Vol.:(0123456789) 1 3
Acta Geophysica
https://doi.org/10.1007/s11600-020-00466-5
RESEARCH ARTICLE - HYDROLOGY
The use of hybrid methods for change points and trends detection
in rainfall series of northern Algeria
Bilel Zerouali
1
· Mohamed Chettih
1
· Zaki Abda
1
· Mohamed Mesbah
2
· Mohammed Djemai
3
Received: 4 February 2020 / Accepted: 29 July 2020
© Institute of Geophysics, Polish Academy of Sciences & Polish Academy of Sciences 2020
Abstract
The aim of this research is to assess relatively new hybrid methods for changes points and trends detection on rainfall series:
Dynamic Programming Bayesian Change Point Approach (BA), Şen’s innovative trend method (ITM) and its double (D-ITM)
and triple (T-ITM) version using the multi-scale analysis of the discrete wavelet transform (DWT) as a coupling method.
Three representatives rainfall stations of northern Algeria were analysed at annual scale during the period 1920–2011.
Moreover, correlation and spectral analysis (CSA) was applied for periodicity analysis. The CSA indicates the dominance
of interannual to multidecadal rainfall periodicity fuctuations (2-years, 5-years and 20-years) characterising long term
structured processes. Moreover, an abrupt downward trend with signifcant probability was detected from the 1970s with a
relatively wet period between the periods 1950–1970 and 2001–2011. The latter is observed in particular in the central and
eastern stations, well-explained by the BA-DWT. The results showed that the comparison results from diferent modelling
approaches found that the hybrid models (BA-DWT, ITM-DWT, D-ITM-DWT, T-ITM-DWT) often perform better than the
conventional approach (BA, ITM, D-ITM, T-ITM), where the computation time is very reasonable. The analysis revealed
that information stemming from discrete wavelet spectrums signifcantly increased the accuracy of the methods for detect-
ing hidden change points and trends.
Keywords Changes points · Trends · Hybrid methods · Discrete wavelet transform · Algeria
Introduction
Precipitation is the ultimate source of water resources and a
key element in climate characterization at a particular loca-
tion. From the beginning of the twentieth century and based
on negative human impacts on environment, the character-
istics of precipitation on a global level have been marked by
a signifcant change on a spatial and temporal scale (Hallouz
et al. 2020; Oroud 2018; Rashid and Beecham 2019; Mrad
et al. 2019; Pandey et al. 2017; Almazroui et al. 2018; Santos
et al. 2018; Spinoni et al. 2018; Zerouali et al. 2018; Par-
tal 2017; Chakraborty et al. 2017; Rashid et al. 2015; Kisi
2015; Nourani et al. 2015; Şen 2012; Nalley et al. 2012;
Meddi et al. 2010). This change in water cycle components
is the greatest environmental, technological, economic and
socio-political threat ever faced by humanity and the biggest
challenge. This problem is one of the most discussed topics
in the 5th report of the Intergovernmental Panel on Climate
Change (IPCC 2014).
The analysis of the precipitation evolution and trends
that can be detected, there are of the greatest interest for a
region, where the water resources constitute one of the key
aspects of environmental management. After the birth of
computer revolution in the 1960s, the hydrologic modelling
took a giant leap forward (Singh 2018), where signifcant
increase in hydrology and climatology research subjects in
several parts of the world, are oriented towards analysis and
assessment studies of trends and changes in hydrometeoro-
logical parameters (Da Silva et al. 2015, 2020; Mellak and
* Bilel Zerouali
b.zerouali@lagh-univ.dz
1
Research Laboratory of Water Resources, Soil
and Environment, Department of Civil Engineering,
Faculty of Civil Engineering and Architecture, Amar Telidji
University, P. O. Box 37.G, 03000 Laghouat, Algeria
2
LGBO, Laboratory, Earth Sciences Faculty, University
of Science and Technology Houari Boumediene, BP 32,
16311 Bab Ezzouar, Algeria
3
LGEA, Laboratory of Geomaterials, Environment
and Development, Department of Civil Engineering,
Mouloud Mammeri University, BP no 10.RP,
Hasnaoua, Tizi-Ouzou, Algeria