¿Una foto del futuro próximo para las áreas costeras del mundo?
Inundaciones recientes en el norte de Manila, Filipinas
Lo que sigue es largo y por momentos tedioso, pero vale la pena invertir unos minutos en el caso y sus implicancias. Hace poco más de un mes una serie de climatólogos estadounidenses sostuvieron que el proceso de calentamiento global actualmente en curso iba a tener consecuencias prácticas mucho más dramáticas que lo sugerido previamente en informes del Comité Internacional sobre el Cambio Climático. En particular, los climatólogos hicieron hincapié en la posibilidad de un aumento brusco, a lo largo de este siglo, del nivel del mar en varios metros (no menos de tres metros hacia fin de siglo, pero posiblemente más). Adicionalmente postularon un aumento exponencial de "supertormentas" y el eventual enfriamiento del Atlántico Norte (efecto Corriente del Golfo).
Primero vayamos
al artículo en sí, del climatólogo James Hansen y otros 16 colaboradores. Los
autores lo dieron a conocer en forma online antes de que el trabajo fuera
arbitrado y aprobado por los árbitros (los pares de los autores, esto es, otros
climatólogos) y el comité editorial de la revista Atmospheric Chemistry and
Physics. No jodamos: esta práctica (publicar un paper antes de su crítica y
eventual re-escritura posterior) es repudiable y debería ser eliminada de la
práctica científica usual. Pero ese es tema para otra discusión. Vayamos ahora
a una versión sumarizada del artículo:
Título: Ice Melt,
Sea Level Rise and Superstorms: Evidence from Paleoclimate Data, Climate
Modeling, and Modern Observations that 2°C Global Warming is Highly Dangerous
Autores: James
Hansen, Makiko Sato, Paul Hearty, Reto Ruedy, Maxwell Kelley, Valerie
Masson-Delmotte, Gary Russell, George Tselioudis, Junji Cao, Eric Rignot,
Isabella Velicogna, Evgeniya Kandiano, Karina von Schuckmann, Pushker Kharecha,
Allegra N. Legrande, Michael Bauer y Kwak-Wai L.
Resumen: “There
is evidence of ice melt, sea level rise to +5-9 meters, and extreme storms in
the prior interglacial period that was less than 1°C warmer than today.
Human-made climate forcing is stronger and more rapid than paleo forcings, but
much can be learned by combining insights from paleoclimate, climate modeling,
and on-going observations. We argue that ice sheets in contact with the ocean
are vulnerable to non-linear disintegration in response to ocean warming, and
we posit that ice sheet mass loss can be approximated by a doubling time up to
sea level rise of at least several meters. Doubling times of 10, 20 or 40 years
yield sea level rise of several meters in 50, 100 or 200 years. Paleoclimate
data reveal that subsurface ocean warming causes ice shelf melt and ice sheet
discharge. Our climate model exposes amplifying feedbacks in the Southern Ocean
that slow Antarctic bottom water formation and increase ocean temperature near
ice shelf grounding lines, while cooling the surface ocean and increasing sea
ice cover and wáter column stability. Ocean surface cooling, in the North
Atlantic as well as the Southern Ocean, increases tropospheric horizontal
temperature gradients, eddy kinetic energy and baroclinicity, which drive more
powerful storms. We focus attention on the Southern Ocean’s role in affecting
atmospheric CO2 amount, which in turn is a tight control knob on global
climate. The millennial (500-2000 year) time scale of deep ocean ventilation
affects the time scale for natural CO2 change, thus the time scale for paleo
global climate, ice sheet and sea level changes. This millennial carbon cycle
time scale should not be misinterpreted as the ice sheet time scale for
response to a rapid human-made climate forcing. Recent ice sheet melt rates
have a doubling time near the lower end of the 10-40 year range. We conclude
that 2°C global warming above the preindustrial level, which would spur more
ice shelf melt, is highly dangerous. Earth’s energy imbalance, which must be
eliminated to stabilize climate, provides a crucial metric.”
Finalmente,
pasemos a las Summary Implications:
“Humanity faces
near certainty of eventual sea level rise of at least Eemian proportions, 5-9
m, if fossil fuel emissions continue on a business-as-usual course, e.g., IPCC
scenario A1B that has CO2 ~700 ppm in 2100 (Fig. S21). It is unlikely that
coastal cities or low-lying areas such as Bangladesh, European lowlands, and
large portions of the United States eastern coast and northeast China plains
(Fig. S22) could be protected against such large sea level rise.
