The January 2018 Fram Strait Cyclones

We’ve covered similar events in the recent past, but this one looks like it will take the proverbial biscuit.

Here’s the 6 hour wave forecast for the Fram Strait from 12:00 UTC this afternoon:

Significant_height_of_combined_w in multi_1.glo_30mext-20180113-12z+6

Mean_period_of_wind_waves_surfac in multi_1.glo_30mext-20180113-12z+6

Look at the scales carefully then compare the wave height and period with previous similar events. Here’s the cause of those giant waves, two powerful cyclones off Greenland pumping heat and moisture northwards from a long way south:

Synopsis-20180113-18Z-Crop

Also bear in mind the current sea ice area around Svalbard:

osisaf_svalbard_plot_20180112

and the current weather forecast for the capital Longyearbyen:

svalbard_forecast_20180113

Note in particular the anomalously high temperatures and the severe weather warnings for both rain and avalanches. In the middle of January.

Finally, for the moment at least, here’s a Sentinel 1B image of the sea ice in the Fram Strait earlier this morning:

S1B_Fram_20180113T063817

 

[Edit – January 14th]

The temperature in Longyearbyen is forecast to drop below freezing point early on Tuesday and then remain there, which I guess counts as good news?

svalbard_forecast_20180114

However the southernmost of the two cyclones off Greenland is now down to a central MSLP of 942 hPa:

Synopsis-20180114-12Z-Crop

 

[Edit – January 15th]

The cyclone now centred near Iceland looks as though it bottomed out at a MLSP of 939 hPa earlier today:

Synopsis-20180115-00Z-Crop

Watch this space!

The 2017/18 Festive Season in the Arctic

Christmas is coming, and Santa’s secret summer swimming pool has frozen over once again. However the same can’t be said for the Chukchi Sea! More on that in due course, but first let’s take a look at the PIOMAS volume graph at the end of November, courtesy of the wondrous Wipneus on the Arctic Sea Ice Forum:

piomas-trnd4-2017-11

2017 is currently third lowest, behind 2012 and 2016. Next let’s take a look at Wipneus’ PIOMAS Arctic sea ice thickness map:

PIOMAS-thk-20171130

followed by the University of Bremen’s SMOS Arctic sea ice thickness map:

20171205_hvnorth__l1c

Note the large area of pale blue open ocean still visible in the Chukchi Sea towards the top left of both maps.

For another perspective on Arctic sea ice thickness here’s the latest Cryosat-2 map, which currently is based on the month up to November 24th:

CS2-thk_28-2017-11-24

Finally, for the moment at least, here’s our very own Arctic Freezing Degree Days graph based on the DMI’s >80N data:

DMI-FDD-2017-12-06

2017 is currently occupying the wide open space between the astonishingly low numbers last year and all previous years in DMI’s record. Here’s their graph for 2017 so far:

DMI-meanT_2017-12-06

 

[Edit – December 10th]

Current Arctic sea ice area and extent derived from the University of Hamburg’s high resolution AMSR2 data:

UH-Arctic-Area-2017-12-09

UH-Arctic-Extent-2017-12-09

Plus the latest update on the Chukchi Sea situation:

UH-Chukchi-Area-2017-12-09

 

[Edit – December 20th]

Wipneus has released his mid month PIOMAS update for December:

piomas-trnd4-2017-12-15

PIOMAS-thk-dec152017

The Chukchi Sea is now mostly covered in sea ice, as is the Kara Sea. Volume is still 3rd lowest behind 2016 and 2012.

Whilst on the subject of sea ice thickness a related subject is sea ice age. Here’s a new paper on that topic:

A new tracking algorithm for sea ice age distribution estimation

Note that these assorted sea ice age maps are all for January 1st 2016!

Figure-6-Comparison-of-SIA-for-the-1-Jan-2016-calculated-with-the-following-combinations

Watch this space!

Pine Island Glacier Calves Again

An image captured earlier this morning by the Sentinel 1A satellite’s synthetic aperture radar reveals that another huge chunk of the Pine Island Glacier in Antarctica has broken loose:

S1A_PIG_20170923T035511

P.S. Here’s an animation of the calving courtesy of Wipneus:

Pine_Island_Glacier_Sentinel_1A_20170911-20170923

Via Stef Lhermitte on Twitter:

 

[Edit – September 24th]

The latest image from Sentinel 1A:

S1A_IPIG_20170924T043546

Click it for a much closer look.

