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Extras

Six Degrees

25 Nov 2007 by eric

“Alarmism” is a term that gets bandied about a lot. It is often said that one should not call out “fire” in a crowded building. But it really depends, one might say, on whether the “calling out” is done in such a way as to simultaneously prevent a stampede and prevent anyone getting burned.

This riddle was very much on my mind as I sat down to write my thoughts on Mark Lynas’s book, Six Degrees: Our Future on a Hotter Planet (London: Fourth Estate, 2007). I don’t read much popular science literature, and I doubt I would have read this book if I hadn’t made the mistake of referring to it (in a negative manner) in the comments section of a RealClimate post. I don’t think my error was very grave. What I actually said was that if what I had heard about the book from the press materials were true, then the book was probably alarmist and not worth reading. But I don’t blame the author for asking me to read the book and see for myself. He said that the press (in this case Sunday Times (London)) had misconstrued what he says in the book, and he assured me that is was all based on very careful review of the scientific literature. I was thus both curious and obligated to read the book.

Mark Lynas will no doubt be pleased that I very much like the book. To be sure, it is alarming, but the question of whether it is alarmist is a more difficult one, and I don’t think the answer lies in debating the book. Rather, it lies in looking closely at the underlying science the book builds on. I don’t intend to do that here, but I do think that all climate scientists (particularly those that talk to the public) ought to read this book, and ask themselves a question. I’ll get to that question at the end, after saying a bit more about the book.

Six Degrees, as the title suggests, is comprised of six main chapters (plus an introduction and a conclusion). Each of the main chapters examine what the earth might look like as we raise the planet’s temperature by 1o, 2o, etc. degrees Celsius, based on what the scientific literature has to say about it. Laying out the book this way makes for a good logical progression of ideas, and a fair bit of suspense. Very few people, Lynas says, have got “the slightest idea what two, four or six degrees of average warming actually means in reality, and I’m sure he is right.

In Chapter 1, at 1o, we have predictions of, for example, an annually ice free Arctic ocean. Yes, quite plausible and supported by the literature, and perhaps occurring a little sooner than expected. At 2o, we have, “so whilst southern China can expect more flooding as the two-degree line is approached, the oceanic time lag means that it may take much longer for the rain-bearing summer monsoon to reach the drought-stricken north.” Yes, certainly plausible based on the studies Lynas cites. At 4o, we have “with global sea levels half a meter or more above current levels, [the Egyptian city of] Alexandria’s long lifespan will be drawing to a close. Even in today’s climate, a substantial part of the city lies below sea level, and by the latter part of this century a terminal inundation will have begun. … a rise in sea levels of 50 cm would displace 1.5 million people and cause $35 billion of damage.” Alarmist? Hardly. A 50 cm rise in sea level, is well within the conservative IPCC projections, even for temperature rises less than four degrees.

At 5o and 6o, the book really does start to sound alarmist, with the analogy to Dante’s Inferno – used to good literary effect throughout the book – coming very much to the fore. At five degrees, we have “an entirely new planet is coming into being – one largely unrecognizable from the Earth we know today. At six degrees, “… the pump is primed … not for flourishing palm trees in Alaska, but for the worst of all earthly outcomes: mass extinction.”

Aha, say the skeptics! It is alarmist after all. But is it? Lynas’s reference to the “entirely different planet” actually refers to the fact that at five degrees, the “remaining ice sheets are eventually eliminated from both poles.” That’s entirely true. And unlike in Gore’s discussion of sea level in Inconvenient Truth Lynas does emphasize the long timescales (thousands of years) in this case. Furthermore, there is published research that raises the likelihood of the significant loss of ice sheets at lower temperatures, and Lynas could have claimed certainty of a disappearing Greenland ice sheet in an earlier chapter. That he doesn’t do that is characteristic of the book: it doesn’t tend to go beyond the published literature. This is what Lynas claims at the outset — “all of the material in the book comes from the peer-reviewed scientific literature” – and I think he does an admirable job.

And that brings us back to the question I promised to raise at the beginning, which is this:

If a reading of the published scientific literature paints such a frightening picture of the future as Six Degrees suggests – even while it honestly represents that literature – then are we being too provocative in the way we write our scientific papers? Or are we being too cautious in the way we talk about the implications of the results?