Rapid large sea
level rise may begin sooner than generally assumed. Amplifying feedbacks,
including slowdown of SMOC and cooling of the near-Antarctic ocean surface with
increasing sea ice, may spur nonlinear growth of Antarctic ice sheet mass loss.
Deep submarine valleys in West Antarctica and the Wilkes Basin of East
Antarctica, each with access to ice amounting to several meters of sea level,
provide gateways to the ocean. If the Southern Ocean forcing subsurface
warming) of the Antarctic ice sheets continues to grow, it likely will become
impossible to avoid sea level rise of several meters, with the largest
uncertainty being how rapidly it will occur.
The Greenland ice
sheet does not have as much ice subject to rapid nonlinear disintegration, so
the speed at which it adds to 21st century sea level rise may be limited.
However, even a slower Greenland ice sheet response is expected to be faster
than carbon cycle or ocean termal recovery times. Therefore, if climate forcing
continues to grow rapidly, amplifying feedbacks will assure large eventual mass
loss. Also with present growth of freshwater injection from Greenland, in
combination with increasing North Atlantic precipitation, we already may be on
the verge of substantial North Atlantic climate disruption.
Storms conjoin
with sea level rise to cause the most devastating coastal damage. End-Eemian
and projected 21st century conditions are similar in having warm tropics and
increased freshwater injection. Our simulations imply increasing storm
strengths for such situations, as a stronger temperature gradient caused by ice
melt increases baroclinicity and provides energy for more severe weather
events. A strengthened Bermuda High in the warm season increases prevailing
northeasterlies that can help account for stronger end-Eemian storms. Weakened
cold season sea level pressure south of Greenland favors occurrence of
atmospheric blocking that can increase wintertime Arctic cold air intrusions
into northern midlatitudes.
Effects of
freshwater injection and resulting ocean stratification are occurring sooner in
the real world than in our model. We suggest that this is an effect of
excessive small scale mixing in our model that limits stratification, a problem
that may exist in other models (Hansen et al., 2011). We encourage similar
simulations with other models, with special attention to the model’s ability to
maintain realistic stratification and perturbations. This issue may be
addressed in our model with increased vertical resolution, more accurate finite
differencing method in ocean dynamics that reduces noise, and use of a smaller
background diffusivity.
There are many
other practical impacts of continued high fossil fuel emissions via climate
change and ocean acidification, including irreplaceable loss of many species,
as reviewed elsewhere (IPCC, 2013, 2014; Hansen et al., 2013a). However, sea
level rise sets the lowest limit on
allowable human-made climate forcing and CO2, because of the extreme
sensitivity of sea level to ocean warming and the devastating economic and
humanitarian impacts of a multimeter sea level rise. Ice sheet response time is
shorter than the time for natural geologic processes to remove CO2 from the
climate system, so there is no morally defensible excuse to delay phase.out of
fossil fuel emissions as rapidly as possible.
We conclude that
the 2°C global warming “guardrail”, affirmed in the Copenhagen Accord (2009),
does not provide safety, as such warming would likely yield sea level rise of
several meters along with numerous other severely disruptive consequences for
human society and ecosystems. The Eemian, less than 2°C warmer than
pre-industrial Earth, itself provides a clear indication of the danger, even
though the orbital drive for Eemian warming differed from today’s human-made
climate forcing. Ongoing changes in the Southern Ocean, while global warming is
less than 1°C, provide a strong warning, as observed changes tend to confirm
the mechanisms amplifying change. Predicted effects, such as cooling of the
surface ocean around Antarctica, are occurring even faster than modeled.
Our finding of
global cooling from ice melt calls into question whether global temperature is
the most fundamental metric for global climate in the 21st century. The first
order requirement to stabilize climate is to remove Earth’s energy imbalance,
which is now about +0.6 W/m2, more energy coming in than going out. If other
forcings are unchanged, removing this imbalance requires reducing atmospheric
CO2 from ~400 ppm to ~350 ppm (Hansen et al., 2008, 2013a).
