Latest facts
Latest...
Login
Kevin Trenberth to Michael Mann, Oct 12, 2009:
The fact is that we can’t account for the lack of warming at the moment and it is a travesty that we can’t. The CERES data published in the August BAMS 09 supplement on 2008 shows there should be even more warming: but the data are surely wrong. Our observing system is inadequate.
Kevin Trenberth to Tom Wigley, Oct 14, 2009
Hi Tom
How come you do not agree with a statement that says we are no where close to knowing where
energy is going or whether clouds are changing to make the planet brighter. We are not
close to balancing the energy budget. The fact that we can not account for what is
happening in the climate system makes any consideration of geoengineering quite hopeless as
we will never be able to tell if it is successful or not! It is a travesty!
Kevin
Leo Tolstoy
“I know that most men, including those at ease with problems of the greatest complexity, can seldom accept even the simplest and most obvious truth if it be such as would oblige them to admit the falsity of conclusions which they have delighted in explaining to colleagues, which they have proudly taught to others, and which they have woven, thread by thread, into the fabric of their lives.”
Phil Jones
“We have 25 or so years invested in the work. Why should I make the data available to you, when your aim is to try and find something wrong with it.” -
Phil Jones to Michael Mann Feb 21, 2005:
The IPCC comes in for a lot of stick.
Leave it to you to delete as appropriate !
Cheers
Phil
PS I'm getting hassled by a couple of people to release the CRU station temperature data.
Don't any of you three tell anybody that the UK has a Freedom of Information Act !
Tom Wigley to Phil Jones Sep 27, 2009:
If you look at the attached plot you will see that the
land also shows the 1940s blip (as I'm sure you know).
So, if we could reduce the ocean blip by, say, 0.15 degC,
then this would be significant for the global mean — but
we'd still have to explain the land blip.
I've chosen 0.15 here deliberately. This still leaves an
ocean blip, and i think one needs to have some form of
ocean blip to explain the land blip (via either some common
forcing, or ocean forcing land, or vice versa, or all of
these). When you look at other blips, the land blips are
1.5 to 2 times (roughly) the ocean blips — higher sensitivity
plus thermal inertia effects. My 0.15 adjustment leaves things
consistent with this, so you can see where I am coming from.
Removing ENSO does not affect this.
It would be good to remove at least part of the 1940s blip,
but we are still left with "why the blip".
Let me go further. If you look at NH vs SH and the aerosol
effect (qualitatively or with MAGICC) then with a reduced
ocean blip we get continuous warming in the SH, and a cooling
in the NH — just as one would expect with mainly NH aerosols.
The other interesting thing is (as Foukal et al. note — from
MAGICC) that the 1910-40 warming cannot be solar. The Sun can
get at most 10% of this with Wang et al solar, less with Foukal
solar. So this may well be NADW, as Sarah and I noted in 1987
(and also Schlesinger later). A reduced SST blip in the 1940s
makes the 1910-40 warming larger than the SH (which it
currently is not) — but not really enough.
So ... why was the SH so cold around 1910? Another SST problem?
(SH/NH data also attached.)
This stuff is in a report I am writing for EPRI, so I'd
appreciate any comments you (and Ben) might have.
Tom.
Tim Osborn to Michael Mann and Ian Macadam , Oct 5, 1999:
Dear Mike and Ian
Keith has asked me to send you a timeseries for the IPCC multi-proxy
reconstruction figure, to replace the one you currently have. The data are
attached to this e-mail. They go from 1402 to 1995, although we usually
stop the series in 1960 because of the recent non-temperature signal that
is superimposed on the tree-ring data that we use. I haven't put a 40-yr
smoothing through them - I thought it best if you were to do this to ensure
the same filter was used for all curves.
Keith Briffa:
Briffa:
For the record, I do believe that the proxy data do show unusually
>warm conditions in recent decades. I am not sure that this unusual warming
>is so clear in the summer responsive data. I believe that the recent warmth
>was probably matched about 1000 years ago. I do not believe that global
>mean annual temperatures have simply cooled progressively over thousands of
>years as Mike appears to and I contend that that there is strong evidence
>for major changes in climate over the Holocene (not Milankovich) that
>require explanation and that could represent part of the current or future
>background variability of our climate. I think the Venice meeting will be
>a good place to air these isssues.