 

[Edit – October 16th]

Another animation from Wipneus, showing the recently calved section of the Pine Island Glacier coming apart at the seams:

Pine_Island_Glacier_Sentinel_Calving_Crumbles_1A_20171003-20171015

 

[Edit – December 11th]

Another revealing image from Wipneus via the Arctic Sea Ice Forum:

Pine-Island-Glacier-SW-crack-Landsat8-nat-30m-20171210

New cracks are opening on the Pine Island Ice Shelf.

 

[Edit – December 22nd]

Via Susan Anderson at the Arctic Sea Ice Forum:

Pine Island Iceberg Under the Midnight Sun
Pine Island Iceberg Under the Midnight Sun

In September 2017, a new iceberg calved from Pine Island Glacier—one of the main outlets where the West Antarctic Ice Sheet flows into the ocean. Just weeks later, the berg named B-44 shattered into more than 20 fragments.

On December 15, 2017, the Operational Land Imager (OLI) on Landsat 8 acquired this natural-color image of the broken berg. An area of relatively warm water, known as a polyna, has kept the water ice free between the iceberg chunks and the glacier front. NASA glaciologist Chris Shuman thinks the polynya’s warm water could have caused the rapid breakup of B-44.

The image was acquired near midnight local time. Based on parameters including the azimuth of the Sun and its elevation above the horizon, as well as the length of the shadows, Shuman has estimated that the iceberg rises about 49 meters above the water line. That would put the total thickness of the berg—above and below the water surface—at about 315 meters.

 

[Edit – December 23rd]

Another graphic Landsat PIG GIF from Wipneus on the ASIF:

Pine-Island-Glacier_SW-crack_growing_landsat-8_20171219

The 2017 Arctic Sea Ice Metric Minima

September has arrived once again, the month in which the assorted Arctic area and extent metrics (almost) always reach their respective annual minima. Now we can start to speculate about what the assorted minima will be, and on what date.

First of all let’s take a look at “Snow White’s” favourite high resolution AMSR2 metrics derived by “Wipneus” from University of Hamburg AMSR2 concentration data:

UH-Arctic-Area-2017-09-02

UH-Arctic-Extent-2017-09-02

As you can see, today’s values are both higher than yesterday’s. Hence we already have potential minima to consider! In this case:

UH AMSR2 Area – 3.65 million km² on September 1st
UH AMSR2 Extent – 4.30 million km² on September 1st

Personally I don’t think those numbers will last long, and here’s one reason why. The “surf forecast” for the far North Atlantic for midday on September 6th:

Significant_height_of_combined_w in multi_1.glo_30mext.20170903_00029

Mean_period_of_swell_waves_order in multi_1.glo_30mext.20170903_00029

Some significant swells are currently forecast to batter the ice edge on the Atlantic side of the Arctic over the next few days.

 

[Edit – September 3rd PM]

Shock news! Tony Heller has made a prediction about this year’s minimum!! Unlike last year, this year the NSIDC 5 day average extent seems to be his Arctic metric of choice:

Charctic-20170902

Tony tells his faithful flock:

The Arctic sea ice minimum this year is very likely going to be be larger than 2016, 2015, 2012, 2011 and 2007.

It is also likely that the minimum extent will be higher than 2010 and 2008.

Instead of reporting the huge gain in ice and massive failure of their forecasts, climate alarmists will report that extent was “8th lowest on record.”

All those years are on the graph above. We shall see.

 

[Edit – September 15th]

Our normal Arctic sea ice extent 2017 minimum service will be restored as soon as possible. Meanwhile here is the test card:

That comes to you via the Daily Express of all places!

On the way the cruise’s resident naturalist and Smithsonian lecturer, Michael Scott, risked the wrath of Trump supporters by pointing to some of the changes Greenland is undergoing.

A Nasa map based on data between 2004 and 2014 revealed that the ice is melting across most of Greenland – an area nine times the size of the UK.

Pulling together several papers, Michael said Greenland’s summer melt season now lasts 70 days longer than in the early 1970s.

This melting is unfreezing the fringes of the permafrost, which may explain why Nasa satellites are picking up fires raging where the ice has retreated.

