Uncertainty and Climate Variability in the Design and Operation of Water Resources Projects : Examples and Case Studies, Volume 2. Annexes

There are two common problems in flood hydrology: 1) estimate the return period for a given flood; and 2) estimate the flood for a given return period. A commonly used procedure to solve these problems is to fit a probability density function such...

Full description

Bibliographic Details
Main Authors: Rodriguez-Iturbe, Ignacio, Valdes, Juan B.
Format: Other Environmental Study
Language:English
en_US
Published: Washington, DC: World Bank 2013
Subjects:
Online Access:http://documents.worldbank.org/curated/en/2013/11/17837368/uncertainty-climate-variability-design-operation-water-resources-projects-examples-case-studies-vol-2-2-final-report
http://hdl.handle.net/10986/15814
id okr-10986-15814
recordtype oai_dc
spelling okr-10986-158142021-04-23T14:03:22Z Uncertainty and Climate Variability in the Design and Operation of Water Resources Projects : Examples and Case Studies, Volume 2. Annexes Rodriguez-Iturbe, Ignacio Valdes, Juan B. ACTUAL EVAPOTRANSPIRATION AVAILABLE WATER AVERAGE RAINFALL BASINS CALIBRATION CLASSIFICATION CLAY CLIMATE CLIMATE CHANGE CLIMATE VARIABILITY CLIMATOLOGY CONDUCTIVITY DIRECT RUNOFF DISCHARGE DROUGHT DRY YEARS ECOSYSTEMS EVAPOTRANSPIRATION FIELD CAPACITY FLOODS GEOLOGICAL SURVEY GROUND SURFACE GROUNDWATER GROUNDWATER DISCHARGE GROUNDWATER RECHARGE GROUNDWATER STORAGE GROWING SEASON HYDROLOGIC MODELS HYDROLOGY MOISTURE CONTENT POLLUTION POROSITY PRECIPITATION PRECIPITATION EVENTS RAINFALL RAINFALL INTENSITY RAINFALL RATE RECHARGE REGIONAL CLIMATE RETURN PERIOD RIVER RIVER BASIN ROOT ZONE ROOTING ZONE SAMPLE SIZE SAND SEA SEAS SNOW SOIL MOISTURE SOIL MOISTURE STORAGE STATISTICAL METHODS SURFACE RUNOFF TOPOGRAPHY VALUABLE INFORMATION VEGETATION WATER HOLDING CAPACITY WATER LEVEL WATER LEVELS WATER LOSS WATER RESOURCES WATER TABLE WATER TABLE DEPTH WETLAND WETLAND ECOSYSTEMS WETLAND VEGETATION WETLANDS There are two common problems in flood hydrology: 1) estimate the return period for a given flood; and 2) estimate the flood for a given return period. A commonly used procedure to solve these problems is to fit a probability density function such as the Gumbel, Pearson type three or the generalized extreme value distributions to the historical data. The Pearson probability distribution was named after the statistician Pearson, it is also called the three-parameter gamma distribution. The Mann-Kendall test is a non-parametric test for identifying trends in time series data. The test compares the relative magnitudes of sample data rather than the data values them. One benefit of this test is that the data need not conform to any particular distribution. The data values are evaluated as an ordered time series. Each data value is compared to all subsequent data values. There are basically two approaches to downscale coupled climate model projections: statistical and dynamic downscaling. 2013-09-25T18:45:03Z 2013-09-25T18:45:03Z 2011-11 http://documents.worldbank.org/curated/en/2013/11/17837368/uncertainty-climate-variability-design-operation-water-resources-projects-examples-case-studies-vol-2-2-final-report http://hdl.handle.net/10986/15814 English en_US CC BY 3.0 IGO http://creativecommons.org/licenses/by/3.0/igo/ World Bank Washington, DC: World Bank Economic & Sector Work :: Other Environmental Study Economic & Sector Work
repository_type Digital Repository
institution_category Foreign Institution
institution Digital Repositories
building World Bank Open Knowledge Repository
collection World Bank
language English
en_US
topic ACTUAL EVAPOTRANSPIRATION
AVAILABLE WATER
AVERAGE RAINFALL
BASINS
CALIBRATION
CLASSIFICATION
CLAY
CLIMATE
CLIMATE CHANGE
CLIMATE VARIABILITY
CLIMATOLOGY
CONDUCTIVITY
DIRECT RUNOFF
DISCHARGE
DROUGHT
DRY YEARS
ECOSYSTEMS
EVAPOTRANSPIRATION
FIELD CAPACITY
FLOODS
GEOLOGICAL SURVEY
GROUND SURFACE
GROUNDWATER
GROUNDWATER DISCHARGE
GROUNDWATER RECHARGE
GROUNDWATER STORAGE
GROWING SEASON
HYDROLOGIC MODELS