South America
RUTI South America
Fig1 South America was divided into the above areas. As generally in the RUTI project, I divide into areas of most possible homogenous temperature trends. This is to achieve the most correct results: If you average temperature trends from areas of significantly different trends, and the years represented by temperature records are very different, then averaging will induce significant errors. Averaging errors are most significant when data series are available for different years, which is a normal situation for publicly available Unadjusted GHCN data.
Fig 2 NW South America I started examining this area using a smaller area “The Panama area” north of the dotted line.
Fig3, “The Panama area” Just a few stations are publicly available before 1950, and thus it is not easy to evaluate differences coastal vs. non-coastal.
Further south, coastal stations seems to confirm the above Panama area trends (strong decline in temperature after 1940) and the full NW South America areas thus becomes:
Fig4. NW South America trends. Although the years 1920-45 are not available for most non-urban sites, still a handful of stations around the area combined makes the NW South America strong temperature decline after 1940 appear solid and useful.
Fig 5. North SA area.
Fig6, North SA, non-coastal temperature trends. For this area, close to the Panama area etc, temperature data from non-urban non-coastal stations are not public available before 1950.
Fig7. SA North, coastal: More temperature data available than for non-coastal, and a warm trend can be spotted al the way from year 1900.
Fig8. NE and SE Brazil areas.
Fig9 NE Brazil, non-coastal temperature trends.
Fig10. NE Brazil coastal temperature trends.
Fig11 NE Brazil coastal vs. non-coastal.
FIG12, SE Brazil, non-coastal.
Fig13, SE Brazil, coast
Fig14, SE Brazil, coastal vs. non-coastal.
Fig15. Chile area, Argentina area and North Argentina area.
Fig16. The Northern Argentina area has rather different temperature trends compared to near by larger areas. For the North Argentina area, even the non-coastal temperature series has heat trend.
A difference costal vs. non-coastal is hard to see, but we should be aware, that only one costal temperature station (not too urban) was available (!)
Fig17. Argentina area, Non-coastal temperature trends
Fig18, Argentina area, Coastal trends.
Fig19. Argentina area, Coastal vs. non-coastal trends.
Fig20. For the Chile area, the land area is rather narrow, and thus I have to zoom in to show which stations are more coastal than others. On fig6 we see the coastal station, very well representing Marine air.
Fig21. Chile area, Non-coastal stations.
Fig22. Trend differences coastal vs. non-coastal for the Chile area: The Classic pattern of warmer non-coastal stations before around 1950 is strongly visible in data even though all non-coastal station here has been cut of before 1940.
Fig23. However, much further south we actualy have one non-coastal stations that is public available for many more years, Punto Arenas.
Fig24. The non-coastal Punto Arena compared with the more coastal Ushuaia A. Also at the southern tip of South America we have the classic pattern of more heat trend in coastal stations.
Fig25. All stations on the Antarctic Peninsula are more less coastal. However, most data from this region are available only after 1950, and thus the cosatl effect may not be that important here.
Fig26 “SA West” and “Amazonas” areas.
Fig27. SA West, Non-coastal trends…
Fig28. SA West, Coastal trends
Fig29. SA West non-coastal vs. Coastal temperature trends. We see the classical differences before, although perhaps not quite as significant differences as seen in other areas of the Earth. If we go further North, NW South America, then I did not find differences at all – although data was scarce in that area.
At the Western SA Coast, we have significant influence by ENSO (La-Nina/El-Nino) related ocean temperatures. These vary much faster than ocean temperatures in general, so perhaps its not surpricing that this area seems to behave slightly different than most other areas on Earth.
Fig 30. Temperature trends for the “Amazonas” area.
In this area we have a significant temperature rise all the way back from 1920.
Kevin Trenberth to Michael Mann, Oct 12, 2009:
The fact is that we can’t account for the lack of warming at the moment and it is a travesty that we can’t. The CERES data published in the August BAMS 09 supplement on 2008 shows there should be even more warming: but the data are surely wrong. Our observing system is inadequate.