 

[Edit – September 16th]

It is of course still to early to be 100% certain about this. However:

UH-Arctic-Extent-2017-09-15

It certainly looks as though the bottom is in for the University of Hamburg AMSR2 extent: 4.25 million km² on September 11th.

It’s much the same story for JAXA extent:

VISHOP_Extent-20170915

4.47 million km² on September 9th and 10th.

 

[Edit – September 19th]

The NSIDC have followed in Snow White’s glass slippered footsteps and tentatively called the minimum:

On September 13, Arctic sea ice appears to have reached its seasonal minimum extent of 4.64 million square kilometers (1.79 million square miles), the eighth lowest in the 38-year satellite record. The overall rate of ice loss this summer was slowed by a persistent pattern of low sea level pressure focused over the central Arctic Ocean.

Please note that this is a preliminary announcement. Changing winds or late-season melt could still reduce the Arctic ice extent, as happened in 2005 and 2010. NSIDC scientists will release a full analysis of the Arctic melt season, and discuss the Antarctic winter sea ice growth, in early October.

The ever industrious Wipneus has also called the PIOMAS minimum volume for 2017:

Minimum volume was reached at 11th September: 4.542 103km3, which is fourth lowest after 2012, 2011 and 2016 (resp 3.673, 4.302, 4.402) and just below 2010 (4.582).

piomas_gridded_thickness_20170911

 

[Edit – September 23rd]

Here’s the 2017 edition of our annual NSIDC daily max/min extent graph:

NSIDC-NH-MaxMin-2017

The maximum extent was the lowest in the satellite record, and the minimum was just fractionally above the trend line. For those that concern themselves with “statistical significance”, the PIOMAS minimum volume was a “statistical tie” for second place:

PIOMAS-20170915

Watch this space!

Reductio Ad Absurdum

A somewhat surreal modern Arctic art installation:

 

 

 

 

 

 

Crystal Serenity Sails the Northwest Passage in 2017

After a voyage through the Northwest Passage untroubled by sea ice in 2016, the cruise liner Crystal Serenity has set sail for the Bering Strait and beyond once again. The SailWX tracking map shows her passing the Aleutian Islands:

Serenity-20170818

and although there is of course no sea ice to be seen yet her forward facing webcam reveals Dutch Harbor as her next port of call:

cybridge-20170817-2214

Much like last year, it looks as though the British icebreaker Ernest Shackleton is on its way to assist her:

Shackleton-20170818

Having an icebreaker in attendance might well prove to be essential this year, since, according to the Canadian Ice Service, Larsen Sound is currently still full of sea ice:

Maud-SoD-20170817

 

[Edit – August 21th]

Heading westwards to meet Crystal Serenity, this is what met the RRS Ernest Shackleton in Franklin Strait:

Shackleton_20170820_1003

Meanwhile Crystal Serenity is about to pass through the (ice free!) Bering Strait:

Serenity-20170821

 

[Edit – August 29th]

Crystal Serenity is now heading through Queen Maud Gulf:

Serenity-20170829

but there is as yet no sign of any sea ice:

SerenityVictoriaStrait

Shackleton_20170829_0303

However some should come into view later today. Here are the latest Canadian Ice Service sea ice charts of the area:

Maud-Conc-20170828

Maud-SoD-20170828

 

[Edit – August 29th 11:30]

Crystal Serenity has spotted some sea ice!

SerenityStarboard-20170829-0404

 

[Edit – August 29th 17:30]

Crystal Serenity and Ernest Shackleton are well in amongst the ice now, as are the former’s passengers:

SerenityStarboard-20170829-1114

 

[Edit – August 30th]

Crystal Serenity is now entering the Franklin Strait in the wake of TWO icebreakers:

Serenity-20170830-2000

SerenityBridge-20170830-1519

eswebcam_20170830_190303_02_m

Watch this space!

The Northern Sea Route in 2017

Depending on whether you’re reading an “alarmist” or a “skeptical” web site you may have been told either that the Northern Sea Route is already “open” or that the “icebreaker stuck in the sea ice off Pevek” escaped very late this summer. Here at Great White Con we like to think of ourselves as “realists”, so what are the actual facts of the matter.

