It looks like you're using an Ad Blocker.
Please white-list or disable AboveTopSecret.com in your ad-blocking tool.
Thank you.
Some features of ATS will be disabled while you continue to use an ad-blocker.
www.pnas.org...
On the other hand, the relatively sulfur-poor eruption of Mt. St. Helens (VEI 5) (2, 7) in 1980 contributed very little sulfate mass to the stratospheric aerosol layer (6). The fact that Mt. St. Helens’ plume was emitted at an angle also reduced the amount of possible stratospheric injections by this volcano.
The source for the elevated aerosol levels in the second half of 2006 and 2007 has been identified as the eruption of the Soufri`ere Hills volcano (16.72 N, 62.18W, Montserrat, West Indies), on 20 May 2006.
ntrs.nasa.gov...
The increase of backscatter coefficient in the lower stratosphere in late 2006 in the southern hemisphere is due to aerosol originating with the October 2006 Tavurvur eruption that appears to have been transported preferentially to southern latitudes in late 2006 in fashion similar to the 1990 eruption of Kelut (Thomason et al. 1997).
source
As used here, “colossal” or “major” refers to specific volcanic eruptions that have been generally recognized not only as extremely large but also as having injecting a great deal of gaseous sulfur directly into the tropical stratosphere.
Perhaps not surprisingly, the talk about geoengineering has fed into conspiracy theories about how governments are already manipulating the climate, or worse. (Try googling chemtrails.) Keith has received hate mail, and Gates’ involvement has fueled suspicions that a cabal of the powerful is hatching secret plots.
The latest to do so is David G. Victor, a professor of law at Stanford who directs a program on energy and sustainable development at the university. With four academic colleagues–Victor M. Granger, Jay Apt, John Steinbruner and Katherine Ricke–Victor has written an essay in Foreign Affairs called “The Geoengineering Option” that calls for more scientific research and policy debate about geoengineering.
Yet, as Victor and his colleagues point out in Foreign Affairs, there’s a scarcity of scientific research into the topic:
Despite years of speculation and vague talk, peer-reviewed research on geoengineering is remarkably scarce. Nearly the entire community of geoengineering scientists could fit comfortably in a single university seminar room, and the entire scientific literature on the subject could be read during the course of a transatlantic flight. Geoengineering continues to be considered a fringe topic.
Professor Benford (U.C. Irvine, CA), wrote the following regarding the public in a Reason.com article in 1997: “…But perhaps the greatest unknown is social: How will the politically aware public react--those who vote, anyway? If geoengineers are painted early and often as Dr. Strangeloves of the air, they will fail. Properly portrayed as allies of science--and true environmentalism--they could become heroes… A major factor here will be whether mitigation looks like yet another top-down contrivance, another set of orders from the elite. source credit
Oh, yes all that blather defending the billions and billions of dollars every year
just on "research" alone. *SIGH*
The data is there. Either you haven't looked at it, you don't understand it, or you reject it. If you reject it you are rejecting the data which you claim is proof of geoengineering. If you reject the data you...have...nothing.
The study found that it doesn't take large volcanoes to have a significant effect on stratospheric aerosols. Small eruptions make a significant contribution. The spikes seen in the data correspond eruptions of smaller volcanos.
“Stratospheric aerosol increased surprisingly rapidly in that time, almost doubling during the decade,” Daniel said.
The reasons for the 10-year increase in stratospheric aerosols are not fully understood and are the subject of ongoing research, says coauthor Ryan Neely, with the University of Colorado and the Cooperative Institute for Research in Environmental Sciences (CIRES).
We find that, following the 1991 eruption of Mount Pinatubo, stratospheric aerosol levels increased by as much as two orders of magnitude and only reached “background levels” between 1998 and 2002. From 2002 onwards, a systematic increase has been reported by a number of investigators.
However, we demonstrate with these satellite measurements that the observed trend is mainly driven by a series of moderate but increasingly intense volcanic eruptions primarily at tropical latitudes. These events injected sulfur directly to altitudes between 18 and 20 km.
However, the fate of volcanic plumes injected below 20km is very different. Indeed, they disappear within 1–3 months and are diluted every winter, directly or after horizontal transport from middle latitudes to the tropics, by rapid injection of clean air (SR
I have shown that, depending on the source, from two current studies, sulphur in the stratosphere warms us and sulphur in the stratosphere cools us.
and yet the study itself disputes you in stating:
...
and you further quote a propoganda study to support your fantasy point:
which disputes its' own findings within the study itself:
and disputes your 18 to 20 kilometer statements. Are you confused yet?
www.agu.org...
These events injected sulfur directly to altitudes between 18 and 20 km. The resulting aerosol particles are slowly lofted into the middle stratosphere by the Brewer-Dobson circulation and are eventually transported to higher latitudes.