Filed Under: Climate Science, Reviews

Storm World: A Review

18 Jun 2007 by mike

If you are a RealClimate regular, you are undoubtedly aware of our ongoing interest in the developments in the scientific understanding of potential hurricane-climate change linkages. This is an area of the science where a substantial body of significant new research has emerged even since RealClimate’s inception in late 2004. The scientific research in this area, and the media frenzy and political theatrics that have inescapably followed it, are thoughtfully placed in a broader historical context in a fascinating new book by Chris Mooney entitled Storm World: Hurricanes, Politics, and the Battle over Global Warming. Anyone who is at all interested in the scientific history that has led to our current understanding of Hurricanes and their potential linkages with climate change, will find this book a page turner. The book is a nice complement to Kerry Emanuel’s recent book Divine Wind: The History and Science of Hurricanes (which too is so readable that it lies on our coffee table). Mooney in a sense picks up where Emanuel’s left off. Like Emanuel, he explores the history of the science. But he uses this historical context, and his studies of the personalities of key actors, to explore how the current scientific debate can be traced back to a rift that has emerged over many decades between distinct communities of atmospheric scientists.
[Read more…] about Storm World: A Review

Filed Under: Climate Science, Hurricanes, Reviews

Start here

22 May 2007 by group

[Note this is page is updated somewhat regularly. Please notify us of any dead links. Last update: 10 May 2022.]

We’re often asked to provide a one stop link for resources that people can use to get up to speed on the issue of climate change, and so here is a selection. Unlike our other postings, we’ll amend this as we discover or are pointed to new resources. Different people have different needs and so we will group resources according to the level people start at.

For complete beginners:

NCAR: Weather and climate basics
Center for Climate and Energy Solutions: Climate basics
Wikipedia: Global Warming
NASA: Global Warming
National Academy of Science: America’s Climate Choices (2011)
Encyclopedia of Earth: Climate Change
Global Warming: Man or Myth? (Scott Mandia, SUNY Suffolk)
Open Learn: The Basics of Climate Prediction

There is a booklet on Climate Literacy from multiple agencies (NOAA, NSF, AAAS) available here (pdf).

The UK Govt. had a good site on The Science of Climate Change (archived).

The portal for climate and climate change of the ZAMG (Zentralaanstalt für Meteorologie und Geodynamik, Vienna, Austria). (In German) (added Jan 2011).

Those with some knowledge:

The IPCC Frequently Asked Questions are an excellent start (AR4 version here , updates were provided in the 5th Assessment report (pdf) and again for AR6).

The UK Royal Society and US National Academies of Science produced a joint Q&A on climate change in 2014, and an update in 2017.

RealClimate: Start with our index.

Informed, but in need of more detail:

Science: You can’t do better than the IPCC reports themselves (AR6 2021, AR5 2013, AR4 2007, TAR 2001). Also the Climate Science Special Report for the US National Climate Assessment.

History: Spencer Weart’s “Discovery of Global Warming” (AIP)

Informed, but seeking serious discussion of common contrarian talking points:

All of the below links have indexed debunks of most of the common points of confusion:

  • Coby Beck’s How to talk to Global Warming Skeptic
  • New Scientist: Climate Change: A guide for the perplexed
  • RealClimate: Response to common contrarian arguments
  • NERC (UK): Climate change debate summary (archived)
  • UK Met Office: Climate Science
  • Brian Angliss A Thorough Debunking
  • John Cook Skeptical Science
  • The Global Warming Debate (Presentations from around 2010 resurrected)

Please feel free to suggest other suitable resources, particularly in different languages, and we’ll try to keep this list up to date.

A Slovak translation is available here

Tłumaczenie na polski dostępne jest tutaj
A Bulgarian translation is available here (via Ivan Boreev).

Filed Under: Climate Science, FAQ, IPCC

Does a Global Temperature Exist?Existe uma temperature global?

25 Mar 2007 by rasmus

Does a global temperature exist? This is the question asked in a recently published article in Journal of Non-Equilibrium Thermodynamics by Christopher Essex, Ross McKitrick, and Bjarne Andresen. The paper argues that the global mean temperature is not physical, and that there may be many other ways of computing a mean which will give different trends.

The common arithmetic mean is just an estimate that provides a measure of the centre value of a batch of measurements (centre of a cloud of data points, and can be written more formally as the integral of x f(x) dx. The whole paper is irrelevant in the context of a climate change because it missed a very central point. CO2 affects all surface temperatures on Earth, and in order to improve the signal-to-noise ratio, an ordinary arithmetic mean will enhance the common signal in all the measurements and suppress the internal variations which are spatially incoherent (e.g. not caused by CO2 or other external forcings). Thus the choice may not need a physical justification, but is part of a scientific test which enables us to get a clearer ‘yes’ or ‘no’. One could choose to look at the global mean sea level instead, which does have a physical meaning because it represents an estimate for the volume of the water in the oceans, but the choice is not crucial as long as the indicator used really responds to the conditions under investigation. And the global mean temperature is indeed a function of the temperature over the whole planetary surface.

