Arctic sea ice melt in summer 2007: Sunlight, water, and ice NSIDC Sept 2007.
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Transcript of Arctic sea ice melt in summer 2007: Sunlight, water, and ice NSIDC Sept 2007.
A long list of suspects
Examine the mass balance of the ice
• Warmer air temperature• Longer melt season• Winds• Export of perennial ice• Advection of ocean heat• Clouds• Enhanced solar heating• Ice albedo feedback
Sea ice mass balance
Simple, but powerful observation
• Simple concept• ice growth• surface melt• bottom melt
• Equipment• ablation stakes and thickness gauges• autonomous buoys
• Powerful tool – attributes change
Above
Below
Monitoring the mass balance
Observations in Beaufort and North Pole
http://www.crrel.usace.army.mil/sid/IMB
Beaufort Sea buoy
End of August – peak bottom melt
20-4040-60
60-80
80-100
150 km
August 27
• Warmer air temperature• Longer melt season• Winds• Export of perennial ice• Advection of ocean heat• Clouds• Enhanced solar heating• Ice albedo feedback
Estimate of solar heating
Incident solar, ice concentration, and albedo -> heat input
Focn = Fr (1 – ) (1 – C)
Input:• 25 x 25 km equal area grid • Incident (Fr) from ERA-40, ECMWF• Ice concentration (C) - SSMI• Water albedo () = 0.07
Output:Solar input to the ocean (Focn)
Neglect ice for now
Mean annual input: 1979 – 2005
Ice edge evident, concentric rings from solar input
MJ m-2
3 MJ m-2 = 1 cm m-2 of ice melt
Percent anomaly in 2007
Heat input near buoy 400 to 500 % greater
through 22 Sept 800
700
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300
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0
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Percent
Conclusions
Was there a trigger?
• North Pole• business as usual
• Beaufort Sea• typical surface melt• huge bottom melt
• Solar incident comparable• Ice concentration much less• Solar input twice melt• Ice albedo feedback
Total solar heat input to ocean
Heat input near buoy from 600 to 800 MJ m-2
through 22 Sept 2007Units = MJ m-2
3 MJ m-2 ~ 1 cm thinning
Incident shortwave anomaly
Not much of a difference
• Incident shortwave from reanalysis • Pan – Arctic Ocean• 25 x 25 km equal area grid• Average 1979 – 2005
(2007 – average) % anomaly
%