1. What makes high latitude fluxes different from more equatorward?
Frequent high winds
Frequent large ΔT, Δq
From Sampe and Xie,
BAMS, Dec 2007

2. Observations at high winds
Despite over 7000 hours of ID and Covariance fluxes in ETL database, only 133 & 85 hours are for U > 15 m/s (Fairall et al 2003)
So a lack of flux obs. under high winds is synonymous with lack of flux obs. at high latitudes.

3. Low-level (30-50 m) flights from Greenland Flow Distortion experiment
- Feb-Mar 2007
- Thicker lines = low-level

6. Scatter at high winds is large
Probably still not enough in situ observations at high windspeeds

7. 2A) Are all flux parameterizations similar in their estimates of fluxes?
- Below leg 6 from B276 flight on GFDex, over water.

8. Fluxes over ice
Over MIZ and sea ice there appears to be even more scatter in covariance observations and even fewer observations available.
Below from GFDex; next few pages from recent Antarctic campaign

9. Hot off the press…
February 2008 fieldwork by Emma Fiedler (UEA) in collaboration with BAS

10. Coastal Polynya Aircraft Observations

14. Results
Decrease in sensible heat flux with fetch due to reduction in air-surface temperature difference
– warming of the CIBL
– surface temperature decrease

15. Results
Decrease in sensible heat flux with fetch due to reduction in air-surface temperature difference
– warming of the CIBL
– surface temperature decrease

16. Transfer coefficients
Consider only values from lower level legs due to the increased scatter at higher level
Mean values same (flights 24hrs apart)
CDN10 = 1.0 x 10-3
CHN10 = 6.8 x 10-4
Values are at lower end of previous observations
No significant linear trend with fetch

17. Is there a variation with surface characteristics?
Only the two lowest level legs were considered as the data is more reliable
There is no significant difference between the means of the coefficients for the two regimes (F54 to 30km, F57 to 55km)
As an indicator of surface ice type, the relationships between CD and CH with albedo and surface temperature were examined
No significant linear trends found (r2 values ~0.1)
Split into the two regimes, no clear distinction
At surface temperatures above
~-10 oC and albedos below ~0.4 there may be a linear relationship (but limited data)

18. Fluxes over ice
Ice concentration, thickness and type possibly important for flux estimates
But hard to observe & model
Most models set 1 exchange coefficients for sea ice, and possibly 1 for MIZ.