The blogger “Chris PT” mentioned me in a YouTube video,
In the process he mentioned how watching sea-ice shrink and grow in the Arctic can be a bit like a sporting event, in that Alarmists all cheer wildly when more-than-expected melts, and Skeptics all cheer wildly when less-than-expected melts. I’m not sure I approve, considering billions of dollars are at stake, not to mention the fate of the planet (if you believe Alarmists.) Also the arguing tends to disintegrate into discussions of the mental state and sanity of opponents, which has little to do with sea-ice, to put it mildly. Therefore I’m going to try to steer clear of such debate, when possible, and if I ridicule anyone it will be myself.
I will expose myself to ridicule by making a guess at what I think will happen. Then I will be wrong. Then I can have all the fun of ridiculing someone, by ridiculing myself.
One forecast sure to be correct this time of year is, “Warmer.” Temperatures shoot upwards at the Pole, under the 24-hour-a-day sunshine, until they get above freezing and level off in late June. (The average climb in temperature is the green line in the graph below, and you can see how steep the climb is, from April through June.)
What is more difficult to forecast is whether the red line in the graph below will be above or below the green line. For some reason this is the third straight year that temperatures dipped below normal in May. It remains to be seen if they stay below normal for the rest of the summer, as they did the past two summers. I forecast that they will.
One way to get an idea how thick the ice is, which gives you a hint about how enduring it might be, is to study the NRL ice-thickness map.
If you watch this over a period of time some events become obvious. For example, all winter the ice was pushed from the northwest to the southeast across Hudson Bay, and by April the ice was piled up and thick to the southeast, and newly-formed and thin to the northwest. Therefore it is obvious ice will melt away first in the northwest. I forecast there will be some ice still left in the southeast of Hudson Bay in August.
In the like manner, a lot of ice was pushed out of the Kara Sea, so I expect it will melt more swiftly in the Kare Sea this year. The Laptev Sea, on the other hand, did not export as much ice as last year. Last year the cross-polar-flow was so extreme that ice was pushed far from shore, leaving so much newly-formed, thin ice that, once melting began, an area of open water I dubbed “The Laptev Notch” formed during the summer, and stabbed north of 80 degrees latitude for a time. I forcast that notch to be far smaller this summer, and to have trouble melting north of 80 degrees.
If you don’t have the time to study the thickness-laps on a regular basis, you can watch a whole year be animated here:
What impresses me most in that animation is the bite the Pacific takes out ice north of the Bering Strait. That ice is solid and thick, at the start, but the influx of milder, Pacific water at the surface melts the ice from underneath, and ice that is ten feet thick in April can be gone by September.
I am expecting quite a bite to be taken from that ice this year, because the PDO (Pacific Decadal Oscillation) is going through a “warm spike”, and the water coming in through the Bering Strait ought be especially warm. However already I’ve blown my forecast in some ways. For one thing, to the south of Bering Strait the water on the Siberian side has become much colder than normal, and that makes me nervous. If it becomes involved, the water coming in through Bering Strait won’t be so mild.
Also the nice, mild breezes that have been rushing up from the south, and affirming my forecast, are putting me through the old switcheroo. They are swinging to the east and becoming colder.
The coldest air is currently parked over the Pole, and along the north coast of Greenland.
However a high pressure is parked north of Bering Strait,
In three days the cold air will be pulled off the Pole, and it seems the yearly warm-up will be well underway.
The problem with the above map is that it shows the Beaufort Sea during the warmest part of the day. Even under 24-hour-sunshine the sun is higher at noon, and a diurnal variation does occur. Therefore, to play it safe, we look at the situation under the midnight sun,
Now the situation north of Bering Strait and in the Beaufort Sea suddenly looks much colder. This does not bode well, in the short term, for my forecast of melting in that area.
The GFS model makes it look like the high pressure will remain parked roughly where it is, and an easterly flow will move a lot of the cold air north of Greenland to the west, along the Canadian coast and finally to the Alaskan coast. Yesterday I noticed Buoy 2015B: had dropped from above freezing to -3.19° C, and while it has rebounded to -1.33° in the “noontime” heating, the water its camera shows in a nearby lead looks suspiciously like it is skimming over with ice.
O-buoy #12 (which is due north of Bering Strait and most likely to first feel the effects of the “warm” PDO), has fallen from above freezing to -5°.
To the east across the Beaufort Sea, our old friend Obuoy 10 also shows an abrupt temperature drop
The buoy I’ll be watching is Buoy Buoy 2015A: , which is right on the coast of Alaska and effected by the sun-baked tundra just to its south. It’s camera is currently showing a lot of melt-water pools and temperatures are at +0.66°. If the camera starts to show the melt-water pools freezing over, then we’ll know the cold air has really backed west.
Of course, the cold will have to come from somewhere, and if the Pole is robbed of all its sub-freezing air, temperatures will likely rise up that way. They may even get their first thaw of the year. As it is, it is currently -8.42° C up at Buoy 2015D: , which is hard to see but is to the left of this picture, taken by North Pole Camera 1.
In conclusion, what is really fun about watching ice melt is seeing surprises occur, and what you don’t expect. I did not expect this cold shot into the Beaufort Sea.
What happened last summer, and I expect to happen again this summer, is for there to be some of these cold spells that come right out of the blue, with their origins more or less a mystery. After all, you reach a point where there is no more cold air left at the Pole. In the current situation the Beaufort cold can be explained-away as a case of Robbing-Peter-to-pay-Paul, but later in the summer Peter is broke, so you can’t rob him. It is when there are suddenly temperatures below freezing in July, without any apparent “source reason,” that your sense of wonder starts to come into play.
I’m looking forward to that.