Our customary way of looking at such things is to use the Canadian Ice Service’s definition of “open” for the Northwest Passage, which seems to be 3/10 or less concentration along the entire route. That would allow an intrepid little yacht like Northabout through without too much trouble, but that point has not quite been reached yet this year. The NSR looks to be eminently “open” already if you only look at an AMSR2 concentration map:

Arc_20170808_res3.125_LARGE

However according to the Russian Arctic and Antarctic Research Institute (AARI for short) there is still not a suitably simple way through Vilkitsky Strait. Here’s their latest ice chart of the area:

AARI_20170808_KARA

Convoys led by nuclear powered icebreakers have already passed through the Vilkitsky Strait this summer. See for example this tracking map of Yamal from a few days ago:

Yamal-20170730

Also an unaccompanied liquid natural gas carrier has made it through the Vilkitsky Strait already this year. According to a Total press release:

After loading its cargo at the Snøhvit LNG export terminal in Norway, in which Total has an 18.4% interest, the Christophe de Margerie is taking the Northern Sea Route to Boryeong in South Korea, where it will deliver a cargo for Total Gas & Power. It’s the first unescorted merchant LNG vessel ever to take this route, which makes it possible to reach Asia via the Bering Strait in 15 days versus 30 days via the Suez Canal.

This technological feat was made possible through the participation of Total teams to the design of these next-generation LNG carriers. Compilations of technology, they efficiently transport large quantities of LNG year-round, without requiring escort icebreakers during the period from July to November. The Christophe de Margerie is the first of a total of 15 planned LNG carriers that will be gradually deployed.

As you can see, whilst it travels forwards in open water the Christophe de Margerie goes into reverse when breaking ice! Little yachts and other unaccompanied vessels lacking an ice class certificate will have to wait just a little longer however, unless of course they are inclined to be “intrepid”.

 

[Edit – August 19th]

As Cesium points out below, there is now a <= 3/10 concentration channel through the Vilkitsky Strait on the AARI maps.

AARI_20170818_KARA

AARI_20170818_LAPTEV

Here’s a couple of Sentinel 1A tiles from this morning stitched together:

S1A_Vilkitsky_20170819

We can now safely declare the Northern Sea Route “open”, even for less intrepid little yachts.

Facts About the Arctic in August 2017

What seems likely to be the most interesting period of the 2017 Arctic sea ice melting season is upon us! The PIOMAS gridded data hasn’t been released yet, but the overall volume numbers reveal that 2017 has now relinquished its “lowest ever” position to 2012. Here’s Wipneus’ graph of the volume data:

piomas-trnd4-20170731

plus his anomaly plot:

piomas-anomaly-20170731

Our favourite high resolution AMSR2 area and extent graphs now also allow comparison with 2012. Here’s how they look at the moment:

UH-Arctic-Extent-2017-08-04

UH-Arctic-Area-2017-08-04

As you can see, round about now is when 2012 Arctic sea ice extent started to noticeably race ahead of the rest of the pack. Will 2017 follow suit? Are there any Arctic cyclones on the horizon for example? Well, the one forecast for August 4th hasn’t materialised. Here’s this morning’s Environment Canada synopsis:

Synopsis-20170804-00Z-Crop

However both ECMWF and GFS agree that a sub 985 hPa storm should have arrived by Sunday morning. Here’s the ECMWF version from MeteoCiel:

ECH1-20170804+48h

There’s stronger storms in the forecast further out, but once again we’ll believe them if and when we see them!

We’re keeping a close eye on the Northwest Passage once again this year. Most of the southern route is open already, but as we predicted the old ice in Larsen Sound has a lot of melting still to do. Here’s how it looked from the icebreaker Nordica a few days ago:

On top of that the old ice around O-Buoy 14 is currently rushing south down the McClintock Channel to replenish it. Here’s how that looks at the moment:

OBuoy14-20170803-0301

Meanwhile the melt along the Northern Sea Route is well ahead of last year. Here’s the University of Hamburg AMSR2 concentration map of the area:

Arc_20170803_res3.125_LARGE

There’s also now a lot of open water on the Pacific side of the Arctic, and Sunday’s cyclone is forecast to create a large area of 2 meter plus waves heading in the direction of the ice edge:

Significant_height_of_combined_w in multi_1.glo_30mext.20170804_00024

I expect that to have a noticeable effect on the already fragile sea ice by early next week, assuming the storm arrives as forecast! There is an ice mass balance buoy handily placed out on the ice in the path of the storm. Buoy 2017A is currently located near 77 N, 147 W, and its assorted sensors suggest the ice underneath it is now less than 20 cm thick:

2017A-2017-07-30

2017A_thick_20170731

Here’s how the area around the buoy looked a couple of weeks ago:


Image of 2017A from WARM 6 on July 18th 2017. NSF project: NSF OPP #1603548

The $64,000 question now is will the 2017 Arctic sea ice metrics stay in amongst the recent pack, or race after 2012 instead?