[Read more…] about Does a Global Temperature Exist?Existe uma temperature global?

Filed Under: Climate Science, FAQ, RC Forum

Has Pacific Northwest snowpack declined? Yes.

20 Mar 2007 by eric

There has been a bit of a flap here at the University of Washington over the state of the snowpack in United States Pacific Northwest region. The Seattle city mayor, Greg Nickels (a well known advocate for city-based CO2 reduction initiatives) wrote in an Op-Ed piece in the Seattle Times that

The average snowpack in the Cascades has declined 50 percent since 1950 and will be cut in half again in 30 years if we don’t start addressing the problems of climate change now. That snow not only provides our drinking water, it powers the hydroelectric dams that keep our lights on.
[Read more…] about Has Pacific Northwest snowpack declined? Yes.

Filed Under: Climate Science, FAQ, Instrumental Record, Reporting on climate

Swindled! Aldatıldık!

9 Mar 2007 by group

By William and Gavin

On Thursday March 8th, the UK TV Channel 4 aired a programme titled “The Great Global Warming Swindle”. We were hoping for important revelations and final proof that we have all been hornswoggled by the climate Illuminati, but it just repeated the usual specious claims we hear all the time. We feel swindled. Indeed we are not the only ones: Carl Wunsch (who was a surprise addition to the cast) was apparently misled into thinking this was going to be a balanced look at the issues (the producers have a history of doing this), but who found himself put into a very different context indeed [Update: a full letter from Wunsch appears as comment 109 on this post]

So what did they have to say for themselves?
[Read more…] about Swindled! Aldatıldık!

Filed Under: Climate Science, Extras, Paleoclimate, Reporting on climate, Reviews, Sun-earth connections

Aerosols: The Last Frontier? Aerossóis: A Última Fronteira?

21 Feb 2007 by group

Guest commentary from Juliane Fry, UC Berkeley

The recently released IPCC 2007 Fourth Assessment Report Summary for Policymakers reminds us that aerosols remain the least understood component of the climate system. Aerosols are solid or liquid particles suspended in the atmosphere, consisting of (in rough order of abundance): sea salt, mineral dust, inorganic salts such as ammonium sulfate (which has natural as well as anthropogenic sources from e.g. coal burning), and carbonaceous aerosol such as soot, plant emissions, and incompletely combusted fossil fuel. As should be apparent from this list, there are many natural sources of aerosol, but changes have been observed in particular, in the atmospheric loading of carbonaceous aerosol and sulphates, which originate in part from fossil fuel burning. While a relatively minor part of the overall aerosol mass, changes in the anthropogenic portion of aerosols since 1750 have resulted in a globally averaged net radiative forcing of roughly -1.2 W/m2, in comparison to the overall average CO2 forcing of +1.66 W/m2.
[Read more…] about Aerosols: The Last Frontier? Aerossóis: A Última Fronteira?

Filed Under: Aerosols, Climate Science, FAQ, IPCC

What triggers ice ages? O que Dispara as Eras Glaciais? Buzul Çağlarını Tetikleyen Nedir?Qu’est ce qui déclenche les glaciations?

16 Feb 2007 by rasmus

by Rasmus Benestad, with contributions from Caspar & Eric

In a recent article in Climatic Change, D.G. Martinson and W.C. Pitman III discuss a new hypothesis explaining how the climate could change abruptly between ice ages and inter-glacial (warm) periods. They argue that the changes in Earth’s orbit around the Sun in isolation is not sufficient to explain the estimated high rate of change, and that there must be an amplifying feedback process kicking in. The necessity for a feedback is not new, as the Swedish Nobel Prize winner (Chemistry), Svante Arrhenius, suggested already in 1896 that CO2 could act as an amplification mechanism. In addition, there is the albedo feedback, where the amount of solar radiation that is reflected back into space, scales with the area of the ice- and snow-cover. And are clouds as well as other aspects playing a role.

