2,924 research outputs found

    A summary of research on the NASA-Global Atmospheric Sampling Program performed by the Atmospheric Sciences Research Center

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    The annual variations of ozone near the tropopause are derived from aircraft exhibit year-to-year differences which are not explicitly accounted for by the simple, classical ozone transport theory. Phenomena such as tropopause lifting, interannual variations in the rates of stratospheric-tropospheric exchange and meridional mixing, contribute differently to the distribution of ozone in this altitude region. Ozone encounter climatologies have been represented by global maps which show the probabilities of exceeding ambient ozone levels of 200, 300, and 400 ppbV along flight routes during the year. Continuous ozone records obtained from the GASP system revealed the presence of gravity waves whose wavelength is of the order 20 km. The GASP data cannot, however, be utilized for the evaluation of horizontal fluxes of such quantities as ozone, sensible heat, and zonal momentum; the data are too sparsely and irregularly distributed for the computation of stable correlations. Multiple species data from the unique circumglobal flight of a Pan American airliner on 28-30 October 1977 are discussed with particular regard to the apparent interhemispheric differences in tropospheric species concentrations, variation between the Arctic and Antarctic stratospheres, to possible covariations between species, and to potential source regions for various constituents

    Atmospheric ozone measurements made from B-747 AIRLINERS: Spring 1975

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    Atmospheric ozone in the upper troposphere and lower stratosphere north of the equator has been registered aboard two commercial B-747 airliners. The composite ozone, flight and meteorological data are reported. Attention is drawn particularly to the vertical profiles of atmospheric ozone mixing ratio as a function of both distance from the tropopause and curvature of the streamlines. The GASP observations suggest that ozone levels typical of the lower stratosphere are often embedded in the upper troposphere, principally during occassions when cyclonic wind curvature was noted

    An analysis of the first two years of GASP data

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    Distributions of mean ozone levels from the first two years of data from the NASA Global Atmospheric Sampling Program (GASP) show spatial and temporal variations in agreement with previous measurements. The standard deviations of these distributions reflect the large natural variability of ozone levels in the altitude range of the GASP measurements. Monthly mean levels of ozone below the tropopause show an annual cycle with a spring maximum which is believed to result from transport from the stratosphere. Correlations of ozone with independent meteorological parameters, and meteorological parameters obtained by the GASP systems show that this transport occurs primarily through cyclogenesis at mid-latitudes

    Combinatorics of linear iterated function systems with overlaps

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    Let p0,...,pm1\bm p_0,...,\bm p_{m-1} be points in Rd{\mathbb R}^d, and let {fj}j=0m1\{f_j\}_{j=0}^{m-1} be a one-parameter family of similitudes of Rd{\mathbb R}^d: fj(x)=λx+(1λ)pj,j=0,...,m1, f_j(\bm x) = \lambda\bm x + (1-\lambda)\bm p_j, j=0,...,m-1, where λ(0,1)\lambda\in(0,1) is our parameter. Then, as is well known, there exists a unique self-similar attractor SλS_\lambda satisfying Sλ=j=0m1fj(Sλ)S_\lambda=\bigcup_{j=0}^{m-1} f_j(S_\lambda). Each xSλ\bm x\in S_\lambda has at least one address (i1,i2,...)1{0,1,...,m1}(i_1,i_2,...)\in\prod_1^\infty\{0,1,...,m-1\}, i.e., limnfi1fi2...fin(0)=x\lim_n f_{i_1}f_{i_2}... f_{i_n}({\bf 0})=\bm x. We show that for λ\lambda sufficiently close to 1, each xSλ{p0,...,pm1}\bm x\in S_\lambda\setminus\{\bm p_0,...,\bm p_{m-1}\} has 202^{\aleph_0} different addresses. If λ\lambda is not too close to 1, then we can still have an overlap, but there exist x\bm x's which have a unique address. However, we prove that almost every xSλ\bm x\in S_\lambda has 202^{\aleph_0} addresses, provided SλS_\lambda contains no holes and at least one proper overlap. We apply these results to the case of expansions with deleted digits. Furthermore, we give sharp sufficient conditions for the Open Set Condition to fail and for the attractor to have no holes. These results are generalisations of the corresponding one-dimensional results, however most proofs are different.Comment: Accepted for publication in Nonlinearit

    Sixty Years of Fractal Projections

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    Sixty years ago, John Marstrand published a paper which, among other things, relates the Hausdorff dimension of a plane set to the dimensions of its orthogonal projections onto lines. For many years, the paper attracted very little attention. However, over the past 30 years, Marstrand's projection theorems have become the prototype for many results in fractal geometry with numerous variants and applications and they continue to motivate leading research.Comment: Submitted to proceedings of Fractals and Stochastics

    Equilibrium states of the pressure function for products of matrices

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    Let {Mi}i=1\{M_i\}_{i=1}^\ell be a non-trivial family of d×dd\times d complex matrices, in the sense that for any nNn\in \N, there exists i1...in{1,...,}ni_1... i_n\in \{1,..., \ell\}^n such that Mi1...Min0M_{i_1}... M_{i_n}\neq {\bf 0}. Let P ⁣:(0,)RP \colon (0,\infty)\to \R be the pressure function of {Mi}i=1\{M_i\}_{i=1}^\ell. We show that for each q>0q>0, there are at most dd ergodic qq-equilibrium states of PP, and each of them satisfies certain Gibbs property.Comment: 12 pages. To appear in DCD

    Golden gaskets: variations on the Sierpi\'nski sieve

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    We consider the iterated function systems (IFSs) that consist of three general similitudes in the plane with centres at three non-collinear points, and with a common contraction factor \la\in(0,1). As is well known, for \la=1/2 the invariant set, \S_\la, is a fractal called the Sierpi\'nski sieve, and for \la<1/2 it is also a fractal. Our goal is to study \S_\la for this IFS for 1/2<\la<2/3, i.e., when there are "overlaps" in \S_\la as well as "holes". In this introductory paper we show that despite the overlaps (i.e., the Open Set Condition breaking down completely), the attractor can still be a totally self-similar fractal, although this happens only for a very special family of algebraic \la's (so-called "multinacci numbers"). We evaluate \dim_H(\S_\la) for these special values by showing that \S_\la is essentially the attractor for an infinite IFS which does satisfy the Open Set Condition. We also show that the set of points in the attractor with a unique ``address'' is self-similar, and compute its dimension. For ``non-multinacci'' values of \la we show that if \la is close to 2/3, then \S_\la has a nonempty interior and that if \la<1/\sqrt{3} then \S_\la$ has zero Lebesgue measure. Finally we discuss higher-dimensional analogues of the model in question.Comment: 27 pages, 10 figure

    Higher-dimensional multifractal value sets for conformal infinite graph directed Markov systems

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    We give a description of the level sets in the higher dimensional multifractal formalism for infinite conformal graph directed Markov systems. If these systems possess a certain degree of regularity this description is complete in the sense that we identify all values with non-empty level sets and determine their Hausdorff dimension. This result is also partially new for the finite alphabet case.Comment: 20 pages, 1 figur

    A renormalisation approach to excitable reaction-diffusion waves in fractal media

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    Of fundamental importance to wave propagation in a wide range of physical phenomena is the structural geometry of the supporting medium. Recently, there have been several investigations on wave propagation in fractal media. We present here a renormalization approach to the study of reaction-diffusion (RD) wave propagation on finitely ramified fractal structures. In particular we will study a Rinzel-Keller (RK) type model, supporting travelling waves on a Sierpinski gasket (SG), lattice
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