 

[Edit – August 6th]

This morning’s synopsis from Environment Canada suggests the cyclone has bottomed out at a MSLP of 982 hPa:

Synopsis-20170806-06Z-Crop

Here’s how the cyclone looked from space yesterday:

NASA Worldview “true-color” image of the sea ice north of the Beaufort Sea on August 5th 2017, derived from the VIIRS sensor on the Suomi satellite
NASA Worldview “true-color” image of the sea ice north of the Beaufort Sea on August 5th 2017, derived from the VIIRS sensor on the Suomi satellite

I think that I can convince myself that the salinity profile from ice tethered profiler 97, currently located at 73° N, 134° W, reveals mixing from depth in the wake of the storm:

itp97-Salinity-20170806

The synthetic aperture radar on the Sentinel 1B satellite can certainly see through the clouds, and reveals open water in the Central Arctic north of the Beaufort Sea yesterday evening (UTC):

Sentinel 1B image of Arctic sea ice at 79N, 160W on August 5th 2017
Sentinel 1B image of Arctic sea ice at 79° N, 160° W on August 5th 2017

 

[Edit – August 7th]

Here is Wipneus’ latest AMSR2 concentration delta map:

AMSR2-Delta-20170806

The effects of this weekend’s storm are readily apparent! Just in case you’re wondering Wipneus reports:

Area: -172.0 (+324k vs 2016, +138k vs 2015, -669k vs 2014, -523k vs 2013, +493k vs 2012)

UH-Arctic-Area-2017-08-06

 

[Edit – August 8th]

The next pulse of swell is currently forecast to be somewhat higher and longer period than the last one. This one is also taking aim at the Beaufort Sea MIZ:

Significant_height_of_combined_w in multi_1.glo_30mext.20170808-12Z_00045

Mean_period_of_wind_waves_surfac in multi_1.glo_30mext.20170808-12Z_00045

 

[Edit – August 9th]

According to Environment Canada the latest cyclone is already down to 980 hPa MSLP:

Synopsis-20170808-06Z-Crop

 

[Edit – August 9th PM]

The MSLP of the current cyclone is now down to 976 hPA:

Synopsis-20170808-18Z-Crop

The latest WaveWatch III forecast has increased the predicted peak height and period of the resulting waves once again:

Significant_height_of_combined_w in multi_1.glo_30mext.20170809_00037

Mean_period_of_wind_waves_surfac in multi_1.glo_15mext.2070809_00037B

 

[Edit – August 10th]

Large holes are appearing in the sea ice on the other side of the Arctic too. Take a look north of the Laptev Sea for example:

NASA Worldview “true-color” image of the "Laptev Bite" polynya on August 10th 2017
NASA Worldview “true-color” image of the “Laptev Bite” polynya on August 10th 2017

Meanwhile the current cyclone on the Pacific side of the North Pole appears to have bottomed out at 974 hPa:

Synopsis-20170810-06Z-Crop

 

[Edit – August 11th]

Here’s the latest sea ice concentration one day delta map from Wipneus:

AMSR2-Delta-20170810
Despite the expected divergence caused by a low pressure area crossing the ice, both are and extent of sea ice on the Pacific side of the Arctic are still falling.

 

[Edit – August 12th]

The waves are considerably smaller in the Beaufort Sea today, but not in the Bering Strait!

Significant_height_of_combined_w in multi_1.glo_30mext.20170812-00Z_00007

Here’s the latest one day delta map:

AMSR2-Delta-20170811

and here’s video showing the motion of sea ice in the Beaufort & Chukchi Seas so far this summer:

 

[Edit – August 13th]

Here’s an animation from Wipneus revealing the effect of the two recent cyclones on the Pacific side, plus everything else that’s been going on in the Arctic:

AMSR2-Basin-Anim-20170812-600

Click the image to see a much larger (3.3 Mb) version.

