The document discusses developing a Groundwater Risk Index (GRI) to assess groundwater depletion risk conditions in the Middle East and North Africa region. It first summarizes conducting a regional groundwater resource assessment using groundwater storage reserves estimates and groundwater storage change data. It then outlines developing the GRI using indicators for groundwater reserves, storage change, governance, food security, and groundwater extraction costs. The GRI is computed by weighting and aggregating the normalized indicators. Results show varying degrees of risk and rank changes between countries from 2003 to 2014. A sensitivity analysis examines the robustness of results to excluding individual indicators and using different normalization schemes.
Fitting Probability Distribution Functions To Discharge Variability Of Kaduna...IJMER
International Journal of Modern Engineering Research (IJMER) is Peer reviewed, online Journal. It serves as an international archival forum of scholarly research related to engineering and science education.
Day 2 UN-ESCWA Alignment with the 10-Year Strategic Plan of UNCCD: Climate Ch...elodieperrat
Workshop on Alignment & implementation of National Action programmes with the UNCCD 10-year Strategy in the Arab Region
League of Arab States (18- 20 June 2014), Dubai - UAE
UN-ESCWA Mr Tarek Ismael
Sea level rise and storm surge tools and datasets supporting Municipal Resili...GrowSmart Maine
Why plan for growth and change, when it seems so much easier to simply react?
When there is a distinct and shared vision for your community - when residents, businesses and local government anticipate a sustainable town with cohesive and thriving neighborhoods - you have the power to conserve your beautiful natural spaces, enhance your existing downtown or Main Street, enable rural areas to be productive and prosperous, and save money through efficient use of existing infrastructure.
This is the dollars and sense of smart growth.
Success is clearly visible in Maine, from the creation of a community-built senior housing complex and health center in Fort Fairfield to conservation easements creating Forever Farms to Rockland's revitalized downtown. Communities have options. We have the power to manage our own responses to growth and change.
After all, “Planning is a process of choosing among those many options. If we do not choose to plan, then we choose to have others plan for us.” - Richard I. Winwood
And in the end, this means that our children and their children will choose to make Maine home and our economy will provide the opportunities to do so.
The Summit offers you a wonderful opportunity to be a part of the transformative change in Maine that we’ve seen these gatherings produce. We encourage you to consider the value of being actively involved in growing Maine’s economy and protecting the reasons we choose to live here.
Fitting Probability Distribution Functions To Discharge Variability Of Kaduna...IJMER
International Journal of Modern Engineering Research (IJMER) is Peer reviewed, online Journal. It serves as an international archival forum of scholarly research related to engineering and science education.
Day 2 UN-ESCWA Alignment with the 10-Year Strategic Plan of UNCCD: Climate Ch...elodieperrat
Workshop on Alignment & implementation of National Action programmes with the UNCCD 10-year Strategy in the Arab Region
League of Arab States (18- 20 June 2014), Dubai - UAE
UN-ESCWA Mr Tarek Ismael
Sea level rise and storm surge tools and datasets supporting Municipal Resili...GrowSmart Maine
Why plan for growth and change, when it seems so much easier to simply react?
When there is a distinct and shared vision for your community - when residents, businesses and local government anticipate a sustainable town with cohesive and thriving neighborhoods - you have the power to conserve your beautiful natural spaces, enhance your existing downtown or Main Street, enable rural areas to be productive and prosperous, and save money through efficient use of existing infrastructure.
This is the dollars and sense of smart growth.
Success is clearly visible in Maine, from the creation of a community-built senior housing complex and health center in Fort Fairfield to conservation easements creating Forever Farms to Rockland's revitalized downtown. Communities have options. We have the power to manage our own responses to growth and change.
After all, “Planning is a process of choosing among those many options. If we do not choose to plan, then we choose to have others plan for us.” - Richard I. Winwood
And in the end, this means that our children and their children will choose to make Maine home and our economy will provide the opportunities to do so.
The Summit offers you a wonderful opportunity to be a part of the transformative change in Maine that we’ve seen these gatherings produce. We encourage you to consider the value of being actively involved in growing Maine’s economy and protecting the reasons we choose to live here.
Application of GIS and MODFLOW to Ground Water Hydrology- A ReviewIJERA Editor
Groundwater is one of the most valuable natural resources, which supports human health, economic
development and ecological diversity. Due to over exploitation, the ground water systems are affected and
require management to maintain the conditions of ground water resources within acceptable limits. With the
development of computers and advances in information technology, efficient techniques for water management
has evolved. The main intent of the paper is to present a comprehensive review on application of GIS
(Geographic Information System) followed by coupling with MODFLOW package for ground water
management and development. Two major areas are discussed stating GIS applications in ground water
hydrology. (i) GIS based subsurface flow and pollution modelling (ii) Selection of artificial recharge sites.
Although the use of these techniques in groundwater studies has rapidly increased since last decade the sucess
rate is very limited. Based on this review , it is concluded that integation of GIS and MODFLOW have great
potential to revolutionize the monitoring and management of vital ground water resources in the future.
Floodplain Modelling Materials and MethodologyIDES Editor
A floodplain is the normally dry land area adjoining
river or stream that is inundated during flood events. The
most common reason for flooding could be overtopping of river
or stream due to heavy downfall. The floodplain carries flow
in excess of the river or stream capacity. Flood frequency and
flood water-surface elevations are the crucial components for
the evaluation of flood hazard. This paper presents the
methodology that incorporates advanced technologies for
hydrologic and hydraulic analyses that are needed to be carried
out to predict the flood water-surface elevations for any
ungaged watershed.