Let's continue with some basic information on volcanic sulphur and the stratosphere:
Volcanic contributions to the permanent stratospheric aerosol layer
For the first time, those moderate events have been detected over a long period, demonstrating that eruptions with a volcanic explosivity index between three and four and located in the tropics can be an important source of aerosols for the stratosphere, a fact not fully recognized until now. For the first time, those moderate events have been detected over a long period, demonstrating that eruptions with a volcanic explosivity index between three and four and located in the tropics can be an important source of aerosols for the stratosphere, a fact not fully recognized until now. The sulfuric dioxide initially injected at 19–20km is oxidized into sulfuric acid droplets and transported by the general circulation—also called Brewer-Dobson (BD) circulation—into the middle tropical stratosphere, forming a reservoir.
Apparently whoever wrote that was unaware of what satellite observations have shown (see above) or wrote it before the data was available.
Volcanic aerosols
Volcanic emissions sufficiently cataclysmic to penetrate the stratosphere are rare.
Rather than focusing on fantasy studies, focus on how those aerosols at 18 to 20 kilometers took up residence in the stratosphere for years.
But I am confused about the point you're trying to make.
And then you try to exclude by quoting something about something called a 'Brewer-Dobson' whatever.
Brewer-Dobson circulation is a model of atmospheric circulation, proposed by Alan Brewer in 1949 and Gordon Dobson in 1956, which attempts to explain why tropical air has less ozone than polar air, even though the tropical stratosphere is where most atmospheric ozone is produced. It is a simple circulation model that posits the existence of a slow current in the winter hemisphere which redistributes air.
I don't think so, I don't know what the Bergestrom principle is.
And then you try to exclude by quoting something about something called a 'Brewer-Dobson' whatever. Is this like the Bergestrom principle causing hole punch clouds?
www.agu.org...
These events injected sulfur directly to altitudes between 18 and 20 km. The resulting aerosol particles are slowly lofted into the middle stratosphere by the Brewer-Dobson circulation and are eventually transported to higher latitudes.
Sure. As the article says, material which does not get lifted to higher altitudes (as discussed in the prior paragraph) doesn't remain for very long. That which does lasts much longer and ends up getting distributed throughout the stratosphere and affects aerosol levels.
Below 20 kilometers. That's what I said from the studies I linked - care to respond?
The long-range transport in the tropics of several small-scale volcanic plumes has been monitored using these observations, which are unprecedented in their scope and detail. Their fate demonstrates the importance of even minor volcanic events on stratospheric-aerosol levels.
I'm confused because the article you quoted clearly states that moderate eruptions contribute to stratospheric aerosol levels. I'm confused about why you would cite such an article to defend your position.
a systematic increase has been reported by a number of investigators
Brewer-Dobson circulation is a model of atmospheric circulation, proposed by Alan Brewer in 1949 and Gordon Dobson in 1956, which attempts to explain why tropical air has less ozone than polar air, even though the tropical stratosphere is where most atmospheric ozone is produced.
Oh,BTW that is real science, so before you throw out comments about fake science you should at the very least Google it and understand what it is.
The solution: start inching down on the plume height limits for stratospheric impact. It started with 19-20 kilometers and when that wasn't quite enough, it got backed on down to 18-20. Basically fit as you go. Then you dust off and trot out a theory from 1949:
Only the puny tropical volcanoes had an impact that outshone Pinatubo in 'cooling' us.
Perfect. Because a phenomenon which you've never heard of but has been known about for decades appears in a scientific article, it must be some sort of fabrication.
Originally posted by Phage
reply to post by luxordelphi
No.
Brewer Dobson Circulation is well established as a phenomenon. It is there. It happens. It is common knowledge among meteorologists and climatologists.
www.eoearth.org...
Brewer Dobson Circulation is well established as a phenomenon. It is there. It happens. It is common knowledge among meteorologists and climatologists.
[First published in the Encyclopedia of Earth March 30, 2010; Last revised Date October 28, 2011; Retrieved March 17, 2012
This article is written at a definitional level only. Authors wishing to improve this entry are inivited to expand the present treatment, which additions will be peer reviewed prior to publication of any expansion.
Originally posted by Phage
reply to post by Gmoneycricket
Because something is described as a definition, it means it isn't real
Or did I miss your point?
chemtrail
Pronunciation: /ˈkɛmtreɪl/ noun
a visible trail left in the sky by an aircraft and believed by some to consist of chemical or biological agents released as part of a covert operation, rather than the condensed water of a vapour trail: conspiracy theorists have been going wild with speculation over the nature and purpose of chemtrails
Origin: 1990s: blend of chemical and trail, on the pattern of contrail