 

[Edit – August 16th]

AMSR2 Arctic sea ice extent has taken another tumble, and has dropped below 2016:

UH-Arctic-Extent-2017-08-15

Only 2012 left to beat!

 

[Edit – August 18th]

A PIOMAS mid month update has been released, including gridded thickness data. 2017 modelled volume has failed to follow 2012’s trajectory towards the September minimum, and is now on a par with 2011:

piomas-20170815

piomas_thickness_20170815

 

[Edit – August 21st]

After a “brief hiatus” in the wake of the recent cyclones Arctic sea ice area has posted a new low for the year:

UH-Arctic-Area-2017-08-20

Extent has yet to follow suit:

UH-Arctic-Extent-2017-08-20

The main loss of area has been in the “Beaufort Bite” once again:

AMSR2-Delta-20170820

 

[Edit – August 24th]

The SIPN August sea ice outlook has been released. Here are the predictions:

Watch this space!

What Opening Arctic Sea Routes Mean for the UK

The United Kingdom Government has just published details of its Foresight “Future of the sea” project’s investigation into the implications of declining Arctic sea ice. According to the overview:

The Arctic is losing sea ice at a dramatic rate and this decline is expected to continue. This is creating opportunities for shorter global trade links between East Asia and the UK, via the Arctic.

Arctic routes are seasonally open most years, although normally icebreaker ships are required and available routes are close to the coast. Currently the Arctic shipping season is short and highly variable with optimum conditions in September and/or October.

Due to climate change, the Arctic shipping season could become three times longer and more reliable, so that by mid-century it will likely be possible to directly cross the North Pole during late summer. During this time, voyages from East Asia to the UK could save 10 to 12 days by using Arctic routes.

However, the extra costs associated with operating in the harsh Arctic environment may detract from their appeal.

Foresight-ArcticShipping

The full report goes into much greater detail. According to the executive summary:

There are mixed views on whether trans-Arctic routes will become economically viable. The Russian government wishes to develop the Northern Sea Route as a commercial enterprise and offers substantial fee-based services such as ice-breaking support and pilotage, which are certainly necessary for future investment and development of the route. However Arctic transport is also likely to grow due to increased destination shipping to serve natural resource extraction projects and cruise tourism.

The UK is well positioned, geographically, geopolitically, and commercially, to benefit from a symbiotic relationship with increasing Arctic shipping. The UK has a prominent role in Arctic science and a world-leading maritime services industry based in London, including the International Maritime Organization (IMO), one of the world’s leading financial centres, and Europe’s largest insurance sector. Arctic economic growth is focused in four key sectors – mineral resources, fisheries, logistics, and tourism – all of which require shipping, and could generate investment reaching $100bn (US Dollars and hereafter) or more in the Arctic region over the next decade. The UK had a fundamental role in preparing the UN IMO Polar Code which came into operation in January 2017. The Polar Code is an historic milestone in addressing the specific risks faced by Arctic shipping and acts to supplement the existing Safety of Life at Sea (SOLAS) and Marine Pollution (MARPOL) conventions for protecting the environment while ensuring safe shipping in international waters.

Much of the investment into Arctic shipping projects is from China but northern European countries are also playing an increasing role. Potential opportunities for the UK include the development of UK-based Arctic cruise tourism, and a UK-based trans-shipment port – transferring goods from ice-classed vessels to conventional carriers. The UK’s active diplomatic role in many international organisations means it is well placed to ensure that increased activity in the Arctic is accomplished in line with established UN maritime conventions, many of which were written with significant UK contributions. The UK’s leading role in Arctic science has wide reaching positive implications for international collaboration. To enhance predictions of the future Arctic, further developments in climate modelling and science are required.

From the concluding remarks:

If anthropogenic greenhouse gas concentrations can be reduced sharply in line with the UN Paris climate change agreements, Arctic ice melt and shipping opportunities will still continue to increase for the majority of the 21st century. However, even with continually increasing greenhouse gas concentrations, climate models suggest there will always be some Arctic sea ice during winters through the 21st century. Although the Arctic shipping season length and reliability is likely to increase dramatically, for the vast majority of the current global shipping fleet sailing trans-Arctic will remain a seasonal endeavour. Based on the current activity and physical climate changes this suggests that trans-Arctic shipping is likely to increase, focused on the Northern Sea Route; however, it is likely to remain a niche market for specialist operators.