The message that
the climate science delivers to policymakers, instead of defining a safe
“guardrail”, is that fossil fuel CO2 emissions must be reduced as rapidly as
practical. Hansen et al. (2013a) conclude that this implies a need for a rising
carbon fee or tax, an approach that has the potential to be near-global, as
opposed to national caps or goals for emission reductions. Although a carbon fee
is the sine qua non for phasing out emissions, the urgency of slowing emissions
also implies other needs including widespread technical cooperation in clean
energy technologies (Hansen et al., 2013a).
The task of
achieving a reduction of atmospheric CO2 is formidable, but not impossible.
Rapid transition
to abundant affordable carbon-free electricity is the core requirement, as that
would also permit production of net-zero-carbon liquid fuels from electricity.
The rate at which CO2 emissions must be reduced is about 6%/year to reach 350
ppm atmospheric CO2 by about 2100, under the assumption that improved
agricultural and forestry practices could sequester 100 GtC (Hansen et al.,
2013a). The amount of CO2 fossil fuel emissions taken up by the ocean, soil and
biosphere has continued to increase (Fig. S23), thus providing hope that it may
be possible to sequester more than 100 GtC. Improved understanding of the
carbon cycle and non-CO2 forcings are needed, but it is clear that the
essential requirement is to begin to phase down fossil fuel CO2 emissions
rapidly. It is also clear that continued high emissions are likely to lock-in
continued global energy imbalance, ocean warming, ice sheet disintegration, and
large sea level rise, which young people and future generations would not be
able to avoid. Given the inertia of the climate and energy systems, and the
grave threat posed by continued high emissions, the matter is urgent and calls
for emergency cooperation among nations.
***
Pasemos ahora al
tratamiento periodístico del tema. Así lo vio Chris Mooney el 23 de Julio de
2015 en el Washington Post, un diario conservador tradicionalmente en contra
del “alarmismo” de los climatólogos en torno al cambio climático:
Título: James
Hansen’s controversial sea level rise paper has now been published online
Epígrafe: It has
been widely discussed — but not yet peer reviewed. Now, though, you can at
least read it for yourself and see what you think.
Texto: A lengthy,
ambitious, and already contested paper by longtime NASA climate scientist James
Hansen and 16 colleagues appeared online Thursday in Atmospheric Chemistry and
Physics Discussion, an open-access journal published by the European
Geosciences Union. The paper, entitled “Ice melt, sea level rise and
superstorms: evidence from paleoclimate data, climate modeling, and modern
observations that 2 ?C global warming is highly dangerous” is now open for
comment — peer review in this journal happens in public.
And given how
much attention the work has already received, it’s likely to generate plenty of
comments from fellow scientists.
The study raises
the possibility of a more rapid rate of sea level rise in this century than
forecast by the U.N.’s Intergovernmental Panel on Climate Change, whose
research is widely regarded as the gold standard of climate research — but also
often criticized for being too conservative.
Moreover, the
study postulates that this faster sea level rise, brought on by the melting of
parts of Antarctica and Greenland, could lead to a number of climate change
“feedbacks” that could shut down the oceans’ circulation; stratify the polar
seas with warmer waters trapped below cold surface layers; increase the
temperature difference between low and high latitudes; and generate stronger
storms.
In reporting on
the paper this week, The Post solicited comments from five noted climate
scientists — as did other journalists — so in a sense, the peer review has
already begun. One of them — Kevin Trenberth of the National Center for
Atmospheric Research — strongly criticized the study, saying that “there are
way too many assumptions and extrapolations for anything here to be taken
seriously other than to promote further studies.”
Other researchers
also expressed skepticism about some parts of the work — particularly the
suggested feedbacks — but acknowledged that they, too, have great concerns
about sea level rise from the melting of ice sheets, especially if global
warming exceeds 2 degrees Celsius above pre-industrial levels.
So it remains to
be seen what the scientific community, overall, will make of this work.
Nevertheless, it
is already notable that a group of prominent scientists — not just Hansen, but
also his 16 co-authors, working in fields, such as glaciology, oceanography,
and paleo-climatology (or the study of the climates of past planetary eras) —
are worried that sea level rise of more than 1 meter is a threat this century.
Now, the question becomes to what extent the broader scientific community does —
or does not — agree.
In the end, that
process could very well lead many researchers to seek out a middle ground. In
fact, some already have.
“There is no
doubt that the sea level rise, within the IPCC, is a very conservative number,”
says Greg Holland, a climate and hurricane researcher at the National Center
for Atmospheric Research, who has also reviewed the Hansen study. “So the truth
lies somewhere between IPCC and Jim.”