Kevin Trenberth to Tom Wigley, Oct 14, 2009
Hi Tom
How come you do not agree with a statement that says we are no where close to knowing where
energy is going or whether clouds are changing to make the planet brighter. We are not
close to balancing the energy budget. The fact that we can not account for what is
happening in the climate system makes any consideration of geoengineering quite hopeless as
we will never be able to tell if it is successful or not! It is a travesty!
Kevin
Leo Tolstoy
“I know that most men, including those at ease with problems of the greatest complexity, can seldom accept even the simplest and most obvious truth if it be such as would oblige them to admit the falsity of conclusions which they have delighted in explaining to colleagues, which they have proudly taught to others, and which they have woven, thread by thread, into the fabric of their lives.”
Phil Jones
“We have 25 or so years invested in the work. Why should I make the data available to you, when your aim is to try and find something wrong with it.” -
Phil Jones to Michael Mann Feb 21, 2005:
The IPCC comes in for a lot of stick.
Leave it to you to delete as appropriate !
Cheers
Phil
PS I'm getting hassled by a couple of people to release the CRU station temperature data.
Don't any of you three tell anybody that the UK has a Freedom of Information Act !
Tom Wigley to Phil Jones Sep 27, 2009:
If you look at the attached plot you will see that the
land also shows the 1940s blip (as I'm sure you know).
So, if we could reduce the ocean blip by, say, 0.15 degC,
then this would be significant for the global mean — but
we'd still have to explain the land blip.
I've chosen 0.15 here deliberately. This still leaves an
ocean blip, and i think one needs to have some form of
ocean blip to explain the land blip (via either some common
forcing, or ocean forcing land, or vice versa, or all of
these). When you look at other blips, the land blips are
1.5 to 2 times (roughly) the ocean blips — higher sensitivity
plus thermal inertia effects. My 0.15 adjustment leaves things
consistent with this, so you can see where I am coming from.
Removing ENSO does not affect this.
It would be good to remove at least part of the 1940s blip,
but we are still left with "why the blip".
Let me go further. If you look at NH vs SH and the aerosol
effect (qualitatively or with MAGICC) then with a reduced
ocean blip we get continuous warming in the SH, and a cooling
in the NH — just as one would expect with mainly NH aerosols.
The other interesting thing is (as Foukal et al. note — from
MAGICC) that the 1910-40 warming cannot be solar. The Sun can
get at most 10% of this with Wang et al solar, less with Foukal
solar. So this may well be NADW, as Sarah and I noted in 1987
(and also Schlesinger later). A reduced SST blip in the 1940s
makes the 1910-40 warming larger than the SH (which it
currently is not) — but not really enough.
So ... why was the SH so cold around 1910? Another SST problem?
(SH/NH data also attached.)
This stuff is in a report I am writing for EPRI, so I'd
appreciate any comments you (and Ben) might have.
Tom.
Tim Osborn to Michael Mann and Ian Macadam , Oct 5, 1999:
Dear Mike and Ian
Keith has asked me to send you a timeseries for the IPCC multi-proxy
reconstruction figure, to replace the one you currently have. The data are
attached to this e-mail. They go from 1402 to 1995, although we usually
stop the series in 1960 because of the recent non-temperature signal that
is superimposed on the tree-ring data that we use. I haven't put a 40-yr
smoothing through them - I thought it best if you were to do this to ensure
the same filter was used for all curves.
Keith Briffa:
Briffa:
> For the record, I do believe that the proxy data do show unusually
>warm conditions in recent decades. I am not sure that this unusual warming
>is so clear in the summer responsive data. I believe that the recent warmth
>was probably matched about 1000 years ago. I do not believe that global
>mean annual temperatures have simply cooled progressively over thousands of
>years as Mike appears to and I contend that that there is strong evidence
>for major changes in climate over the Holocene (not Milankovich) that
>require explanation and that could represent part of the current or future
>background variability of our climate. I think the Venice meeting will be
>a good place to air these isssues.
