Steve,
Gradient multiplication by maps, being a multiplicative
random process, inherently introduces important aspects of intermittency,
as shown in LEM Part 6. ODT eddy correlations are another intermittency
mechanism, but it's not yet determined whether this makes ODT more accurate
overall than LEM with regard to intermittency (a good fundamental question for
someone to study). Triplet maps with unequal sizes of the three map images
would be inherently more intermittent (consider the limit in which one or two of
the images is/are very small, corresponding to a very high gradient
amplification factor) so this provides the freedom to tune LEM (or ODT)
intermittency. This would be another worthwhile study, recently
rendered feasible by the adaptive mesh implementation.
These
points could be of general interest, so I'm cc'ing the google
group.
Alan
From: Steve Krueger
[mailto:arcus...@earthlink.net]
Sent: Thursday, February 12, 2009
10:06 AM
To: Kerstein, Alan
Subject: Re: ODT Discussion -
dates
I suggested that John could contribute to implementing better
treatments of these, especially (1), and perhaps (2). It is less obvius to me
how to implement (2) in LEM. It would seem to require correlated intermittency
in space and time, which ODT does nicely, but LEM can't do without some type of
memory.
On Feb 10, 2009, at 9:13 AM, Kerstein, Alan wrote:
Did your discussion with Patrick resolve his
concerns?
that sounds good. I'd rather get you when you're FOA. (like
FOB...).
I had a nice chat with Patrick Chuang after the POST workshop about LEM,
EMPM, cluscoll.
He had some good questions, including:
1. Should we sample from a pdf of entrained blob sizes in EMPM?
2. How could we represent intermittency in the EMPM, etc?
Steve