Submit to Water Review for Water Propose a Special Issue

Journal Browser

Statistical Analysis and Stochastic Modelling of Hydrological Extremes

Print Special Issue Flyer
Special Issue Editors
Special Issue Information
Keywords
Published Papers

A special issue of Water (ISSN 2073-4441). This special issue belongs to the section "Water Resources Management, Policy and Governance".

Deadline for manuscript submissions: closed (31 May 2019) | Viewed by 70240

Printed Edition Available!
A printed edition of this Special Issue is available here.

Special issue Statistical Analysis and Stochastic Modelling of Hydrological Extremes book cover image

Share This Special Issue

Special Issue Editor

Dr. Hossein Tabari

E-Mail Website
Guest Editor

Department of Civil Engineering, University of Leuven (KU Leuven), Heverlee, Belgium
Interests: statistical analysis of hydrological extremes; climate change/variability impact assessment on hydrology and water resources; monitoring and modeling of water availability and drought/water scarcity
Special Issues, Collections and Topics in MDPI journals

Special Issue Information

Dear Colleagues,

Assessment of hydrological extremes is of paramount importance, as they have the potential to affect society in terms of human health and mortality, and also may have effects on the ecosystem and economy (e.g., infrastructure and agriculture). In the last few decades, millions of people have been affected by hydrological extremes. The risk of these hazards will increase in the future as a result of climate change, and as population and infrastructure continue to increase and occupy areas exposed to higher risks. This Special Issue invites original research articles, as well as review articles, that address statistical analysis and stochastic modelling of hydrological extremes under current and future climate conditions. We are particularly interested in studies related to innovative stochastic and statistical approaches to analyze hydrological extremes. Potential topics include, but are not limited to:

Decadal anomaly and trend analysis of historical hydrological extremes
Anthropogenic and atmospheric drivers
Assessment of uncertainties in hydrological projections and observations
Application of statistical and dynamical downscaling methods
Hydrological modeling under extreme conditions
Early warning and forecasting systems
Regional and global drought and flood analyses
Adaptation and mitigation strategies
Socio-environmental consequences of hydrological extremes

Dr. Hossein Tabari
Guest Editor

Manuscript Submission Information

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Water is an international peer-reviewed open access semimonthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2600 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

Hydrological extremes
Pluvial and fluvial floods
Hydrological drought
Forecasting models
Climate change
Decadal climate variability
Uncertainty analysis

Published Papers (14 papers)

Download All Papers

Editorial

Jump to: Research

11 pages, 226 KiB

Open AccessEditorial

Statistical Analysis and Stochastic Modelling of Hydrological Extremes

by Hossein Tabari

Water 2019, 11(9), 1861; https://doi.org/10.3390/w11091861 - 07 Sep 2019

Cited by 17 | Viewed by 4234

Abstract

Analysis of hydrological extremes is challenging due to their rarity and small sample size and the interconnections between different types of extremes and gets further complicated by an untrustworthy representation of meso-scale processes involved in extreme events by coarse spatial and temporal scale models as well as biased or missing observations due to technical difficulties during extreme conditions. The special issue “Statistical Analysis and Stochastic Modelling of Hydrological Extremes”—motivated by the need to apply and develop innovative stochastic and statistical approaches to analyze hydrological extremes under current and future climate conditions —encompass 13 research papers. Case studies presented in the papers exploit a wide range of innovative techniques for hydrological extremes analyses. The papers focus on six topics: Historical changes in hydrological extremes, projected changes in hydrological extremes, downscaling of hydrological extremes, early warning and forecasting systems for drought and flood, interconnections of hydrological extremes and applicability of satellite data for hydrological studies. This Editorial provides an overview of the covered topics and reviews the case studies relevant for each topic. Full article

(This article belongs to the Special Issue Statistical Analysis and Stochastic Modelling of Hydrological Extremes)

