Аннотация
Although most models for rainfall extremes focus on pointwise rainfall, it is
rainfall aggregated over areas up to river catchment scale that is of the most
interest. Parsimonious and effective models for the extremes of precipitation
aggregates that can capture their joint behaviour between different spatial
resolutions must be built with knowledge of the underlying spatial process.
Precipitation is driven by a mixture of processes acting at different scales
and intensities, e.g., convective and frontal, with extremes of aggregates for
typical catchment sizes arising from extremes of only one of these types,
rather than a combination of them. The specific process that dominates the
extremal behaviour of the aggregate will be dependent on the area aggregated.
High-intensity convective events cause extreme spatial aggregates at small
scales but the contribution of lower-intensity large-scale fronts is likely to
increase as the area aggregated increases. Thus, to model small to large scale
spatial aggregates within a single approach requires a model that can
accurately capture the extremal properties of both convective and frontal
events. Previous extreme value methods have ignored this mixture structure and
so we propose a spatial extreme value model which is a mixture of two
components with different marginal and dependence models that are able to
capture the extremal behaviour of convective and frontal rainfall and more
faithfully reproduces spatial aggregates for a wide range of scales. Modelling
extremes of the frontal component raises new challenges due to it exhibiting
strong long-range extremal spatial dependence. Our modelling approach is
applied to fine-scale, high-dimensional, gridded precipitation data, where we
show that accounting for the mixture structure improves the joint inference on
extremes of spatial aggregates over regions of different sizes.
Пользователи данного ресурса
Пожалуйста,
войдите в систему, чтобы принять участие в дискуссии (добавить собственные рецензию, или комментарий)