Monitoring and Reporting Landscape Condition on Defence Lands Richard Thackway
Defence has an obligation under Commonwealth legislation and under internal Defence policy for the long-term sustainable management of Defence land. A vital part of Defence’s commitment to environmental stewardship is the ongoing monitoring of the biophysical characteristics of the landscape, to establish limitations and the likelihood of degradation under Defence activities. The long-term biophysical management of the environment is critical to support Defence logistics, accommodation and training functions, day to day and in future. Land management actions are set out under a broad range of management constraints, which require ongoing monitoring to inform on future landscape management approaches. The application of landscape condition assessment provides a measurable threshold for land managers to make more informed decisions surrounding their land management practices, and to maintain Defence land that is fit for purpose.
Presented at the Defence and Industry Conference 2018, Hyatt Hotel, Canberra 14 February 2018. Jim Nikolareas, Richard Thackway and Chelayne Evans
International Journal of Computational Engineering Research(IJCER) is an intentional online Journal in English monthly publishing journal. This Journal publish original research work that contributes significantly to further the scientific knowledge in engineering and Technology.
Justin Hawley March, GIS Rangers
To better assess relationships within a wetland, GIS Rangers, in partnership with the Coon Creek Watershed District, has
developed a geoprocessing method that analyzes wetland functional capacity with the use of readily available inputs.
This method can be deployed in almost any environment, and examines the overall relationship between all wetland
components, rather than individual components by themselves.The method utilizes the process put forth in “A Rapid
Procedure for Assessing Wetland Functional Capacity base on Hydrogeomorphic (HGM) Classification” by Dennis W.
Magee. In this process, individual variables of the environment are analyzed and evaluated in terms of the type of
landscape they are found in.These individual variables are then assigned a value dependent not only upon the
landscape position, but upon the type of preliminary analysis being done. Preliminary analyses put forward in the HGM
method include groundwater recharge, wildlife abundance, storm water storage, and several others. Once the preliminary
analyses are performed to get separate, independent, functional valuations, the individual analyses are then easily
summed into a total functional capacity. In terms of GIS processing, the method utilizes readily-available vector files
such as the National Wetland Inventory, the NRCS Soil Survey, as well as localized data such as elevation and land use.
These vector files are evaluated and categorized into types denoted by the “Rapid Assessment Procedure.”The types are
then assigned a “Functional Value” (Generally a value between 1 and 3).With the Functional Value established, these
vector files are converted to raster format.These raster files are then “added” together with the use of raster math giving a summarized functional value for each pixel.This approach combines the benefits of scalability, portability and modularity to accomplish the evaluation of functional capacity of a given wetland, watershed, or region.
Edited presentation from the one given at the Wisconsin Land Information Association 2012 conference to be able to upload. Please feel free to contact us using the phone numbers or email addresses listed in the presentation to ask questions, discuss, or criticize.
Application of GIS and MODFLOW to Ground Water Hydrology- A ReviewIJERA Editor
Groundwater is one of the most valuable natural resources, which supports human health, economic
development and ecological diversity. Due to over exploitation, the ground water systems are affected and
require management to maintain the conditions of ground water resources within acceptable limits. With the
development of computers and advances in information technology, efficient techniques for water management
has evolved. The main intent of the paper is to present a comprehensive review on application of GIS
(Geographic Information System) followed by coupling with MODFLOW package for ground water
management and development. Two major areas are discussed stating GIS applications in ground water
hydrology. (i) GIS based subsurface flow and pollution modelling (ii) Selection of artificial recharge sites.
Although the use of these techniques in groundwater studies has rapidly increased since last decade the sucess
rate is very limited. Based on this review , it is concluded that integation of GIS and MODFLOW have great
potential to revolutionize the monitoring and management of vital ground water resources in the future.
Floodplain Modelling Materials and MethodologyIDES Editor
A floodplain is the normally dry land area adjoining
river or stream that is inundated during flood events. The
most common reason for flooding could be overtopping of river
or stream due to heavy downfall. The floodplain carries flow
in excess of the river or stream capacity. Flood frequency and
flood water-surface elevations are the crucial components for
the evaluation of flood hazard. This paper presents the
methodology that incorporates advanced technologies for
hydrologic and hydraulic analyses that are needed to be carried
out to predict the flood water-surface elevations for any
ungaged watershed.
Monitoring and Reporting Landscape Condition on Defence Lands Richard Thackway
Defence has an obligation under Commonwealth legislation and under internal Defence policy for the long-term sustainable management of Defence land. A vital part of Defence’s commitment to environmental stewardship is the ongoing monitoring of the biophysical characteristics of the landscape, to establish limitations and the likelihood of degradation under Defence activities. The long-term biophysical management of the environment is critical to support Defence logistics, accommodation and training functions, day to day and in future. Land management actions are set out under a broad range of management constraints, which require ongoing monitoring to inform on future landscape management approaches. The application of landscape condition assessment provides a measurable threshold for land managers to make more informed decisions surrounding their land management practices, and to maintain Defence land that is fit for purpose.
Presented at the Defence and Industry Conference 2018, Hyatt Hotel, Canberra 14 February 2018. Jim Nikolareas, Richard Thackway and Chelayne Evans
International Journal of Computational Engineering Research(IJCER) is an intentional online Journal in English monthly publishing journal. This Journal publish original research work that contributes significantly to further the scientific knowledge in engineering and Technology.
Justin Hawley March, GIS Rangers
To better assess relationships within a wetland, GIS Rangers, in partnership with the Coon Creek Watershed District, has
developed a geoprocessing method that analyzes wetland functional capacity with the use of readily available inputs.
