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Re: The Western Interior Seaway (and computers)
Good point. There is not much physical evidence (none?) for a Mesozoic
arctic sea ice sheet, so if there was a WIS dynamo it may have been a
very weak one. A sea ice sheet might be a feature that a computer model
could predict (or eliminate as a possibility). If it existed, perhaps
the sea ice
was only a seasonal feature.
Our current Arctic Ocean sea ice sheet is eroding at an alarmingly rapid
rate. How small can it get before the dynamo shuts down?
<pb>
--
On Wed, 29 Jun 2005 05:45:11 +0100 Aidan Karley
<aidan_karley@yahoo.co.uk> writes:
> In article <20050628.130115.-985265.4.bigelowp@juno.com>, Phil
> Bigelow
> wrote:
> > I was thinking way back to my Geo. 101 lab days. Cold water at
> the poles
> > sinks, drawing the warm water from the equator northward to take
> its
> > place. The cold water then upwells near the tropics to begin the
> process
> > over.
> >
> AIUI, the driver process is the change in sea-water density
> caused
> by cooling and by the removal of significant fresh water to form
> pack ice.
> There's also a simple thermal contribution too, but it's less
> important as
> indicated by the Heinrich events (Laurentide/ Greenland deglaciation
> yields
> lots of fresh-water runoff to the North Atlantic, which inhibits the
>
> sinking of water in the NE Atlantic and shuts down the system.
> Seabed
> sediment data indicates this happens on the timescale of years not
> decades,
> providing some justification for the (allegedly) atrocious
> climate-foul-up
> film of last year. [sorry, brain has drawn a blank on it's name.
> It's late
> here. Whatever.])
>
> > Did hydraulic
> > shear occur at mid-depth between the northward-flowing warm water
> and the
> > southward flowing colder water?
> >
> Well it happens these days, so presumably it could have
> happened in
> the past.
>
> --
> Aidan Karley,
> Aberdeen, Scotland,
> Location: 57°10' N, 02°09' W (sub-tropical Aberdeen), 0.021233
> Written at Wed, 29 Jun 2005 04:07 +0100
>
>
>
>
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