Prediction is hard, especially of the future.

Guest Post by Willis Eschenbach

[UPDATE]: I have added a discussion of the size of the model error at the end of this post.

Over at Judith Curry’s climate blog, the NASA climate scientist Dr. Andrew Lacis has been providing some comments.  He was asked:

Please provide 5- 10 recent ‘proof points’ which you would draw to our attention as demonstrations that your sophisticated climate models are actually modelling the Earth’s climate accurately.

To this he replied (emphasis mine),

Of note is the paper by Hansen, J., A. Lacis, R. Ruedy, and Mki. Sato, 1992: Potential climate impact of Mount Pinatubo eruption. Geophys. Res. Lett., 19, 215-218, which is downloadable from the GISS webpage.

It contains their model’s prediction of the response to Pinatubo’s eruption, a prediction done only a few months after the eruption occurred in June of 1991:

Figure 1. Predictions by NASA GISS scientists of the effect of Mt. Pinatubo on global temperatures. Scenario “B” was Hansen’s “business as usual” scenario. “El” is the estimated effect of a volcano the size of El Chichón. “2*El” is a volcano twice the size of Chichón. The modelers assumed the volcano would be 1.7 times the size of El Chichón. Photo is of Pinatubo before the eruption.

Excellent, sez’ I, we have an actual testable prediction from the GISS model. And it should be a good one if the model is good, because they weren’t just guessing about inputs. They were using early estimates of aerosol depth that were based on post-eruption observations. But with GISS, you never know …

Here’s Lacis again talking about how the real-world outcome validated the model results. (Does anyone else find this an odd first choice when asked for evidence that climate models work? It is a 20-year-old study by Lacis. Is this his best evidence he has?) But I digress … Lacis says further about the matter:

There we make an actual global climate prediction (global cooling by about 0.5 C 12-18 months following the June 1991 Pinatubo volcanic eruption, followed by a return to the normal rate of global warming after about three years), based on climate model calculations using preliminary estimates of the volcanic aerosol optical depth. These predictions were all confirmed by subsequent measurements of global temperature changes, including the warming of the stratosphere by a couple of degrees due to the volcanic aerosol.

As always, the first step in this procedure is to digitize their data. I use a commercial digitizing software called “GraphClick” on my Mac, there are equivalent programs for the PC, it’s boring tedious hand work. I have made the digitized data available here as an Excel worksheet.

Being the untrusting fellow that I am, I graphed up the actual temperatures for that time from the GISS website. Figure 2 shows that result, along with the annual averages of their Pinatubo prediction (shown in detail below in Figure 3), at the same scale that they used.

Figure 2. Comparison of annual predictions with annual observations. Upper panel is Figure 2(b) from the GISS prediction paper, lower is my emulation from digitized data. Note that prior to 1977 the modern version of the GISS temperature data diverges from the 1992 version of the temperature data. I have used an anomaly of 1990 = 0.35 for the modern GISS data in order to agree with the old GISS version at the start of the prediction period. All other data is as in the original GISS prediction. Pinatubo prediction (blue line) is an annual average of their Figure 3 monthly results.

Again from their paper:

Figure 2 shows the effect of E1 and 2*El aerosol son simulated global mean temperature. Aerosol cooling is too small to prevent 1991 from being one of the warmest years this century, because of the small initial forcing and the thermal inertia of the climate system. However, dramatic cooling occurs by 1992, about 0.5°C in the 2*El case. The latter cooling is about 3 σ [sigma], where σ is the interannual standard deviation of observed global annual-mean temperature.This contrasts with the 1-1/2 σ coolings computed for the Agung (1963)and El Chichon (1982) volcanos

So their model predicted a large event, a “three-sigma” cooling from Pinatubo.

But despite their prediction, it didn’t turn out like that at all. Look at the red line above showing the actual temperature change. If you didn’t know there was a volcano in 1991, that part of the temperature record wouldn’t even catch your eye. Pinatubo did not cause anywhere near the maximum temperature swing predicted by the GISS model. It was not a three-sigma event, just another day in the planetary life.

