Poles Are Melting, So What?

What really are the global consequences of melting ice caps and glaciers?

New research alarmingly points in the same direction: glaciers and ice caps are melting. The Arctic could become ice-free within the next decade. Antarctica is hitting record-low icy cover year after year, both for summer and winter. Glaciers in Antarctica are losing their structural integrity, which will accelerate their melting; Greenland has already lost more ice than we previously thought. These are not models; these are empirical observations.

Antarctic glacier comparison between January 24, 1973 and January 20, 2024. Images from NASA Earth Observatory

At first, you may be tempted to rub your shoulders and claim, “Who cares? It’s just less ice; this will not affect me.” But is it true?

We know that glaciers and ice caps are melting. What consequences could these trends have on human populations? Let’s dig deeper.

Sea Level Rise

The primary driver of the rise in sea level is the addition of water from melting land ice. But it is important to note that sea ice doesn’t have the same effect. Imagine you have ice cubes floating on water. Once they melt, the ice cubes are still in the water; they have just changed their state and won’t add any extra volume. On the other hand, land ice enters the ocean after melting on the continent, adding to the additional volume of ocean water on Earth.

As temperatures rise, these massive reservoirs of frozen water steadily shrink. The Intergovernmental Panel on Climate Change (IPCC) reports that glaciers are losing mass alarmingly, contributing significantly to rising sea levels. Projections suggest that under a high-emissions scenario, global sea levels could rise by up to 1 meter by 2100. This could displace millions of people and submerge low-lying coastal areas.

Chart showing Sea level rise predictions from NASA Earth Observatory
Sea level rise predictions from NASA Earth Observatory

The consequences of rising sea levels are far-reaching. Coastal communities, particularly those in developing nations, face the most impacts. Rising seas will inundate low-lying areas, displacing entire communities and destroying critical infrastructure.

Rising sea levels also threaten ecosystems and biodiversity. Inundated coastal wetlands, crucial habitats for diverse marine life, will lead to habitat loss and species extinction. Rising seawater can contaminate freshwater sources, impacting coastal agriculture and disrupting coastal ecosystems.

Beyond the immediate and local impacts, rising sea level has broader implications for the global climate. Melting glaciers disrupt ocean currents, which are vital in regulating global temperatures. This disruption can lead to unpredictable weather patterns, including increased frequency and intensity of extreme weather events like heat waves, droughts, floods, and hurricanes.

Disrupted Weather Patterns

As I discussed in my previous posts, melting ice is already causing changes in ocean currents. These currents, driven by temperature and salinity differences, transport global heat and act as a planetary thermostat. As freshwater from melting ice disrupts this delicate balance, the flow and strength of currents can change. This can cause regional warming and cooling, impacting weather patterns like precipitation and temperature fluctuations.

An Earth globe showing The global conveyor belt, shown in part here, circulates cool subsurface water and warm surface water throughout the world. The Atlantic Meridional Overturning Circulation is part of this complex system of global ocean currents. This illustration is captured from a short video produced by NOAA Science on a Sphere.
The global conveyor belt, shown in part here, circulates cool subsurface water and warm surface water throughout the world. The Atlantic Meridional Overturning Circulation is part of this complex system of global ocean currents. This illustration is captured from a short video produced by NOAA Science on a Sphere.

The Arctic, in particular, is experiencing rapid warming due to melting ice. This weakens the jet stream, a high-altitude wind current that steers weather systems. A weakened jet stream allows weather systems to meander more, leading to prolonged heatwaves and severe cold spells in unexpected regions.

Seasonal anomaly patterns for near-surface air temperatures (in °C) relative to the baseline period 1981–2010 in autumn 2018 (a), winter 2019 (b), spring 2019 ©, and summer 2019 (d). Temperature anomalies are from slightly above the surface layer (at 925 hPa level) to emphasize large spatial patterns rather than local features. Data accessed from NOAA/ESRL, Boulder, CO, at https://www.esrl.noaa.gov/psd/.
Seasonal anomaly patterns for near-surface air temperatures (in °C) relative to the baseline period 1981–2010 in autumn 2018 (a), winter 2019 (b), spring 2019 ©, and summer 2019 (d). Temperature anomalies are from slightly above the surface layer (at 925 hPa level) to emphasize large spatial patterns rather than local features. Data accessed from NOAA/ESRL, Boulder, CO, at https://www.esrl.noaa.gov/psd/.

Additionally, changes in ice cover affect Earth’s albedo, the planet’s ability to reflect sunlight. As reflective ice melts, exposing darker surfaces like oceans and land, more heat is absorbed, further accelerating warming and fueling even more extreme weather events.

Impact on Marine Ecosystems

Rising sea levels disrupt coastal habitats crucial for numerous marine species. They inundate essential breeding grounds, nursery areas, and feeding grounds, leading to habitat loss and fragmentation. This disruption can significantly impact fish populations, marine mammals, and coastal birds, threatening their survival and reproductive cycles (see figure below).

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Furthermore, melting glaciers introduce large amounts of freshwater into the ocean, altering its salinity and temperature. This disrupts the delicate balance of the water column, impacting salinity and the distribution of nutrients. This disruption has cascading effects on entire ecosystems, affecting all trophic levels, from plankton to fish and marine mammals.