por Rasmus Benestad, com contribuições de Caspar & Eric

Em um artigo recente da Climatic Change, D.G. Martinson e W.C. Pitman III discutem uma nova hipótese que explica como o clima pode mudar abruptamente entre eras glaciais e períodos interglaciais (quentes). Eles argumentam que as mudanças na órbita da Terra ao redor do Sol em isolado não são suficientes para explicar as altas taxas de mudanças estimadas, e que deve necessariamente haver a ação de um mecanismo de feedback (ou retro-alimentação) amplificando o processo. A necessidade de um feedback não é nova, pois o sueco ganhador do Prêmio Nobel (Química), Svante Arrhenius, já havia sugerido em 1896 que o CO2 deveria agir como um mecanismo de amplificação. Além do mais, existe o feedback do albedo, pelo qual a quantidade de radiação solar que é refletida de volta ao espaço é escalonável com a área de cobertura de gelo e neve. E existem nuvens bem como outros aspectos envolvidos.

Orbital forcing A hipótese de Martinson & Pitman III formula que a entrada de água doce funciona em consonância com o ciclo de Milankovitch e o feedback de albedo. Eles concluem que os ‘maiores’ términos podem somente acontecer após um acúmulo de gelo grande o suficiente para isolar o Artico, inibindo o fluxo de entrada de água doce até um ponto em que o aumento da salinidade na camada superficial, através de um vagaroso e contínuo crescimento do gelo marinho, causa uma inversão das águas marinhas do Ártico (pelo efeito na circulação atmosférica e nas correntes oceânicas). A inversão vertical traz água quente de baixo para cima, promovendo condições mais favoráveis ao degelo. A salinidade também tem um papel, mas a hipótese não menciona variações de gases de efeito estufa (GEE). Algumas questões: Martinson e Pitman III esqueceram disso? Ou os GEE representam somente uma pequena contribuição? E, não poderiam as mudanças nos GEE explicar boa parte da variabilidade? Por outro lado, parece plausível que mudanças na salinidade e na entrada de água doce poderiam afetar a formação de gelo marinho e a convecção profunda. Contudo, até o presente, a hipótese proposta por Martinson and Pitman III é meramente uma especulação, e estamos aguardando para ver se a hipótese pode ser testada através de experimentos de modelos numéricos (o que pode requerer modelos oceânicos e de gelo marinho com maior resolução que os atualmente usados em modelos climáticos globais). Seria interessante conduzir experimentos para avaliar a significância individual da água doce, dos GEE e o efeito combinado.

Uma reação ao trabalho de Martison e Pittman é: Onde está o cálculo de energia? Gases de efeito estufa contribuem somente com alguns W/m2, em contraste com uma forçante >40 do ciclo sazonal de Milankovich. Para esta nova idéia ter mérito, teria sido melhor ter no mínimo fluxos de calor em paralelo com a forçante radioativa do CO2. Estudos de modelagem anteriores encontraram que GEE produzem aproximadamente 50% de todo Último Máximo Glacial (inglês, LGM) para a resposta da temperatura atual (veja por exemplo Broccoli & Manabe), a outra parte sendo o albedo, etc., que respondem ao ciclo sazonal de irradiância. É muito difícil isolar completamente as causas individuais pois as mudanças nos GEE podem produzir alterações na distribuição de nuvens e gelo marinho. Mas a grosso modo, se você rodar um LGM e somente somente reduzir o nível do mar, introduzir as calotas de gelo, mudar a vegetação, adicionar alguma poeria (embora esta ainda seja grosseira), então você alcançaria ao redor de 50% do caminho que você quer ir. Mude a concentração de GEE e você chegaria mais próximo. Isso é mais ou menos o que Manabe e Stouffer mostraram há quinze anos atrás. A questão é se realmente precisamos de algo mais, e se esse ‘algo mais’ tem força suficiente.

traduzido por Ivan B. T. Lima e Fernando M. Ramos.


[Read more…] about What triggers ice ages? O que Dispara as Eras Glaciais? Buzul Çağlarını Tetikleyen Nedir?Qu’est ce qui déclenche les glaciations?

Filed Under: Arctic and Antarctic, Climate modelling, Climate Science, FAQ, Reporting on climate

Fraser Institute fires off a damp squib

3 Feb 2007 by group

New addition: Download an annotated pdf of the Fraser report. An interactive pdf file, to be read on the screen, is here, and a printable version is here. Suggestions for further commenting are welcome. Additions to the pdf have to be short, and tied to particular pieces of text or figures. And of course we will only incorporate comments that we deem to be scientifically sound and cogent.

