Arctic sea ice extent again at record low for time of year

For some time, Arctic sea ice extent has again been at a record low for the time of the year. The image below shows Arctic sea ice extent on October 26, 2016, when extent was only 6.801 million km².

One reason for the low sea ice extent is the high and rising temperature of the Arctic Ocean. On October 27, 2016, the Arctic Ocean was as warm as 14.8°C or 58.6°F (green circle near Svalbard), 12.1°C or 21.7°F warmer than 1981-2011, as the image below shows.

On October 29, 2016, the Arctic Ocean was as warm as 14.9°C or 58.8°F (green circle near Svalbard), 12.1°C or 21.8°F warmer than 1981-2011, as the image below shows.

As the sea ice shrinks, less sunlight gets reflected back into space, while more open water and higher sea surface temperatures also cause storms and cyclones to become stronger. Stronger cyclones also cause greater amounts of water vapor to move up the Pacific Ocean and the Atlantic Ocean toward the Arctic.

[ click on image to enlarge ]

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Less Arctic sea ice and a warmer Arctic Ocean make that more heat and water vapor gets transferred from the Arctic Ocean to the atmosphere. The two above images show temperature forecasts for November 1 & 2, 2016. In both cases, temperatures over the Arctic as a whole are forecast to be as much as 6.40°C higher than 1979-2000.

As these images show, temperature anomalies in many places are at the top end of the scale, i.e. +20°C or +36°F.

Above combination image shows record low Arctic sea ice for the time of the year (left) and near record low Antarctic sea ice for the time of the year (right), with a combined sea ice extent of only 23.751 million km² on October 28, 2016. In other words, the world is now absorbing a lot of sunlight that was previously reflected back into space.

Below are two further temperature forecast:

Above image shows forecasts for October 31, 2016. The Arctic is forecast to be 6.07°C warmer than 1979-2000, while the Antarctic is forecast to be 4.56°C warmer than 1979-2000.

Above image shows forecasts for November 1, 2016. The Arctic is forecast to be 6.42°C warer than 1979-2000, while the Antarctic is forecast to be 3.70°C warmer than 1979-2000.

Rising temperatures over the Arctic further contribute to a rise in the amount of water vapor in the air over the Arctic at a rate of 7% more water vapor for every 1°C warming. Since water vapor is a potent greenhouse gas, more water vapor further accelerates warming in the Arctic.

The Climate Reanalyzer image below shows the temperature rise in the Arctic over time.

In the video below, Dr. Walt Meier of NASA Goddard Space Flight Center describes how the Arctic has been losing its thicker and older sea ice over the years (1991 to September 2016).

The Naval Research Lab 30-day thickness animation below (up to October 28, 2016, with forecasts up to November 5, 2016) further shows minimal recent growth of the Arctic sea ice, especially in terms of the ice with a thickness of 1m or above.

As the Arctic Ocean gets warmer, the danger grows that large amounts of methane will erupt from destabilizing hydrates at its seafloor. Ominously, high methane levels are visible over the Arctic on the image below, showing methane levels as high as 2424 ppb on October 24, 2016.

The animation below, made with images from another satellite (and a different scale), shows high methane levels over th Arctic Ocean from October 26 to 28, 2016.

The situation is dire and calls for comprehensive and effective action, as described in the Climate Plan.

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Cyclones continue to hit Northern Hemisphere

As the 2015 El Niño gets stronger, the Northern Hemisphere continues to get hit by strong winds and cyclones. The image below shows strong winds over the Arctic Ocean, as hurricane Joaquin approaches the coast of North America.



On above image, hurricane Joaquin is clocked at a speed of 79 mph (127 km/h) on October 1, 2015. NOAA warned that on that day the maximum sustained wind speed had increased to near 120 mph (195 km/h) with higher gusts.

For reference, NOAA uses four categories:
D: Tropical Depression – wind speed less than 39 mph (63 km/h)
S: Tropical Storm – wind speed between 39 mph and 73 mph (63 km/h - 118 km/h)
H: Hurricane – wind speed between 74 mph and 110 mph (118 km/h - 177 km/h)
M: Major Hurricane – wind speed greater than 110 mph (over 177 km/h)

NOAA issued the image below on September 30, 2015, warning that Hurricane Joaquin is likely to cause wind damage across a large part of the eastern coast of North America.

The NOAA animation below gives an idea of the strength of hurricane Joaquin.

[ click on image to enlarge, note that this is a 1.4 MB file that may take some time to fully load ]

Meanwhile, sea surface temperatures off the North American coast, as well as in the Arctic Ocean, are very high, as illustrated with the image on the right.

In the Arctic Ocean, the sea ice in many places is now less thick than it was in 2012, as illustrated by the image further below, showing sea ice thickness on October 7, 2012 (panel left) and a forecast for October 7, 2015 (panel right).

The water in the Arctic Ocean was already very warm this year. The main factor causing both these strong winds and the dramatic decrease in thickness of the multi-year sea ice is ocean heat, as also illustrated by the image below, showing high sea surface temperature anomalies in the Arctic as at September 30, 2015.

As the image below shows, nearly all the thick (over 3 m) multi-year sea ice has now disappeared, setting up a dangerous situation for the future that is much more dangerous than the situation was back in 2012. The thicker sea ice used to act as a buffer, consuming ocean heat in the melting process. Without thicker sea ice, ocean heat threatens to melt the sea ice from below right up to the surface, causing the entire sea ice to collapse as more open water will go hand in hand with stronger winds and waves. In case of such a collapse, sunlight that was previously reflected back into space will instead be absorbed by the water, causing rapid rise of the temperature of the water. In places such as the East Siberian Arctic Shelf, the water is on a average only 50 m deep, so warmer water is able to reach the seafloor more easily there.

The water of the Arctic Ocean is very warm, not only at the surface, but even more so underneath the surface. The danger is that strong winds will mix warm water all the way down to the seafloor, where it could destabilize sediments that can contain huge amounts of methane in the form of hydrates and free gas.

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The image on the right illustrates the impact of winds over the East Siberian Arctic Shelf on September 26, 2015.

NSIDC specialist Julienne Stroeve recently warned: “In 2007 more than 3m of bottom melt was recorded by [an] ice mass balance buoy in the region, which was primarily attributed to earlier development of open water that allowed for warming of the ocean mixed layer. But perhaps some of this is also a result of ocean mixing.”

As discussed in an earlier post, sea surface anomalies of over 5°C were recorded in August 2007 in the Arctic Ocean. Strong polynya activity caused more summertime open water in the Laptev Sea, in turn causing more vertical mixing of the water column during storms in late 2007 and bottom water temperatures on the mid-shelf increased by more than 3 degrees Celsius compared to the long-term mean.

The situation is dire and calls for comprehensive and effective action, as discussed at the Climate Plan.

As the 2015 El Niño gets stronger, the Northern Hemisphere continues to get hit by strong winds and cyclones. The image…
Posted by Sam Carana on Thursday, October 1, 2015

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