Snow cover hits record lows

December 4, 2012, European Space Agency
Captured by Envisat’s MERIS instrument on 13 February, this image shows an unusual view of Italy: almost all of the country is covered with snow. Credit: ESA

(—Santa Claus may someday need wheels for his sleigh – satellites show a decreasing amount of snow in the Northern Hemisphere.

A new analysis of snow cover observed by satellites shows record lows in Eurasia for June each year since 2008. In addition, three of the past five years have seen record low cover in North America.

This is the lowest June snow extent since began some 45 years ago. June snow cover is found to be falling much faster than expected from , and is disappearing even quicker than summertime Arctic sea-ice.

These results, published in in October and based on snow chart data from the US (NOAA), are consistent with indications of a decline in monthly-average snow mass, published last year as part of ESA's GlobSnow project.

The results show that the maximum amount of snow across the is slowly falling, while spring snow – particularly at – is melting significantly earlier.

Time series of Northern Hemisphere June snow cover (red), June sea-ice extent (black) and September sea-ice extent (grey). Thick lines denote five-year running mean. Relative to a 1979–2000 baseline, June snow cover – also known as ‘snow areal extent’ – has declined by 17.6%, whereas September sea-ice has declined by 13.0%. Credit: C. Derksen & R. Brown, Environment Canada (Data from the US National Snow and Ice Data Center & Rutgers University Global Snow Lab)

GlobSnow produced a long time-series of snow mass from 1979 to 2012, as well as a time-series of snow cover from 1995 to 2012.

The snow mass time-series is the first daily dataset of its kind for the Northern Hemisphere that extends over 30 years and is from satellite sensors measuring Earth's .

Information on snow mass and area is used to monitor and understand changes in seasonal snow cover that are important for the climate and hydrology. This information can only be provided by satellites since they observe large areas on a regular basis.

Along with geophysical applications, reliable data on snow cover can assist decision-makers and policy-makers in creating strategies to adapt to the changes. For this reason, the European Environment Agency has included GlobSnow results in its new "Climate Change, Impacts and Vulnerability in Europe 2012" report.

Yearly Northern Hemisphere snow mass (measured as ‘snow water equivalent’) for the month of March, showing a 5.5% decline over the period 1982–2011. March is usually the month with the maximum snow mass during each winter season. The information was derived from NASA’s SSM/I and AMSR/E satellite instruments. Credit: K. Luojus, Finnish Meteorological Institute; GlobSnow project

"The satellite-derived information from GlobSnow on total snow mass provides us with an important indicator that helps us to monitor changes in European and Arctic climate," notes Hans-Martin Fuessel of the .

A two-year extension of the GlobSnow project is underway, ensuring continuity in producing snow information and improving the data processing. Based on new methods, all data from the first phase of GlobSnow will be reprocessed.

The Envisat satellite was lost in April 2012 so NOAA's satellites are filling the gap until ESA's new Sentinel-3 satellite is launched in 2014.

On 4–5 December, ESA and Eumetsat – the European Organisation for the Exploitation of Meteorological Satellites – will co-host a workshop in Germany to look at existing European satellite snow monitoring capabilities and to set a strategy for their development.

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3 / 5 (2) Dec 04, 2012
This is the lowest June snow extent since satellite observations began some 45 years ago. June snow cover is found to be falling much faster than expected from climate models, and is disappearing even quicker than summertime Arctic sea-ice.

Garbage in garbage out. They have not used all of the positive feed backs.

The loss of snow packs, lake ice, and other inland ice at lower latitudes is actually the largest component of the albedo feed back, as it occurs at parts of the year where sunlight is more direct as compared to arctic Sea Ice Minimum, when the day is already shrinking.

So being at a lower latitude and melting at an earlier part of the year, and accumulating less each year, the loss of snow pack is a far larger component of albedo feedback than is the loss of Sea Ice in the N. Hemisphere. Additionally, the surface area of a square degree of Earth is larger at lower latitudes, meaning there's far more area to work with, and each unit area is more powerful.
3 / 5 (2) Dec 04, 2012
One need only look at the trend and the rapid fall-off of the Arctic Sea Ice area graphs to see that the Albedo Feed back does not become "self-reinforcing" from the Arctic itself until mid-August, and stops again in mid-September, because before then it hasn't melted enough to expose the ocean, and then after mid-september the Earth is already starting to tilt away too much for that tiny difference in Albedo to add up quickly enough.

Yes, the Albedo feed back from loss of Sea Ice matters, and it's a large value, and it's part of the reason the summer melt value increases 2.5 times faster than the winter melt values, but it's actually small compared to the albedo changes of lower latitudes of land-locked snow packs and ice, which melts a week or a month or two ahead of time now.
5 / 5 (2) Dec 04, 2012
Not only have the last two weeks or more of North American climatological winter been lost. So too have several weeks of winter been lost at the start of the winter season.

It is as if the coldest month - February - has been cut out of winter entirely.
1 / 5 (1) Dec 08, 2012
Garbage in garbage out. They have not used all of the positive feed backs.

I'm not sure what your concern is here. On the one hand you seem to be saying that you don't believe the data being presented here, yet on the other hand you seem to be defending their findings.

Regardless, yet another different line if research showing a warming planet.

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