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Weekend round-up

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A few interesting pieces from around the web relevant to some previous postings:

  • The latest satellite imagery from the Wilkins Ice Sheet (discussed recently) is not looking good. And most curiously the collapse is happening in winter.
  • The Weather Channel “Forecast Earth” team make a valiant attempt to explain the problems and promise for regional climate change projections by 2050. See our post on the general subject from last year).
  • And for those of you following the various sagas of political interference in the communication of climate science, a nice interactive graphic summary, courtesy of UCS.

Next week will be a little quiet – it is mid-summer after all – so apologies in advance if the moderation is a somewhat slow. You may also note that we have instituted a “captcha” step to the commenting process. This uses reCAPTCHA which as well as providing protection against spam, helps with the digitization of old books.

All-paper salutes to the environment

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The Onion last week had a great (recycled) spoof on the various ‘green’ special issues being published but, not to be outdone, the contributors to RealClimate have also been busy producing paper products about the environment.

Surprisingly perhaps, as well as having day jobs and writing for this blog, collectively we have written a number of popular science books about climate change. Some of these have already been published, but there are a few more “in the pipeline”. We try not to overdo self-promotion on this website (for instance, we don’t blog about most of our own technical publications) but since these projects are synergistic with our aims here, it makes sense to let people know what we’ve been up to. We have therefore set up a page listing “Our Books” that we will keep up-to-date as more titles become available. It’s also linked from the new animated gif image on the side bar.

Ice Shelf Instability

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Guest contribution from Mauri S. Pelto

Ice shelves are floating platforms of ice fed by mountain glaciers and ice sheets flowing from the land onto the ocean. The ice flows from the grounding line where it becomes floating to the seaward front, where icebergs calve. For a typical glacier when the climate warms the glacier merely retreats, reducing its low elevation, high melting area by increasing its mean elevation. An ice shelf is nearly flat and cannot retreat in this fashion. Ice shelves cannot persist unless the entire ice shelf is an accumulation zone, where snowpack does not completely melt even in the summer.


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The Global Cooling Bet – Part 2 Apuesta al Enfriamiento Global – Segunda ParteLa scommessa sul raffreddamento globale – II parte

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Last week we proposed a bet against the “pause in global warming” forecast in Nature by Keenlyside et al. and we promised to present our scientific case later – so here it is.

Una traduzione in italiano è disponibile qui
Dieser Beitrag erscheint zeitgleich auf deutsch auf Klimalounge


Traducido por Angela Carosio

La semana pasada propusimos una apuesta contra el pronóstico en un artículo de la revista Nature “pausa en el calentamiento global” por Keenlyside et al. y prometimos presentar nuestro caso científico en otra ocasión, y aquí está.

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Butterflies, tornadoes and climate modelling

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Ed Lorenz hiking Many of you will have seen the obituaries (MIT, NYT) for Ed Lorenz, who died a short time ago. Lorenz is most famous scientifically for discovering the exquisite sensitivity to initial conditions (i.e. chaos) in a simple model of fluid convection, which serves as an archetype for the weather prediction problem. He is most famous outside science for the ‘The Butterfly Effect’ described in his 1972 paper “Predictability: Does the Flap of a Butterfly’s Wings in Brazil Set Off a Tornado in Texas?”. Lorenz’s contributions to both atmospheric science and the mathematics of dynamical systems were wide ranging and seminal. He also directly touched the lives of many of us here at RealClimate, and both his wisdom, and quiet personal charm will be sorely missed.

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Moulins, Calving Fronts and Greenland Outlet Glacier Acceleration Sifones, frentes glaciares y la aceleración de los glaciares exteriores de Groenlandia

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Guest Commentary by Mauri Pelto

The net loss in volume and hence sea level contribution of the Greenland Ice Sheet (GIS) has doubled in recent years from 90 to 220 cubic kilometers/year has been noted recently (Rignot and Kanagaratnam, 2007). The main cause of this increase is the acceleration of several large outlet glaciers. There has also been an alarming increase in the number of photographs of meltwater draining into a moulin somewhere on the GIS, often near Swiss Camp (35 km inland from the calving front). The story goes—warmer temperatures, more surface melting, more meltwater draining through moulins to glacier base, lubricating glacier bed, reducing friction, increasing velocity, and finally raising sea level. Examining this issue two years RealClimate suggested this was likely the correct story. A number of recent results suggest that we need to take another look at this story.