This method can be deployed in almost any environment, and examines the overall relationship between all wetland
components, rather than individual components by themselves.The method utilizes the process put forth in “A Rapid
Procedure for Assessing Wetland Functional Capacity base on Hydrogeomorphic (HGM) Classification” by Dennis W.
Magee. In this process, individual variables of the environment are analyzed and evaluated in terms of the type of
landscape they are found in.These individual variables are then assigned a value dependent not only upon the
landscape position, but upon the type of preliminary analysis being done. Preliminary analyses put forward in the HGM
method include groundwater recharge, wildlife abundance, storm water storage, and several others. Once the preliminary
analyses are performed to get separate, independent, functional valuations, the individual analyses are then easily
summed into a total functional capacity. In terms of GIS processing, the method utilizes readily-available vector files
such as the National Wetland Inventory, the NRCS Soil Survey, as well as localized data such as elevation and land use.
These vector files are evaluated and categorized into types denoted by the “Rapid Assessment Procedure.”The types are
then assigned a “Functional Value” (Generally a value between 1 and 3).With the Functional Value established, these
vector files are converted to raster format.These raster files are then “added” together with the use of raster math giving a summarized functional value for each pixel.This approach combines the benefits of scalability, portability and modularity to accomplish the evaluation of functional capacity of a given wetland, watershed, or region.
Edited presentation from the one given at the Wisconsin Land Information Association 2012 conference to be able to upload. Please feel free to contact us using the phone numbers or email addresses listed in the presentation to ask questions, discuss, or criticize.
DEM-based Methods for Flood Risk Mapping at Large ScaleSalvatore Manfreda
Oral presentation given during the meeting "Valutazione e Gestione del Rischio Alluvioni – Governance del territorio e contributo del mondo scientifico" of the project "Mettiamoci in Riga"
Presented by Charlotte MacAlister, Birhanu Zemadim, Teklu Erkossa, Amare Haileslassie, Dan Fuka, Tammo Steenhuis, Solomon Seyoum, Holger Hoff, Kinde Getnet, and Nancy Johnson to the Nile Basin Development ChallengeScience and Reflection Workshop, Addis Ababa, 4-6 May 2011
Efficiency and Capability of Remote Sensing (RS) and Geographic Information ...nitinrane33
In this review paper, the potential of remote sensing (RS) and geographic information systems (GIS) for sustainable groundwater management and development is explored. Recent literature on the use of RS and GIS in groundwater resource management is analyzed, evaluating the efficiency and capability of these technologies throughout various stages of groundwater management. Challenges and limitations associated with their use are also highlighted, with potential solutions proposed to overcome them. Ultimately, the review concludes that RS and GIS are powerful tools for sustainable groundwater management and development, with significant benefits in terms of cost-effectiveness, accuracy, and time-efficiency. However, more research is needed to improve their integration in groundwater management and address current limitations. Overall, this review offers valuable insights into the potential of RS and GIS in sustainable groundwater management and development.
Similar to Dissertation Defense Powerpoint FINAL (20)
Efficiency and Capability of Remote Sensing (RS) and Geographic Information ...
Dissertation Defense Powerpoint FINAL
1. Advisor: Adam Milewski
Committee: Eugene Yan
Jeffrey Mullen
Marshall Shepherd
AN INTEGRATED ASSESSMENT OF GROUNDWATER
SCARCITYAND RISK CONDITIONS IN THE ARAB
MIDDLE EAST AND NORTH AFRICA REGION
Khalil Lezzaik
2. Groundwater Storage
Reserves
Groundwater
Storage Change Groundwater
Scarcity
Assessment
Overview
Governance
Government Effectiveness
Regulatory Quality
Rule of Law
Control of Corruption
Food
Security Affordability
Accessability
Nutritional Profile
Groundwater
Extraction
Cost
WTD Lift Energy
Energy Costs
2
The integration of current and gridded remote sensing (e.g.
GRACE) and modelled datasets, with distributed GIS
models is capable of producing accurate assessments and
characterizations of groundwater scarcity and risk conditions,
especially in data scarce regions.
3. 3
Outline
Introduction (Motivation, Research Questions, Research Objectives)
Regional Groundwater Resource Assessment
Groundwater [Depletion] Risk Index Development
Groundwater Risk Index Sensitivity Analysis
Conclusion
4. 4
Motivation
“ The next war in the Middle East will be fought over water, not politics.”
Boutros Boutros-Ghali, UN Secretary-General (1992-1996)
“ The wars of the 21st century will be fought over water…”
Ismail Serageldin, World Bank Vice President (1993-1998)
“ …people think the only place, there is potential conflict over water is the Middle East, they
are wrong, it is a problem all over the world.”
Kofi Annan, UN Secretary-General (1996-2006)
“ Whiskey is for Drinking. Water is for Fighting.”
Mark Twain
5. 5
Motivation
“ Aquifer depletion is already a significant issue facing the global population…that will be
exacerbated by climate change and population growth”
Lester Brown, Earth Policy Institute
“ Global ground water supplies, crucial for sustaining agriculture, are being depleted at an
alarming rate with dangerous security implications…
…Further declines in groundwater availability may well trigger more civil uprising and
international violent conflict in the already-water stressed region of the world”
Jay Famiglietti, NASA Scientist
7. 7
7
Research Questions
Can the development and use of distributed GIS models parametrized with current gridded
datasets, and remote sensing datasets, such as the Gravity Recovery and Climate
Experiment’s (GRACE) gravimetric datasets, provide better quantitative assessments of
groundwater resources in the MENA region than currently available assessments?