Research

Jump to: Editorial

30 pages, 13926 KiB

Open AccessArticle

Non-Stationary Bayesian Modeling of Annual Maximum Floods in a Changing Environment and Implications for Flood Management in the Kabul River Basin, Pakistan

by Asif Mehmood, Shaofeng Jia, Rashid Mahmood, Jiabao Yan and Moien Ahsan

Water 2019, 11(6), 1246; https://doi.org/10.3390/w11061246 - 14 Jun 2019

Cited by 12 | Viewed by 4755

Abstract

Recent evidence of regional climate change associated with the intensification of human activities has led hydrologists to study a flood regime in a non-stationarity context. This study utilized a Bayesian framework with informed priors on shape parameter for a generalized extreme value (GEV) model for the estimation of design flood quantiles for “at site analysis” in a changing environment, and discussed its implications for flood management in the Kabul River basin (KRB), Pakistan. Initially, 29 study sites in the KRB were used to evaluate the annual maximum flood regime by applying the Mann–Kendall test. Stationary (without trend) and a non-stationary (with trend) Bayesian models for flood frequency estimation were used, and their results were compared using the corresponding flood frequency curves (FFCs), along with their uncertainty bounds. The results of trend analysis revealed significant positive trends for 27.6% of the gauges, and 10% showed significant negative trends at the significance level of 0.05. In addition to these, 6.9% of the gauges also represented significant positive trends at the significance level of 0.1, while the remaining stations displayed insignificant trends. The non-stationary Bayesian model was found to be reliable for study sites possessing a statistically significant trend at the significance level of 0.05, while the stationary Bayesian model overestimated or underestimated the flood hazard for these sites. Therefore, it is vital to consider the presence of non-stationarity for sustainable flood management under a changing environment in the KRB, which has a rich history of flooding. Furthermore, this study also states a regional shape parameter value of 0.26 for the KRB, which can be further used as an informed prior on shape parameter if the study site under consideration possesses the flood type “flash”. The synchronized appearance of a significant increase and decrease of trends within very close gauge stations is worth paying attention to. The present study, which considers non-stationarity in the flood regime, will provide a reference for hydrologists, water resource managers, planners, and decision makers. Full article

(This article belongs to the Special Issue Statistical Analysis and Stochastic Modelling of Hydrological Extremes)

► Show Figures

Figure 1

15 pages, 4594 KiB

Open AccessArticle

Extreme Precipitation in China in Response to Emission Reductions under the Paris Agreement

by Jintao Zhang and Fang Wang

Water 2019, 11(6), 1167; https://doi.org/10.3390/w11061167 - 04 Jun 2019

Cited by 6 | Viewed by 2879

Abstract

To avoid more severe impacts from climate change, countries worldwide pledged to implement intended nationally determined contributions (INDCs) for emission reductions (as part of the Paris Agreement). However, it remains unclear what the resulting precipitation change in terms of regional extremes would be in response to the INDC scenarios. Here, we analyzed China’s extreme precipitation response of the next few decades to the updated INDC scenarios within the framework of the Paris Agreement. Our results indicate increases in the intensity and frequency of extreme precipitation (compared with the current level) in most regions in China. The maximum consecutive five-day precipitation over China is projected to increase ~16%, and the number of heavy precipitation days will increase as much as ~20% in some areas. The probability distributions of extreme precipitation events become wider, resulting in the occurrence of more record-breaking heavy precipitation in the future. We further considered the impacts of precipitation-related extremes and found that the projected population exposure to heavy precipitation events will significantly increase in almost all Chinese regions. For example, for heavy precipitation events that exceed the 20 year baseline return value, the population exposure over China increases from 5.7% (5.1–6.0%) to 15.9% (14.2–16.4%) in the INDC-pledge scenario compared with the present-day level. Limiting the warming to lower levels (e.g., 1.5 °C or 2.0 °C) would reduce the population exposure to heavy precipitation, thereby avoiding impacts associated with more intense precipitation events. These results contribute to an improved understanding of the future risk of climate extremes, which is paramount for the design of mitigation and adaptation policies in China. Full article

(This article belongs to the Special Issue Statistical Analysis and Stochastic Modelling of Hydrological Extremes)

