A new month has arrived, and during January several Arctic sea ice metrics have been drifting towards the bottom of their respective decadal ranges. To begin with here is AWI’s high resolution AMSR2 extent graph, which is currently very close to being lowest for the date in the AMSR2 record:
However that is less the case for area:
Taylor is keen to see the PIOMAS volume data for January, but whilst we wait for the latest Polar Science Center update here is the CryoSat-2/SMOS volume graph, which now includes a couple of month’s worth of reanalysed results as well as more recent near real time numbers:
Here too is the start of month CS2/SMOS thickness map:
At the beginning of the New Year all the central regions of the Arctic are now refrozen apart from a small area of the Kara Sea:
Most Arctic sea ice metrics are near the middle of their respective ranges over the last decade. By way of example, here is a graph of Arctic Freezing Degree Days based on the Danish Meteorological Institute’s temperature data for the area north of 80 degrees latitude:
Here too are the high resolution AWI AMSR2 area and extent graphs:
The latest AWI CryoSat-2/SMOS volume graph tells a similar story:
Although overall volume is in the middle of the pack, the associated thickness map:
and the thickness anomaly map from the Finnish Meteorological Institute reveal an unusual distribution of thicker ice:
A considerable volume of ice currently situated between Svalbard and North East Greenland seems destined to exit the Central Arctic Basin via the Fram Strait over the coming months.
[Edit – January 24th]
In a somewhat belated mid month update, here’s the PIOMAS daily Arctic sea ice volume graph:
together with the PIOMAS thickness map on January 15th:
For comparison purposes here’s the AWI CryoSat-2/SMOS thickness map using the same scale:
Note the change of scale from the beginning of the month CS2/SMOS map at the top.
Here too is Lars Kaleschke’s animation of recent Arctic sea ice concentration, with the width of leads exaggerated to reveal ice motion:
Click to animate (10 Mb!)
Evidently sea ice export from the so called “last ice area” is continuing via the Nares Strait and in particular via the Fram Strait between Greenland and Svalbard.
Although not on the same scale as the cyclone at around the same time last year, surface pressure of a storm near Svalbard bottomed out at 965 hPa yesterday:
It will be interesting to see what effect the storm has on the ice on the Atlantic periphery over the next few days.
A new month is upon us and Christmas is coming! Here’s another look at Lars Kaleschke’s high resolution AMSR2 area and extent graphs for the Arctic as a whole:
Extent increase stalled for the last few days of November, and as a result extent is now in a “statistical tie” with 2017 for 4th lowest extent for the date in the AMSR2 record.
A change is allegedly as good as a rest, so here’s an alternative view of high resolution AMSR2 area and extent created using the experimental tools provided by the AWI’s Lars Kaleschke at: https://sites.google.com/view/sea-ice/
After a brief pause mid-month the refreeze has accelerated again. Both metrics are in the upper half of the decadal range, with extent this year just above 2021 and area just below last year.
Next let’s take a look at sea ice concentration at the end of October:
Recently Judith Curry published a series of articles on the topic of blackouts. Since attempting to prevent such things is my “professional” speciality I’ve spent a bit of time over at “Climate Etc.” recently. Hence I couldn’t help but notice Judith’s article on Tim Palmer‘s new book, entitled “The Primacy of Doubt”. According to Judith:
This book is a physics-intellectual feast. Must read.
Hence I immediately rushed online and bought a copy from amazon.co.uk, which arrived today. A more detailed overview will follow once I’ve had a chance to read the whole book, but leafing through it this evening I couldn’t help but notice this quotation from Richard Feynman at the very start:
Our freedom to doubt was born of a struggle against authority in the early days of science. It was a very deep and strong struggle. Permit us to question — to doubt, that’s all — not to be sure.
My gaze also alighted on the final paragraph of chapter 10 – “Decisions! Decisions!”:
Just as with weather prediction, a cost-loss analysis can help you make a decision about whether to take anticipatory action regarding climate change…
Based on the way we value our own existence in other areas of life, there does indeed seem to be a strong argument that we should act now, uncertainties about future climate change notwithstanding.
But this is ultimately a decision which each of us must make, e.g. in deciding which politicians to vote for.
Of course being a citizen of the once Great British banana republic I don’t get to vote on our next Prime Minister!
I think I’ll go and pass this news on to Judith and her denizens forthwith. Meanwhile here’s a quotation from the back cover. According to Suki Manabe, winner of the 2021 Nobel Prize in Physics:
The Primacy of Doubt is an important book by one of the pioneers of dynamical weather prediction, indispensable for daily life, describing how the approach can be used for prediction in other areas, such as climate, health, economy, and conflict.
[Edit – October 22nd]
I’m still rather busy trying to help keep the UK’s lights on, so I have yet to even begin reading “The Primacy of Doubt” from cover to cover. However here is another brief extract, from the chapter on “Climate Change”:
We understand these [water vapour, albedo] feedback processes reasonably well. However, there is another feedback process associated with water that we understand rather poorly. This is the cloud feedback process.
