From: bill.sloman on
On 27 nov, 00:51, Eeyore <rabbitsfriendsandrelati...(a)hotmail.com>
wrote:
> bill.slo...(a)ieee.org wrote:
> > Eeyore <rabbitsfriendsandrelati...(a)hotmail.com> wrote:
>
> > > as we look headed for the coldest winter in decades here in the UK.
>
> > That's something of a stretch. You are claiming that a little short
> > term random noise on the long-term global warming trend invalidates
> > classical thermodynamics.
>
> Oh but the AGWists use noise to support their hypothesis when it suits them.

So you claim. You won't be able produce an example of an AGWist
actually doing this - you never can - and your own claim is simply
silly.

--
Bill Sloman, Nijmegen

From: bill.sloman on
On 26 nov, 19:42, James Arthur <bogusabd...(a)verizon.net> wrote:
> Al Bedo wrote:
> > bill.slo...(a)ieee.org wrote:
> > [regarding orbital variation with feedback]
>
> >> The point is that we need a healthy dose of positive feedback to make
> >> the explanation work and similar positive feedback mechanisms could
> >> turn today's barely significant global warming into an end-Permian
> >> style global extinction. It isn't a high probability scenario, but we
> >> are taling about the only planet we've got.
>
> > So what feedback are you suggesting?
>
> > Not ice/albedo feedback of the glacials since that ice
> > extended to mid-latitudes where there was enough insolation
> > to matter.
>
> > Not water vapor feedback because that doesn't seem to be occurring.
>
> > What then?
>
> He means methane hydrates, stores of methane frozen underseas
> (that might be freed if temperatures rise enough).
>
> Note that by saying "It isn't a high probability scenario", he's
> saying it's something but might happen, but isn't certain.
>
> IOW, "We don't understand, and we don't know.  We're guessing."

We understand quite bit and know quite a bit. We don't know enough to
put particulalry tight numerical constraints on what might happen and
when it might happen.

The negative carbon isotope ratio spikes around the end-Permian mass
extinction do suggest that methane clathrates have let go in the
remote past, and contributed to a fairly spectacular mass extinction.

--
Bill Sloman, Nijmegen
From: bill.sloman on
On 26 nov, 19:52, Al Bedo <c...(a)dark.side.of.the.moon> wrote:
> James Arthur wrote:
>
> [Regarding feedbacks]
>
> > He means methane hydrates, stores of methane frozen underseas
> > (that might be freed if temperatures rise enough).
>
> Since orbitals are similar to the last glaciation,
> one could argue that glaciation is a more likely risk.
>
> So we should be trying to prevent glaciation
> rather than warming.

According to William Ruddiman, the next glaciation should be well
underway already, but we stopped the glaciers in their tracks when we
took up agriculture

http://en.wikipedia.org/wiki/William_Ruddiman

We've now injected more than enough fossil carbon dioxide into the
atmosphere to make sure that glaciation isn't going to be a problem
for the next thousand years or so.

--
Bill Sloman, Nijmegen
From: JosephKK on
On Wed, 26 Nov 2008 14:04:38 +0000, Eeyore
<rabbitsfriendsandrelations(a)hotmail.com> wrote:

>
>
>bill.sloman(a)ieee.org wrote:
>
>> On 26 nov, 06:22, Eeyore <rabbitsfriendsandrelati...(a)hotmail.com>
>> wrote:
>> > bill.slo...(a)ieee.org wrote:
>> > > I certainly don't command the computing capacity required to run that
>> > > kind of model
>> >
>> > Wouldn't matter if you did. The models are FUCKED !
>>
>> You may think so, but - as you demonstrate below - you don't know
>> anything about mathematical modelling either.
>
>I was using mathematical modelling software 20 years ago. MathCad for DOS !
>
>Graham

Compared to decent thermal modeling for houses mathcad is an
incomplete and flimsy tool. I have and use it, it is nice within its
area of capability. It is a non-starter for anything like weather or
climate models.

From: JosephKK on
On Wed, 26 Nov 2008 14:11:15 +0000, Eeyore
<rabbitsfriendsandrelations(a)hotmail.com> wrote:

>
>
>bill.sloman(a)ieee.org wrote:
>
>> It's successors might be more interesting - the computers available in
>> 1960 weren't all that impressive. I wrote my first program in 1965 for
>> Melbourne University's IBM 7040/44 which had 32k of 36bit words of
>> core memory, and relied on magnetic tape for mass storage, and cost
>> the university a million dollars.
>
>And you're clearly stuck in some surreal time warp.
>
>Hey, I programmed on an Elliot Automation 803. And an IBM 360. Then an Epson HX-20
>followed by a BBC- Model B with 128kB of memory (bank switched) and then the
>ubiquitous 8051 family. And don't forget the Z80 !
>
>
>Graham

Wuss, i was programming 18 bit and 30 bit computers in the very early
1970s and switched to a 32 bit computer in 1973. I wouldn't buy a PC
until the 80386 hit, though i would have considered a 68000 or an NS
16000/32000. I even thought about using an AMD 29000. I would have
loved to got my hands on a DG micronova, did get to use a microVAX.
And de regur i have used 6502, 6802, 1802, 8051 and others along the
way.