► Show Figures

Figure 1

18 pages, 2947 KiB

Open AccessArticle

Statistical Analysis of Extreme Events in Precipitation, Stream Discharge, and Groundwater Head Fluctuation: Distribution, Memory, and Correlation

by Shawn Dawley, Yong Zhang, Xiaoting Liu, Peng Jiang, Geoffrey R. Tick, HongGuang Sun, Chunmiao Zheng and Li Chen

Water 2019, 11(4), 707; https://doi.org/10.3390/w11040707 - 05 Apr 2019

Cited by 10 | Viewed by 4594

Abstract

Hydrological extremes in the water cycle can significantly affect surface water engineering design, and represents the high-impact response of surface water and groundwater systems to climate change. Statistical analysis of these extreme events provides a convenient way to interpret the nature of, and interaction between, components of the water cycle. This study applies three probability density functions (PDFs), Gumbel, stable, and stretched Gaussian distributions, to capture the distribution of extremes and the full-time series of storm properties (storm duration, intensity, total precipitation, and inter-storm period), stream discharge, lake stage, and groundwater head values observed in the Lake Tuscaloosa watershed, Alabama, USA. To quantify the potentially non-stationary statistics of hydrological extremes, the time-scale local Hurst exponent (TSLHE) was also calculated for the time series data recording both the surface and subsurface hydrological processes. First, results showed that storm duration was most closely related to groundwater recharge compared to the other storm properties, while intensity also had a close relationship with recharge. These relationships were likely due to the effects of oversaturation and overland flow in extreme total precipitation storms. Second, the surface water and groundwater series were persistent according to the TSLHE values, because they were relatively slow evolving systems, while storm properties were anti-persistent since they were rapidly evolving in time. Third, the stretched Gaussian distribution was the most effective PDF to capture the distribution of surface and subsurface hydrological extremes, since this distribution can capture the broad transition from a Gaussian distribution to a power-law one. Full article

(This article belongs to the Special Issue Statistical Analysis and Stochastic Modelling of Hydrological Extremes)

► Show Figures

Figure 1

20 pages, 4302 KiB

Open AccessArticle

Third-Order Polynomial Normal Transform Applied to Multivariate Hydrologic Extremes

by Yeou-Koung Tung, Lingwan You and Chulsang Yoo

Water 2019, 11(3), 490; https://doi.org/10.3390/w11030490 - 08 Mar 2019

Cited by 3 | Viewed by 2843

Abstract

Hydro-infrastructural systems (e.g., flood control dams, stormwater detention basins, and seawalls) are designed to protect the public against the adverse impacts of various hydrologic extremes (e.g., floods, droughts, and storm surges). In their design and safety evaluation, the characteristics of concerned hydrologic extremes affecting the hydrosystem performance often are described by several interrelated random variables—not just one—that need to be considered simultaneously. These multiple random variables, in practical problems, have a mixture of non-normal distributions of which the joint distribution function is difficult to establish. To tackle problems involving multivariate non-normal variables, one frequently adopted approach is to transform non-normal variables from their original domain to multivariate normal space under which a large wealth of established theories can be utilized. This study presents a framework for practical normal transform based on the third-order polynomial in the context of a multivariate setting. Especially, the study focuses on multivariate third-order polynomial normal transform (TPNT) with explicit consideration of sampling errors in sample L-moments and correlation coefficients. For illustration, the modeling framework is applied to establish an at-site rainfall intensity–duration-frequency (IDF) relationship. Annual maximum rainfall data analyzed contain seven durations (1–72 h) with 27 years of useable records. Numerical application shows that the proposed modeling framework can produce reasonable rainfall IDF relationships by simultaneously treating several correlated rainfall data series and is a viable tool in dealing with multivariate data with a mixture of non-normal distributions. Full article

(This article belongs to the Special Issue Statistical Analysis and Stochastic Modelling of Hydrological Extremes)