***
Veamos ahora cómo
cuenta el caso (más sobriamente, obvio) un blog a cargo de una climatóloga
profesional, Judith Curry, del sitio web Climate.etc (http://judithcurry.com):
Título: Hansen’s backfire
Epígrafe: Jim Hansen’s new paper, and his PR strategy, are
raising a whole host of issues that are arguably a backfire for his objectives.
Texto: Last week, several media articles appeared about an
alarming new paper by Jim Hansen, that was just being submitted to a journal
and was not yet publicly available:
Washington Post: The
world’s most famous climate scientist just outlined an alarming scenario for
our planet’s future
National Observer: 2-degree target may still cause catastrophic
sea level rise, James Hansen warns
The Daily Beast: Climate Seer James Hansen Issues His Direst
Forecast Yet
My first reaction was this:
Why, of all the major news outlets,
is only the Washington Post carrying this? No AP, etc.?
Why haven’t I received a copy of this paper (usually a reporter or one
of the skeptical news outlets would send me a copy). I figured the press
release and paper were sent to only a few favored journalists?
The ‘favored journalists’ hypothesis quickly evaporated as
articles like this then started to appear:
The Conversation: Study
predicts multi-meter sea level rise this century but not everyone agrees
Mashable: The godfather
of global warming’s frightening prediction is getting the cold shoulder
The paper is in Atmospheric Chemistry and Physics Discussions,
the discussion forum of the European Geosciences Union journal Atmospheric
Chemistry and Physics [link]
Andy Revkin has two superb posts on the paper, which I will be
referencing in my discussion below:
Whiplash warning: when climate science is publicized before peer
review and publication
A rocky first review for a climate paper warning of a stormy
coastal crisis
Reviews of the science
While the paper has not yet undergone formal peer review by the
journal, journalists have elicited numerous reviews/comments from scientists.
From the Washington Post:
Michael Mann “Their climate model scenario wherein Greenland and
Antarctic meltwater caused by warming poles, leads to a near total shutdown of
ocean heat transport to higher latitudes, cooling most of the globe
(particularly the extratropics), seems rather far-fetched to me.” “Whether or
not all of the specifics of the study prove to be correct, the authors have
initiated an absolutely critical discussion.”
Kevin Trenberth, called the paper“provocative and intriguing but
rife with speculation and ‘what if’ scenarios.” Trenberth objected in
particular to the climate modeling scenarios used to study freshwater injection
as ice sheets melt. “These experiments introduce a lot of very cold fresh water
in various places, and then they see what happens.” “The question is how
relevant these are to the real world and what is happening as global warming
progresses? They do not seem at all realistic to me.” “There are way too many
assumptions and extrapolations for anything here to be taken seriously other
than to promote further studies.”
Richard Alley,“Many parts of the new paper are likely to
stimulate much technical discussion and further research in our community, as
we try to weave together the deep-time and recent history to provide useful
projections for the future.” “This new paper is not ‘the answer,'” “Particularly,
replacing the simple assumptions about doubling times of ice loss with
physically based insights is a major focus of our field, but is not yet done
and not likely to be ready really quickly.” Alley acknowledged that the IPCC’s
sea level rise estimate “is well on the optimistic low-rise side of the
possible outcomes,” and added that “the estimates in the new paper of
freshening, and discussion of stabilization of the southern ocean and
influences on precipitation, are interesting and important.”
From Revkin’s second post:
Tad Pfeffer: If you look at this from the point of view of
somebody who’s trying to use this information for anything other than
scientific satisfaction, whether or not these very, very rapid rates of sea
level rise happen in the next few decades or the next few centuries makes all
the difference in the world. The question of when does this start is not really
addressed in this paper that I can find, and has been addressed only
peripherally in most of the papers about ice sheet instability that I have
seen. Ian Joughin made some statements recently [context] that I thought were
pretty solid about it being a few centuries before this kind of very rapid sea
level rise can take place and that makes sense to me because there are some very
important things that you have to do in order to turn on the rapid response of
the Antarctic ice sheet – you have to get rid of a couple of big ice shelves
for starters. And it’s going to take a few centuries to do that. From a
strictly geophysical, glaciological, point of view, a few centuries may not
make much difference. But from the point of view of a planner, a policymaker,
again these are the people who care about what exactly we’re saying. It makes
all the difference in the world. And that’s the part I find missing in this
paper. They have to say something about when this is going to occur. They may
not be able to say with any great precision, but they have to say something.
