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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
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
Outline
 Introduction (Motivation, Research Questions, Research Objectives)
 Regional Groundwater Resource Assessment
 Groundwater [Depletion] Risk Index Development
 Groundwater Risk Index Sensitivity Analysis
 Conclusion
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
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
6
6
Motivation
Global Discharge Network
Temporal Distribution
Global Water Stress
Global Water Availability
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
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
Outline
 Introduction (Motivation, Research Questions, Research Objectives)
 Regional Groundwater Resource Assessment
 Groundwater [Depletion] Risk Index Development
 Groundwater Risk Index Sensitivity Analysis
 Conclusion
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.
11
11
Regional Groundwater Resource Assessment – Methodology
1
Groundwater
Storage
Reserves
(GWR)
2
Groundwater
Storage
Changes
(GWSC)
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
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
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
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
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).
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
1818
18
Outline
 Introduction (Motivation, Research Questions, Research Objectives)
 Regional Groundwater Resource Assessment
 Groundwater [Depletion] Risk Index Development
 Groundwater Risk Index Sensitivity Analysis
 Conclusion
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
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.
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
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
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
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
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.
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.
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)
2828
27
Groundwater Risk Index – Results
2929
28
Groundwater Risk Index – Results
Most RiskLeast Risk
Average normalized scores of final GRI results between 2003 and 2014
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.
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.
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
3333
3032
Outline
 Introduction (Motivation, Research Questions, Research Objectives)
 Regional Groundwater Resource Assessment
 Groundwater [Depletion] Risk Index Development
 Groundwater Risk Index Sensitivity Analysis
 Conclusion
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.
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
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).
Outline
 Introduction (Motivation, Research Questions, Research Objectives)
 Regional Groundwater Resource Assessment
 Groundwater [Depletion] Risk Index Development
 Groundwater Risk Index Sensitivity Analysis
 Conclusion
3036
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
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
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.
Thank You
Questions?
3039
Back Up Slides
Groundwater Risk Index – Indicator Selection (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
Country
GRI original GRI excl. GWR GRI excl. GWSC GRI excl. GOV GRI excl. FS GRI excl. GWEC
Scores Rank Score Rank Score Rank Score Rank Score Rank Score Rank
Israel and PT 68.1 1 72.2 2 (-1) 73.7 1 60.8 1 67.2 1 67.2 1
Qatar 66 2 77 1 (+1) 70.2 2 58.3 2 58.8 2 66 2
UAE 56.4 3 55.1 4 (-1) 59.4 4 (-1) 48.2 4 (-1) 58.7 3 62.8 3
