GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • 2020-2024  (1)
Document type
Language
Years
Year
  • 1
    Online Resource
    Online Resource
    San Diego :Elsevier Science & Technology,
    Keywords: Droughts. ; Groundwater flow. ; Hydrogeology. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (740 pages)
    Edition: 2nd ed.
    ISBN: 9780323916790
    DDC: 551.49
    Language: English
    Note: Front Cover -- Hydrological Drought -- Hydrological Drought Processes and Estimation Methods for Streamflow and Groundwater -- Copyright -- Brief contents -- Contents -- Contents on GitHub1 -- 1. Data -- 2. Worked examples -- 3. Self-guided tours -- 4. Supporting documents -- 5. Supporting code -- List of contributors -- Preface -- Acknowledgements -- Glossary -- Introduction -- Drought-related terms and description -- REFERENCES -- Abbreviations, symbols and catchment descriptors -- Abbreviations -- Symbols -- Catchment descriptors as used in Chapter 8 -- I - Drought as a natural hazard -- 1 - Introduction -- 1.1 Scope -- 1.2 Hydrological drought -- 1.3 The drought hazard -- 1.4 International low flow and drought studies -- 1.5 Outline -- 1.6 Further reading -- References -- bksec2_1 -- 2 - Hydroclimatology∗ -- 2.1 Introduction -- 2.2 Drought in different climates -- 2.2.1 Global atmospheric circulation -- 2.2.2 Hydrology and drought in the world's climate zones -- 2.2.2.1 A-climates -- 2.2.2.2 B-climates -- 2.2.2.3 C-climates -- 2.2.2.4 D-climates -- 2.2.2.5 E-climates -- 2.2.3 Atmospheric circulation and drought -- 2.2.3.1 Regional atmospheric causes -- 2.2.3.2 Large-scale atmospheric causes -- 2.2.3.3 Coupled ocean-atmosphere causes -- 2.3 Drought initiation and termination -- 2.3.1 From meteorological anomaly to hydrological drought -- 2.3.2 Drought termination -- 2.4 Space-time variability -- 2.4.1 Spatial variability -- 2.4.2 Temporal variability -- 2.5 Climate change and drought -- 2.5.1 Observed climate change -- 2.5.2 Future climate change -- 2.6 Summary -- 2.7 Further reading -- References -- bksec2_10 -- 3 - Drought-generating processes∗ -- 3.1 Introduction -- 3.2 Catchment water balance -- 3.3 Soil system - unsaturated zone -- 3.3.1 Introduction -- 3.3.1.1 Actual evapotranspiration -- 3.3.1.2 Soil infiltration. , 3.3.1.3 Groundwater recharge -- 3.3.2 Effects on the water balance -- 3.3.2.1 Low precipitation -- 3.3.2.2 High potential evapotranspiration -- 3.3.3 Variability in evapotranspiration and groundwater recharge as simulated for two contrasting catchments -- 3.3.3.1 Evapotranspiration deficit in two different climates -- 3.3.3.2 Groundwater recharge in two different climates -- 3.3.4 Influence of soil characteristics, land use and water-table depth on actual evapotranspiration and groundwater recharge -- 3.3.4.1 Soil characteristics -- 3.3.4.2 Land use -- 3.3.4.3 Water-table depth -- 3.4 Groundwater system - saturated zone -- 3.4.1 Groundwater levels -- 3.4.1.1 Groundwater levels in different hydrogeological settings and climates -- 3.4.2 Groundwater flow systems and groundwater discharge -- 3.4.2.1 Flow systems -- 3.4.2.2 Groundwater discharge -- 3.4.3 Spring flow -- 3.5 Surface water system -- 3.5.1 River flow generation -- 3.5.1.1 Overland flow and total river flow -- 3.5.1.2 Throughflow -- 3.5.1.3 Surface water network -- 3.5.1.4 River flow -- 3.5.2 Lakes and wetlands -- 3.5.2.1 Influence of lakes on downstream flow in two contrasting climates -- 3.5.2.2 Wetlands -- 3.6 Hydrological drought in cold climates -- 3.7 Drought typology -- 3.8 Summary -- 3.9 Further reading -- References -- bksec2_10 -- II - Estimation methods -- 4 - Hydrological data∗ -- 4.1 Introduction -- 4.2 Definitions and concepts -- 4.2.1 What is meant by 'data'? -- 4.2.2 Time series data -- 4.2.3 Spatial data -- 4.2.4 Metadata -- 4.2.5 Importance of scale: spatial and temporal -- 4.2.6 Uncertainty -- 4.3 Data for hydrological drought -- 4.3.1 River level data -- 4.3.2 Rating curves and spot gaugings -- 4.3.2.1 Spot gaugings -- 4.3.2.2 Rating curves -- 4.3.2.3 Factors affecting the stage-discharge relation -- 4.3.3 Continuous river flow measurements. , 4.3.3.1 Velocity-area gauging stations -- 4.3.3.2 Weirs and flumes -- 4.3.3.3 Acoustic gauging stations -- 4.3.4 Other sensing technologies -- 4.3.5 Measurement challenges at low flow -- 4.3.6 Groundwater level data -- 4.3.6.1 Automatic recording of groundwater levels -- 4.3.6.2 Manual groundwater level monitoring -- 4.3.6.3 Estimating groundwater recharge -- 4.3.6.4 Monitoring groundwater discharge -- 4.3.6.5 Groundwater storage -- 4.3.7 Quality control -- 4.3.7.1 The nature of errors -- 4.3.7.2 Good practice -- 4.3.7.3 Data validation -- 4.3.7.4 Missing data -- 4.3.8 Supporting hydrometeorological time series data -- 4.3.8.1 Precipitation -- 4.3.8.2 Evaporation -- 4.3.8.3 Soil moisture -- 4.3.9 Human interventions -- 4.3.9.1 Flow naturalisation -- 4.4 Spatial and large-sample datasets -- 4.4.1 Local-scale data -- 4.4.2 Regional to global scale data -- 4.4.2.1 Large-scale physiographic data -- 4.4.2.2 Large-sample hydrological data -- 4.4.2.3 Large-scale hydrological data -- 4.4.2.4 Large-scale climatological data -- 4.4.2.5 Satellite data -- 4.4.3 Spatial data access -- 4.4.3.1 Data catalogues -- 4.4.3.2 Data access -- 4.4.3.3 Spatial data sharing, integration and dissemination -- 4.5 Example datasets -- 4.5.1 International Dataset -- 4.5.2 Regional Dataset of Eastern Austria -- 4.5.3 Local datasets -- 4.5.3.1 Upper-Guadiana catchment (Spain) -- 4.5.3.2 The Stonor Park well, Henley on Thames (UK) -- 4.6 Summary -- 4.7 Further reading -- References -- bksec2_22 -- 5 - Hydrological drought characteristics∗ -- 5.1 Introduction -- 5.2 Drought terminology -- 5.3 Low flow characteristics -- 5.3.1 Percentiles from the flow duration curve -- 5.3.2 Mean annual minimum flow -- 5.3.3 Base flow indices -- 5.3.3.1 The Base Flow Index -- 5.3.4 Recession indices -- 5.3.4.1 Analytical expression -- 5.3.4.2 Derivation of a characteristic recession. , 5.4 Drought deficit characteristics -- 5.4.1 Threshold level method -- 5.4.1.1 Threshold selection -- 5.4.1.2 Time resolution -- 5.4.2 Indices for intermittent and ephemeral rivers -- 5.4.2 Indices for intermittent and ephemeral rivers -- 5.4.3 The sequent peak algorithm -- 5.5 Standardised indices -- 5.5.1 Empirical quantiles -- 5.5.2 Standardised (to the normal distribution) indices -- 5.6 Multivariate indices -- 5.6.1 Modelled indices -- 5.6.2 Combined indices -- 5.7 Spatial drought characteristics -- 5.7.1 Examples of non-contiguous