Because if this is something that’s going to happen in the next few decades,
yeah, it’s something we’ve really got to wake up and pay attention about. If
it’s something that’s going to happen in the next few centuries then there are
a lot of other issues that we have to sort out first.
Without going into any details here, Revkin’s second post
provides scientists’ comments that shows the whole section on Eemian
superstorms appears to be without basis.
JC comments on the science:
This is an intriguing and wide-sweeping paper that has put
together a multi-disciplinary team to examine the possibility of near term
catastrophic sea level rise.
For context, Hansen et
al. present a much more extreme scenario than the last report from the Intergovernmental Panel
on Climate Change and the most recent assessment in 2014 “Expert assessment of sea-level rise by AD
2100 and AD 2300.”
Should we only pay attention to UN and NAS sanctioned
assessments by expert teams? Absolutely
not (note I will have a follow on post in a day or two that delves into this
issue). As stated in my previous post
What is the plausible ‘worst scenario’ for climate change?, we should be
putting extreme scenarios out there and assess whether they are plausible,
possible, or essentially impossible.
The biggest issue raised by Hansen is the potential (plausible?
possible?) for a catastrophic >5 m sea level rise in the 21st century.
Hansen et al. have proposed a a new
mechanism for faster sea level rise – can we falsify this? The collapse of the West Antarctic ice sheet
(WAIS) is arguably the most alarming
potential impact of global warming. WAIS
has collapsed before during previous interglacials, and will undoubtedly
collapse again (with or without AGW), with a ~5 m sea level rise. The issue is whether the WAIS can collapse on
timescales of decades to a century.
Based on what we know (summarized by Tad Pfeffer above), this is a
process that would take centuries.
I am not an expert on sea level rise or ice sheets, but here are
a few things that frame my own understanding, including some recent research:
Sea level has been rising for millennia. I am not convinced that there is a
significant acceleration of sea level rise that can be attributed to human
caused global warming (see this previous post).
Recent research from Scripps finds that the Greenland ice sheet
did not melt as much as expected during the Eemian but that may mean Antarctic
ice sheets melted more than expected
A new paper summarized by Cato that found that the size of the
Greenland ice sheet—especially the best observed portions covering the west and
southwestern parts of Greenland—during the mid-Holocene was smaller than it is
today—but not by a whole lot.
Study finds surprisingly high geothermal heating beneath west
antarctic ice sheet [link]
So it looks like we should be more worried about WAIS than about
Greenland, and it seems that natural processes (natural climate change and
geothermal processes) have caused large sea level changes in the past during
interglacial periods (albeit not rapid ones) and will continue to cause sea
level to changes in the future. Human
contribution so far to sea level rise does not seem particularly significant,
given the early 20th century rate of sea level rise is about the same as the
current rate. Our ways of inferring
future rates of sea level rise from ice sheet melting is crude – we can
speculate but not with much confidence.
The danger posed by sea level rise is a function of the rate of change
far more than the actual sea level itself.
Does Hansen et al. make any contribution to all this? Well their proposed mechanism with feedbacks
is of interest and should be explored further. But their conclusions regarding
an alarming rate of sea level rise are at best possible (and not plausible).
Policy relevance
The policy relevance of the Hansen et al. paper is the
articulation of a possible worst case scenario of sea level rise. In robust decision making, the plausible
worst case scenario informs decision making but does not necessarily dominate
the decision making process.
What role does a ‘possible’ worst case scenario play, apart from
clarifying what is plausible? Well, to
alarm people and to help build political will to ‘act’ on emissions reductions,
particularly for forthcoming Paris COP.
Regarding the policy relevance of the paper, Science Insider
writes:
Whether this paper will become a key point of reference in the
ongoing climate talks isn’t clear. In advance of the Paris meetings,
negotiators from nearly every country in the world have provisionally agreed to
the 2°C target. That there is even such an agreement in the offing seems like a
victory, but whether it will be reached is still up in the air. Recognizing
this, 24 academic and professional institutions in the United Kingdom yesterday
issued a sternly worded joint communiqué that called on the international
community to take immediate action on reducing emissions. The statement
suggested that to have a chance of reaching that 2°C goal, Earth must become a
zero-carbon world by the second half of the century. . . But how influential
this paper will be is unclear, given its flaws.
