A simple approach for stochastic generation of spatial rainfall patterns

被引:26
作者
Tarpanelli, A. [1 ]
Franchini, M. [2 ]
Brocca, L. [1 ]
Camici, S. [1 ]
Melone, F. [1 ]
Moramarco, T. [1 ]
机构
[1] CNR, Res Inst Geohydrol Protect, I-06128 Perugia, Italy
[2] Univ Ferrara, Dipartimento Ingn, I-44128 Ferrara, Italy
关键词
Stochastic rainfall generation; Spatial rainfall correlation; Neyman-Scott Rectangular Pulse (NSRP) model; POINT PROCESS MODELS; DAILY PRECIPITATION; FLOOD FREQUENCY; TEMPORAL MODEL; SIMULATION; VARIABILITY; UNCERTAINTY; TEMPERATURE; BASIN;
D O I
10.1016/j.jhydrol.2012.09.010
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Rainfall scenarios are of considerable interest for design flood and flood risk analysis. To this end, the stochastic generation of continuous rainfall sequences is often coupled with the continuous hydrological modelling. In this context, the spatial and the temporal rainfall variability represents a significant issue, especially for basins in which the rainfall field cannot be approximated through the use of a single station. Therefore, methodologies for the spatially and temporally correlated rainfall generation are welcome. An example of such a methodology is the well-established Spatial-Temporal Neyman-Scott Rectangular Pulse (STNSRP), a modification of the single-site Neyman-Scott Rectangular Pulse (NSRP) approach, designed to incorporate specific features to reproduce the rainfall spatial cross-correlation. In order to provide a simple alternative to the STNSRP, a new method of generating synthetic rainfall time series with pre-set spatial temporal correlation is proposed herein. This approach relies on the single-site NSRP model, which is used to generate synthetic hourly independent rainfall time series at each rain gauge station with the required temporal autocorrelation (and several other appropriately selected statistics). The rank correlation method of Iman and Conover (IC) is then applied to these synthetic rainfall time series in order to introduce the same spatial cross-correlation that exists between the observed time series. This combination of the NSRP model with the IC method consents the reproduction of the observed spatial-temporal variability of a rainfall field. In order to verify the proposed procedure, four sub-basins of the Upper Tiber River basin are investigated whose basin areas range from 165 km(2) to 2040 km(2). Results show that the procedure is able to preserve both the rainfall temporal autocorrelation at single site and the rainfall spatial cross-correlation at basin scale, and its performance is comparable with that of the STNSRP model for rainfall field generation. Given its simple formal structure (based on well established methods: i.e. NSRP and IC), we believe that the proposed approach can be conveniently utilized to generate spatially and temporally correlated rainfall scenarios. (C) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:63 / 76
页数:14
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