HYDROLOGY
MOISTURE CONTENT
POLLUTION
POROSITY
PRECIPITATION
PRECIPITATION EVENTS
RAINFALL
RAINFALL INTENSITY
RAINFALL RATE
RECHARGE
REGIONAL CLIMATE
RETURN PERIOD
RIVER
RIVER BASIN
ROOT ZONE
ROOTING ZONE
SAMPLE SIZE
SAND
SEA
SEAS
SNOW
SOIL MOISTURE
SOIL MOISTURE STORAGE
STATISTICAL METHODS
SURFACE RUNOFF
TOPOGRAPHY
VALUABLE INFORMATION
VEGETATION
WATER HOLDING CAPACITY
WATER LEVEL
WATER LEVELS
WATER LOSS
WATER RESOURCES
WATER TABLE
WATER TABLE DEPTH
WETLAND
WETLAND ECOSYSTEMS
WETLAND VEGETATION
WETLANDS
spellingShingle ACTUAL EVAPOTRANSPIRATION
AVAILABLE WATER
AVERAGE RAINFALL
BASINS
CALIBRATION
CLASSIFICATION
CLAY
CLIMATE
CLIMATE CHANGE
CLIMATE VARIABILITY
CLIMATOLOGY
CONDUCTIVITY
DIRECT RUNOFF
DISCHARGE
DROUGHT
DRY YEARS
ECOSYSTEMS
EVAPOTRANSPIRATION
FIELD CAPACITY
FLOODS
GEOLOGICAL SURVEY
GROUND SURFACE
GROUNDWATER
GROUNDWATER DISCHARGE
GROUNDWATER RECHARGE
GROUNDWATER STORAGE
GROWING SEASON
HYDROLOGIC MODELS
HYDROLOGY
MOISTURE CONTENT
POLLUTION
POROSITY
PRECIPITATION
PRECIPITATION EVENTS
RAINFALL
RAINFALL INTENSITY
RAINFALL RATE
RECHARGE
REGIONAL CLIMATE
RETURN PERIOD
RIVER
RIVER BASIN
ROOT ZONE
ROOTING ZONE
SAMPLE SIZE
SAND
SEA
SEAS
SNOW
SOIL MOISTURE
SOIL MOISTURE STORAGE
STATISTICAL METHODS
SURFACE RUNOFF
TOPOGRAPHY
VALUABLE INFORMATION
VEGETATION
WATER HOLDING CAPACITY
WATER LEVEL
WATER LEVELS
WATER LOSS
WATER RESOURCES
WATER TABLE
WATER TABLE DEPTH
WETLAND
WETLAND ECOSYSTEMS
WETLAND VEGETATION
WETLANDS
Rodriguez-Iturbe, Ignacio
Valdes, Juan B.
Uncertainty and Climate Variability in the Design and Operation of Water Resources Projects : Examples and Case Studies, Volume 2. Annexes
description There are two common problems in flood hydrology: 1) estimate the return period for a given flood; and 2) estimate the flood for a given return period. A commonly used procedure to solve these problems is to fit a probability density function such as the Gumbel, Pearson type three or the generalized extreme value distributions to the historical data. The Pearson probability distribution was named after the statistician Pearson, it is also called the three-parameter gamma distribution. The Mann-Kendall test is a non-parametric test for identifying trends in time series data. The test compares the relative magnitudes of sample data rather than the data values them. One benefit of this test is that the data need not conform to any particular distribution. The data values are evaluated as an ordered time series. Each data value is compared to all subsequent data values. There are basically two approaches to downscale coupled climate model projections: statistical and dynamic downscaling.
format Economic & Sector Work :: Other Environmental Study
author Rodriguez-Iturbe, Ignacio
Valdes, Juan B.
author_facet Rodriguez-Iturbe, Ignacio
Valdes, Juan B.
author_sort Rodriguez-Iturbe, Ignacio
title Uncertainty and Climate Variability in the Design and Operation of Water Resources Projects : Examples and Case Studies, Volume 2. Annexes
title_short Uncertainty and Climate Variability in the Design and Operation of Water Resources Projects : Examples and Case Studies, Volume 2. Annexes
title_full Uncertainty and Climate Variability in the Design and Operation of Water Resources Projects : Examples and Case Studies, Volume 2. Annexes
title_fullStr Uncertainty and Climate Variability in the Design and Operation of Water Resources Projects : Examples and Case Studies, Volume 2. Annexes
title_full_unstemmed Uncertainty and Climate Variability in the Design and Operation of Water Resources Projects : Examples and Case Studies, Volume 2. Annexes
title_sort uncertainty and climate variability in the design and operation of water resources projects : examples and case studies, volume 2. annexes
publisher Washington, DC: World Bank
publishDate 2013
url http://documents.worldbank.org/curated/en/2013/11/17837368/uncertainty-climate-variability-design-operation-water-resources-projects-examples-case-studies-vol-2-2-final-report
http://hdl.handle.net/10986/15814
_version_ 1764431137577369600