*****************

While most of the world’s climate scientists were following the IPCC fest last week, a few contrarians left out in the cold were trying to to organize their own party.

An unofficial, “Independent Summary for Policymakers” (ISPM) of the IPCC Fourth Assessment report has been delivered by the Fraser Institute. It’s a long, imposing-looking document, resembling, come to think of it, the formatting of the real Summary for Policymakers (SPM) document that was released on Friday after final negotiations of the IPCC in Paris last week. The Fraser Institute has assembled an awesome team of 10 authors, including such RC favorites as tilter-against-windmills-and-hockey-sticks Ross McKitrick, and other luminaries such as William Kininmonth, MSc, M.Admin — whose most recent paper is “Don’t be Gored into Going Along” in the Oct-Nov issue of Power Engineer. To be fair, he did publish a paper on weather forecasting, back in 1973. According to the press release, the London kickoff event will be graced by the presence of “noted environmentalist” David Bellamy. It’s true he’s “noted,” but what he’s noted for is his blatant fabrication of numbers purporting to show that the world’s glaciers are advancing rather retreating, as reported here.

[Read more…] about Fraser Institute fires off a damp squib

Filed Under: Climate Science, Extras, IPCC, Reviews

Stern Science La science de SternA ciência de Stern

28 Jan 2007 by group

Halldór Björnsson, William Connolley and Gavin Schmidt

Late last year, the UK Treasury’s Stern Review of the Economics of Climate Change was released to rapturous reception from all sides of the UK political spectrum (i.e. left and right). Since then it has been subject to significant criticism and debate (for a good listing see Rabbett Run). Much of that discussion has revolved around the economic (and ethical) issues associated with ‘discounting’ (how you weight welfare in the future against welfare today) – particularly Nordhaus’s review. We are not qualified to address those issues, and so have not previously commented.

However, as exemplified by interviews on a recent Radio 4 program (including with our own William Connolley), some questions have involved the science that underlies the economics. We will try and address those.
Halldór Björnsson, William Connolley and Gavin Schmidt (traduit par Etienne Pesnelle)

A la fin de l’an dernier, le Trésor britannique a publié le rapport Stern sur les conséquences économiques du changement climatique, qui a été reçu avec enthousiasme par l’ensemble de la classe politique du Royaume-Uni, c’est à dire la gauche et la droite Depuis, il a fait l’objet de nombreux débats et critiques (voir la liste qu’a établie Rabbett Run). L’essentiel de la discussion a tourné autour des problèmes économiques (et éthiques) associés à “l’actualisation” (c’est-à-dire comment mesurer le bien-être futur à l’aune du bien-être actuel), ce dont traite notamment Nordhaus . Nous ne sommes pas qualifiés pour discuter de ces points, aussi ne les avons-nous pas commentés précédemment.

Toutefois, comme l’illustrent les interviews données lors d’une émission récente de Radio 4 (dont une avec notre William Connolley), certaines questions ont concerné la science qui sous-tend les calculs économiques. Nous allons essayer de les aborder.
Halldór Björnsson, William Connolley e Gavin Schmidt (traduzido por F. M. Ramos e I. B. T. Lima)

No fim do ano passado, o Tesouro britânico publicou o Relatório Stern sobre as conseqüências econômicas das mudanças climáticas, que foi recebido com entusiasmo pelo conjunto da classe política do Reino Unido, isto é a esquerda e a direita. Depois, ele foi objeto de inúmeros debates e críticas (ver a lista que preparou Rabbett Run). O essencial da discussão realizou-se em torno dos problemas econômicos (e éticos) associados à “atualização” (isto é, como medir o bem-estar futuro em comparação ao bem-estar atual) – particularmente o Relatório Nordhaus. Nós não estamos qualificados para comentar estes assuntos, assim como não comentamos no passado.

No entanto, como ilustram as entrevistas concedidas durante um recente programa de Radio
4
(das quais uma com William Connolley), certas questões diziam respeito à ciência que sustenta os cálculos econômicos. Vamos tentar abordá-las a seguir. Ao contrário de um relatório mais antigo da Câmara dos Lordes, Stern não perde tempo tentando trapacear, e essencialmente busca a ciência no relatório do IPCC, com algumas atualizações de trabalhos mais recentes. A maior parte da ciência está resumida no capítulo um, e um leitor casual familiarizado com o relatório IPCC encontrará poucas surpresas em seções que incluem afirmações como “Uma massa esmagadora de evidências científicas indica que o clima da Terra está mudando rapidamente, predominantemente pelo efeito do crescimento dos gases de efeito estufa causado pelas atividades humanas” etc. Entretanto, as possibilidades científicas em Stern são ponderadas de maneira levemente diferente que nos relatórios do IPCC uma vez que, como ele afirma, “os tomadores de decisão devem levar em conta os riscos extremos, além das previsões médias, por que seria muito grave se estes riscos viessem a se materializar” (Stern reply to Byatt et al).