The paper also gave the monthly predicted reaction to the eruption. Figure 3 shows detailed results, month by month, for their estimate and the observations.

Figure 3. GISS observational temperature dataset, along with model predictions both with and without Pinatubo eruptions. Upper panel is from GISS model paper, lower is my emulation. Scenario B does not contain Pinatubo. Scenario P1 started a bit earlier than P2, to see if the random fluctuations of the model affected the result (it didn’t). Averages are 17-month Gaussian averages. Observational (GISS) temperatures are adjusted so that the 1990 temperature average is equal to the 1990 Scenario B average (pre-eruption conditions). Photo Source

One possibility for the model prediction being so far off would be if Pinatubo didn’t turn out to be as strong as the modelers expected. Their paper was based on very early information, three months after the event, viz:

The P experiments have the same time dependence of global optical depth as the E1 and 2*El experiments, but with r 1.7 times larger than in E1 and the aerosol geographical distribution modified as described below. These changes crudely account for information on Pinatubo provided at an interagency meeting in Washington D.C. on September 11 organized by Lou Walter and Miriam Baltuck of NASA, including aerosol optical depths estimated by Larry Stowe from satellite imagery.

However, their estimates seem to have been quite accurate. The aerosols continued unabated at high levels for months. Optical depth increased by a factor of 1.7 for the first ten months after the eruption. I find this (paywall)

Dutton, E. G., and J. R. Christy, Solar radiative forcing at selected locations and evidence for global lower tropospheric cooling following the eruptions of El Chichon and Pinatubo, Geophys. Res. Lett., 19, 2313-1216, 1992.

As a result of the eruption of Mt. Pinatubo (June 1991), direct solar radiation was observed to decrease by as much as 25-30% at four remote locations widely distributed in latitude. The average total aerosol optical depth for the first 10 months after the Pinatubo eruption at those sites is 1.7 times greater than that observed following the 1982 eruption of El Chichon

and from a 1995 US Geological Service study:

The Atmospheric Impact of the 1991 Mount Pinatubo Eruption ABSTRACT

The 1991 eruption of Pinatubo produced about 5 cubic kilometers of dacitic magma and may be the second largest volcanic eruption of the century. Eruption columns reached 40 kilometers in altitude and emplaced a giant umbrella cloud in the middle to lower stratosphere that injected about 17 megatons of SO2, slightly more than twice the amount yielded by the 1982 eruption of El Chichón, Mexico. The SO2 formed sulfate aerosols that produced the largest perturbation to the stratospheric aerosol layer since the eruption of Krakatau in 1883. … The large aerosol cloud caused dramatic decreases in the amount of net radiation reaching the Earth’s surface, producing a climate forcing that was two times stronger than the aerosols of El Chichón.

So the modelers were working off of accurate information when they made their predictions. Pinatubo was just as strong as they expected, perhaps stronger.

Finally, after all of that, we come to the bottom line, the real question. What was the difference in the total effect of the volcano, both in observations and in reality? What overall difference did it make to the temperature?

Looking at Fig. 3 we can see that there is a difference in more than just maximum temperature drop between model results and data. In the model results, the temperature dropped earlier than was observed. It also dropped faster than actually occurred. Finally, the temperature stayed below normal for longer in the model than in reality.

To measure the combined effect of these differences, we use the sum of the temperature variations, from before the eruption until the temperature returned to pre-eruption levels. It gives us the total effect of the eruption, in “degree-months”. One degree-month is the result of changing the global temperature one degree for one month. It is the same as lowering the temperature half a degree for two months, and so on.

It is a measure of how much the volcano changed the temperature. It is shown in Fig. 3 as the area enclosed by the horizontal colored lines and their respective average temperature data (heavier same color lines). These lines mark the departure from and return to pre-eruption conditions. The area enclosed by each of them is measured in “degree – months” (degrees vertically times months horizontally).