What are the drivers behind groundwater risk in arid environments such as the MENA
region? Is groundwater risk determined by either physical hydrogeological systems, social-
adaptive factors, or both?
8. 8
8
Research Objectives
Evaluating and estimating regional groundwater resources in the MENA region by
integrating modeled groundwater reserves estimates with groundwater storage changes
Developing and constructing a Groundwater Risk Index (GRI) designed for assessing and
visualizing the spatio-temporal vulnerability of MENA countries to groundwater depletion
Testing the robustness of GRI’s results by conducting a sensitivity analysis to examine the
impact of different methodological choices on GRI country performance.
9. 9
9
Outline
Introduction (Motivation, Research Questions, Research Objectives)
Regional Groundwater Resource Assessment
Groundwater [Depletion] Risk Index Development
Groundwater Risk Index Sensitivity Analysis
Conclusion
10. 10
10
Regional Groundwater Resource Assessment – Review
Results: Renewable water
resources.
Model: PCR-GLOBWB,
parameterized with climatic,
ET, soil, land cover,
topographic data.
Limitations: Does not
Account for non-renewable
groundwater resources.
“The 2 most striking regional
hydrological phenomena in
the MENA region are the
extreme scarcity of renewable
water resources and the
predominance of fossil
groundwater resources” –
Burdon et al., 1982.
12. 12
Regional Groundwater Resource Assessment – GWR (1)
12
12
Fan et al., 2013
Water Table Depth (WTD)
Laske et al., 2013
Sedimentary Thickness (SDT)
Hsat = SDT-WTD
Lithological Classification
Hartmann and Moosdorf, 2012
Effective Porosity values
McWhorter and Sunada, 1977
Assign effective
porosity values
to distributed
lithological
units (φe)
GWR =Hsat . ϕe
13. 1313
13
Regional Groundwater Resource Assessment – GWSC (2)
Δ GWS/dt = Δ TWS – Δ LSP {SM + SW + CW}
Process and Analyze
GRACE dTWS data
from JPL, CSR, and GFZ
centers.
To minimize uncertainty
an ensemble GRACE
product was used.
[Sakumura et al., 2014]
Spatio-temporal land
surface parameters (LSP)
generated by GLDAS Land
surface models, integrated
with observation and
satellite-based data.
LSP are used to isolate
dGWS from dTWS
GRACE measurements.
Δ GWS/dt: groundwater storage anomaly; Δ TWS: terrestrial water storage;
Δ LSP: land surface parameters;
SM: soil moisture; SW: snow water; CW: canopy water
14. 1414
14
Regional Groundwater Resource Assessment – Results (GWR)
GWR reserves
estimates based on
aquifer saturated
thickness and effective
porosity
Min and Max GWR
estimates, to account
for margin of error,
are a function a range
of effective porosity
values.
GW Reserves are
lowest in and around
Precambrian outcrops.
Alternatively, they are
highest in the deep
sedimentary basins of
the Saharan and
Arabian aquifer
systems
15. 1515
15
Regional Groundwater Resource Assessment – Results (GWSC)
Very clear association between
groundwater declines and
major urban and demographic
concentrations
Indications of possible
groundwater recharge in
aquifer systems categorized as
“non-renewable”:
1) GRACE/GLDAS Uncertainties
2) Diffuse recharge [Goncalves et
al. 2013]
3) Groundwater flow [Ahmed et al.,
2011]
Muscat
16. 1616
16
Regional Groundwater Resource Assessment – Results (GWSC)
Negligible changes in groundwater
reserves between 2003 and 2014
Consistent with GWSC results,
largest declines underlie urban and
demographic concentrations
Quantitatively, there is no short-term
threat to groundwater supplies.
Lezzaik, K.A., and A.M. Milewski (2015), A Quantitative Assessment of Groundwater Resources in the Middle East
and North Africa Region, Journal of Arid Environments (Submitted).
17. 1717
17
Groundwater Storage
Reserves
Groundwater
Storage Change Groundwater
Scarcity
Assessment
Governance
Government Effectiveness
Regulatory Quality
Rule of Law
Control of Corruption
Food
Security Affordability
Accessability
Nutritional Profile
Groundwater
Extraction
Cost
WTD Lift Energy
Energy Costs
18. 1818
18
Outline
Introduction (Motivation, Research Questions, Research Objectives)
Regional Groundwater Resource Assessment
Groundwater [Depletion] Risk Index Development
Groundwater Risk Index Sensitivity Analysis
Conclusion
19. 1919
19
Groundwater Risk Index (GRI) - Review
What is a Composite Index?
A multi-dimensional tool, formed from a grouping of indicators or variables that are combined
in a standardized way, intended to assess concepts are relative, dimensionless and non-
measurable in nature.
Examples:
Body Mass Index (BMI) University Ranking Human Development Index
20. 2020
20
Groundwater Risk Index – Purpose and Objective
To shift the focus of the public, policy-makers, and academics on groundwater
depletion risk and its causes, from a purely physical perspective to a more multi-
dimensional viewpoint that accounts for the role of political and socio-economic
criteria in determining environmental risks
To provide an assessment tool that addresses the limitations of existing water indices,
that primarily focus on surface water scarcity and stress assessments, and disregard
the groundwater risk assessments.
To develop a tool designed at evaluating and pinpointing hotspots that are highly
susceptible to groundwater depletion and the associated adverse effects.