Há três componentes científicas no relatório Stern: a sensibilidade climática, as emissões futuras dos gases de efeito estufa, e os impactos de uma dada mudança, expressas na forma de anomalia de temperatura global por razões de comodidade.

A sensibilidade climática (já discutida aqui anteriormente) foi considerada como provavelmente estando no intervalo de 1.5 a 4.5 C do IPCC TAR, e no intervalo de 2 a 5 C nos modelos utilizados no relatório Stern. No entanto, a probabilidade de valores maiores tem um papel importante no relatório. Especificamente, Meinshausen* (2006) [estabelece] que há “entre 2% a 20% de probabilidade que o aquecimento possa ser maior que 5 C”. Isto é verdade, mas o relatório esquece de mencionar que outros novos estudos (Annan and Hargreaves; Hegerl et al) sugerem que é insignificante a probabilidade que a sensibilidade climática seja superior a 5 C.

A incerteza sobre o aquecimento futuro não se reduz à incerteza sobre a sensibilidade, mas depende também daquela relacionada aos níveis futuros dos gases de efeito estufa (GEE). Existe uma ampla gama de cenários e de estimativas sobre níveis futuros de GEE que são utilizados nos relatórios do IPCC. O cenário utilizado pelo Relatório Stern é o A2, mas neste cenário, os níveis de GEE na segunda metade do século XXI são superiores àqueles do cenário A1b, por exemplo. A questão não é se o cenário A2 é menos sólido que o A1, mas simplesmente que o Relatório Stern escolheu trabalhar com um dos cenários de “fortes emissões”. Além disso, o relatório reconhece também a grande incerteza (mas não claramente quantificável) de feedbacks positivos nas emissões de CO2 e CH4 de origem natural.

Com relação aos impactos das mudanças climáticas, a estória é semelhante: a maior parte dos impactos são declarados mas sua probabilidade de ocorrência é sujeita à debate. Por exemplo: o enfraquecimento da corrente termohalina sob 1 grau de aquecimento, risco de colapso em 3 graus, risco de derretimento irreversível da calota de gelo da Groenlândia para um aquecimento de 2 graus, a elevação dos mares de 5 a 12 metros durante muitos séculos, – estas eventualidades são questionáveis, e deveriam ser consideradas como “o cenário adverso” dentre os possíveis impactos.

Em conclusão: Stern de um modo geral utiliza bem a ciência do clima, mas desvia-se para o lado das estimativas mais impactantes e as utiliza em seu sumário. Este viés altista faz com que o relatório seja vulnerável a acusações de “alarmismo”. O relatório é justo em apontar que os danos e seus custos crescem de maneira desproporcional com o aumento da mudança de temperatura e portanto, dada esta assimetria, os tomadores de decisão têm razão de levá-los em conta. Entretanto, parece que a maior crítica deste relatório será atribuída (em outros foros) à parte econômica.

NB: De modo previsível, alguns dos “céticos” habituais atacaram igualmente a ciência do relatório Stern. No entanto, uma indicação de sua falta fundamental de seriedade é que, quando há realmente importantes incertezas (por exemplo, a probabilidade de que a sensibilidade seja superior àquela geralmente estimada), eles as ignoram para fazer as mesmas repetitivas, desinteressantes e incorretas afirmações que sempre fazem.

*Meinshausen, M. (2006): ‘What does a 2C target mean for greenhouse gas concentrations? A brief analysis based on multi-gas emission pathways and several climate sensitivity uncertainty estimates’ (“O que significa um alvo de +2°C em termos de concentração de gás de efeito estufa? Uma rápida análise fundamentada em caminhos de emissão multi-gás e várias estimativas de incerteza da sensibilidade climática”), Avoiding dangerous climate change (Evitando uma perigosa mudança climática), in H.J. Schellnhuber et al. (eds.), Cambridge: Cambridge University Press, pp. 265 a 280.
[Read more…] about Stern Science La science de SternA ciência de Stern

Filed Under: Climate modelling, Climate Science, Extras, IPCC, Reviews

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