There is warning level rise of water level due to melting glaciers. Alaska’s melting glaciers are adding enough water to the Earth’s oceans to cover the state of Alaska with a 1-foot thick layer of water every seven years.

The observation found that climate-related melting is the primary control on mountain glacier loss. Glacier loss from Alaska is unlikely to slow down, and this will be a major driver of global sea level change in the coming decades.

Since long been, a primary player in the global sea level budget is the Alaska region. But the exact details on the drivers and mechanisms of Alaska glacier change have been stubbornly elusive.

The UAF and U.S. Geological Survey research team analyzed surveys of 116 glaciers in the Alaska region across 19 years to estimate ice loss from melting and iceberg calving. The team collected airborne lidar altimetry data as part of NASA’s Operation IceBridge and integrated the new data with information from the 1990s collected by UAF scientist.

They combined their observations with a new mountain glacier inventory that characterizes the size and shape of every glacier in the Alaska region, which includes the glaciers of Alaska, southwest Yukon Territory and coastal northern British Columbia.

This leads to a much more detailed assessment and attribution of recent glacier change than previously possible with the help of large dataset of direct observations.

Mountain glaciers hold less than 1 percent of the Earth’s glacial ice volume. The rest is held in ice sheets on Antarctica and Greenland. However, the rapid shrinking of mountain glaciers causes nearly one-third of current sea level rise.

In the global sea level rise, Alaska has been identified as a global sea level rise contributor for years. But until now, there had not been a clear understanding of the processes responsible for the rapid changes of these glaciers.

The observation used the airborne observations to compare the changes of two main types of glaciers: those that end on the land, and those that end in lakes or the ocean, referred to as calving glaciers. Any glacier can lose mass through surface melting, but only those ending in water can lose ice through iceberg calving.

Observations have long wondered what the contribution of iceberg calving could be across the entire state. The key finding in the observation come up to Columbia Glacier in Prince William Sound. It has retreated more than 19 kilometers (12 miles) mostly because of iceberg calving and thinned by more than 450 vertical meters (1,500 vertical feet) since 1980.

Using the newly enabled ability to separate glaciers into different categories using the observed data, the researchers made some surprising discoveries. Their discoveries show the regional contribution of tidewater glaciers to sea level rise to be almost negligible. Tidewater glaciers are glaciers that end in the ocean. Instead, shocking discoveries come out for the glaciers ending on land which are losing mass exceptionally fast, overshadowing mass changes due to iceberg calving, and making climate-related melting the primary control on mountain glacier mass loss.

This observational work has important implications for global sea level projections. With improved understanding of the processes responsible for Alaska glacier changes, models of the future response of these glaciers to climate can be improved.

Thinking about the global climate change is proportional to thinking about future existence. It relates that rates of loss from Alaska are unlikely to decline, since surface melt is the predominant driver, and summer temperatures are expected to continue to increase. There is a lot of momentum in the system, and Alaska will continue to be a major driver of global sea level change in upcoming decades.