[Stoch] Preprint "A stochastic model for the transition to stong convection" by Stechmann and Neelin
Sam Stechmann
stechmann at wisc.edu
Mon Apr 18 08:21:41 MDT 2011
Hi All
Below are a link and the abstract for a paper by me and David Neelin, "A
stochastic model for the transition to stong convection," which was
recently accepted to JAS.
Best
Sam Stechmann
-------------------------------------------------------
A stochastic model for the transition to stong convection
by Stechmann and Neelin
to appear in JAS
Preprint:
https://www.math.wisc.edu/~stech/publications/StechmannNeelin2011.pdf
Abstract:
A simple stochastic model is designed and analyzed in order to further
understand the transition to strong convection. The transition has been
characterized recently in observational data by an array of statistical
measures, including (i) a sharp transition in mean precipitation, and a
peak in precipitation variance, at a critical value of column water vapor
(CWV), (ii) approximate power-law in the probability density of
precipitation event size, (iii) exponential tails in the probability
density of CWV values, when conditioned on either precipitating or
non-precipitating locations, and (iv) long and short autocorrelation times
of CWV and precipitation, respectively, with approximately exponential and
power-law decays in their autocorrelation functions, respectively. The
stochastic model presented here captures these four statistical features
in time series of CWV and precipitation at a single location. In addition,
analytic solutions are given for the exponential tails in (iii), which
directly relates the tails to model parameters. The model parameterization
includes three stochastic components: a stochastic trigger turns the
convection on and off (a two-state Markov jump process), and stochastic
closures represent variability in precipitation and in external forcing
(Gaussian white noise). This stochastic external forcing is seen to be
crucial for obtaining extreme precipitation events with high CWV and long
lifetimes, as it can occasionally compensate the heavy precipitation and
encourage more of it. This stochastic model can also be seen as a
simplified stochastic convective parameterization, and it demonstrates
simple ways to turn a deterministic parameterization - the trigger and/or
closure - into a stochastic one.
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