Sea ice: physical properties, processes and trends. Stephen Howell Climate Research Division, Environment and Climate Change Canada July 18, 2017
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1 Sea ice: physical properties, processes and trends Stephen Howell Climate Research Division, Environment and Climate Change Canada July 18, 2017
2 3-Part Sea Ice Lecture Overview 1. Physical properties, processes and trends 2. Observations 3. Canadian Arctic Page 2 July 18, 2017
3 Outline Introduction Ice types Seasonal cycle Sea ice dynamics Snow on sea ice Recent trends Page 3 July 18, 2017
4 Introduction: global distribution Sea ice is any form of ice that is found at sea and has originated from the freezing of sea water On average, sea ice covers about 25 million km 2 of the Earth, or about two-and-a-half times the area of Canada Arctic Min: 7 million km 2 * Max: 15 million km 2 Antarctica Min: ~3 million km 2 Max: 18 million km 2 Page 4 July 18, 2017
5 Introduction: importance 1. Has a high albedo and this keeps the planet cool. 2. Fills a central role in the lives and customs of Inuit. 3. Provides a place for polar bears, seals, and other animals to live. 4. Influences ocean circulation. Does not raise sea level when it melts, because it forms from ocean water. NSIDC Page 5 July 18, 2017
6 Sea Ice Types
7 Sea ice types New Ice: Recently formed ice composed of ice crystals that are only weakly frozen together (if at all) and have a definite form only while they are afloat. Nilas: A thin elastic crust of ice (up to 10 cm in thickness), easily bending on waves and swell and under pressure growing in a pattern of interlocking "fingers" (finger rafting). Young Ice: Ice in the transition stage between nilas and first-year ice, cm in thickness. Page 7 July 18, 2017 CIS
8 Sea ice types First-Year Ice: Sea ice of not more than one winter's growth, developing from young ice, with a thickness of 30 cm to ~2 m. Page 8 July 18, 2017
9 Sea ice types Multi-year/old ice: Sea ice that has survived at least one summer's melt. Hummocky topography from freeze-thaw. Page 9 July 18, 2017
10 Sea ice types Multi-year/old ice: Sea ice that has survived at least one summer's melt. Hummocky topography from freeze-thaw BUT can be heavily ridged. Page 10 July 18, 2017
11 Sea ice microstructure First-year ice: Winebrenner et al., 1988 Page 11 July 18, 2017
12 Sea ice microstructure Multi-year ice: Winebrenner et al., 1988 Page 12 July 18, 2017
13 Sea ice concentration Given in tenths e.g. 10/10 is 100% covered Extent = concentration 1.5/10 x area Coverage = concentration x area MANICE Page 13 July 18, 2017
14 Seasonal Cycle
15 The seasonal cycle of Arctic sea ice: extent Page 15 July 18, 2017 University of Bremen/NASA
16 The seasonal cycle of sea ice: thickness Page 16 July 18, 2017 Maykut and Untersteiner, 1971
17 The seasonal cycle of sea ice: snow Page 17 July 18, 2017 Matthew Sturm
18 The seasonal cycle of sea ice: snow Snow cover acts as a blanket, slowing down the flow of heat from the water. Snow cover plays an important role during ice growth. This is because its large air content makes it a poor conductor of heat (but a good insulator) with a thermal conductivity between 0.1 and 0.4 Wm -1 K -1 compared to 2 Wm -1 K -1 for sea ice. Page 18 July 18, 2017
19 The seasonal cycle of sea ice: snow Page 19 July 18, 2017 Howell et al., 2016
20 The seasonal cycle of sea ice: albedo Page 20 July 18, 2017 Perovich et al., 2002
21 The seasonal cycle of sea ice: albedo feedback The transition to melt conditions is directly related to the albedo of the surface warming of the snowpack. Page 21 July 18, 2017 NASA
22 The seasonal cycle of sea ice: timing of melt and freeze onset Page 22 July 18, 2017 Perovich et al., 2011
23 Sea Ice Dynamics
24 Sea Ice Dynamics Page 24 July 18, 2017
25 Sea Ice Dynamics The exchange of momentum due to turbulent process controls sea ice motion. most important related processes are divergence and convergence. Page 25 July 18, 2017 C. Haas
26 Sea ice dynamics: divergence Leads result from local ice divergence creating long narrow channels also induced by tides. Flaw leads form along the edge of landfast ice and the polar pack. Page 26 July 18, 2017
27 Sea ice dynamics: convergence Mean thickness of a region is more dependent on the number (and thickness) of ridges than the thickness of level ice The overall volume within an ice region, dynamics are more important than thermodynamics Page 27 July 18, 2017 Kwok and Cunningham, 2015
28 Trends
29 Arctic sea ice trends: extent September Arctic sea ice is declining at a rate of 13.3% per decade over the period. The ten lowest September ice extents over the satellite record have all occurred in the ten years. Page 29 July 18, 2017 NASA/NSIDC
30 Arctic sea ice trends: 2017 extent Page 30 July 18, 2017
31 Arctic sea ice trends: thickness Arctic sea ice volume between Page 31 July 18, 2017 Kwok and Cunningham, 2015
32 Arctic sea ice trends: age Page 32 July 18, 2017 NSIDC
33 Arctic sea ice trends: age Page 33 July 18, 2017 NASA
34 Arctic sea ice trends: melt/freeze All Arctic: melt onset earlier by 2 days per decade, freeze onset delayed by 3 days per decade and melt season length is increasing at 5 days per decade. Page 34 July 18, 2017 Stroeve et al., 2014
35 Next Lecture: Observations Page 35 July 18, 2017
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Ice-Albedo Feedback Process in the Arctic Ocean Donald K. Perovich John Weatherly Mark Hopkins Jacqueline A. Richter-Menge U. S. Army Cold Regions Research and Engineering Laboratory 72 Lyme Road Hanover
The Seasonal Evolution of Sea Ice Floe Size Distribution
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. The Seasonal Evolution of Sea Ice Floe Size Distribution Jacqueline A. Richter-Menge and Donald K. Perovich CRREL, 72 Lyme