Sea ice
Sébastien Barrault Safety Course January 2008
Content
• UNIS & Sea ice
• Ice location & Dynamics
• Sea ice physics
• Scale and Ice feature
• Sea ice extent around Svalbard
• Decay
• Useful links
Sea ice & UNIS
Barrault Haig
• Cruises on research vessels
• Snow scooter driving on ice
Sea ice in the northern hemisphere
Ice dynamics
• Triple point – 3 phases are in equilibrium: T = 273.16 K, p = 611.7 kPa
• H2O expands on freezing
• Other examples: Silicone, germanium
• The crystals reveal the hexagonal symmetry of the crystal lattice of ice (0°C< Ih<- 80°C)
• Basal plane with hexagonalsymmetry and c-axis
Continuous molecular structure
(Løset et al., 2006)
Initial discs, size ≈1 mm Stellar ice crystals Growing of isolated crystals
(Løset et al., 2006)
New ice Recently formed ice:
¾Frazil ice
¾Grease ice
¾Slush
¾Shuga
Nilas ¾Dark nilas < 5 cm thick.
¾Light nilas > 5 cm thick.
Pancake ice Circular pieces of ice 0.3-3 m in diameter, up to about 10 cm in thickness.
Young ice Ice in the transition stage between nilasand first-year ice, 10-30 cm thick.
¾Grey ice 10-15 cm thick.
¾Grey-white ice 15-30 cm thick.
First-year ice Developing from young ice, thickness 0.3 m –2 m.
¾Thin FY ice: 0.3-0.7 m thick
¾Medium FY ice: 0.7-1.2 m thick.
¾Thick FY ice: over 1.2 m thick.
Old ice ¾Second year ice: < 2.5 m thick.
¾Multi-year ice: up to 3 m or more thick
Ice growth: definition
Barrault Barrault Barrault
• No snow
• No radiation
• No heat transfer from the ocean, qocean= 0
• A linear temperature profile through the ice sheet
• qice = -kΔT/ Δ z
• qlatent = qice = qsurface
l –latent heat of fusion (333.4 kJ/kg) ρ –density of ice (917 kg/m3)
k –thermal conductivity (2.2 W/m°C)
i s f
ice h
T kT
q −
−
=
dt ldh
qlatent =ρ i
qocean = 0 qsurface
Ta
Ts
ice air
water T
hi dhi z
FreezingDegreeDays [°Cdays]
Ice growth: Stefan’s law
Tf
l –latent heat of fusion (333.4 kJ/kg) ρ–density of ice (917 kg/m3)
k –thermal conductivity (2.2 W/m°C)
Ice growth: Stefan’s law
Ts= -10C
C. E. Bøggild (2007)
H ∼ t
Structure of sea year sea ice
(Løset et al., 2006)
1000 g of sea water contains:
23.5 g NaCl 4.5 g MgCl
23.9 g Na
2SO
41.1 g CaCl
2+ rest
34.5 g of salt
Sea icelanguage : 34.5 psu or ppt
Chemical composition of sea ice & Freezing point
T
f= - 1.86°C Freezing point vs salinity:
T
f( ° C) = -0.0539 ⋅ S(psu)
Salinity profile
C - shape
-70 -60 -50 -40 -30 -20 -10 0
0 1 2 3 4 5 6 7 8
Salinity [psu]
depth [cm]depth[cm]
-1,3 -1,2 -1,1 -1 -0,9 -0,8 -0,7 -0,6 -0,5 -0,4 -0,3 -0,2 -0,1 0 0,1 0,2 0,3 0,4 0,5 0,6 0,7 0,8 0,9 1 1,1 1,2
-25 -20 -15 -10 -5 0
Temperature (Deg C)
Depth (m)
Temperature profile
Scales in sea ice research
• microscale 10
-4- 10
-1m physics
• local scale 10
-1- 10
1m engineering
• floe scale 10
2- 10
3m
• mesoscale 10
4- 10
5m geophysics
• large scale 10
6m geophysics
Moslet
Barrault
Barrault Løset
Ice Ridge, NW Barents Sea –drift ice
Ice floes – drift ice Iceberg, Franz Josef Land – drift ice
Landfast ice, Franz Josef Land
Marchenko
Løset Marchenko
Ice features
FY ice ridge
wind
sail keel
Ice blocks, Ridge Sail
Ice rubble-blocks, Ridge Keel
Shafrova
Ice ridge
FY
SY MY
Ice cover zones of different dynamic character:
• Landfast ice
• Shear zone
• Marginal ice zone (MIZ)
• Central pack
Ice floes in MIZ zone
0 10 20 30 40 50
0 20 40 60 80
Distance from the ice edge (km)
Mean floe size (m)
Transition zone Interior Edge
(Løsetet al., 1989)
Drift ice divided as:
Description of drift ice
(Løsetet al., 2006)
Sea ice extent around Svalbard
DNMI data (IDAP report, 1994) USSR Atlas of the Oceans, 1980
August, September
(USSR Atlas of the Oceans, 1980)
April September
Sea ice extent around Svalbard in 2004
7 Dec2003
12 Jan 2004
17 Feb2004 27 May 2004
13 May 2004 14 Apr2004
22 Jun 2004
11 Aug2004
6 Sep 2004
Sea ice decay
Norwegian Meteorology Institute
• http://met.no/kyst_og_hav/iskart.html (ice maps)
Also on:
W:\COURSE MTR & DATA StudentsReadOnly\Common Data Library
UNIS entrance