The observations showed that Pinatubo caused a total decrease in the global average temperature of eight degree-months. This occurred over  a period of 46 months, until temperatures returned to pre-eruption levels.

The model, however, predicted twice that, sixteen degree-months of cooling. And in the model, temperatures did not return to pre-eruption conditions for 63 months. So that’s the bottom line at the end of the story — the model predicted twice the actual total cooling, and predicted it would take fifty percent longer to recovery than actually happened … bad model, no cookies.

Now, there may be an explanation for that poor performance that I’m not seeing. If so, I invite Dr. Lacis or anyone else to point it out to me. Absent any explanation to the contrary, I would say that if this is his evidence for the accuracy of the models, it is an absolute  … that it is a perfect … well, upon further reflection let me just say that I think the study and prediction is absolutely perfect evidence regarding the accuracy of the models, and I thank Dr. Lacis for bringing it to my attention.

[UPDATE] A number of the commenters have said that the Pinatubo prediction wasn’t all that wrong and that the model didn’t miss the mark by all that much. Here’s why that is not correct.

Hansen predicted what is called a “three sigma” event. He got about a two sigma event (2.07 sigma). “Sigma” is a measure of how common it is for something to occur. However, it is far from linear.

A two sigma event is pretty common. It occurs about one time in twenty. So in a dataset the size of GISSTEMP (130 years) we would expect to find somewhere around 130/20 = six or seven two sigma interannual temperature changes. These are the biggest of the inter-annual temperature swings. And in fact, there are eight two-sigma temperature swings in the GISSTEMP data.

A three sigma event, on the other hand, is much, much rarer. It is a one in a thousand event. The biggest inter-annual change in the record is 2.7 sigma. There’s not a single three sigma year in the entire dataset. Nor would we expect one in a 130 year record.

So Hansen was not just making a prediction of something usual. He was making a prediction that we would see a temperature drop never before seen, a once in a thousand year drop.

Why is this important? Remember that Lacis is advancing this result as a reason to believe in climate models.

Now, suppose someone went around saying his climate model was predicting a “thousand-year flood”, the huge kind of millennial flood never before seen in people’s lifetimes.  Suppose further that people believed him, and spent lots of money building huge levees to protect their homes and cities and jacking up their houses above predicted flood levels.

And finally, suppose the flood turned out to be the usual kind, the floods that we get every 20 years or so.

After that, do you think the flood guy should go around citing that prediction as evidence that his model can be trusted?

But heck, this is climate science …

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Joel Shore
December 30, 2010 8:50 pm

KD: I am not saying that climate change is not a monumental and in some ways unique challenge. However, there are potentially large costs either way. The most intelligent thing to do is not to wait until we know exactly what will happen for sure before doing anything but to hedge our bets so that we have maximum flexibility to either speed up or back off on the transformations of our use of energy (and implementation of sequestration). If you think making the transformation will be expensive if we do it gradually over the next several decades, imagine how much more expensive it will be if we continue on our orgy of burning fossil fuels at ever-increasing rates and then have to do a crash-diet once we find out that, yes, the problem is about as serious as most scientists have thought it to be.
Also, the prediction aspect is not as dire as you make it sound. It’s not like we need a weather forecast for a hundred years out. In that case, you would have errors that accumulate in time. Here, we just need (at least as a first understanding of the scope of the problem) to understand roughly how large a perturbation we would be making to the climate system. For that, all we need to understand is if the basic picture of radiative forcings governing things is correct and roughly how large the climate sensitivity is. And, the evidence from Mt. Pinatubo, along with evidence from the glacial – interglacial periods, and so forth tend to confirm this view and to point to at least a moderate climate sensitivity.

December 30, 2010 9:43 pm

Willis,
“Thanks, Mosh. If you take a look at Fig. 3 you’ll see that during the time in question, the control run varied little from zero. As a result, there is little difference between what I show, and the (projection minus control run) that you are talking about.”
I wasnt suggesting that here ( cause you dont have the control run) I’m suggesting that in general. Have a look at the video I linked to. Some interesting stuff in there
WRT this article. If Lacis offers this up as evidence that we should have trust in the models, I’d say its a fairly slim reed, but a reed nonetheless.