21. 2121
21
Define phenomenon being
measured and selection of
variables into a
meaningful composite
indicator
Theoretical
Framework and
Component Selection
Imputation of
Missing Data
Estimation of missing
data to provide complete
datasets, using multiple
Imputation and alternate
datasets
Normalization
Render data comparable,
in a manner consistent
with theoretical
framework and data
properties
Weighting and
Aggregation
Selection of weighting
and aggregation methods,
along the lines of the
theoretical framework and
data properties
Groundwater Risk Index – Design and Development
22. 2222
22
Define phenomenon being
measured and selection of
variables into a
meaningful composite
indicator
Theoretical
Framework and
Component Selection
Imputation of
Missing Data
Estimation of missing
data to provide complete
datasets, using multiple
Imputation and alternate
datasets
Normalization
Render data comparable,
in a manner consistent
with theoretical
framework and data
properties
Weighting and
Aggregation
Selection of weighting
and aggregation methods,
along the lines of the
theoretical framework and
data properties
Groundwater Risk Index – Design and Development
GW
Reserves
Governance
Food
Security
Groundwater
Extraction
Cost
GW
Storage
Change
GRI = w1GWR + w2GWSC + w3GOV + w4FS + w5GWEC
GW
Reserves
23. Groundwater Risk Index – Governance Indicator
2323
23
Reallocation
Mechanisms
Accountability
and Corruption
Control Over
Water Rights
Groundwater
Depletion
Governance Indicators:
Freedom House
Worldwide Governance Indicators
International Country Risk Guide
Transparency International
24. Groundwater Risk Index – Governance Indicator
2424
23
Reallocation
Mechanisms
Accountability
and Corruption
Control Over
Water Rights
Groundwater
Depletion
Governance Indicators:
Freedom House
Worldwide Governance Indicators
International Country Risk Guide
Transparency International
Voice and Accountability
Government Effectiveness
Regulatory Quality
Rule of Law
Control of Corruption
GI =
1
𝑁 1
𝑁
Gov 𝐷𝑖𝑚
25. 2525
24
Groundwater Risk Index – Food Security Indicator
Affordability
(40%)
Availability
(44%)
Nutritional
Diversity
(16%)
Proxy measure of societies’ capacity to engage in external
virtual water trade.
Inverse relationship between food security and
groundwater depletion.
Reliance on virtual water trade already a reality in the
MENA Region.
Subindicators Data Sources
Affordability Gross Domestic Product per Capita (PPP, USD)
World Bank Database (http://data.worldbank.org/indicators/)
United Nations Statistical Division (http://unstats.un.org/unsd/)
Availability
Average Food Supply per Capita
(calories/day/person)
Volatility of Domestic Agricultural Production
(CV)
Food and Agriculture Organization Database
(http://faostat.fao.org/)
Nutritional Profile
Percent of energy from non-staples
Modified Shannon Entropy
Remans, Roseline, et al. "Measuring nutritional diversity of
national food supplies." Global Food Security 3.3 (2014): 174-182.
26. 2626
25
Groundwater Risk Index – GW Extraction Cost Indicator
(1)
Vdiesel/kwh:
Fuel heat * Heat Rate
Diesel amount for GW extraction:
Vdiesel/kwh * (2)
(3)
Monetize GW extraction
using country-level pump
(real) price for diesel fuel
Asymmetrical and skewed energy – water nexus: groundwater abstraction, conveyance,
and distribution is heavily reliant on fossil fuel energy resources.
Groundwater abstraction in the MENA region is one of the most energy intensive
processes.
Energy implications on water demand and consequent groundwater extraction.
27. 2727
26
Define phenomenon being
measured and selection of
variables into a
meaningful composite
indicator
Theoretical
Framework and
Component Selection
Imputation of
Missing Data
Estimation of missing
data to provide complete
datasets, using multiple
Imputation and alternate
datasets
Normalization
Render data comparable,
in a manner consistent
with theoretical
framework and data
properties
Weighting and
Aggregation
Selection of weighting
and aggregation methods,
along the lines of the
theoretical framework and
data properties
Groundwater Risk Index – Design and Development
Imputation of Missing Data:
1. using alternative datasets
2. multiple imputation
Min-Max Normalization [0, 100]:
1. ease of interpretation
2. preserves relationship between original data
Weighting and Aggregation:
1. Equal Weighting
2. Additive Arithmetic Mean (GRI = 1
𝑛
𝑤 𝑛 𝑞 𝑛)
29. 2929
28
Groundwater Risk Index – Results
Most RiskLeast Risk
Average normalized scores of final GRI results between 2003 and 2014
30. Groundwater Risk Index – Results
3030
29
Bump Graph Displaying Annual Temporal Changes in Groundwater Risk Ranking between 2003 and 2014
+ 2
+ 1
+ 1
+ 2
- 4
+ 3
- 2
+2
- 2
- 2
+ 1
+ 3
+ 1
- 3
- 2
- 1
Kuwait (R: 2 6, -4 )
Syria (R: 12 15, -3)
Varying degrees of rank change:
Jordan (R: 2 6, +3 )
Yemen (R: 12 15, +3)
Relatively stable period between 2003 and 2007, with heightened changes afterwards.
31. 3131
30
Groundwater Risk Index – Results
Average spatial variations in groundwater depletion risk in the MENA region between 2003 and 2014. Pie charts
reflect the impact of individual indicators on groundwater risk outcomes in MENA countries.
32. 3232Lezzaik, K., A. Milewski, and J. Mullen (2016), The Groundwater Risk Index: Development and Application in the Middle East and
North Africa Region, Earth-Science Reviews. 31
Groundwater Risk Index – Results
Fundamental key points:
1. Groundwater allocations are an ineffective determinant of groundwater risk conditions.
2. A combination of efficient governance and developed high income economy is the best prescription to
mitigating groundwater depletion.