Una traducción está disponible aquí
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Air Capture Captura de Aire

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Guest Commentary by Frank Zeman

[This is one of an occasional series on the science of mitigation/adaptation/geo-engineering that we hope to continue. Since this isn’t our core expertise, we’d especially appreciate balanced contributions from other scientists.]

One of the central challenges of controlling anthropogenic climate change is developing technologies that deal with emissions from small, dispersed sources such as automobiles and residential houses. Capturing these emissions is more difficult as they are too small to support infrastructure, such as pipelines, and may be mobile, as with cars. For these reasons, proposed solutions, such as switching to using hydrogen or electricity as a fuel, rely on the carbon-free generation of electricity or hydrogen. That implies that the fuel must be made either by renewable generation (wind, solar, geothermal etc.), nuclear or by facilities that capture the carbon dioxide and store it (CCS).

There is however an alternative that gets some occasional attention: Air Capture (for instance, here or here). The idea would be to let people emit the carbon dioxide at the source but then capture it directly from the atmosphere at a separate facility.

Par Frank Zeman, traducido por Angela Carosio
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The global cooling mole La excusa del enfriamiento global

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By John Fleck and William Connolley

To veterans of the Climate Wars, the old 1970s global cooling canard – “How can we believe climate scientists about global warming today when back in the 1970s they told us an ice age was imminent?” – must seem like a never-ending game of Whack-a-mole. One of us (WMC) has devoted years to whacking down the mole (see here, here and here, for example), while the other of us (JF) sees the mole pop up anew in his in box every time he quotes contemporary scientific views regarding climate change in his newspaper stories.

Una traducción está disponible aqui
Tłumaczenie na polski dostępne jest tutaj.

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Tropical cyclone history – part II: Paleotempestology still in its infancy

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Guest Commentary from Urs Neu

While analyzing tropical cyclone records is difficult enough (see ‘Tropical cylone history – part I’), it is even more challenging to reliably estimate hurricane activity back in time. Recently, Nature published an attempt to reconstruct past major hurricane activity back to 1730 (Nyberg et al. 2007). The authors concluded that the phase of enhanced hurricane activity since 1995 is not unusual compared to other periods of high hurricane activity in the record and thus appears to represent a recovery to normal hurricane activity. The paper was advertised in a press release put out by Nature and received broad media attention.

Although the approach outlined by the authors is interesting, the study contains in my view a number of problems, as outlined in a comment published in Nature today (Neu 2008):

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Tropical cyclone history – part I: How reliable are past hurricane records?

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Guest Commentary from Urs Neu

When discussing the influence of anthropogenic global warming on hurricane or tropical cyclone (TC) frequency and intensity (see e.g. here, here, and here), it is important to examine observed past trends. As with all climate variables, the hurricane record becomes increasingly uncertain when we go back in time. However, the hurricane record has some peculiarities: hurricanes are highly confined structures, so you have to be at the right place at the right time to observe them. Secondly, hurricanes spend most of their life in the open oceans, i.e. in regions where there are very few people and no fixed observations. This means that the reliability of the long-term hurricane record is dependent on who was measuring them, and how, at any given time. The implementation of new observation methods, for example, might have altered the quality of the record considerably. But how much? This crucial question has been widely discussed in the recent scientific literature (e.g. Chang and Guo 2007, Holland and Webster 2007, Kossin et al. 2007, Landsea 2007, Mann et al. 2007). Where do we stand at the moment? This post will concentrate on the North Atlantic, which has the longest record.

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