Matt G
December 31, 2010 6:53 am

Not notice if anyone did mention this, but SO2 emissions affect global temperatures only when in the high atmosphere. SO2 emissions in the troposphere has no noticable affect on temperature. It is quickly removed out of the air with precipitation and when in strong enough concentrations causes acid rain. Therefore how much a volcanoe affects global temperatures depends of how many tons reach the stratosphere. Human SO2 emissions never reach the stratosphere and therefore can’t affect global temperatures, but can affect the local environment.

Joel Shore
December 31, 2010 7:29 am

Matt G: Your statement is not quite right. You are right that for the SO2 from volcanoes, it is that which makes it into the stratosphere that has most of the effect because of the quick removal of that which stays in the troposphere. However, human SO2 (and other aerosol) emissions are emitted continuously and thus at any time there is some that is not yet washed out…and this concentration is enough to have an effect on global temperatures too. What is true is that SO2 concentrations in the troposphere are essentially proportional to current emissions, as opposed to CO2 concentrations that are essentially proportional to the cumulative amount of emissions (i.e., the integral of emissions with respect to time).
It is also worth noting that, while there is considerable uncertainty in regards to the radiative forcing due to aerosols in the troposphere, there is less uncertainty for the radiative forcing due to aerosols in the stratosphere. This is primarily because of the so-called “indirect effect” of aerosols in the troposphere due to their effect on the nucleation of liquid droplets and hence on clouds. I think another issue is that to the extent that aerosols absorb rather than reflect solar radiation, this doesn’t really produce a negative forcing when in the troposphere but do when they are in the stratosphere. (This is because the heat produced when the energy is absorbed in the troposphere can mix down to the surface.)

BlueIce2HotSea
December 31, 2010 9:53 am

Matt G says:
December 31, 2010 at 6:53 am
“Human SO2 emissions never reach the stratosphere and therefore can’t affect global temperatures…”

Are you sure about this?
According to the IPCC Third Assessment, the global mean radiative cooling due to anthropogenic sulphate emissions in 2000 relative to 1750 was 0.5 W/sq. m. By definition, this figure does not include volcanic emissions.

KD
December 31, 2010 11:44 am

Joel Shore says:
December 30, 2010 at 8:50 pm
KD: I am not saying that climate change is not a monumental and in some ways unique challenge. However, there are potentially large costs either way. The most intelligent thing to do is not to wait until we know exactly what will happen for sure before doing anything but to hedge our bets so that we have maximum flexibility to either speed up or back off on the transformations of our use of energy (and implementation of sequestration). If you think making the transformation will be expensive if we do it gradually over the next several decades, imagine how much more expensive it will be if we continue on our orgy of burning fossil fuels at ever-increasing rates and then have to do a crash-diet once we find out that, yes, the problem is about as serious as most scientists have thought it to be.
Also, the prediction aspect is not as dire as you make it sound. It’s not like we need a weather forecast for a hundred years out. In that case, you would have errors that accumulate in time. Here, we just need (at least as a first understanding of the scope of the problem) to understand roughly how large a perturbation we would be making to the climate system. For that, all we need to understand is if the basic picture of radiative forcings governing things is correct and roughly how large the climate sensitivity is. And, the evidence from Mt. Pinatubo, along with evidence from the glacial – interglacial periods, and so forth tend to confirm this view and to point to at least a moderate climate sensitivity.
——————
So no example the? Falling back on the precautionary principle? Assuming there is no consequence or opportunity cost to the path you propose?
Wish there was enough wealth in the world to throw $s after the POSSIBILITY that there may be a problem, but in the world I know there isn’t. Just a bit of a financial crisis these days.
Love your last paragraph. Don’t need to project out 100 years, just a few. But the model has shown us a 100% error in just a few years. So why should we believe it? Better still, why should we base policy decisions on it?
I find your arguments to be lacking of facts and circular in nature. Given that, I’ll keep my money and my carbon fuels for now, thank you.