3. Centrality of governance in groundwater risk determinations.
A typology of
MENA countries
based on: (1)
hydrological
systems, and (2)
political economies
33. 3333
3032
Outline
Introduction (Motivation, Research Questions, Research Objectives)
Regional Groundwater Resource Assessment
Groundwater [Depletion] Risk Index Development
Groundwater Risk Index Sensitivity Analysis
Conclusion
34. 3434
3033
Groundwater Risk Index – Sensitivity Analysis (SA)
Construction of composite indices involves stages where judgements have to be made.
Sources of Sensitivity:
1. Indicator Selection
One-Factor-at-a-time (OFAT), involves:
1. Change/remove one input variable/methodological choice, while keeping others constant,
2. Run model or function,
3. Compare resultsmodified with resultsoriginal
2. Normalization Scheme 3. Aggregation Method
GRI sensitivity assessments are based on:
∆ scorec= scoreoriginal,c – scoremodified,c
∆ rankc= rankoriginal,c – rankmodified,c
∆ scorec represents score change for country c; scoreoriginal, c represents original GRI score for country c; and scoremodified,c represents modified GRI
score for country c; ∆ rankc represents rank shift for country c; scoreoriginal, c represents original GRI rank for country c; and scoremodified,c
represents modified GRI rank for country c.
35. 3535
3034
Groundwater Risk Index – Sensitivity Analysis (SA)
Inclusion/Exclusion of individual indicators:
1. Exclusion of an individual indicator
2. Execute the composite index
3. Examine Δ in country rank and score
GRIoriginal = GWR + GWSC + GOV + FS + GWEC
GRImodified = GWR + GWSC + GOV + FS + GWEC
Run GRI using the following normalization Schemes:
Min-Max Normalization
(baseline)
𝑥𝑖 − 𝑥 𝑚𝑖𝑛
𝑥 𝑚𝑎𝑥 − 𝑥 𝑚𝑖𝑛
Standardization (z-score)
𝑥𝑖 − 𝑚𝑒𝑎𝑛
𝑠𝑡𝑑
Reference to Distance
𝑥𝑖
𝑥 𝑟𝑒𝑓
Run GRI using the following aggregation methods:
Additive Arithmetic Aggregation
(baseline)
1
𝑛
𝑞 𝑐
Multiplicative Geometric Aggregation
(𝑞 𝑐 )1/𝑛
36. 3636
3035
Groundwater Risk Index – Sensitivity Analysis
35
Sensitivity Analysis ALG EGY IRQ IPT JOR KWT LEB LIB MOR OMN QTR SDA SYR TUN UAE YMN
Subindicator
Exclusion/Inclusion
GRI excl. GWR 35 41 27 72 50 59 46 31 53 49 77 41 31 48 55 31
GRI excl. GWSC 29 32 19 74 43 63 44 24 47 42 70 32 27 41 59 22
GRI excl. GOV 35 35 31 61 39 52 48 36 47 36 58 32 37 39 48 32
GRI excl. FS 32 34 25 67 46 53 46 25 49 44 59 35 31 42 59 32
GRI excl. GWEC 37 39 28 67 46 58 45 34 42 49 66 45 37 43 63 28
Normalizati
onScheme
Min - Max 33 36 26 68 45 56 46 30 47 44 66 37 33 43 56 29
Z - Score 19 26 0 100 51 72 36 4 46 54 99 35 12 43 81 7
Indicization 23 28 0 100 57 58 36 6 51 58 91 40 12 46 88 14
Aggregation
Method
Arithmetic Mean 33 36 26 68 45 56 46 30 47 44 66 37 33 43 56 29
Geometric Mean 25 29 17 65 36 32 44 18 41 33 33 23 25 35 44 22
GRIOriginal Score 34 36 26 68 45 56 47 30 47 44 66 37 33 43 56 29
GRIOriginal Rank 12 11 16 1 7 4 6 14 5 8 2 10 13 9 3 15
GRIModified Score 30 34 20 74 46 56 44 24 47 45 69 36 28 42 61 25
GRIModified Rank 12 11 16 1 6 4 8 15 5 7 2 10 13 9 3 14
Δ GRI Score 4 2 6 -6 -1 0 3 6 0 -1 -3 1 5 0 -5 4
Δ GRI Rank 0 0 0 0 1 0 -2 -1 0 1 0 0 0 0 0 1
ALG (Algeria); EGY (Egypt); IRQ (Iraq); IPT (Israel and Palestinian Territories); JOR (Jordan); KWT (Kuwait); LEB (Lebanon); LIB (Libya); MOR (Morocco); OMN (Oman); QTR (Qatar); SDA (Saudi
Arabia); SYR (Syria); TUN (Tunisia); UAE (United Arab Emirates); YMN (Yemen).
Aggregating sources of sensitivity using arithmetic averaging displays:
1. Modified GRI values are negligibly different than original baseline values in both score and rank terms
2. The robustness of GRI and its insensitivity to the aforementioned methodological alternatives
3. Did not affect overall analysis of groundwater risk in the MENA region using typological interpretation
Lezzaik, K.A., and A.M. Milewski (2016), Sensitivity Analysis of the Groundwater Risk Index in the Middle East and
North Africa Region, Water Resources Research (Submitted).
37. Outline
Introduction (Motivation, Research Questions, Research Objectives)
Regional Groundwater Resource Assessment
Groundwater [Depletion] Risk Index Development
Groundwater Risk Index Sensitivity Analysis
Conclusion
3036
38. Conclusion
Groundwater is unevenly distributed, with 75% of the reserves occurring in deep
sedimentary basins underlying four MENA countries.