► Show Figures

Figure 1

17 pages, 2170 KiB

Open AccessArticle

Combing Random Forest and Least Square Support Vector Regression for Improving Extreme Rainfall Downscaling

by Quoc Bao Pham, Tao-Chang Yang, Chen-Min Kuo, Hung-Wei Tseng and Pao-Shan Yu

Water 2019, 11(3), 451; https://doi.org/10.3390/w11030451 - 03 Mar 2019

Cited by 45 | Viewed by 6169

Abstract

A statistical downscaling approach for improving extreme rainfall simulation was proposed to predict the daily rainfalls at Shih-Men Reservoir catchment in northern Taiwan. The structure of the proposed downscaling approach is composed of two parts: the rainfall-state classification and the regression for rainfall-amount prediction. Predictors of classification and regression methods were selected from the large-scale climate variables of the NCEP reanalysis data based on statistical tests. The data during 1964–1999 and 2000–2013 were used for calibration and validation, respectively. Three classification methods, including linear discriminant analysis (LDA), random forest (RF), and support vector classification (SVC), were adopted for rainfall-state classification and their performances were compared. After rainfall-state classification, the least square support vector regression (LS-SVR) was used for rainfall-amount prediction for different rainfall states. Two rainfall states (i.e., dry day and wet day) and three rainfall states (dry day, non-extreme-rainfall day, and extreme-rainfall day) were defined and compared for judging their downscaling performances. The results show that RF outperforms LDA and SVC for rainfall-state classification. Using RF for three-rainfall-states classification and LS-SVR for rainfall-amount prediction can improve the extreme rainfall downscaling. Full article

(This article belongs to the Special Issue Statistical Analysis and Stochastic Modelling of Hydrological Extremes)

► Show Figures

Figure 1

22 pages, 8205 KiB

Open AccessArticle

Recent Precipitation Trends and Floods in the Colombian Andes

by Álvaro Ávila, Faisury Cardona Guerrero, Yesid Carvajal Escobar and Flávio Justino

Water 2019, 11(2), 379; https://doi.org/10.3390/w11020379 - 22 Feb 2019

Cited by 40 | Viewed by 7140

Abstract

This study aims to identify spatial and temporal precipitation trends by analyzing eight extreme climate indices of rainfall in the High Basin of the Cauca River in Southwestern Colombia from 1970 to 2013. The relation between historical floods and El Niño Southern Oscillation (ENSO) is also analyzed. Results indicate that in general, the reduction of precipitation, especially in the center of the basin with negative annual and seasonal trends in intensity indices, namely, the annual maximum 1-day precipitation amount (RX1day) and annual maximum 5-day precipitation amount (RX5day). Sixty-four percentage of the stations exhibit an increasing trend in September–October–November in the consecutive dry days. In December–January–February interval, positive trends in most of the stations is noted for total precipitation and for the number of wet days with rainfall greater than or equal to 1 mm. The findings also show that sea surface temperature (SST) in the equatorial Pacific is statistically correlated (r) with indices of extreme precipitation (r ≥ −0.40). However, the effect of ENSO is evident with a time lag of 2–3 months. These results are relevant for forecasting floods on a regional scale, since changes in SST of the equatorial Pacific may take place 2–3 months ahead of the basin inundation. Our results contribute to the understanding of extreme rainfall events, hydrological hazard forecasts and climate variability in the Colombian Andes. Full article

(This article belongs to the Special Issue Statistical Analysis and Stochastic Modelling of Hydrological Extremes)

► Show Figures

Graphical abstract

24 pages, 8997 KiB

Open AccessArticle

Characteristics of Heavy Storms and the Scaling Relation with Air Temperature by Event Process-Based Analysis in South China

