products and parameters
Pan Arctic…from 1987 to present
• Description of solar partitioning • Monthly values from 1987 to 2007 of
• Incident solar energy• Reflected solar energy• Absorbed in snow and ice, • Transmitted to ocean
• Spectral, integrated, PAR • Pan – Arctic over ocean • All on 25 x 25 km EASE grid (Equal Area Scalable Earth)
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Approach
Integrative and synthetic
• Combine observations and models• Iterative process• Observations
• Satellite data• Field results• Laboratory studies
• Models• Process (ponds, clouds, bio…)• Radiative transfer• Ice – ocean• Global climate
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Incident solar radiation
Field observations, satellite data, reanalysis, RT models
Courtesy of A. Schweiger
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Albedo – large-scale
Large-scale from satellite
1982
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Albedo – evolution
1. Dry snow: albedo of 0.85.2. Melting snow: linearly decreasing albedo (0.80 to 0.71).3. Pond formation: linearly decreasing albedo (0.67 to 0.50).4. Pond evolution: remainder of melt season - linearly decreasing albedo (minimum of 0.20).5. Fall freezeup: albedo linearly increases to 0.85.
Dry snow Fall freezeupPond evolutionM
elti
ng
sn
ow
Po
nd
fo
rma
tion
Details from field observations and models
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• Optical observations from SHEBA• SHEBA data indicate
• larger transmittance to ocean• some near infrared transmittance
• Plane parallel radiative transfer model • Includes vertical variation• Inherent optical properties
• Absorption coefficient• Scattering coefficient• Phase function
• Compare to CCSM3 parameterization
Light transmission
Observations, radiative transfer models,GCM parameterizations
100 W m-2 incident
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Ice extent, type and concentration
Satellite data
No data Land Ocean Melt First-year Mixed-ice Multi-year
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Snow cover climatologyData sources include:• High-Latitude Airborne Annual Expeditions• North Pole Drifting Ice Stations• Coastal Stations: Canada, U.S., Russia• Field Experiments (ARK, SHEBA, etc.)
North Pole Stations (1937-1991)
Products:•Monthly means and distribution•Dates of
• first snow, • onset of melt, • snow removal• fall freezeup
Field observations, reanalysis, satellite
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Vertical meltwaterpercolation
Melt ponds• Pond evolution is a key to solar partitioning
• Albedo is smaller and changing• “Skylight” to ocean
• Pond physical evolution controlled by• Surface meltwater production• Ice topography• Ice permeability
• Couple pond hydrology model with• Surface topography statistics• Melt rate data• Optical observations• Radiative transfer model
Significant uncertainty in pond evolution
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Influx of upper ocean heat
Recent results indicate Bering Strait fluxes increased from 2001 to 2004
• Heat – melt 640,000 m3
• Volume - 0.7 to 1.0 Sv• Freshwater – 800 km3
Ocean heat input is considerable
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Ice – ocean• Drive Arctic stand-alone CCSM ice-ocean model with collected solar data • Investigate impact of ice-albedo feedback on ice-mass balance. • Assess decadal variability in solar heating of the Arctic A-I-O
Global climate model•Assess variability in solar heating – control climate versus IPCC scenarios.• Compare model changes in net sunlight and mass balance to A-I-O model
Large – scale modeling
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Outreach
Synthesize and collaborate
Scientific community• Archived datasets• Web site
• Map based• One click to data
• Integrated datasets will benefit• Sea ice mass balance• Oceanography• Atmospheric chemistry• Large-scale modeling• Future field planning
Public• General interest article on ice-albedo feedback• K-5 synthesis puzzles
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End of slideshow