Finally, for the moment at least, here’s the latest IMO video on search and rescue in the polar environment:

The emphasis in the video is on Antarctica, but one cannot help but wonder when the next search and rescue operation will take place in the Arctic. Later this summer perhaps? Note that under the new Polar Code avoiding the use of heavy fuel oil is mandatory in the Antarctic, but merely “encouraged” in the Arctic:

PolarCode-1

IPSO OKs Matt Ridley’s Toxic Pausebuster “Opinion”

Way back in February Bob Ward of the Grantham Institute complained to the Great British Independent Press Standards Organisation about a Matt Ridley article in the no longer Great or British Times newspaper. According to Mr. Ward:

In a characteristically error-filled article (‘Politics and science are a toxic combination’, 6 February 2017), Viscount Ridley made a number of inaccurate and misleading statements.

He claimed that a blog by Dr John Bates “alleges that scientists themselves have been indulging in alternative facts, fake news and policy-based evidence”. This is hyperbolic nonsense. In fact, the blog does not contain such allegations. Instead, it primarily accuses a former colleague, Dr Thomas Karl, at the United States National Oceanic and Atmospheric Administration (NOAA) of failing to archive his data for a research paper (PDF) in accordance with strict new rules governing ‘operational data’.

IPSO have now published the findings of their investigation into the matter:

Findings of the Committee

22. The newspaper was entitled to report on the views of Dr Bates, a leading former climate scientist at the NOAA, about the ‘Pausebuster’ paper and the circumstances surrounding its publication. While acknowledging the newspaper’s position that Dr Bates had reviewed the article before publication, the primary question for the Committee was whether Dr Bates’ concerns had been presented in a significantly inaccurate or misleading way.

23. The columnist’s characterisation of the substance of Dr Bates’ claims was very strong: he had asserted that Dr Bates has alleged that scientists were indulging in “alternative facts, fake news and policy-based evidence”. The Committee noted that this appeared on its face to conflict with Dr Bates’ subsequent public statement that there had been “no data tampering, no data changing, nothing malicious”. However, Dr Bates had claimed in the blog that a “thumb on the scale” pushed for decisions that would create a desired outcome, and described the process as a “flagrant manipulation of scientific integrity guidelines”. “Fake news” and “alternative facts” are currently ill-defined terms, and the Committee concluded on balance that the nature of these allegations was such that the columnist was entitled to characterise them in this way. There was no breach of the Code on that point.

24. Dr Bates had made clear in his blog that he considered that the paper had been rushed, and deliberately timed to influence the Paris Climate Conference; he had said that the NOAA had breached its own rules on scientific integrity; he had said that the data had been faulty, because he believed that both datasets had been flawed. These concerns were clearly distinguished as Dr Bates’ claims based on his professional experience, which was explained, and had been accurately reported in the column, as claims. The columnist also acknowledged, albeit critically, that defenders of the paper had responded that other data sets had come to similar conclusions. While the Committee noted the grounds for the complainant’s disagreement with the columnist (and with Dr Bates) in relation to these matters, the columnist had not failed to take care over the accuracy of these claims, and it did not establish any significant inaccuracies in the column’s discussion of these issues.

25. The columnist had been further entitled to express his opinion on the significance of these claims; to draw comparisons between previous “scandals” within the scientific community; and to comment on the wider implications of Dr Bates’ concerns in that community, as well as on policy decisions on climate change. These were statements of the columnist’s opinion. His views, however controversial, did not raise a breach of Clause 1. There was no breach of the Code in relation to his discussion of these issues.

Conclusion

37. The complaint was not upheld.

According to Bob Ward’s analysis of IPSO’s verdict:

It decided not to uphold my complaint on the grounds that its Complaints Committee considered Viscount Ridley’s column to be wholly opinion.

This is consistent with IPSO’s previous rulings about the systematic misreporting of climate change issues by some newspapers, in which it confines itself to assessing whether opinions are accurately represented, rather than whether the opinions are based on facts or falsehoods.

We now eagerly await IPSO’s Complaints Committee’s verdict on a similar complaint by Bob Ward about a similar article by David Rose in the Mail on Sunday