by Cuilin Pan, Xianwei Wang, Lin Liu, Dashan Wang and Huabing Huang

Water 2019, 11(2), 185; https://doi.org/10.3390/w11020185 - 22 Jan 2019

Cited by 11 | Viewed by 3795

Abstract

The negative scaling rate between precipitation extremes and the air temperature in tropic and subtropic regions is still a puzzling issue. This study investigates the scaling rate from two aspects, storm characteristics (types) and event process-based temperature variations. Heavy storms in South China are developed by different weather systems with unique meteorological characteristics each season, such as the warm-front storms (January), cold-front storms (April to mid-May), monsoon storms (late May to June), convective storms, and typhoon storms (July to September). This study analyzes the storm characteristics using the hourly rainfall data from 1990 to 2017; compares the storm hyetographs derived from the one-minute rainfall data during 2008–2017; and investigates the interactions between heavy storms and meteorological factors including air temperature, relative humidity, surface pressure, and wind speed at 42 weather stations in Guangzhou during 2015–2017. Most storms, except for typhoon and warm-front storms, had a short duration (3 h) and intense rates (~13 mm/h) in Guangzhou, South China. Convective storms were dominant (50%) in occurrence and had the strongest intensity (15.8 mm/h). Storms in urban areas had stronger interactions with meteorological factors and showed different hyetographs from suburban areas. Meteorological factors had larger variations with the storms that occurred in the day time than at night. The air temperature could rise 6 °C and drop 4 °C prior to and post-summer storms against the diurnal mean state. The 24-h mean air temperature prior to the storms produced more reliable scaling rates than the naturally daily mean air temperature. The precipitation extremes showed a peak-like scaling relation with the 24-h mean air temperature and had a break temperature of 28 °C. Below 28 °C, the relative humidity was 80%–100%, and it showed a positive scaling rate. Above 28 °C, the negative scaling relation was likely caused by a lack of moisture in the atmosphere, where the relative humidity decreased with the air temperature increase. Full article

(This article belongs to the Special Issue Statistical Analysis and Stochastic Modelling of Hydrological Extremes)

► Show Figures

Figure 1

24 pages, 2600 KiB

Open AccessArticle

Applicability of ε-Support Vector Machine and Artificial Neural Network for Flood Forecasting in Humid, Semi-Humid and Semi-Arid Basins in China

by Thabo Michael Bafitlhile and Zhijia Li

Water 2019, 11(1), 85; https://doi.org/10.3390/w11010085 - 06 Jan 2019

Cited by 60 | Viewed by 4393

Abstract

The aim of this study was to develop hydrological models that can represent different geo-climatic system, namely: humid, semi-humid and semi-arid systems, in China. Humid and semi-humid areas suffer from frequent flood events, whereas semi-arid areas suffer from flash floods because of urbanization and climate change, which contribute to an increase in runoff. This study applied ɛ-Support Vector Machine (ε-SVM) and artificial neural network (ANN) for the simulation and forecasting streamflow of three different catchments. The Evolutionary Strategy (ES) optimization method was used to optimize the ANN and SVM sensitive parameters. The relative performance of the two models was compared, and the results indicate that both models performed well for humid and semi-humid systems, and SVM generally perform better than ANN in the streamflow simulation of all catchments. Full article

(This article belongs to the Special Issue Statistical Analysis and Stochastic Modelling of Hydrological Extremes)

► Show Figures

Figure 1

22 pages, 4729 KiB

Open AccessArticle

Improved Forecasting of Extreme Monthly Reservoir Inflow Using an Analogue-Based Forecasting Method: A Case Study of the Sirikit Dam in Thailand

by Somchit Amnatsan, Sayaka Yoshikawa and Shinjiro Kanae

Water 2018, 10(11), 1614; https://doi.org/10.3390/w10111614 - 09 Nov 2018

Cited by 27 | Viewed by 5508

Abstract

Reservoir inflow forecasting is crucial for appropriate reservoir management, especially in the flood season. Forecasting for this season must be sufficiently accurate and timely to allow dam managers to release water gradually for flood control in downstream areas. Recently, several models and methodologies have been developed and applied for inflow forecasting, with good results. Nevertheless, most were reported to have weaknesses in capturing the peak flow, especially rare extreme flows. In this study, an analogue-based forecasting method, designated the variation analogue method (VAM), was developed to overcome this weakness. This method, the wavelet artificial neural network (WANN) model, and the weighted mean analogue method (WMAM) were used to forecast the monthly reservoir inflow of the Sirikit Dam, located in the Nan River Basin, one of the eight sub-basins of the Chao Phraya River Basin in Thailand. It is one of four major dams in the Chao Phraya Basin, with a maximum storage of 10.64 km³, which supplies water to 22 provinces in this basin, covering an irrigation area of 1,513,465 hectares. Due to the huge extreme monthly inflow in August, with inflow of more than 3 km³ in 1985 and 2011, monthly or longer lead time inflow forecasting is needed for proper water and flood control management of this dam. The results of forecasting indicate that the WANN model provided good forecasting for whole-year forecasting including both low-flow and high-flow patterns, while the WMAM model provided only satisfactory results. The VAM showed the best forecasting performance and captured the extreme inflow of the Sirikit Dam well. For the high-flow period (July–September), the WANN model provided only satisfactory results, while those of the WMAM were markedly poorer than for the whole year. The VAM showed the best capture of flow in this period, especially for extreme flow conditions that the WANN and WMAM models could not capture. Full article

