One implication of climate change is sea level rise. Sea level is the average height of the ocean relative to the land, between the high and low tides. The rising global temperature is causing both land ice and sea ice to melt.
Land ice and sea ice are not the same. They form differently, and the consequences of their melting affect the planet in different ways.
Land ice – glaciers, ice shelves and ice sheets
Glaciers, ice shelves and ice sheets are land ice. They are all masses of frozen freshwater and are named for their different sizes and locations.
Glaciers are bodies of ice formed from snow that has accumulated and been compacted over long periods of time. They form in mountainous areas and high latitudes. Glaciers are found on every continent except Australia.
Ice shelves are masses of thick glacial ice that extend from the coastlines and float on the sea. Ice shelves are only found in Antarctica, Greenland and the Arctic.
Ice sheets are large masses of glacial ice on the land. To be called an ice sheet, ice must cover more than 50,000 km2. Ice sheets are only found in Antarctica and Greenland.
To put this all in context, there are several glaciers that make up the Ross Ice Shelf, which is part of the larger Western Antarctic Ice Sheet.
Sea ice is frozen seawater. It forms, grows and melts in the sea. Sea ice forms more slowly than freshwater ice due to a combination of factors. First, the freezing point of saltwater is lower than freshwater. The seawater temperature must get down to -1.8°C. It often takes longer to reach this temperature because, as seawater cools, it sinks. The top 100–150 m of seawater often needs to cool to -1.8°C for ice to form.
Sea ice is found in both the Arctic and Antarctic regions, with some areas covered in sea ice year round. Sea ice forms during the winter, and some of it melts during the summer. It is often covered by snow.
Melting ice and sea level rise
Melting land ice leads to sea level rise, whereas melting sea ice has minimal impact. To understand why this is, imagine a jug of ice and water. As the ice warms and melts, the total volume of water in the jug does not change, so the water level stays the same. It’s the same with sea ice – when it melts, it does not change the volume of water in the sea.
Melting land ice is different. It adds water to the sea. This is similar to adding more water to the jug of ice and water. The volume of water in the jug increases – and will overflow if too much is added.
Although melting sea ice does not cause sea level rise, it does have other implications for the global climate. Sea ice has a light-coloured surface and reflects some of the sunlight that hits it. When sea ice melts, it exposes the darker sea surface, which absorbs solar energy (heat). This causes further temperature rises and causes more ice to melt.
Thermal expansion and sea level rise
Warming seawater also causes sea level rise. Water expands when it warms up – heat energy makes its molecules move around more and take up more space. Because the molecules are more spread out, the density decreases.
Climate change – additional implications
The ocean is a complex and continuous body of water that covers two-thirds of our planet. Melting land and sea ice affect many of the properties that drive the ocean’s chemical, physical and biological processes. Read about the properties – and the impacts climate change will cause – in the articles Ocean temperature, Ocean density, Ocean salinity and Ocean motion (currents and circulation).
Nature of science
For most of history, the only way to study sea ice was through fieldwork. It was costly and dangerous work. Remote sensing via satellites has progressed scientific knowledge immensely. However, scientists still conduct fieldwork to validate (verify) the accuracy of satellite measurements and climate models.
The Hub has three simple melting ice and climate change-related activities:
Collection of related content
The Science Learning Hub team has curated a collection of resources related to climate change. Login to make this collection part of your private collection, just click on the copy icon. You can then add additional content, notes and make other changes. Registering an account for the Science Learning Hubs is easy and free – sign up with your email address or Google account. Look for the Sign in button at the top of each page.
Dr Mike Williams, physical oceanographer at NIWA, explains the importance of sea ice in the video Sea ice and climate change.
The NZ SeaRise: Te Tai Pari O Aotearoa programme has released location specific sea level rise projections out to the year 2300 for every 2 km of the coast of Aotearoa New Zealand. This very informative site includes maps (you can find the possible impact on your local area) and there are resources such as posters and videos.
See NIWA’s Sea levels and sea-level rise it has lots of information including: how sea levels are measured, what is contributing to rising sea levels, future rise projections and why we should worry.
NASA has numerous articles and updates about climate change and ice shelves.
The National Snow & Ice Data Center has a series of articles: All About Sea Ice.
The Ministry of Education's Climate Change Learning Programme is a level 4 programme focused on climate change that includes specific student activities; the wellbeing guide focuses on student wellbeing and hauora when navigating climate change as an area of learning and action. Many of the suggestions are relevant to other learning levels.
Scientists continue to research climate change from the unique clues that the Antarctic environment holds. Discover more about Victoria University of Wellington’s Antarctic Research Centre Te Puna Pātiotio's key research areas and how they approach them. The team won the 2019 Prime Minister’s Science Prize.
NASA's Eyes on the Earth site shows the positions of their Earth observation satellites. Use the tabs at the bottom of the page to filter for greenhouse gases and other measurements, such as sea level.