Hansen has previously suggested that scientists are often too
hesitant to say just how dire the situation is. A 2007 paper he co-authored,
titled “Scientific Reticence and Sea Level Rise,” suggested that scientists
felt constrained from sounding a full-fledged alarm on how high the waters will
get, in part because of the cautious nature of scientific inquiry and the
scientific method. But, he says in that paper’s abstract, “there is a danger in
excessive caution.” The new paper, he told reporters yesterday, is “significantly
more persuasive than anything previously published about just how dangerous 2°C
warming would be.”
Hansen’s political agenda is evident as per Revkin’s post:
The new paper, which Hansen told me he’s been working on for
eight years, was being rushed into public view with the hope of influencing
negotiations at the December round of talks in Parisaimed at crafting a new
global climate change agreement. You can hear from Hansen on the reasoning in
the recording of his phone conference call with some reporters on Monday.
Also from Revkin regarding a passage apparently in the press
release:
The paper got attention in advance because of this passage:
We conclude that continued high emissions will make multi-meter
sea level rise practically unavoidable andlikely to occur this century. Social
disruption and economic consequences of such large sea level rise could be
devastating. It is not difficult to imagine that conflicts arising from forced
migrations and economic collapse might make the planet ungovernable,
threatening the fabric of civilization. This image of our planet with
accelerating meltwater includes growing climate chaos and storminess, as meltwater
causes cooling around Antarctica and in the North Atlantic while the tropics
and subtropics continue to warm. Rising seas and more powerful storms together
are especially threatening, providing strong incentive to phase down CO2
emissions rapidly.
The backfire
The cited criticisms of the paper all make valid points. The criticisms of Mann and Trenberth are
somewhat surprising to me, since I have seen them support papers that are at
least as dubious as Hansen et al. Apart
from the paper’s flaws, I suspect some of the backlash from these
scientists is associated with the fact
that this paper has not yet been peer reviewed, and is an integrative,
interdisciplinary assessment that challenges the IPCC and other established
assessment reports. Revkin cites Tad
Pfeffer: “One of the things that troubles me most is that the rapid-fire
publication of unsettled results in highly visible venues creates the
impression that the scientific community has no idea what’s going on.” There is
clearly a concern that such independent assessments, especially by well known
and/or reputable scientists, can undermine the authority and messaging of
‘establishment’ assessment and scientists.
Revkin provides some interesting insights into their publicity
push and the media response:
But by late Tuesday, as other coverage built, so did questions
about the way the study was released, and the quality of its analysis. Another
sign of trouble was that, despite the
publicity push, the Associated Press, The New York Times, the BBC and The
Guardian (despite its yearlong push for climate action blending advocacy and
reporting) were among those who steered clear of the study. Listen to the taped
call to get a visceral sense of the concerns of Seth Borenstein, the longtime
climate reporter at the A.P.
That portentous section above — which in many ways is the only
part of the paper that is news given how it centers on the “likely” inundation
of most coastal cities in this century without aggressive emissions cuts — is
not in the version the journal has posted. It’s in a shorter version, lacking
references, that a publicist at Glover Park told me was going into more of a
lay publication.
The final draft posted for discussion has more nuanced language,
in line with what those arguing for more near-term climate and coastal risk
have already articulated.
Maybe we’ll all be a little slower on the draw next time when
work is promoted before it is publicized or peer reviewed. There are other
merits to slowing down a bit in examining an issue that will be with us for
generations — long past Paris. This is amarathon, not a sprint.
I think part of the backfire is associated with having Glover
Park handle the media push. Glover Park
provides strategic communications campaigns for corporations, non-profit
organizations and industry associations.
The Group is also involved in lobbying, but it definitely seems to be
non-partisan (i.e. open to pretty much all paying customers – I wonder how much
Hansen paid for their services and where the funds came from).
I’m not sure I’ve ever seen publicity for a research paper being
handled by such a group (Glover doesn’t seem to have prior experience with
this, since they rather bungled it for Hansen).
Press releases are usually issued by universities, journals or funding
agencies. Advocacy groups and think
tanks also issue press releases for their own reports. But what about retired or independent
scientists? And for scientists whose
universities won’t issue a press release?
E.g., Georgia Tech declined to issue a press release on Lewis and Curry;
the paper was publicized on my blog and by the GWPF. In Hansen’s case, presumably NASA or Columbia
could have issued the press release. But
probably not including Hansen’s most alarming statements.
