Neven is another citizen scientist who has done a great service.I
feel very similarly about things.
'Like
watching a train wreck': Blogger quits writing about climate change
CBC,
15
December, 2016
To hear podcast GO
HERE
When
Neven Curlin began his Arctic Sea Ice blog in 2010, it was a labour
of love. Though he isn't a scientist, as an environmentalist he had a
natural interest in the state of Arctic sea ice and how it was being
affected by global warming.
'Describing
the train wreck all the time is not very productive.'
- Neven Curlin
But
now six years later, after amassing a sizeable following while
blogging about sea ice melt multiple times a week, Curlin says he has
to take a step back from his blog because of "Arctic burnout."
"It's
like watching a train wreck in slow motion," Curlin tells The
Current's Anna Maria Tremonti.
"And
just describing the train wreck all the time is not very productive.
So I just need some time to step away."
As
his blog has been growing, Curlin has also been building an
ecologically-friendly home with his wife in Fürstenfeld, Austria.
Between
that and his work as a freelance translator, Curlin says he doesn't
have the time anymore to focus on his blog. But he's also been
finding it too depressing to keep writing about bad news day after
day.
Sea
ice melting in the Arctic "is going really, really fast,"
he says.
"It's
going much faster than what mainstream science anticipated ... and it
just keeps going."
To
hear podcast GO
HERE
TRANSCRIPT
AMT: Well,
let's go now from one pole to another from the Antarctic to the
Arctic. Climate change continues to have a devastating effect on
northern sea ice. This past year has seen the hottest average
temperature in the Arctic ever. There's simply no sign of that
slowing down. Neven Curlin knows this all too well. His Arctic Sea
Ice blog began as a hobby about six years ago. It's since become a
second home on the Internet for sea ice enthusiasts—amateur and
professional alike. All the bad news has been too much, however. He's
finding it too depressing to continue. Neven Curlin is on the line
from Fürstenfeld, Austria. Hell.
NEVEN
CURLIN: Hi
there.
AMT: Tell
us about your blog. Why did you start it?
NEVEN
CURLIN: Oh.
Well, that was back in 2010 and my hands were itching to do something
and I was very interested in online discussions on global warming and
climate change. And the Arctic, I found it really fascinating,
especially the sea ice. And I thought that maybe it deserved a place
of its own.
AMT: How
many people use this?
NEVEN
CURLIN: Well,
if you look at page views, during the summer melt when attention is
greatest, maybe five to 10,000 people or page views is what the blog
receives. And the graphs page, I think maybe 1,000 people every day
or more.
AMT: In
your last blog post, you announced you needed a break from it. Why is
that?
NEVEN
CURLIN: Well,
two things actually. In the end, I just don't have time enough to
give it the attention it deserves. And on the other hand, as
fascinating a subject as it is, it's also somewhat depressing if you
think about the consequences of Arctic sea ice loss and everything.
At some point, I had to decide to just step away so I can refocus and
also because I need that time to continue reducing my impact on the
climate and everything. So what they call walking the walk, I
believe, in English.
AMT: Hmm.
So you found it depressing because you're actually tracking it over
time and there's not a not a good ending here.
NEVEN
CURLIN: Well,
we don't know exactly what the ending will be. If you can be certain
how bad the ending will be you can at least prepare for it. But yeah,
it's as if you're watching a train wreck in slow motion and while
you're doing it, you have these denial mechanisms where you just
focus on the analysis or when something exciting happens that hasn't
happened before. But when you sit back and you think about okay,
geez, this is going really, really fast. It's going much faster than
what mainstream science anticipated even 10 years or maybe even five
years ago and it just keeps going. And if you then look at what the
potential consequences are, yeah, it makes you swallow. And also,
like I said, just describing the train wreck all the time, it's not
very productive. So I just need some time to step away from the
weekly duty to write about it so that I can develop maybe new ideas
or new perspectives because I'm convinced that the Arctic will go
ice-free at some point. Maybe soon, maybe a bit later. It's not
really relevant. And I'm already thinking about what happens after
that. And what do we need for that time also, from the science side.
AMT: How
discouraging is it for you when you see people voting for politicians
who express real skepticism about climate change?
NEVEN
CURLIN: Yeah.