[Edit – October 25th]
Here’s another extract from chapter 6 (page 115):
The question of whether clouds act as a positive or negative feedback on climate change can’t at present be answered unambiguously: indeed, I would say it is the biggest unsolved problem in physical climate-change science.
The 2022/23 freezing season has begun, so to begin with here are Arctic sea ice area and extent during its early stages:
Both metrics are currently tracking 2021 quite closely.
Here too is an AMSR2 animation of the transition from melting to freezing in the Central Arctic. Click to animate, and be warned that the file size is almost 10 Mb:
[Edit – October 4th]
Another big storm is heading for the Chukchi Sea. The GFS forecast currently shows a sub 960 hPa low developing on Thursday:
As in previous years there is already a thread devoted to this year’s minimum extent. By way of a summary here are the end of August numbers for our favourite “high resolution” AMSR2 area and extent metrics:
Extent is currently near the top of the range of the last 10 years.
We have now reached the stage of the “melting season” when “refreezing” has started in the Central Arctic but melting at the periphery is outpacing it. However the Canadian Ice Service stage of development charts now show the arrival of new ice in the high latitudes of the Canadian Arctic Archipelago:
After a long hiatus courtesy of the demise of the annual Barneo ice camp and the Covid-19 pandemic we are pleased to be able to report that an ice mass balance buoy has once again been installed on a floe in the vicinity of the North Pole. Here’s the evidence:
The ship in the background is not a traditional research icebreaker. It is Ponant Cruises’ Le Commandant Charcot, one of a number of new ice hardened cruise ships voyaging across the Arctic Ocean and adjacent seas. Le Commandant Charcot reached 90N on July 13th:
In a press release last week the Alfred Wegener Institute announced that:
From her home port in Bremerhaven, the Polarstern will set course for Fram Strait and the marginal ice zone north of Svalbard, where warm, nutrient-rich Atlantic Water flows into the Arctic Ocean.
The Polarstern starts its voyage to the Arctic from its home port of Bremerhaven. Photo: Nina Machner
Closely monitoring energy and material flows in the marginal ice zone from the ship and from on ice floes is the goal of the team led by Prof Torsten Kanzow, expedition leader and a physical oceanographer at the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI). “We will make transects from the open water into the dense sea ice and back. Along the way, we will gather a variety of physical, chemical and biological measurements in the marginal ice zone, which is especially productive and therefore especially interesting,” explains Kanzow.
“The team will also venture onto the ice to take a closer look at the thickness and characteristics of the sea ice and measure ocean currents and eddies away from the ship. We’ll also deploy so-called gliders in the ocean, buoys on the ice and moorings on the seafloor, all of which will record valuable data for the next several years. Lastly, we’ll extend our research radius with helicopter flights, during which we’ll observe, for instance, the melt ponds on the ice.”
Following the work in the MIZ north of Svalbard Polarstern will be heading for Northeast Greenland:
The two glaciers there (79 N Glacier and Zachariae Isstrom) are both characterised by ocean-driven ice loss and accelerated ice flows, making them contributors to sea-level rise. “We plan to install moorings in order to gauge the sensitivity of ocean-driven glacier melting to changing environmental conditions,” says Kanzow, who’s been pursuing research in the region since 2016. Accompanying geodetic-glaciological studies will be conducted on Greenland. On the one hand, they will assess how the solid ground is rising on extremely small scales, because it is still rebounding from the past weight of ice masses that melted after the last glacial maximum. On the other, they will explore temporal variations in supraglacial lakes; their drainage out to sea can have considerable effects on glacier flow speeds and glacier melting.
The AWI team have installed three seasonal ice mass balance buoys in the MIZ, without the usual thermistor string but with a new conductivity, temperature, depth (CTD) sensor fitted to measure salinity instead. Less colourful than usual sea ice thickness graphs can be viewed on the 2022 ice mass balance buoy page. Here’s one example:
[Edit – July 25th]
The image above updates on a daily basis, but today’s version is worth preserving for posterity:
There is currently a large area of low concentration sea ice around the North Pole, and Polarstern has left its station in the marginal ice zone and is currently heading north of Greenland rather than in the direction of the 79N/ZI glaciers.
Polarstern has been heading even further north to the Aurora Vent field (about 130 nautical miles northwest). As part of an extensive lithospheric study, ocean bottom seismometers will be deployed at depths of more than 4000 meters to record seismological activity as well as the physical properties of the hydrothermal plume.
Polarstern north east of Greenland – Photo: Christian R. Rohleder
Polarstern is now heading south again, where a team from the Technical University of Dresden will be deploying a modified surfboard on supra-glacial lakes! Here’s a test run in a melt pond:
Photo: Erik Loebel[Edit – July 29th]
I discovered something rather interesting whilst browsing the Marine Traffic ship tracking web site this morning:
It appears as if the AWI have recently installed two buoys that support AIS position reporting, as indeed does Polarstern itself:
[Edit – August 6th]
Polarstern is now approaching the 79 N and Zachariae Isstrom glaciers:
Watch this space!
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