Kuwait 55.8 4 58.8 3 (+1) 62.6 3 (+1) 51.8 3 (+1) 53.1 4 57.7 4
Morocco 47.3 5 52.5 5 46.5 5 47.1 6 (-1) 48.7 5 42 10 (-5)
Lebanon 46.5 6 45.5 9 (-3) 44.3 6 48.2 5 (+1) 46.2 6 45.4 7 (-1)
Jordan 44.8 7 50.2 6 (+1) 43 7 39.3 7 46 7 46 6 (+1)
Oman 44.2 8 49 7 (+1) 42.2 8 36.3 10 (-2) 44.1 8 49.3 5 (+3)
Tunisia 42.5 9 48.1 8 (+1) 40.7 9 39.3 8 (+1) 41.8 9 42.9 9
Saudi Arabia 36.9 10 40.8 11 (-1) 32.4 10 31.9 15 (-5) 34.8 10 44.7 8 (+2)
Egypt 36.2 11 40.8 10 (+1) 31.5 11 35.4 12 (-1) 34.1 11 38.6 11
Algeria 33.5 12 34.6 12 28.6 12 34.7 13 (-1) 32.4 12 36.7 12
Syria 32.6 13 31 13 27.2 13 36.6 9 (+4) 30.9 14 (-1) 36.6 13
Libya 29.8 14 30.8 14 23.6 14 35.6 11 (+3) 25.4 15 (-1) 33.6 14
Yemen 28.9 15 30.6 15 21.7 15 32.2 14 (+1) 31.7 13 (+2) 27.7 15
Iraq 25.6 16 26.7 16 18.6 16 30.5 16 24.7 16 27.6 16
Groundwater Risk Index – Normalization Scheme (SA)
 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
Country
Minimum - Maximum Normalization
(GRI original)
Z -Score Standardization Indicization (divide by largest)
Score Ranking Quantile Rank Score Ranking Quantile Rank Score Ranking Quantile Rank
Israel and PT 68.1 1 75th
or higher 2.4 1 75th
or higher 47.4 1 75th
or higher
Qatar 66 2 75th
or higher 2.3 2 75th
or higher 41.6 2 75th
or higher
UAE 56.4 3 75th
or higher 1.7 3 75th
or higher 40 3 75th
or higher
Kuwait 55.8 4 75th
or higher 1.4 4 75th
or higher 20.9 4 75th
or higher
Oman 44.2 8 50th
to 74th
0.7 5 (+3) 50th
to 74th
20.3 5 (+3) 50th
to 74th
Jordan 44.8 7 50th
to 74th
0.6 6 (+1) 50th
to 74th
20.2 6 (+1) 50th
to 74th
Morocco 47.3 5 50th
to 74th
0.4 7 (-2) 50th
to 74th
16.1 7 (-2) 50th
to 74th
Lebanon 46.5 6 50th
to 74th
0.1 9 (-3) 25th to 49th 6.9 10 (-4) 25th to 49th
Tunisia 42.5 9 25th
to 49th
0.3 8 (+1) 50th to 74th 13.1 8 (+1) 50th to 74th
Saudi Arabia 36.9 10 25th
to 49th
0 10 25th
to 49th
9 9 25th
to 49th
Egypt 36.2 11 25th
to 49th
-0.3 11 25th
to 49th
1.7 11 25th
to 49th
Algeria 33.5 12 25th
to 49th
-0.6 12 25th
to 49th
-1.5 12 25th
to 49th
Syria 32.6 13 24th
or lower -0.8 13 24th
or lower -8.7 14 (-1) 24th or lower
Yemen 28.9 15 24th
or lower -1 14 (+1) 24th
or lower -7 13 (+2) 24th or lower
Libya 29.8 14 24th
or lower -1.1 15 (-1) 24th
or lower -12.4 15 (-1) 24th or lower
Iraq 25.6 16 24th
or lower -1.3 16 24th
or lower -16.3 16 24th or lower
Groundwater Risk Index – Aggregation Method (SA)
 Run GRI using the following aggregation methods:
Additive Arithmetic Aggregation
1
𝑛
𝑞 𝑐
Multiplicative Geometric Aggregation
(𝑞 𝑐 )1/𝑛
Country
Weighted Arithmetic Mean (GRIoriginal) Weighted Geometric Mean
Score Rank Quantile Rank Score Rank Quantile Rank
Israel and PT 68.1 1 75th or higher 65.2 1 75th or higher
UAE 56.4 3 75th or higher 44.3 2 (-1) 75th or higher
Qatar 66 2 75th or higher 33.2 7 (+5) 50th to 74th
Lebanon 46.5 6 50th to 74th 43.7 3 (-3) 75th or higher
Kuwait 56 4 75th or higher 32.4 9 (+5) 25th to 49th
Morocco 47.3 5 50th to 74th 40.7 4 (-1) 75th or higher
Jordan 44.8 7 50th to 74th 36.5 5 (-2) 50th to 74th
Tunisia 42.5 9 25th to 49th 34.9 6 (-3) 50th to 74th
Oman 44.2 8 50th to 74th 33.2 8 50th to 74th
Egypt 36.2 11 25th to 49th 29.4 10 (-1) 25th to 49th
Saudi Arabia 36.9 10 25th to 49th 22.5 13 (+3) 24th or lower
Algeria 33.5 12 25th to 49th 24.9 12 25th to 49th
Syria 32.6 13 24th or lower 25.3 11 (-2) 25th to 49th
Yemen 28.9 15 24th or lower 22.5 14 (-1) 24th or lower
Libya 29.8 14 24th or lower 17.6 15 (+1) 24th or lower
Iraq 25.6 16 24th or lower 17.1 16 24th or lower
Groundwater Risk Index – Sensitivity Analysis
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 34 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
Study comparison of groundwater storage capacity in the Arabian Aquifer System,
Nubian Aquifer System, and Northwestern Sahara Aquifer system.
