Sea ice facts for kids
Sea ice is simply frozen ocean water. It forms, grows, and melts in the ocean. In contrast, icebergs, glaciers, ice sheets, and ice shelves all originate on land. Sea ice occurs in both the Arctic and Antarctic.
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Description of Sea Ice
Because sea ice is made of frozen seawater, it is salty (unlike icebergs). Sea ice generally grows in the winter (when it is often dark all day and night) and melts in the summer (when there is twenty-four hour daylight). Sea ice normally covers more area near in the Antarctic than the Arctic. Because the ice is salty, sea ice is heavier, less transparent and easier to break than ice that isn't salty.
Sea Ice Mechanical Properties
The 'mechanical properties' of sea ice refer to how easy it is to bend, break, squash and stretch the ice. This behaviour is dominated by the fact that sea ice is not entirely solid - instead it contains lots of tiny pockets of salt water. Older ice also often contains many air bubbles. This makes it much easier to squash, break and snap than a normal ice cube in a drink.
When two pieces of sea ice squash up against each other, they can crumple up and break to form a 'ridge' at the part where they touch. Before doing this they might bend. It is also relatively easy to pull apart a single piece of sea ice by pulling opposite edges in opposite directions.
Sea Ice Optical Properties
Because sea ice has air bubbles and saltwater pockets inside it, it is much harder to see through than non-salty, clear ice. This is because light can't go through it without hitting the bubbles and pockets. Most sea ice in winter is covered by a layer of snow, which you also can't see through. All this means that when the sun shines on sea ice, not much of its light gets through to the sea below the ice. This limits the amount of algae and tiny plants that can grow in the sea. This is important because when the ice melts, much more light gets through and the algae and tiny plants can then thrive. This effect also keeps the sea below cooler.
Importance to the people that live in the Arctic
Around four million people live in the Arctic, with many of them living near the sea . Many of these people have lived here for centuries, and have learned to use and depend on the sea ice to live. In particular, coastal residents of the Arctic travel over the sea ice and use it to hunt animals. This hunting is done both for food and to make clothes. Because some people spent a lot of their lives on the ice, it becomes very important to them and their communities.
Importance to the animals that live in the polar regions
May animals live on top of and under the sea ice. It makes life more difficult for some, but less difficult for others. Animals like seals and polar bears exist both on top of the sea ice, but also swim in the sea. Because microscopic plants and algae don't grow well under the sea ice because they need the sun, the animals that eat them (like fish) also spend less time under the ice.
Importance to the climate
Although it's not smooth like a mirror, sea ice is very shiny. Most of the sunlight that hits it bounces off and shines back into space. By not absorbing a lot of sunlight, the poles stay cold. Having cold regions near the top and bottom of the earth is important for global weather, because it affects the way cold and warm air moves around. When cold air moves down from the Arctic, it can cause very serious storms. When warm air moves up into the Arctic, it can cause the sea ice to melt and break up.
Sea ice also acts as a barrier between the sea and the air. In the rest of the world, water is often evaporating from the sea to the air. Eventually when the air fills up with water, it rains. Sea ice strongly reduces this transfer, so the air is very dry and it doesn't rain or snow very much.
Sea ice also reduces the amount of heat that flows from the sea to the air.
Sea ice is important for the mixing of the sea surface. When wind blows over the sea, it stirs the water and mixes it up. However when wind blows sea ice around, this mixing is much deeper, and the strength can change. This mixing is important because it affects the lives of microscopic animals that live at the sea surface, and it also affects how salty it is at the sea surface.
Sea ice is changing
Human beings have been releasing a lot of greenhouse gases, which have been making the earth warmer. The Arctic in particular has been getting much warmer. One reason for this is because sea ice formation and melting is very sensitive to temperature changes. When the air is warmer, sea ice grows slower and melts faster.
These temperature rises mean that the sea ice begins growing later in the year, and begins melting earlier in the year. It also means that the area of sea ice is decreasing.
Satellites and Sea Ice
Going to the sea ice is difficult and sometimes dangerous. This makes it impossible to keep track of all the sea ice at once and see how its changing. To solve this, scientists often look at sea ice from space using satellites. There are many ways to do this. Some satellites use cameras that work similarly to common consumer ones. Others make pictures of the sea ice using microwave energy that can go through clouds. Some don't just look at the ice, but send down energy from laser and radar machines and then record how it bounces off the ice.
These satellites allow scientists to measure the area covered by sea ice relatively well. However they are still relatively unsure how thick the sea ice is, in part because it is unclear how much snow is resting on the ice at any one time. Measuring the amount of snow that exists on sea ice is difficult, European scientists are currently designing a new satellite called CRISTAL to help study it.
Images for kids
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Nilas in Baffin Bay
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Satellite image of sea ice forming near St. Matthew Island in the Bering Sea.
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Volume of arctic sea ice over time using a polar coordinate system draw method (time goes counter clockwise; one cycle per year)
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As ice melts, the liquid water collects in depressions on the surface and deepens them, forming these melt ponds in the Arctic. These fresh water ponds are separated from the salty sea below and around it, until breaks in the ice merge the two.
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Aerial view showing an expanse of drift ice offshore Labrador (Eastern Canada) displaying floes of various sizes loosely packed, with open water in several networks of leads. (Scale not available.)
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Aerial view showing an expanse of drift ice in southeastern Greenland, comprising loosely packed floes of various sizes, with a lead developing in the centre.(Scale not available.)
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Aerial view showing an expanse of drift ice consisting mostly of water. (Scale not available.)
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Close-up view inside a drift ice zone: several small rounded floes are separated from each other by slush or grease ice. (Bird at lower right for scale.)
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Example of hummocky ice: an accumulation of ice blocks, here about 20 to 30 cm (7.9 to 11.8 in) in thickness (with a thin snow cover).
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Field example of a pressure ridge. Only the sail (the part of the ridge above the ice surface) is shown in this photograph – the keel is more difficult to document.
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Aerial view of the Chukchi Sea between Chukotka and Alaska, displaying a pattern of leads. Much of the open water inside those leads is already covered by new ice (indicated by a slightly lighter blue color)(scale not available).
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Sea ice off Baffin Island.
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Sea ice imitates the shoreline along the Kamchatka Peninsula.
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Clear view of the Antarctic Peninsula, the Larsen Ice Shelf and the sea ice-covered waters around the region.
See also
In Spanish: Banquisa para niños