That's a good question. You could consider me an activist so that
should interest me. All I care about is raising awareness. So I don't
know about voting for politicians, what's the right thing to do. But
I firmly believe that if enough people are aware of the seriousness
of Arctic sea ice loss and global warming in general, that maybe then
things can move towards a more positive direction. And in this sense,
the Arctic sea ice is so important because we have the satellite
images and we can see, we can see how fast it is going. And in that
sense, the Arctic could be considered an iconic image that maybe
opens the eyes of anyone who—even if he's not willing to look at
it—cannot be denied.
AMT: Neven
Curlin, thank you for speaking with me.
NEVEN
CURLIN: Thank
you for having me.
AMT: Neven
Curlin, the creator of the Arctic Sea Ice blog which is now on ice.
He's in Fürstenfeld, Austria. We'll put a link to it to our
website, www.cbc.ca/thecurrent,
to the blog, not Fürstenfeld. [chuckles] After hearing about the
effects of climate change at both ends of the globe, it might be
fitting to hear from British naturalist Sir David Attenborough. His
parting words on the final broadcast ofBBC
TV's Planet
Earth 2 went
viral online. He stood atop the 95-storey London Shard skyscraper to
deliver this heartfelt plea on the future of the planet
PIOMAS December 2016
Another
month has passed and so here is the updated Arctic sea ice
volumegraph as
calculated by the Pan-Arctic Ice Ocean Modeling and Assimilation
System (PIOMAS) at the Polar
Science Center:
Well,
November definitely was an Oh
Jesus-month.
Just like during
October,
the stall in sea ice extent has been reflected in the PIOMAS sea ice
volume numbers. The Arctic amassed just 2904 km3 of sea ice, as
compared to 3721 km3 for 2012 and 4054 km3 for 2011. The last time a
November clocked in less than 3000 km3 was in 2006 (2567 km3), but
right now 2016 is more than 4000 km3 lower than 2006, which means
there should have been so much more opportunity for expansion. It's
just crazy.
And
so the differences with previous months have only become larger:
Yes,
your eyes are seeing what you think they're seeing: 2016 is 749 km3
lower than 2012, a new record low. Look, here's another visual aid,
the volume graph produced by sea ice data virtuoso Wipneus:
Of
course, the trend line on the PIOMAS sea ice volume anomaly graph is
now firmly lodged in the 2 standard deviation territory:
With
extent and volume being so low at the end of October one would have
expected an explosive increase of thin ice at the edges of the ice
pack. The fact that this didn't happen during November, relatively
speaking, means that average thickness should be somewhat higher. But
the PIJAMAS graph - based on my crude calculation of PIOMAS volume
numbers divided by total JAXA sea ice extent - shows a marginal
increase of just 4 cm (where 10-20 cm has been the norm in the past
decade):
This
means that the thicker ice didn't get that much thicker either,
resulting in this year going lower than 2012 on this graph as well.
The thickness plot from the Polar
Science Center still
has 2012 lowest, but the gap has been as good as closed:
In
this respect it is also interesting to see this animation posted by
seaice.de over on the Forum, depicting the evolution of SMOS numbers
since 2010 (remember, this ESA satellite is quite good at measuring
ice thickness up to 0.5 metres):
There
seems to be very little (thin) ice growth on the Atlantic side of the
Arctic. As surprising as this is, it isn't all that surprising if you
look at the current sea surface temperature anomalies there:
And
how about sea ice volume distribution? Again, I've copied the 2010,
2011 and 2012 difference maps (the three lowest years after 2016)
from the collage Wipneus posts every
month over on the ASIF. This time I'm adding the PIOMAS Ice Thickness
Anomaly for November 2016 relative to 2000-2015:
According
to PIOMAS the ice north of Greenland and the Canadian Arctic
Archipelago is currently thicker than it was in those other ultra-low
years. Mostly elsewhere the ice is thinner and some of that thicker
ice still seems very vulnerable to Fram Strait export.
Last,
but not least, here's a collage of CryoSat images as put
out by
CPOM at University College London, which shows sea ice volume
matching the previous lows of 2011 and 2012, as well as having
thicker ice north of the CAA (hat-tip to Sarat/Taras):
I'm
trying to get into sabbatical mode, so I'm going to finish now.
Suffice to say that if the current trend continues and the ice
doesn't get a chance to thicken sufficiently this winter, things will
get even more worrisome than they already are.
Fortunately, the media
has been writing a lot about the current unprecedentedness of events
in the Arctic (and Antarctic), which is a sign that this serious
situation is getting more and more embedded into the collective
consciousness.
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