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Saturday, August 28, 2010

NOAA's NSIDC Arctic Report, August 17, 2010

Dear Readers, The Northwest and Northeast Passages are both open at the same time for the third time in recorded history (August 27, 2010).  The NSIDC report below has a good description of the factors involved, even though this report dates from August 17.

North by Northwest

The end of summer is approaching in the Arctic; temperatures are dropping and melt is ending in the high latitudes. Yet summer is not quite over in the lower latitudes of the Arctic Ocean, where sea ice extent continues to decline. Sea ice has melted out extensively in the northern route of the Northwest Passage, but the passage is not completely open.
Meanwhile, in the Antarctic, sea ice extent continues to be well above normal, largely because of atmospheric circulation patterns set up by a high Antarctic Oscillation mode.
map from space showing sea ice extent, continentsFigure 1. Daily Arctic sea ice extent on August 16 was 5.95 million square kilometers (2.30 million square miles). The orange line shows the 1979 to 2000 median extent for that day. The black cross indicates the geographic North Pole.Sea Ice Index dataAbout the data—Credit: National Snow and Ice Data Center High-resolution image
Overview of conditions
As of August 16, 2010, Arctic ice extent was 5.95 million square kilometers (2.30 million square miles),1.68 million square kilometers (649,000 square miles) below the 1979 to 2000 average.
graph with months on x axis and extent on y axisFigure 2. The graph above shows daily Arctic sea ice extent as of August 16, 2010. The solid light blue line indicates 2010; dashed green shows 2007; solid pink shows 2008; solid orange shows 2009; and solid gray indicates average extent from 1979 to 2000. The gray area around the average line shows the two standard deviation range of the data. Sea Ice Index data.
—Credit: National Snow and Ice Data CenterHigh-resolution image
Conditions in context
As of August 16, only 2007 and 2008 had lower extent. Approximately one month remains in the melt season.
High pressure has moved in over the central Arctic Ocean, replacing stormier, lower-pressure conditions that persisted during July. Paired with lower pressure on the Siberian side, this pattern generates winds that push the ice northward and reduce the total ice extent, especially since much of the ice pack is spread out.
map showing nw passage and current ice conditionsFigure 3. Top: This image, from the Canadian Space Agency's RADARSAT-2 satellite, shows the northern route of the Northwest Passage this August; although the passage is not completely open, sea ice cover is light. Bright, circular and other sharply defined shapes are sea ice; dark grey indicates calm ocean; white smudged regions are areas of ocean that have been roughened by winds. Bottom: The graph of ice area in the northern route of the Northwest Passage shows that ice retreated earlier than normal. The blue line tracks the area of sea ice for 2010, compared to average and to previous low ice years.
—Credit: NSIDC courtesy Howell, Agnew, Wohlleben, and the Canadian Ice Service 
High-resolution image

Early clearing in the Northwest Passage
Stephen Howell, Tom Agnew, and Trudy Wohlleben from Environment Canada report that sea ice conditions in the Northwest Passage are very light. Ice is still present at the mouth of the M’Clure Strait, in central Viscount-Melville Sound, and in Larsen Sound, as of early August. As a result, neither the northern route (Western Parry Channel) nor the southern route (Amundsen’s Passage) through the Northwest Passage are completely clear of ice. Sea ice area within the northern route is currently well below the 1968-2000 average and almost a month ahead of the clearing that was observed in 2007, according to ice chart data from the Canadian Ice Service. In the southern route, there is still a substantial amount of ice.
This year’s early clearing of sea ice probably resulted from record warm temperatures this past spring over the Western Canadian Arctic, as well as the decline in older, multiyear ice in the channel over recent years. Spring 2010 was the warmest in the region since 1948: some regions of the Western Canadian Arctic were more than 6 °C (11 °F) above normal. These warm conditions helped break the ice up early in the northern route. If winds push sea ice away from the entrance to M’Clure Strait, the northern route of the Northwest Passage could open completely this year. However, even scattered sea ice remains a significant threat to navigation.
figure 4: ice concentrationFigure 4. This map shows ice concentration on August 16, 2010, from the NASA AMSR-E sensor on the Aqua satellite. Lines mark two well-known routes through the Northwest Passage: Amundsen's route is yellow, and the northern route is red. —Credit: NSIDC courtesy University of Bremen IUP
High-resolution image
History of the Northwest Passage
Conditions in the Northwest Passage are quite variable and do not necessarily reflect overall conditions in the Arctic. However, today’s conditions in the Northwest Passage would likely astonish 19th century explorers such as McClure, Franklin, and Amundsen. In upcoming decades, the passage will be increasingly likely to open during summer.
Last month, Canadian investigators located the wreckage of the HMS Investigator, which sank on an expedition led by Captain Robert McClure in the 1850s. The McClure expedition had set out to rescue the Franklin Expedition, which had gone missing after leaving Baffin Bay for the Northwest Passage in 1845. McClure attempted to enter the passage from the west through what is now called M’Clure Strait, but quickly became trapped in the ice. They remained trapped through two winters before being rescued by another ship. The Franklin Expedition was not so fortunate: all 128 men perished. It was another fifty years before Norwegian Roald Amundsen and a small crew successfully navigated the passage. Their trek, by the southern route, took over two years.
figure 4: ice concentrationFigure 5. This image shows melt onset anomalies in the Arctic Ocean for 2010, compared to the 1979 to 2000 average. Green, red, and yellow indicate areas of earlier melt onset, while blue and violet show regions of later melt onset. White and black indicate regions with no data.
—Credit: NSIDC courtesy Thorsten Markus, NASA GSFC/data from DMSP SSM/I and NASA AMSR-E   High-resolution image

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