Part 1: Ice Thickness Calculation
Background:

On January 8th, 2020, the Polarstern was officially farther away from civilization than the International Space Station, which orbits at an altitude of ~400 km (~250 miles) above the Earth's surface! This extreme isolation means that there must be a plan in place in case there is an emergency on the ship where someone needs to be transported quickly back to land. In the photo above (taken by Michael Gallagher aboard one of the expedition helicopters), you can see the recently constructed runway that was built for small planes to land in case of such an emergency. The runway is 400 m (>1300 ft) long and 25 m (~82 ft) wide, and was cleared by a 'PistenBully,' a machine used to groom ski slopes. This might qualify as the world's most remote airplane runway! Photo Credit: Michael Gallagher
Instructions:
Airplanes are an important part of Arctic expeditions both in terms of resupplying the expedition and emergency management. Scientists use Gold's Formula, h=√(P/A), to calculate the ice thickness (h) that is needed to support the weight of something (P). A in this equation is a constant that is related to assumptions about the nature of the ice (is it very cold and hard, is it thawing and weak, or is it somewhere in between)? We recommend using 50 pounds per square inch for A, which is a conservative value for thawing (and thus the least strong) ice.
Part 2: Ice Watch
Background:
MOSAiC scientists participated in the “Ice Watch” program when sailing through the Arctic in transit to and from the Polarstern. The program required scientists to take turns gathering hourly observations of sea ice including the concentration, type, thickness, floe size, among other sea ice characteristics. These sea ice observations were reported to ice services (e.g., National Weather Service, National Ice Center, port authorities) and are used to improve sea ice charts and forecasts. Photo Credit: Anne Gold
Instructions:
There are 8 steps involved in doing an Ice Watch; however, you will be trained to gather sea ice observations related to only steps 2 and 3. Review the descriptions and images describing steps 2 and 3 below and then apply what you’ve learned in the following quiz to gather observations of sea ice!
- Identify a field of view
- Assess the Total Concentration of ice (fractional area/10)
- Identify the ice type(s) in the field of view
- Estimate partial concentrations
- Assess surface features: snow, topography, melt
- Assess thickness of ice and snow
- Any color in the ice?
- Look at the sky
Step 2
Assess the Total Concentration of ice (fractional area/10) - The total ice concentration is the fraction of ocean covered by any type of sea ice and is estimated in tenths (to the nearest 10%).

Figure 1. An Ice Watch observer determined that 9/10 or 90% of the field of view displayed in the image above is covered by sea ice. Reference: ASPECT training CD-ROM.

Figure 2. Use this figure as a guide to help estimate the total ice concentration for any field of view (in-person observation, photo, etc.) Reference: MANICE (Canadian Ice Service, 2005).
Step 3
Identify the ice type(s) in the field of view - This step in the Ice Watch protocol requires the observer to identify the ice type(s) visible in the field of view.
Figure 3. This figure shows photos of 11 different types of sea ice. There are often multiple types of sea ice present in the same field of view. Reference: Reproduced from ASSIST manual v4 (Hutchings, Delamere and Heil, 2016).

Frazil: Needle or plate shaped crystals that form from fresh water (e.g. refreezing ice melt water). They are suspended in the water, not coagulating together and form under calm conditions.
Grease: A thin skin of crystals coagulated on the sea surface. It has a dark, greasy appearance. Grease is the thin light-grey area between the white ice floes in the image above. Credit: Ted Maksym
Shuga: Spongy white lumps, a few centimeters in dimension. From in rough seas as crystals coagulate. Shuga is a precursor stage of development to pancake ice.
Pancakes: Predominantly circular pieces of ice from 30 cm - 3 m in diameter, and up to 10 cm in thickness, with raised rims due to the pieces striking against one another.
Nilas: A thin elastic crust of ice that forms in calm conditions. Ice easily bends on waves, swells and under pressure.
Grey Ice: 10-15 cm thick. Less elastic than nilas, it breaks under swell.
Grey White Ice: 15-30 cm thick. When under pressure this ice is more likely to ridge than grey-ice and nilas.
First Year Ice: 30 cm - 2 m thick. Ice with no more than one winters growth.
Multiyear Ice: Ice that has survived at least one summer’s melt. Most topographic features (ridges) are smoother than first year ice, as they become rounded in melt. Old ice appears whiter than first year ice.
Brash: Common between colliding floes or in regions where pressure ridges have collapsed. It is blocks of ice with dimensions less than 2 m.
Fast Ice: Held in situ by bathymetry, coastline, islands or grounded icebegrs. May encounter in the ocean if ice has been released into the drifting pack. In the Arctic, it has a similar thickness to first year and multiyear ice.