drought area approach -- 5.7.2 Examples of contiguous drought area approach -- 5.7.3 Drought tracking -- 5.8 Application at large scale -- 5.9 Relationship between indices -- 5.9.1 Ranks and correlation coefficients -- 5.10 Summary -- 5.11 Further reading -- References -- bksec2_16 -- 6 - Frequency analysis∗ -- 6.1 Introduction -- 6.2 Basic probability concepts -- 6.2.1 Populations -- 6.2.2 Samples -- 6.3 Data for extreme value analysis -- 6.3.1 Basic assumptions -- 6.3.2 Selection of extreme events -- 6.3.2.1 Annual maximum or minimum series -- 6.3.2.2 Partial duration series -- 6.3.2.3 r-Largest events -- 6.3.2.4 Outliers -- 6.3.3 Minimum values -- 6.3.4 Maximum values -- 6.4 Probability distributions -- 6.4.1 Extreme value distributions -- 6.4.2 The Generalised Extreme Value distribution -- 6.4.3 The Generalised Pareto distribution -- 6.4.4 Other distributions -- 6.4.4.1 The log-Normal distribution -- 6.4.4.2 The Pearson type 3, Gamma and log-Pearson type 3 -- 6.4.5 Mixed distributions -- 6.4.6 Selection of distribution function -- 6.5 Estimation methods -- 6.5.1 Method of moments -- 6.5.1.1 Product moments -- 6.5.1.2 L-moments -- 6.5.2 Maximum likelihood estimators -- 6.5.3 Estimation of design values, uncertainties and risk -- 6.5.4 Non-stationary frequency analysis -- 6.6 At-site frequency analysis. , 6.6.1 Low flow characteristics -- 6.6.2 Deficit characteristics -- 6.7 Regional frequency analysis -- 6.7.1 Regional estimation model -- 6.7.2 L-moment analysis -- 6.7.2.1 L-moment ratio diagrams -- 6.7.2.2 Test of regional homogeneity -- 6.7.2.3 Determination of a regional distribution -- 6.7.3 Generalised least squares regression -- 6.7.3.1 Estimation of index parameter by combining regional and site-specific data -- 6.7.4 Delineation of homogeneous regions -- 6.7.5 Self-guided tour: Regional frequency analysis -- 6.8 Severity-area-frequency curves -- 6.9 Summary -- 6.10 Further reading -- References -- bksec2_24 -- 7 - Statistical analysis of drought series∗ -- 7.1 Introduction -- 7.2 Time-series modelling -- 7.2.1 A simple Gaussian random model -- 7.2.2 Theory of runs -- 7.2.3 Autoregressive modelling and simulation -- 7.2.4 An observed time series of annual discharge -- 7.2.5 Applying and expanding autoregressive models -- 7.3 Regression -- 7.3.1 Linear regression -- 7.3.2 Correlation -- 7.3.3 Multiple linear regression -- 7.3.4 Goodness of fit, calibration and understanding residuals -- 7.3.5 Variable selection -- 7.3.6 Model validation -- 7.3.7 Generalised linear models -- 7.3.7.1 Logistic regression -- 7.3.7.2 Poisson regression -- 7.3.7.3 Gamma regression -- 7.3.8 A note about causality -- 7.4 Trend analysis -- 7.4.1 Linear trends -- 7.4.2 Non-parametric trend analysis -- 7.4.3 Structural change analysis -- 7.5 Spatio-temporal analysis -- 7.5.1 Grid-based correlation -- 7.5.2 Composite analysis -- 7.5.3 Principal component analysis -- 7.5.4 Cluster analysis -- 7.5.5 Canonical correlation analysis -- 7.6 Novel methods -- 7.7 Summary -- 7.8 Further reading -- References -- 8 - Regionalisation procedures - estimation at the ungauged site∗ -- 8.1 Introduction -- 8.2 Physiographic similarity -- 8.2.1 Similarity indices. , 8.2.1.1 River flow similarity.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...