Influence of output size of stochastic weather generators on common climate and hydrological statistical indices

2020 ◽  
Vol 34 (7) ◽  
pp. 993-1021 ◽  
Author(s):  
Abdullah Alodah ◽  
Ousmane Seidou
Climate ◽  
2017 ◽  
Vol 5 (2) ◽  
pp. 26 ◽  
Author(s):  
Sushant Mehan ◽  
Tian Guo ◽  
Margaret Gitau ◽  
Dennis C. Flanagan

2004 ◽  
Vol 26 ◽  
pp. 175-191 ◽  
Author(s):  
B Qian ◽  
S Gameda ◽  
H Hayhoe ◽  
R De Jong ◽  
A Bootsma

2019 ◽  
Vol 9 (1) ◽  
Author(s):  
Fosco M. Vesely ◽  
Livia Paleari ◽  
Ermes Movedi ◽  
Gianni Bellocchi ◽  
Roberto Confalonieri

2018 ◽  
Vol 22 (11) ◽  
pp. 5919-5933 ◽  
Author(s):  
Lionel Benoit ◽  
Mathieu Vrac ◽  
Gregoire Mariethoz

Abstract. Understanding the stationarity properties of rainfall is critical when using stochastic weather generators. Rainfall stationarity means that the statistics being accounted for remain constant over a given period, which is required for both inferring model parameters and simulating synthetic rainfall. Despite its critical importance, the stationarity of precipitation statistics is often regarded as a subjective choice whose examination is left to the judgement of the modeller. It is therefore desirable to establish quantitative and objective criteria for defining stationary rain periods. To this end, we propose a methodology that automatically identifies rain types with homogeneous statistics. It is based on an unsupervised classification of the space–time–intensity structure of weather radar images. The transitions between rain types are interpreted as non-stationarities. Our method is particularly suited to deal with non-stationarity in the context of sub-daily stochastic rainfall models. Results of a synthetic case study show that the proposed approach is able to reliably identify synthetically generated rain types. The application of rain typing to real data indicates that non-stationarity can be significant within meteorological seasons, and even within a single storm. This highlights the need for a careful examination of the temporal stationarity of precipitation statistics when modelling rainfall at high resolution.


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