Bill Illis
January 1, 2011 6:27 am

I still don’t see how this simulation is representative of the capability of climate model predictions.
The Pinatubo forcing change was a reduction in solar radiation of -4.1 watts/m2 (eventually OLR fell as well as we ended up with a net forcing change of -2.9 watts/m2).
Temperatures declined by 0.4C or 0.1C/W/m2 to 0.14C/W/m2
The climate models are saying +3.7 W/m2 in GHG forcings eventually results in +3.0C in temperature increases or 0.81C/W/m2.
How exactly does a short-term climate response of 0.1C/W/m2 confirm 0.81C/W/m2.
If anything, Hansen had 5 or 6 volcanoes from history which could be used to guess at a 0.4C or 0.6C decline. So, when the first GISS Model runs were done (in the 1980s) and came back with -2.0C for a Pinatubo-like valcano – they just adjusted the forcing by two-thirds to get them closer to the -0.5C (see GISS “efficacy of forcings” paper – they just changed it).
So, it does not validate the basis of the climate models. It invalidates them.

Joel Shore
January 1, 2011 10:04 am

Willis Eschenbach says:

Well, you know, speculation is fun, but I tend to look at the numbers. So I got the El Nino numbers from here, and I regressed the GISSTEMP temperature on them, and subtracted the regression from the GISSTEMP temperature. That left me the temperature without El Nino effects.
The surface air temperature (GISSTEMP) dropped from June of ’91 to September of ’92. Without considering the El Nino the drop was slightly more (by 0.04°C) than when the El Nino effect was removed. So the effect, rather than being “perhaps a significant underestimation”, is actually a slight overestimation.

But, September 1992 is a rather special point…It falls in the one short period of time between mid-1991 and mid-to late-1993 when the ENSO indices were close to neutral. In fact, only 6 months before that, they were STRONGLY positive and 6 months later, they were reasonably strongly positive again. The primary discrepancy between the temperature data and the prediction appears to be in both of these regions of time when the ENSO index was quite strongly positive.

The history of carbon in our fuels is one of constantly decreasing carbon ratio. We started with wood and coal, lots of carbon. We moved to diesel and gasoline, less carbon. Now the planet is moving to natural gas, less, carbon still.

…Which is good and suggests that it is not necessary to have high carbon ratio to have prosperous economies. However, there is also a lot of coal that will be used. The market system at present is blind to the fact that there are other significant potential costs associated with the use of carbon, and with such blindness comes a system in which such sources of energy remain artificially cheap. On the other hand, the costs associated with getting off fossil fuels are going to have to be borne eventually since they are finite resources. The only question is whether we get off fossil fuels before or after we have caused major changes to our environment. (If sequestration is cost-effective enough to become a significant component of the solution, we don’t even have to wean ourselves off fossil fuels as quickly but can go through a stage of using them but sequestering the CO2, giving us more time to develop the alternative energy sources. These, of course, are questions that a free market, given the proper signals to account for externalized costs, can decide.)

Here’s how I’d put the odds and the cost:
Odds of a 2°C temperature rise this century if CO2 is stabilized – one in ten
Odds of a 2°C temperature rise this century if CO2 is not stabilized – one in nine
Cost of a 2°C temperature rise this century – zero ± hundreds of trillions of dollars
Mathematical Expectation – zero ± tens of trillions of dollars
Now, we can argue about the numbers.

Yes, we can. Those numbers are nowhere close to where most of the scientists in the field would put those numbers. Do you really think that the world’s policymakers should base their decisions on Willis Eschenbach’s view? Now, you can try to argue your view in the scientific literature and try to get the scientific consensus to move in your direction, but that’s not where it is now (and I would say for good reason although I recognize that you will disagree).