In any event, it is refreshing to see the maturity shown by some
journalists is handling this issue. They
seem to be well trained re the ‘sanctity’ of peer reviewed papers. I am also wondering whether Hansen’s explicit
policy advocacy, coupled with a scientific research paper (esp one that had not
undergone peer review), contributed to distrust of the research? You would hardly expect Jim Hansen to write a
paper saying AGW is less alarming than we thought.
A combination of weak/speculative science, issuing the press
release prior to peer review or at least public availability of the paper, a direct challenge to establishment
assessment reports, policy advocacy, and use of a professional
publicity/marketing/lobbying group to handle the publicity seems to have contributed
to the backfire. I doubt that this paper
will have any serious influence on the Paris deliberations.
JC reflections
That said, I am very sympathetic to what Hansen did. I regard him as a fellow maverick – thinking
for himself and not afraid to challenge the ‘consensus’ – Hansen and I are of
course on opposite ends of the climate maverick spectrum, with Hansen more alarmed
and myself being less alarmed.
I think what Hansen did raises a whole host of very important
issues about climate research, the science-policy interface, and how research
is publicized. I will be addressing
these issues in a follow-on post (which should be up Mon or Tues).
***
Por último,
reproducimos el artículo de Brian Clark Howard para National Geographic el 21
de Julio de 2015:
Título:
Prediction of Rapid Sea Level Rise Won’t Change Global Climate Talks
Epígrafe: A new
study predicting 10 feet of sea level rise by the century’s end isn’t supported
by the mainstream scientific community.
Texto: A
bombshell climate study published this week warns that sea levels may rise a
catastrophic 10 feet (3 meters) by the end of this century, rather than the
currently predicted 3 feet (.9 meters). But mainstream climate scientists say
the report appears speculative and is not in sync with the leading
understanding of melting sea ice.
As a result, the
study is unlikely to change leading scientific consensus or affect the current
negotiations on a comprehensive global agreement on climate change.
The new study,
led by former NASA climate scientist James Hansen (now at Columbia University)
is set to be published in the peer-reviewed journal Atmospheric Physics and
Chemistry. Hansen and 16 colleagues argue in the paper that increasing melting
of the ice sheets over Greenland and Antarctica will lead to a shutdown of the
ocean’s currents. That would lead to warm waters trapped under Antarctica,
which would increase the melting of ice there (if all the continent’s ice
melted, it would raise sea level by around 200 feet).
Hansen’s
prediction is more dire than the scenario deemed most likely by the
Intergovernmental Panel on Climate Change (IPCC), which foresees no more than 3
feet of sea level rise by century’s end. (See an interactive of sea level
rise.)
The 10 feet
Hansen predicts would make many of the world’s coastal cities, from New York to
Shanghai, unlivable. It would also flood South Florida, making everything below
Interstate 75 unlivable (from Ft. Lauderdale on down). Three feet would put
many of New York’s airport runways underwater, but would be much easier to
mitigate with seawalls. (Learn more about the damage expected for Florida.)
A number of
prominent climate scientists are skeptical of Hansen’s conclusions.
Ian Joughin, a
professor of Earth sciences at the University of Washington, says melting
glaciers and ice sheets contribute only about 1 millimeter (0.04 inches) of sea
level rise a year.
While Hansen and
team predict a doubling in the rate of ice melt in Greenland in the coming
years, Joughin says that seems unlikely given past trends and what we currently
know about the processes.
“I don't think
you can extrapolate current melt rates to get to 10 feet,” says Joughin.
Hansen was not
available to comment on the study or the reaction.
Gavin Schmidt, a
climate scientist with NASA's Goddard Institute for Space Studies, says the
Hansen report is merely “one scenario, and not evidence for that scenario.”
Schmidt says the
study “might add to the discussions” but is far enough from conventional
thinking that it is unlikely to change mainstream climate views, international
negotiations on reducing carbon, or the IPCC’s recommendations to world
governments.
“There's plenty
of reason to worry about sea level rise, but I don't see 10 feet happening by
end of century,” says Joughin.
“Ten feet is well
outside the range of peer-reviewed projections and peer-reviewed scientific
literature,” says Benjamin Strauss, a scientist at Climate Central, a
non-profit climate research and journalism organization in Princeton, New
Jersey.
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