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Potholer54 has already exposed the guy for the armchair amateur that he is. But you choose to ignore it. Ah well.
Yeah, ok.
http://di2.nu/foia/1254108338.txt
From: Tom Wigley <wigley@ucar.edu>
To: Phil Jones <p.jones@uea.ac.uk>
Subject: 1940s
Date: Sun, 27 Sep 2009 23:25:38 -0600
Cc: Ben Santer <santer1@llnl.gov>
<x-flowed>
Phil,
Here are some speculations on correcting SSTs to partly
explain the 1940s warming blip.
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.
http://di2.nu/foia/1254108338.txt
From: Tom Wigley <wigley@ucar.edu>
To: Phil Jones <p.jones@uea.ac.uk>
Subject: 1940s
Date: Sun, 27 Sep 2009 23:25:38 -0600
Cc: Ben Santer <santer1@llnl.gov>
<x-flowed>
Phil,
Here are some speculations on correcting SSTs to partly
explain the 1940s warming blip.
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.
OK, here are the results of a quick search. I doubt you'll read any of them, you're probably gonna say 'well these are all conservatives accusing poor old Snopes of being liberal'......if you want to check the other fake 'fact' sites do it yourself, it ain't that hard. Or you can stay uninformed......
That is documented government information, much like the speech shredded by your Queen Pelosi.
Anyway, it seems you're off on your English syntax, so feel better!
It is government data. But it is not necessarily comparable to other government data taken at a different time. You need to very carefully determine how each data set was obtained. And sometimes they are simply not comparable. It is for instance very unlikely that you can compare ice coverage for the modern satellite era to before satellites or even to early satellites.
Any comparison of long term data should have a foot note leading to how the data was normalized. Otherwise total skepticism is required.
One thing that could help would be to use both the old method and the new for say a decade. Then maybe you could figure out how to correlate the new and the old.
No doubt you didn't read the long Snopes article. Right?
Good point StillwaterTownie!
An article in Snoops does indeed change the fact that there is no real global temperature record predating the satellite era.
So, with that out of the way, what was the average surface temperature of the planet on June 26th, 1922?
How does that measurement compare with the average surface temperature on June 26th, 1943?
Is a warming or cooling trend taking place during the period between the two dates, and how can we be sure the data is accurate?
What scientific organization was tasked with insuring the weather data collected was accurate?
What uniform methods were employed by those collecting the data?
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