I advise, as always, the “No Regrets” path. All of the foreordained horrors of the climate Thermageddon are with us now. We have storms and droughts and floods and cyclones wreaking untold human misery today.

This is only a “no regrets” path if one believes that the only thing we would ever want to do is adapt to climate change rather than make any attempts to mitigate it.

As for carbon reduction, the EPA regs are about to kick in. They will cost untold billions of dollars. The EPA itself says that by 2030 the regs will make the world cooler by three hundredths of a degree …

That is because they are…
(1) not aimed at making a significant difference to the temperature in 2030 but rather in getting us on a path that will (in concert with the actions of other countries) help make a significant difference in the latter part of the century. We are pretty much stuck with what warming we are going to get over the next 20 years or so.
(2) not aimed at solving the problem without participation from the rest of the world too. It is a global problem. It is like voting…Why should I ever vote in elections when my one vote makes such an infinitesimal difference to the outcome that it almost never matters. Even in Florida in 2000, it did not come down to one single vote.
Happy New Year’s, Willis!

Dave F
January 1, 2011 11:06 pm

I had a random thought for your thunderstorm hypothesis Willis. Have you considered that changing radiation may change the residence time of water vapor in the atmosphere?
Hotter water vapor will rise faster, release its energy to space, and fall. This would mean that warming can actually shrink the amount of time that water vapor resides in the atmosphere.
Likewise, colder water vapor will rise slower, releasing less of its energy to space, and precipitate less.
Observations bear this idea out, but the idea of changing the residence time of water vapor hasn’t been factored into any discussion I have been a part of. Stephen Wilde’s assertions about speeding up the hydrological cycle seem to be a grasp at this concept, and are part of what made me think of this. I’d like to see what you make of this, given that you have the time/patience I lack to tinker with the models. What happens when you assign a variable to, what I assume to be constant in models, the constant of residence time for H2O that increases the residence time when colder, and decreases the residence time when warmer? This would be a great mechanism for maintaining energy in=energy out. And a new wrinkle for the man behind the curtain.

Matt G
January 2, 2011 12:38 pm

The claim that little continuous human SO2 reaches the stratosphere is based on aerosol data that in low levels has not been distinguished between different types until the 21st century.
While there has been a large reduction in SO2 human production from the 1970’s until 2000’s. In USA, Europe and other cities around the world with a significant reduction in fuel and industrial based sources. Depsite this there has been very little change in stratopshere levels so far and it is not having any noticable affect on the stable tiny rise. Just a few links below showing examples.
http://www.ace.mmu.ac.uk/Resources/Fact_Sheets/Key_Stage_4/Air_Pollution/pdf/Air_Pollution.pdf
http://www.mfe.govt.nz/publications/ser/enz07-dec07/chapter-7.pdf
http://enhealth.nphp.gov.au/council/pubs/pdf/suldiox.pdf
http://www.cleanair.hamilton.ca/default.asp?id=22#Sulphur
Over recent years developing countries have increased SO2 production, but still some cities there have reduced SO2 levels. There are exceptions with especially China having had significant rises in SO2 levels.
http://ww2.unhabitat.org/istanbul+5/68.pdf
http://www.ess.co.at/GAIA/CASES/IND/CAL/CALpollution.html
“According to the IPCC Third Assessment, the global mean radiative cooling due to anthropogenic sulphate emissions in 2000 relative to 1750 was 0.5 W/sq. m. By definition, this figure does not include volcanic emissions.”
Satellites have only being detecting aerosols in the stratosphere since the late 1970’s/early 1980’s and up to 2004 were not able to distinguish low amounts of SO2 compared with ozone.
http://denali.gsfc.nasa.gov/research/so2/article.html
That IPCC claim was based on SO2 levels detected near the surface and all aerosol data in the stratosphere over recent decades. (with low levels of SO2 not distinguishable from ozone) Hence, it was a guess with little scientific evidence.
This changed in 2004 with the launch of a new satellite.
http://www.nasa.gov/vision/earth/lookingatearth/aura_update.html
Overall the rise and fall of human SO2 production is not detected in the stratopshere aerosol levels.

