I guess they really don’t have a full handle on the science and consensus after all.
NSF Releases Online, Multimedia Package Titled, “Clouds: The Wild Card of Climate Change”
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Reader-friendly multimedia package covers the crucial but enigmatic role of clouds on climate change, and how scientists are defining that role
Clouds from an airplane over Michigan. |
November 4, 2010
View a webcast with David Randall, professor of atmospheric science at Colorado State University.
As discussions about climate change continue, one critical factor about this phenomenon has remained largely unknown to the public: the important but enigmatic role of clouds in climate change. The role of clouds is important because at any given time about 70 percent of the Earth is covered by clouds. The role of clouds is enigmatic because clouds can exert opposing forces: Some types of clouds help cool the Earth and some types of clouds help warm it. Which effect will win out as our climate continues to change? So far, no one is certain.
In order to help clear the air on clouds, the National Science Foundation is releasing an online multimedia package on the role of clouds on climate change, entitled, “Clouds: The Wild Card of Climate Change.” It addresses such pressing questions as, will clouds help speed or slow climate change? Why is cloud behavior so difficult to predict? And how in the world are scientists learning to project the behavior of these ephemeral, ever-changing, high-altitude phenomena?
“Clouds: The Wild Card of Climate Change” features:
- a live webcast with cloud and climate expert: David Randall, director of the Center for Multiscale Modeling of Atmospheric Processes and a professor of atmospheric science at Colorado State University;
- informative, easy-to-understand texts;
- eye-catching photos;
- a narrated slide show;
- dynamic animations;
- enlightening interviews with cloud researchers; and
- downloadable documents.
This package–which provides a wealth of information to reporters, policymakers, scientists, educators, the public and students of all levels–is posted on NSF’s website.
-NSF-
I guess the science is still not settled…warm, cold, warm, cold.
Well if you go by our planet moving away from the sun, how can it get any warmer?
There should be very interesting discussions and debates on this topic. I remember Dr. Roy Spencer said that from his initial studies, there is a negative feedback of clouds and water vapor on initial warming by man-made GHGs.
I find the claim that the role of clouds remained largely unknown to the public quite funny. As a member of the public I always felt, for as long as the debate has been going, that the role of the clouds was remaining largely ignored by the alarmists. Perhaps they are finally awakening from their slumber.
My thought is rather simple in that all clouds have an albedo effect. The pro AGW thought is that the net effect is positive, some clouds warm, some cool, some are neutral, depending I suppose on the relative changes in LWIR and SW which reach the surface. The idea being that the clouds increase the residence time of LWIR in the atmosphere while the vast majority of SWR continues to the surface.
My thought is that not all photons are equall due to their relative residence time in earth’s system, both ocean and amotsphere. So a cloud that blocks 5 W/m’2 of SWR through albedo, but has a 15 W/m’2 warming effect through the GHG effect will warm the atmosphere, but do to the far longer residence time of SWR photons entering the ocean the reduction of those 5 W/m’2 reduced SWR will have a stronger long term effect which is cumlitive depending on the duration of the change in cloud cover, and certainly as Stephen Wilde expresses, their laditude, which as they shift poleward obviously effects an ever greater % of the TSI. Ans so some clouds may indeed cause a short term atmospheic warming, but a longer term ocean cooling.
I definitely do not have the numbers to quantify the effect I am considering, primarily because I do not know the residence time of SWR photons entering the ocean vs the residence time of LWIR in the atmosphere. Any help here is appreciated.
In their article on clouds, http://www.nsf.gov/news/special_reports/clouds/question.jsp, the NSF says “many scientists say that if warming were to increase the number or kind of cooling clouds or decrease the presence of warming clouds, the current net cooling effect of clouds on the Earth’s climate would probably increase, and thereby moderate, or offset, ongoing warming“.
Oh dear. Didn’t they read the IPCC report? “the GCMs all predict
a positive cloud feedback” (AR4 8.6.2.3 page 633). Admittedly the IPCC does go on to say “but strongly disagree on its magnitude“, but that still doesn’t allow cloud feedback to be anything but positive.
david says:
November 5, 2010 at 4:57 am
“So a cloud that blocks 5 W/m’2 of SWR through albedo”
is hardly a cloud.
Fixed that for ya. Cloud top albedo is on the order of 80%. That means it reflects 80% of the light from the sun straight back out into space. That’s closer to 500 watts per square meter than it is to 5 watts. At night they reflect less than 50% of the upwelling long wave radiation back towards the surface and to make it even more unbalanced clouds tend to form in the morning and early afternoon and dissipate in the late afternoon and early evening.
The only “mystery” is exactly how unbalanced the situation is on a global average basis but there’s no credible doubt that clouds have a large net cooling effect. There’s also no doubt that there are more clouds when it’s warmer and fewer when it is colder. So if there is any additional forcing (more surface heat) from higher CO2 level this results in more clouds which will negate the additional forcing from CO2.