Country WTD (meters)
WTD+GWSC
(meters)
Δ
Algeria 48.11 48.22 0.22%
Egypt 67.99 68.31 0.47%
Iraq 17.47 16.90 -3.26%
Israel 34.67 35.10 1.23%
Jordan 32.01 31.85 -0.51%
Kuwait 20.23 20.54 1.54%
Lebanon 35.77 34.89 -2.45%
Libya 47.69 47.83 0.31%
Morocco 53.36 53.98 1.16%
Oman 25.42 24.00 -5.59%
Saudi Arabia 30.53 30.79 0.85%
Syria 22.52 22.52 0.02%
Tunisia 34.89 34.77 -0.33%
United Arab Emirates 21.96 22.25 1.33%
Yemen 52.06 51.16 -1.73%
Mus
cat
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
“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.”
“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”
“ 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”
WGI Criticisms
2003
WECG Food S. Gov GWR GWSC
2004
WECG Food S. Gov GWR GWSC
2005
WECG Food S. Gov GWR GWSC
WECG - -0.03 -0.07 0.11 -0.17 WECG - -0.04 -0.08 0.11 -0.24 WECG - -0.04 -0.04 0.11 -0.18
Food S. -0.03 - 0.45 0.04 -0.03 Food S. -0.04 - 0.41 0.04 -0.10 Food S. -0.04 - 0.33 0.02 -0.06
Gov -0.07 0.45 - 0.00 -0.08 Gov -0.08 0.41 - 0.01 -0.08 Gov -0.04 0.33 - 0.01 -0.13
GWR 0.11 0.04 0.00 - 0.02 GWR 0.11 0.04 0.01 - 0.02 GWR 0.11 0.02 0.01 - 0.08
GWSC -0.17 -0.03 -0.08 0.02 - GWSC -0.24 -0.10 -0.08 0.02 - GWSC -0.18 -0.06 -0.13 0.08 -
2006
WECG Food S. Gov GWR GWSC
2007
WECG Food S. Gov GWR GWSC
2008
WECG Food S. Gov GWR GWSC
WECG - -0.06 -0.03 0.11 -0.02 WECG - -0.06 -0.03 0.10 0.02 WECG - -0.09 0.01 0.11 0.17
Food S. -0.06 - 0.28 0.02 -0.23 Food S. -0.06 - 0.33 0.00 -0.15 Food S. -0.09 - 0.35 0.00 0.01
Gov -0.03 0.28 - 0.01 -0.22 Gov -0.03 0.33 - 0.00 -0.21 Gov 0.01 0.35 - -0.01 0.05
GWR 0.11 0.02 0.01 - 0.05 GWR 0.10 0.00 0.00 - -0.01 GWR 0.11 0.00 -0.01 - -0.01
GWSC -0.02 -0.23 -0.22 0.05 - GWSC 0.02 -0.15 -0.21 -0.01 - GWSC 0.17 0.01 0.05 -0.01 -
2009
WECG Food S. Gov GWR GWSC
2010
WECG Food S. Gov GWR GWSC
2011
WECG Food S. Gov GWR GWSC
WECG - -0.06 -0.08 0.10 0.14 WECG - -0.04 -0.02 0.10 0.13 WECG - -0.04 0.00 0.09 0.15
Food S. -0.06 - 0.36 0.00 0.08 Food S. -0.04 - 0.37 -0.02 0.00 Food S. -0.04 - 0.40 -0.03 0.11
Gov -0.08 0.36 - -0.03 0.10 Gov -0.02 0.37 - -0.03 -0.06 Gov 0.00 0.40 - 0.00 0.04
GWR 0.10 0.00 -0.03 - -0.02 GWR 0.10 -0.02 -0.03 - -0.07 GWR 0.09 -0.03 0.00 - -0.04
GWSC 0.14 0.08 0.10 -0.02 - GWSC 0.13 0.00 -0.06 -0.07 - GWSC 0.15 0.11 0.04 -0.04 -
2012
WECG Food S. Gov GWR GWSC
2013
WECG Food S. Gov GWR GWSC
2014
WECG Food S. Gov GWR GWSC
WECG - 0.04 0.05 0.10 0.06 WECG - -0.02 0.10 0.10 0.04 WECG - -0.01 0.05 0.09 0.02