Matt G
January 2, 2011 12:41 pm

Just testing, can’t get my post to work?

Matt G
January 2, 2011 3:02 pm

“According to the IPCC Third Assessment, the global mean radiative cooling due to anthropogenic sulphate emissions in 2000 relative to 1750 was 0.5 W/sq. m. By definition, this figure does not include volcanic emissions.”
Satellites have only being detecting aerosols in the stratosphere since the late 1970’s/early 1980’s and up to 2004 were not able to distinguish low amounts of SO2 compared with ozone.
http://denali.gsfc.nasa.gov/research/so2/article.html
That IPCC claim was based on SO2 levels detected near the surface and all aerosol data in the stratosphere over recent decades. (with low levels of SO2 not distinguishable from ozone) Hence, it was a guess with little scientific evidence.
This changed in 2004 with the launch of a new satellite.
http://www.nasa.gov/vision/earth/lookingatearth/aura_update.html
Overall the rise and fall of human SO2 production is not detected in the stratopshere aerosol levels.

Matt G
January 2, 2011 3:30 pm

The claim that little continuous human SO2 reaches the stratosphere is based on aerosol data that in low levels has not been distinguished between different types until the 21st century.
While there has been a large reduction in SO2 human production from the 1970’s until 2000’s. In USA, Europe and other cities around the world with a significant reduction in fuel and industrial based sources. Depsite this there has been very little change in stratopshere levels so far and it is not having any noticable affect on the stable tiny rise. Just a few links below showing examples.
http://www.ace.mmu.ac.uk/Resources/Fact_Sheets/Key_Stage_4/Air_Pollution/pdf/Air_Pollution.pdf
http://www.mfe.govt.nz/publications/ser/enz07-dec07/chapter-7.pdf
http://enhealth.nphp.gov.au/council/pubs/pdf/suldiox.pdf
http://www.cleanair.hamilton.ca/default.asp?id=22#Sulphur
Over recent years developing countries have increased SO2 production, but still some cities there have reduced SO2 levels. There are exceptions with especially China having had significant rises in SO2 levels.
http://ww2.unhabitat.org/istanbul+5/68.pdf
http://www.ess.co.at/GAIA/CASES/IND/CAL/CALpollution.html

maksimovich
January 2, 2011 10:12 pm

One of the unintended consequences of not understanding assumptions raised in probalistic forecasts is that they can get very wrong,very fast,at great cost to both business and consumers.
The information is often considered to have predictive qualities,when in reality it is a odds based wager.
As we see here by Niwa
December 17, 2010
La Niña conditions are likely to continue through to autumn of 2011 and then to ease. Such La Niña conditions have been indicated by NIWA since mid-2010.
La Niña conditions tend to be associated with below-normal inflows into the main hydro-electricity generating lakes. The graphic below shows the range of total summer inflows (in terms of generation capacity in MW) for non-La Niña and La Niña years. In the summer of 2007/08, La Niña conditions prevailed, much as they do now, and the total inflow was almost exactly the median value indicated for La Niña years in Figure 1.
As outlined in the NIWA seasonal climate outlook, there is a significant risk of below-normal inflows over the summer, especially for the South Island alpine region. The outlook states: seasonal rainfall is likely to be below normal in the western South Island [including the Southern Alps and the headwaters of the main South Island rivers]. River flows and soil moisture levels are very likely to be below normal in the west and south of the South Island.
http://www.niwa.co.nz/news-and-publications/news/all/la-niAa-and-hydro-electricity-supply,-summer-20102011
The consequences were the electricity market (who had both forecast prior to public release) reacted by pricing spikes in December seen here.
http://www.electricityinfo.co.nz/media_releases/261210.pdf
Around the same time 19th heavy rain started falling in the hydro catchments in inflows reached record levels by the end of the month.
http://www.electricityinfo.co.nz/comitFta/ftaPage.hydrology
And as we see pricing fell again to record lows.

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