Javascript must be enabled to continue!
A dichotomy theorem for turbulence
View through CrossRef
In this note we show:Theorem 1.1. Let G be a Polish group and X a Polish G-space with the induced orbit equivalence relation EG Borel as a subset of X × X. Then exactly one of the following:(I) There is a countable languageℒand a Borel functionsuch that for all x1, x2 ∈ Xor(II) there is a turbulent Polish G-space Y and a continuous G-embeddingThere are various bows and ribbons which can be woven into these statements. We can strengthen (I) by asking that θ also admit a Borel orbit inverse, that is to say some Borel functionfor some Borel set B ⊂ Mod(ℒ), such that for all x ∈ Xand then after having passed to this strengthened version of (I) we still obtain the exact same dichotomy theorem, and hence the conclusion that the two competing versions of (I) are equivalent. Similarly (II) can be relaxed to just asking that τ be a Borel G-embedding, or even simply a Borel reduction of the relevant orbit equivalence relations. It is in fact a consequence of 1.1 that all the plausible weakenings and strengthenings of (I) and (II) are respectively equivalent to one another.I will not closely examine these possible variations here. The equivalences alluded to above follow from our main theorem and the results of [3]. That monograph had previously shown that (I) and (II) are incompatible, and proved a barbaric forerunner of 1.1, and gone on to conjecture the dichotomy result above.
Title: A dichotomy theorem for turbulence
Description:
In this note we show:Theorem 1.
1.
Let G be a Polish group and X a Polish G-space with the induced orbit equivalence relation EG Borel as a subset of X × X.
Then exactly one of the following:(I) There is a countable languageℒand a Borel functionsuch that for all x1, x2 ∈ Xor(II) there is a turbulent Polish G-space Y and a continuous G-embeddingThere are various bows and ribbons which can be woven into these statements.
We can strengthen (I) by asking that θ also admit a Borel orbit inverse, that is to say some Borel functionfor some Borel set B ⊂ Mod(ℒ), such that for all x ∈ Xand then after having passed to this strengthened version of (I) we still obtain the exact same dichotomy theorem, and hence the conclusion that the two competing versions of (I) are equivalent.
Similarly (II) can be relaxed to just asking that τ be a Borel G-embedding, or even simply a Borel reduction of the relevant orbit equivalence relations.
It is in fact a consequence of 1.
1 that all the plausible weakenings and strengthenings of (I) and (II) are respectively equivalent to one another.
I will not closely examine these possible variations here.
The equivalences alluded to above follow from our main theorem and the results of [3].
That monograph had previously shown that (I) and (II) are incompatible, and proved a barbaric forerunner of 1.
1, and gone on to conjecture the dichotomy result above.
Related Results
Quantum turbulence
Quantum turbulence
Abstract
Chapter 5 delves into quantum turbulence in superfluid helium and atomic Bose-Einstein condensates (BECs). The foundation of quantum turbulence research ...
Impact of magneto-rotational instability on grain growth in protoplanetary disks
Impact of magneto-rotational instability on grain growth in protoplanetary disks
Grain growth in protoplanetary disks is the first step towards planet formation. One of the most important pieces in the grain growth model is calculating the collisional velocity ...
Characteristic parameters of adaptive optical imaging system in oceanic turbulence
Characteristic parameters of adaptive optical imaging system in oceanic turbulence
Since recently one is interested in underwater communications, imaging, sensing and lidar appeared, it is important to study characteristic parameters of the adaptive optical imagi...
Unraveling the lidar-turbulence paradox
Unraveling the lidar-turbulence paradox
The meteorological community, and in particular the wind energy community, have been trying to establish a methodology to correct/convert turbulence measures derived from measureme...
Stagnation Region Heat Transfer Augmentation at Very High Turbulence Levels
Stagnation Region Heat Transfer Augmentation at Very High Turbulence Levels
A database for stagnation region heat transfer has been extended to include heat transfer measurements acquired downstream from a new high intensity turbulence generator. This work...
Estimating en-route turbulence using ADS-B aircraft data
Estimating en-route turbulence using ADS-B aircraft data
Aviation turbulence is a hazardous weather phenomenon that affects aviation safety and operations. It can be in the form of convective induced turbulence (CIT), clear air turbulenc...
Characterization of low levels of turbulence generated by grids in the settling chamber of a laminar wind tunnel
Characterization of low levels of turbulence generated by grids in the settling chamber of a laminar wind tunnel
AbstractWind tunnel investigations of how Natural Laminar Flow (NLF) airfoils respond to atmospheric turbulence require the generation of turbulence, whose relevant characteristics...
Turbulence near a sandbar island in the lower Missouri River
Turbulence near a sandbar island in the lower Missouri River
AbstractRiver turbulence is spatially variable due to interactions between morphology of rivers and physical mechanics of flowing water. Understanding the variation of turbulence i...