Largest declines in groundwater storage occurred along coastal areas with urban and
demographic concentrations.
Groundwater storage changes are negligible, and present no short term threat to
groundwater reserves.
Groundwater Scarcity Assessment
3037
39. Conclusion
Groundwater Risk Assessment
Groundwater endowments are consistently indeterminant of groundwater depletion
risk, unlike governance and economic factors
Groundwater risk is best mitigated by a combination of good governance and high-
income economies, that provides the capacity to select and implement different
solutions to groundwater scarcity
Overall, GRI is insensitive to alternative methodological choices, with exception to
aggregation methods.
3038
40. 3039
Conclusion
Scientific Contribution and Broader Implications
Results of our uniquely constructed groundwater scarcity assessment and
developed Groundwater Depletion Index (GRI), highlight and contribute to:
The role of global integrated datasets and GIS systems in advancing out
understanding and knowledge of groundwater systems in data scarce regions.
The shifting of discourse on water sector problems from solely the scientific
and technological sphere, to a multidisciplinary approach that formulates
groundwater issues through the integration of hydrological assessments with
non-water sectors solutions, such as governance, international trade, and
energy.
50. Groundwater Depletion Effects
The social and economic impacts of groundwater depletion are directly tied to the
environmental effects it effects:
Greater capital investments in well construction and pumping plants
Imposes economic costs on different societal sectors, especially farmers
Optimizes conflict conditions
Damage public infrastructure and private property
Generates societal instability, conflict and migration waves
51. “Annual recharge variations were also estimated and vary
between 0 and 4.40 km3 yr-1 for the period 2003-2010. These
values correspond to a recharge between 0 and 6.75 mm yr-
1…which is consistent with the expected weak and sporadic
recharge in this semi-arid environments.”
52. “Stable Isotope contents in the groundwater and springs indicate their
recharge sources to be the seasonal monsoon airmasses from the
Indian ocean and Arabian Sea”
53. “ Detailed measurements of the soil retention capacity and the inflow
to the karst yield a yearly groundwater recharge of 44 mm over the last
16 years, contributing significantly to the aquifer”
I’d like to thank everybody for attending my dissertation defense today. I especially want to thank my committee members for helping me, in their own unique capacity. I doubly want to thank my advisor, Dr. Milewski for his unconditional support and encouragement throughout my phd.
I’m here today to present and summarize the my research and output over the past 2.5 years, really an attempt to fast sprint through a marathon. Following my presentation I look forward to any available feedback and questions from the audience and committee.
To start, my dissertation is entitled Title (next Slide)
Before we delve into the details, I want to provide an overview of what was we will be going through today:
1. First, I will be evaluating regional groundwater resources in the MENA region by characterizing groundwater reserves and storage changes
2. Second, I will be assessing groundwater risk by the developing a groundwater index, that is based not just only on hydrogeologic parameters, but also on socio-economic adaptive factors, such as Governance, Food Security, and Energy.
These will be accomplished by using integrated gridded remote sensing and modelled datasets coupled with arcgis models.
I will start by examining the motivation behind my research questions and objectives,
then move on to examining the methodology and results of our regional assessment of MENA groundwater resources between 2003 and 2014,
This is followed by a look the development of the groundwater risk index or GRI and its results,
We also test the robustness of GRI by conducting a sensitivity analysis
Will conclude with a recap of my major results
To better express the motivation behind my research, I wanted to share the following statements by leading international personalities.
Read the first 2 statements.
Even mark twain, agreed with those assessments, in his own way, when he said: read slide.
Water crises are frequently connected to the depletion of groundwater aquifers, as the primary source of freshwater resources globally.
Nasa scientist Jay Famiglietti states Global ground water supplies, crucial for sustaining agriculture, are being depleted at an alarming rate with dangerous security implications…that may well trigger civil uprising and international conflict
Yet looking at the global spatial and temporal distribution of monitoring networks, especially in areas with the highest water scarcity and stress, we identify a gap between the aforementioned bleak assessments and supporting data and knowledge.
In our research, we attempt to address this gap through the use of integrated datasets and arcgis models
The research questions that I’m tackling are the following:
Paraphrase slides
The proposed research questions translate into the following objectives,
Then read the slides
I want to briefly review the state of available water assessments in the MENA region.
(Refer to image one): What you are seeing here is one of the better assessments of water resources in the MENA region that was commissioned by the world bank and performed by droogers in 2012. He basically used an advanced physically based model that quantified renewable water, basically runoff and recharge.
However, if we examine the mena region we find that it is defined by –burden quote) with 75% being groundwater of which 65 percent is non renewable skewed and unrepresentative assessments ( next slide
So in our groundwater assessment we aim at filling that gap by quantifying groundwater reserves on one hand and groundwater storage change on another
Starting with groundwater reserves storage or potential estimation requires integrating 1) aquifer saturated thickness, and effective porosity of the lithology on the other.
So how did we calculate each:
Gridded map (1-degree resolution) of aquifer saturated thickness was provided by sedimentary thickness measurement from the land surface all the wat to the Precambrian basement and then subtracting from that the depth to water table:
Sedimentary thickness estimates were derived from a global crustal thickness model (1-degree) constructed from active source experiment and published moho maps.
WTD were determined from a global water table pattern map constructed from WTD obesrvations and a groundwater model forced by modern climate, terrain, and sea level parameters.