The ONLY significant greenhouse effect from CO2 is that first 100ppm or so raises the average temperature of the earth from below freezing to above freezing which activates the water cycle. Once the water cycle is active it takes over the regulation of surface temperature through negative feedback. The only thing to fear is when CO2 is not enough to keep the surface temperature above freezing. When that happens the water cycle effectively screeches to a halt and the surface gets covered with snow which also reflects 80% of the sun’s light and thus fosters even colder surface temperatures and even more snow in a vicious cycle of falling temperatures.
Evidently the pre-industrial level of 280ppm CO2 isn’t enough to stop the brief interglacial periods from ending as for the past several millions of years the earth is largely covered by glaciers 90% of the time. One can only pray that an anthropogenic driven doubling of CO2 to 560ppm or even a quadrupling to 1100ppm is enough to indefinitely extend the Holocene interglacial. If not then human civilization is in for big trouble. Imagine glaciers two miles thick covering all land surfaces from Washington, D.C. northward and land south of that having harsh winters instead of being above freezing all year round.
Hastening the end of the Holocene interglacial by reducing CO2 emissions is utter insanity.
Watch the pea,
‘Cirrus clouds: These clouds are wispy and feathery, and positioned up to 20 kilometers above the Earth’s surface. Cirrus clouds let much sunlight pass through them and may also trap the Earth’s heat, just as greenhouse gases do. Therefore, they have a net warming effect that helps magnify warming. ‘
So noticeable nowadays.
“The role of clouds is enigmatic because clouds can exert opposing forces: Some types of clouds help cool the Earth and some types of clouds help warm it”
Well that certainly clears up the certain uncertainties!!!
What we don’t know is amazing !!
“Which effect will win out as our climate continues to change?”
Before you use words like that prove to me that climate is actually “changing”. So far all you can show is that it oscillates, and that is not the same thing.
David Springer is absolutely right.
“..moderate, or offset, ongoing warming”?
Do they have a graph yet that shows the on going unstopable global warming and the current contribution of the negative offset global warming that shows a net non-positive global warming problem?
If you have more negative ‘offset global warming’ than you have ‘global warming’ isn’t that just called, well, cooling?
Do there people keep their beer in a warming offset device, or a cooler?
Anytime a cloud comes between the sun and the earth, there is an immediate and noticeable drop in temperatures, that increases the lower a cloud is. That can only mean that the albedo-enhancing effect dominates the heat trapping effect by quite a large margin, so during the day, clouds are a negative feedback.
When the sun isn’t shining however, clouds do keep things warmer than they would otherwise be, therefore they could be said to have a positive feedback effect at nighttime.
Overall, given the same amount of clouds at night and day, the effect would be negative, because they are reflecting away a lot more energy than they are retaining. I’ve never noticed a rise in temperatures at nighttime when a cloud comes over as much as the drop in temperatures in the daytime.
Honesty about climate change uncertainties? My hat is off to the National Science Foundation!!
Whenever I see a straight line I know that I am looking at an artifact. When I see a feedback loop I know that I am looking at a computer programme. If nature allowed continuous looped feedbacks, the universe would have burned up billions of years before we were born.
I find myself continually questioning CO2 levels in the past for three reasons. I question past estimates of CO2 because of the ubiquitous use of fires in every home as the only means of heat, which is not so now. In high population urban centers, this often meant coal fires. Two, fire suppression was also not the order of the day in our past. State-wide fires raged out of control, pumping tons of CO2 into the air. This is not the case now. Three, that these levels of CO2 emissions were not recorded in ice cores could be related to the fact that rain may have washed out these emissions prior to them migrating the long distance to areas of the globe that entrapped CO2 in ice. In addition, it seems logical to include the fact that population has steadily increased towards CO2 trapping ice. Could the increase in trapped CO2 in recent years be more a product of the encroaching population? Is it because CO2 emissions are simply closer to the ice trapping fields now than in the past? Bottom line, I take past estimates of CO2 with a rather large chunk of salt. More the size of a salt pillar.
From “Prof.” J. Collins:
“I’ve looked at clouds from both sides now,
From up and down, and still somehow,
It’s cloud illusions I recall,
I really don’t know clouds, at all. ”
A “golden-oldie” still good today!
david says:
November 5, 2010 at 4:57 am
“My thought is rather simple in that all clouds have an albedo effect. The pro AGW thought is that the net effect is positive, some clouds warm, some cool, some are neutral, depending I suppose on the relative changes in LWIR and SW which reach the surface. The idea being that the clouds increase the residence time of LWIR in the atmosphere while the vast majority of SWR continues to the surface.
My thought is that not all photons are equall due to their relative residence time in earth’s system, both ocean and amotsphere. So a cloud that blocks 5 W/m’2 of SWR through albedo, but has a 15 W/m’2 warming effect through the GHG effect will warm the atmosphere, but do to the far longer residence time of SWR photons entering the ocean the reduction of those 5 W/m’2 reduced SWR will have a stronger long term effect which is cumlitive depending on the duration of the change in cloud cover, and certainly as Stephen Wilde expresses, their laditude, which as they shift poleward obviously effects an ever greater % of the TSI. Ans so some clouds may indeed cause a short term atmospheic warming, but a longer term ocean cooling.
