Abstract
Abstract. Various fields of application, such as risk assessments of the insurance
industry or the design of flood protection systems, require reliable
precipitation statistics in high spatial resolution, including estimates for
events with high return periods. Observations from point stations, however,
lack of spatial representativeness, especially over complex terrain. Current
numerical weather models are not capable of running simulations over
thousands of years. This paper presents a new method for the stochastic
simulation of widespread precipitation based on a linear theory describing
orographic precipitation and additional functions that consider synoptically
driven rainfall and embedded convection in a simplified way. The model is
initialized by various statistical distribution functions describing
prevailing atmospheric conditions such as wind vector, moisture content, or
stability, estimated from radiosonde observations for a limited sample of
observed heavy rainfall events. The model is applied for the stochastic
simulation of heavy rainfall over the complex terrain of southwestern Germany.
It is shown that the model provides reliable precipitation fields despite its
simplicity. The differences between observed and simulated rainfall
statistics are small, being of the order of only ±10 % for return
periods of up to 1000 years.
Subject
General Earth and Planetary Sciences,General Engineering,General Environmental Science
Cited by
13 articles.
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