On the other hand, effective porosity values were extracted from mcworter and sunada. Min, mean, and max effective porosity values were used to account for the natural variability in geologic paramters. Sediment grain size was also accounted for in the determing effective grain size (?). They were spatially assigned using a global lithological ma by hartmann and moosdorf
Evaluating monthly groundwater storage changes between 2003 and 2004 was performed using GRACE and GLDAS.
To those who are not familiar with those terms,
GRACE refers to the Gravity Recovery and Climate Experiment Mission. It is a gravity-based satellite that can detect changes in total water storage. It is basically two satellite flying in tandem at a constant distance of 220 km, and this distance changes as the satellite respond to changes in gravity, which are driven by changes in terrestrial water content.
Now GRACE look at lump sum, we have to isolate changes in groundwater. To do that we use GLDAS to isolate land surface parameters with a water component from the overall grace signal
And here are the results that we get:
Explain figures
In terms of regional groundwater reserves:
they ranged between 816, 000 m3 to 1.93 cubic kilometers and averaged 1.28 million km.
4 countries: Algeria, Libya, Egypt, and Saudi arabia constituted 75% of the region’s total water storage, given that they are located over the deep and prolific sedimentary basins in north sahara and the Arabian peninsula. Alternatively groundwater reserves were lowest in areas with Precambrian extrusions that suc the Arabian shield, haggar mountain range, and atlas mountians.
In term of groundwater storage change:
Explain figure
Very clear association between groundwater declines and urban and demographic concentrations with the exception of Cairo and Rabat
Potential recharge in inland continental desert stretches ranging between 2 to 12 cm over 12 years
In this figure, we compare groundwater storage changes to our first order estimates of groundwater reserves by generating a percentage change in GW reserves as a function of GRACE-derived Groundwater storage change, and we get the two following observations:
Groundwater storage changes between 2003 and 2014 are negligible and pose no threat short term threat groundwater reserves.
Consistent with previous results where the biggest changes underlie urban and demographic concentrations.
Iraq, Saudi arabia, and Oman exihibited the highest declines between 2003 and 2014
Before explaining the development behind GRI, I want to briefly explain what composite indices are: (1) primarily a tool, (2) formed of a grouping of variables that reflect different aspects of a phenomenon that is (3) relative, dimensionless, non measurable concepts.
Some examples: BMI designed to assess healthy weight on the basis of a person’s height and weight
University ranking to assess universities on the basis of publication, funding , graduate students etc…
Refer to slide
The development of an index involves the following main stages
Refer to slide
Refer to the main indicators and subindicators, and tell them you will be focusing on the selection of sub-indicators since the theoretical framework is really the heart of composite indices.
Studies conducting meta-analysis of coupled human-water systems clearly identified unregulated decentralized groundwater pumping as a major pathway to groundwater depletion. Now, unregulated groundwater pumping is driven my governance factors, primarily the lack of reallocation mechanisms, effective implementation over control of water rights and laws, and the lack of stakeholder representation of water systems.
Now, we have many different governance indicators, and we ended up choosing the world bank’s worldwide governance indicators, given that it’s the most comprehensive one that includes different perspective of governance: describe how each governance subindicator relates to drives of groundwater depletion.
Now, we have many different governance indicators, and we ended up choosing the world bank’s worldwide governance indicators, given that it’s the most comprehensive one that includes different perspective of governance: describe how each governance subindicator relates to drives of groundwater depletion.
In The MENA region, 85 to 90 % of freshwater consumption is by the agricultural sector. Consequently the capacity to import water-use products and specifically food products can contribute to a significant reduction in water demand and groundwater extraction pressures.
This indicator is grounded in John Allan’s concept of virtual water trade and is supposed to measure society's capacity to relief local freshwater resources by relying on exogenous virtual water trade.
Food security is measured in terms of affordability, availability, and nutritional profile.
Discuss the subindicators and why you didn’t include more.
Groundwater demand and extraction is not only governed by the physical availability of water but economic cost of extracting groundwater from specific depths and utilizing in other sectors.
Then refer to the bullet points and explain.
Explain process:
Model annual groundwater depths by integrating WTD model with the gw storage variations.
Calculate energy required to lift water from a specific depth
We then use diesel fuel heat content and heat rate to determine how much diesel is required per kwh
Monetize by using diesel annual country specific pump price for diesel
GRI scores range between 0 to 100 with higher values resembling lower groundwater risk and vice versa. Countries with are also ranked from 1 to 16 with 1 referring lowest risk and 16 referring to highest risk.
Countries with least risk are small high income oil exporting countries and inversely high risk countries are those with low governance scores and low incomes.
We ran GRI annually between 2003 and 2014. This graph is a bump graph shows the temporal change in ranks and performance of groundwater risk per country.
Relatively stable between 2003 and 2004, with heightened levels of rank change after that. Possible explanations could be changes in oil prices which affect the GWEC indicator, change in food prices and its effect on food security, but also political turbulence in the region after 2012 and its change.
Talk about how changes about possible explanations behind Kuwait and Syria and highlight also that changes could be of as a actual change in objective conditions or a relative change vis-a vis others.
Spatial variability is driven by the with a spatial component: GWR, GWSC, and GWEC. Consistent with the results that we have seen so far.
Explain some trends: Haggar mountain range and western Libya
The pie charts reflect the degree of influence or impact that is driving the output based on inclusive/exclusive testing (think about it).
Explain how we needed to find a systematic way to look at the results, instead of examining each country on its own.
To organize we created a typology, which is basically a classification according to certain characteristics, based in groundwater endowments on one hand and governance/income on the other. explain further.
Address key points and offer examples.