I definitely do not have the numbers to quantify the effect I am considering, primarily because I do not know the residence time of SWR photons entering the ocean vs the residence time of LWIR in the atmosphere. Any help here is appreciated.”
Photons have practically no residence time anywhere. They travel with the speed of light, whether they are “short wave” (UV or optical) or “long wave”.
The clouds absorb the upward moving long wave radiation, and reemit long wave radiation back to the earths surface, where it is absorbed and reemitted. The tops of clouds will also emit IR radiation upward.
The tops of clouds reflect optical wave length radiation coming from the sun, back into space. The relative amounts of radiation sent back to space, versus sent back to the ground determine the effects of clouds, and are different for upper level and lower level clouds.
I would not recommend Stephen Wilde as a source. He is not a scientist of any sort, he is a solicitor who dabbles in weather, and passes himself off as a Fellow of the Royal Meteorological Society, which he is not.
Why not go the the National Science Foundation cloud web site which is the subject of this post?
“Clouds: The Wild Card of Climate Change”
I disagree, Volcanos are currently the Wild Card of Climate Change, Clouds just represent a giant gap in human knowledge and understanding of Earth’s climate system…
So we don’t know how the oceans affect the climate (at least the models don’t include the oceans) and we don’t know how clouds really affect the climate either, whether warming causes more clouds or whether less clouds causes the warming (which is cause and which is effect), but we know what the climate is going to be in 20, 30, 50 or 100 years? Really?
Dave Springer says:
November 5, 2010 at 5:57 am
“There’s also no doubt that there are more clouds when it’s warmer and fewer when it is colder.”
I need to qualify that, Dave.
It’s certainly true locally (after a short period of adjustment when perversely the opposite applies as the system plays catch up with the temperature change) and perhaps regionally, but globally ? There’s the rub.
The evidence from the Earthshine project is that cloud quantities decreased during the recent warming spell and are now increasing with the cessation of warming and perhaps beginning of cooling. Likewise albedo.
http://bbso.njit.edu/Research/EarthShine/literature/Palle_etal_2006_EOS.pdf
So how could that be ? Strange how so many observations are turning out to have the reverse sign from standard expectations isn’t it ?
I would explain it by reference to the shifting of the jet streams and thus the associated cloud bands latitudinally.
At the same time as the albedo and cloudiness trends reversed in the late 90s I noted that the jets were starting to shift back equatorwards.
So my bet is that in shifting equatorward the cloud bands were stretched along a greater global circumference, increasing the length of the air mass boundaries and allowing more air mass mixing to produce more clouds.
Additionally the equatorward shift makes the clouds more reflective since they block higher intensity insolation.
That is what primarily causes global albedo changes and thereby changes the amount of solar shortwave able to penetrate the oceans.
Considering the general ability of these people to determine cause and effect on anything else, how are they possibly going to determine the long term impact of clouds on climate.
In all likelyhood the long term effect is neutral as clouds are generally a response. This is especially not surprising considering the little to no impact that anthropogenic CO2 has on long term climate.
How can they figure clouds out if CO2 confuses them?
Theinconvenientskeptic.com
Any ‘proper’ cloud reflects most of the sunlight back out into space. As this radiation never actually gets to the surface clouds by definition cool the Earth. Do we have decent records of Earth albedo from projects such as Earthshine and the many satellites we have orbiting us?
Mike Jonas says:
November 5, 2010 at 5:10 am
“In their article on clouds, http://www.nsf.gov/news/special_reports/clouds/question.jsp, the NSF says “many scientists say that if warming were to increase the number or kind of cooling clouds or decrease the presence of warming clouds, the current net cooling effect of clouds on the Earth’s climate would probably increase, and thereby moderate, or offset, ongoing warming“.
“Oh dear. Didn’t they read the IPCC report? “the GCMs all predict
a positive cloud feedback” (AR4 8.6.2.3 page 633). Admittedly the IPCC does go on to say “but strongly disagree on its magnitude“, but that still doesn’t allow cloud feedback to be anything but positive.”
It is very funny, indeed.
Maybe one day they will understand that they need to go back to school, learning about closed feedback loops. Maybe they will be forced to learn about Laplace transformations? One can only hope.
Maybe they could ask Roy Spencer if he can be their teacher?
But that would of course lead to a world wide acknowledgement that we would all be better off spending time on soft sciences as a hobby, and learning hard science at school.
That would be very bad for the post modern types.
massive ice growth in arctic LOL
see DMI
Brian M. Flynn says:
November 5, 2010 at 6:38 am
From “Prof.” J. Collins:
“I’ve looked at clouds from both sides now,
From up and down, and still somehow,
It’s cloud illusions I recall,
I really don’t know clouds, at all. ”
A “golden-oldie” still good today!
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Dang! I had the tune in my head but just couldn’t remember all the words! Beautiful song! Thanks!