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...
Main Authors: | , |
---|---|
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 |