(This article belongs to the Special Issue Statistical Analysis and Stochastic Modelling of Hydrological Extremes)

► Show Figures

Figure 1

22 pages, 5763 KiB

Open AccessArticle

A Multi-GCM Assessment of the Climate Change Impact on the Hydrology and Hydropower Potential of a Semi-Arid Basin (A Case Study of the Dez Dam Basin, Iran)

by Roya Sadat Mousavi, Mojtaba Ahmadizadeh and Safar Marofi

Water 2018, 10(10), 1458; https://doi.org/10.3390/w10101458 - 16 Oct 2018

Cited by 15 | Viewed by 4476

Abstract

In this paper, the impact of climate change on the climate and discharge of the Dez Dam Basin and the hydropower potential of two hydropower plants (Bakhtiari and Dez) is investigated based on the downscaled outputs of six GCMs (General Circulation Models) and three SRES (Special Report on Emission Scenarios) scenarios for the early, mid and late 21st century. Projections of all the scenarios and GCMs revealed a significant rise in temperature (up to 4.9 °C) and slight to moderate variation in precipitation (up to 18%). Outputs of the HBV hydrologic model, enforced by projected datasets, show a reduction of the annual flow by 33% under the climate change condition. Further, analyzing the induced changes in the inflow and hydropower generation potential of the Bakhtiari and Dez dams showed that both inflow and hydropower generation is significantly affected by climate change. For the Bakhtiari dam, this indicates a consistent reduction of inflow (up to 27%) and electricity generation (up to 32%). While, in the Dez dam case, the inflow is projected to decrease (up to 22%) and the corresponding hydropower is expected to slightly increase (up to 3%). This contrasting result for the Dez dam is assessed based on its reservoir and hydropower plant capacity, as well as other factors such as the timely releases to meet different demands and flow regime changes under climate change. The results show that the Bakhtiari reservoir and power plant will not meet the design-capacity outputs under the climate change condition as its large capacity cannot be fully utilized; while there is room for the further development of the Dez power plant. Comparing the results of the applied GCMs showed high discrepancies among the outputs of different models. Full article

(This article belongs to the Special Issue Statistical Analysis and Stochastic Modelling of Hydrological Extremes)

► Show Figures

Figure 1

21 pages, 3993 KiB

Open AccessArticle

Wavelet-ANN versus ANN-Based Model for Hydrometeorological Drought Forecasting

by Md Munir H. Khan, Nur Shazwani Muhammad and Ahmed El-Shafie

Water 2018, 10(8), 998; https://doi.org/10.3390/w10080998 - 27 Jul 2018

Cited by 44 | Viewed by 5276

Abstract

Malaysia is one of the countries that has been experiencing droughts caused by a warming climate. This study considered the Standard Index of Annual Precipitation (SIAP) and Standardized Water Storage Index (SWSI) to represent meteorological and hydrological drought, respectively. The study area is the Langat River Basin, located in the central part of peninsular Malaysia. The analysis was done using rainfall and water level data over 30 years, from 1986 to 2016. Both of the indices were calculated in monthly scale, and two neural network-based models and two wavelet-based artificial neural network (W-ANN) models were developed for monthly droughts. The performance of the SIAP and SWSI models, in terms of the correlation coefficient (R), was 0.899 and 0.968, respectively. The application of a wavelet for preprocessing the raw data in the developed W-ANN models achieved higher correlation coefficients for most of the scenarios. This proves that the created model can predict meteorological and hydrological droughts very close to the observed values. Overall, this study helps us to understand the history of drought conditions over the past 30 years in the Langat River Basin. It further helps us to forecast drought and to assist in water resource management. Full article