Finally, melting ice sheets release harmful pollutants previously trapped within the ice. These pollutants, like heavy metals and persistent organic pollutants, accumulate in marine organisms, threatening their health and impacting humans when we consume seafood.

Key examples of sea-ice ecosystem services.
Key examples of sea-ice ecosystem services. Examples for provisioning (P, yellow), regulating (R, red) habitat/supporting (H, orange), and cultural (C, blue) ecosystem services provided by polar sea-ice ecosystems: (1) Food supply to higher trophic level species and sea birds; (2) Platform for birthing and neonatal care of higher trophic species; (3) Protection from predators for ice-adapted species; (4) Habitat for sympagic algae, bacteria, grazers (ice, melt pond, slush communities); (5) Brine drainage that exports salt (S), total alkalinity (TA), dissolved inorganic carbon (DIC); (6) CO2 exchange; (7) Habitat and food supply for key foraging species (amphipods, Antarctic krill, Arctic cod); (8) Emission of aerosol precursors for cloud condensation nuclei (CCN), including volatile organic compounds (VOC) and dimethylsulfide (DMS); (9) Halogen oxidation via frost flowers and snow; (10) Food supply for higher trophic level species (fish, seals, whales); (11) Carbon export into the (deep) ocean; (12) Food supply to benthic species; (13) Fisheries and harvesting; (14) Nutrient supply to pelagic phytoplankton; (15) Tourism; (16) Platform for human transport and subsistence harvesting; (17) Spiritual connection and inspiration, science and exploration; (18) Nutrient exchange; (19) Medicinal and genetic resources; and (20) all of the intangible, cultural, services that connect coastal communities to the sea ice, such as spiritual experience and Indigenous and local knowledge (see Table 1). DOI: https://doi.org/10.1525/elementa.2021.00007.f1

Loss of Freshwater Sources

One primary concern is the disruption of the natural seasonal water cycle. Glaciers act as natural reservoirs, storing vast amounts of freshwater during colder periods and gradually releasing it during warmer months, supplying rivers and streams throughout the year. As glaciers shrink, this crucial storage capacity diminishes, reducing water flow during the dry season and impacting irrigation, drinking water supplies, and even hydropower generation in regions dependent on glacial meltwater.

Changes in precipitation patterns due to a warming climate exacerbate the situation. Rising temperatures lead to increased evaporation, reducing overall water availability. Additionally, melting glaciers contribute to flooding during the melting season, followed by periods of intense water scarcity later in the year, creating a cycle of extremes that threatens water management and agricultural practices.

Photo of the Ganges River on its pass in Varanassi, India
The Ganges River. Photo by Shiv Prasad on Unsplash

And the impact extends beyond regional concerns. Melting glaciers can disrupt major river systems that supply water to densely populated areas far removed from the glaciers themselves. For example, the Himalayan glaciers feed major Asian rivers like the Ganges and Indus, and their decline threatens the water security of millions of people living downstream.

Extinction of Species

Habitat loss constitutes a primary threat from melting glaciers and ice caps. For example, I previously talked about Polar bears, which rely on sea ice for hunting and breeding. As the ice diminishes, their hunting grounds shrink, making it harder to find food and raise their young. Similarly, mountaintop habitats, crucial for unique amphibians and small mammals, are disappearing as glaciers retreat, leaving these species with unsuitable habitats.

Changing environmental conditions brought on by melting ice can disrupt entire food webs. Melting glaciers alter ocean salinity and temperature, impacting plankton populations, the foundation of the marine food chain. This has cascading effects on higher trophic levels, including fish, marine mammals, and birds that depend on these resources for survival (see figure under Impact on Marine Ecosystems above).

Rising sea levels also inundate coastal ecosystems, critical breeding grounds for numerous species. Sea turtles, for example, lose nesting beaches due to rising water levels, jeopardizing their reproductive success. Additionally, saltwater intrusion into freshwater habitats disrupts sensitive ecosystems, impacting amphibian populations, which can’t survive in saltwater ecosystems, and the delicate balance of wetlands.

Human Impacts

All the consequences listed above would have a cascading effect on human societies, and unfortunately, we are already seeing some of these effects at play. Potential problems include mass displacements due to rising sea levels and extreme weather events; disruptions to agriculture due to water scarcity and altered weather patterns; economic losses from damaged infrastructure and disrupted industries like fisheries and tourism; or increased social unrest and conflict due to resource scarcity and mass displacement.

These are all well-documented consequences that global climate change has already had on the human population, resulting from the loss of glaciers, ice caps, and sea level rise.

Wrapping up

So what? As you can see, the consequences of melting glaciers are far-reaching. And we are already seeing some of the effects. This time, we are not discussing models but empirical and observed events and consequences derived from melting glaciers and ice caps.

What comes next should have us looking for effective policies and laws and for a more sustainable and resilient society. Beyond the effects that losing massive ice masses can have on nature and ecosystems, we need to understand that losing them could have unprecedented consequences on human civilization as we know it. We must act as if our life on the planet depended on it. Because it does.

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