(This article belongs to the Special Issue Statistical Analysis and Stochastic Modelling of Hydrological Extremes)

► Show Figures

Figure 1

19 pages, 7431 KiB

Open AccessArticle

Drought Prediction for Areas with Sparse Monitoring Networks: A Case Study for Fiji

by Jinyoung Rhee and Hongwei Yang

Water 2018, 10(6), 788; https://doi.org/10.3390/w10060788 - 14 Jun 2018

Cited by 11 | Viewed by 6012

Abstract

Hybrid drought prediction models were developed for areas with limited monitoring gauges using the APEC Climate Center Multi-Model Ensemble seasonal climate forecast and machine learning models of Extra-Trees and Adaboost. The models provide spatially distributed detailed drought prediction data of the 6-month Standardized Precipitation Index for the case study area, Fiji. In order to overcome the limitation of a sparse monitoring network, both in-situ data and bias-corrected dynamic downscaling of historical climate data from the Weather Research Forecasting (WRF) model were used as reference data. Performance measures of the mean absolute error as well as classification accuracy were used. The WRF outputs reflect the topography of the area. Hybrid models showed better performance than simply bias corrected forecasts in most cases. Especially, the model based on Extra-Trees trained using the WRF model outputs performed the best in most cases. Full article

(This article belongs to the Special Issue Statistical Analysis and Stochastic Modelling of Hydrological Extremes)

► Show Figures

Graphical abstract

19 pages, 27274 KiB

Open AccessArticle

Spatial Downscaling of Satellite Precipitation Data in Humid Tropics Using a Site-Specific Seasonal Coefficient

by Mohd. Rizaludin Mahmud, Mazlan Hashim, Hiroshi Matsuyama, Shinya Numata and Tetsuro Hosaka

Water 2018, 10(4), 409; https://doi.org/10.3390/w10040409 - 31 Mar 2018

Cited by 15 | Viewed by 6306

Abstract

This paper described the development of a spatial downscaling algorithm to produce finer grid resolution for satellite precipitation data (0.05°) in humid tropics. The grid resolution provided by satellite precipitation data (>0.25°) was unsuitable for practical hydrology and meteorology applications in the high hydrometeorological dynamics of Southeast Asia. Many downscaling algorithms have been developed based on significant seasonal relationships, without vegetation and climate conditions, which were inapplicable in humid, equatorial, and tropical regions. Therefore, we exploited the potential of the low variability of rainfall and monsoon characteristics (period, location, and intensity) on a local scale, as a proxy to downscale the satellite precipitation grid and its corresponding rainfall estimates. This study hypothesized that the ratio between the satellite precipitation and ground rainfall in the low-variance spatial rainfall pattern and seasonality region of humid tropics can be used as a coefficient (constant value) to spatially downscale future satellite precipitation datasets. The spatial downscaling process has two major phases: the first is the derivation of the high-resolution coefficient (0.05°), and the second is applying the coefficient to produce the high-resolution precipitation map. The first phase utilized the long-term bias records (1998–2008) between the high-resolution areal precipitation (0.05°) that was derived from dense network of ground precipitation data and re-gridded satellite precipitation data (0.05°) from the Tropical Rainfall Measuring Mission (TRMM) to produce the site-specific coefficient (SSC) for each individual pixel. The outcome of the spatial downscaling process managed to produce a higher resolution of the TRMM data from 0.25° to 0.05° with a lower bias (average: 18%). The trade-off for the process was a small decline in the correlation between TRMM and ground rainfall. Our results indicate that the SSC downscaled method can be used to spatially downscale satellite precipitation data in humid, tropical regions, where the seasonal rainfall is consistent. Full article

(This article belongs to the Special Issue Statistical Analysis and Stochastic Modelling of Hydrological Extremes)

► Show Figures