Food S. 0.04 - 0.28 0.00 0.13 Food S. -0.02 - 0.23 -0.01 0.17 Food S. -0.01 - 0.29 -0.01 0.20
Gov 0.05 0.28 - -0.01 0.14 Gov 0.10 0.23 - -0.01 0.16 Gov 0.05 0.29 - -0.01 0.16
GWR 0.10 0.00 -0.01 - -0.02 GWR 0.10 -0.01 -0.01 - 0.00 GWR 0.09 -0.01 -0.01 - 0.01
GWSC 0.06 0.13 0.14 -0.02 - GWSC 0.04 0.17 0.16 0.00 - GWSC 0.02 0.20 0.16 0.01 -
12 Year
Average
WECG Food S. Gov GWR GWSC
WECG - -0.04 -0.01 0.10 0.01
Food S. -0.04 - 0.34 0.00 0.01
Gov -0.01 0.34 - -0.01 -0.01
GWR 0.10 0.00 -0.01 - 0.00
GWSC 0.01 0.01 -0.01 0.00 -
Dissertation Defense Powerpoint FINAL
Dissertation Defense Powerpoint FINAL
Dissertation Defense Powerpoint FINAL

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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
  • 6. 6 6 Motivation Global Discharge Network Temporal Distribution Global Water Stress Global Water Availability
  • 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.
  • 11. 11 11 Regional Groundwater Resource Assessment – Methodology 1 Groundwater Storage Reserves (GWR) 2 Groundwater Storage Changes (GWSC)
  • 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.
  • 43. Groundwater Risk Index – Indicator Selection (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 Country GRI original GRI excl. GWR GRI excl. GWSC GRI excl. GOV GRI excl. FS GRI excl. GWEC Scores Rank Score Rank Score Rank Score Rank Score Rank Score Rank Israel and PT 68.1 1 72.2 2 (-1) 73.7 1 60.8 1 67.2 1 67.2 1 Qatar 66 2 77 1 (+1) 70.2 2 58.3 2 58.8 2 66 2 UAE 56.4 3 55.1 4 (-1) 59.4 4 (-1) 48.2 4 (-1) 58.7 3 62.8 3 Kuwait 55.8 4 58.8 3 (+1) 62.6 3 (+1) 51.8 3 (+1) 53.1 4 57.7 4 Morocco 47.3 5 52.5 5 46.5 5 47.1 6 (-1) 48.7 5 42 10 (-5) Lebanon 46.5 6 45.5 9 (-3) 44.3 6 48.2 5 (+1) 46.2 6 45.4 7 (-1) Jordan 44.8 7 50.2 6 (+1) 43 7 39.3 7 46 7 46 6 (+1) Oman 44.2 8 49 7 (+1) 42.2 8 36.3 10 (-2) 44.1 8 49.3 5 (+3) Tunisia 42.5 9 48.1 8 (+1) 40.7 9 39.3 8 (+1) 41.8 9 42.9 9 Saudi Arabia 36.9 10 40.8 11 (-1) 32.4 10 31.9 15 (-5) 34.8 10 44.7 8 (+2) Egypt 36.2 11 40.8 10 (+1) 31.5 11 35.4 12 (-1) 34.1 11 38.6 11 Algeria 33.5 12 34.6 12 28.6 12 34.7 13 (-1) 32.4 12 36.7 12 Syria 32.6 13 31 13 27.2 13 36.6 9 (+4) 30.9 14 (-1) 36.6 13 Libya 29.8 14 30.8 14 23.6 14 35.6 11 (+3) 25.4 15 (-1) 33.6 14 Yemen 28.9 15 30.6 15 21.7 15 32.2 14 (+1) 31.7 13 (+2) 27.7 15 Iraq 25.6 16 26.7 16 18.6 16 30.5 16 24.7 16 27.6 16
  • 44. Groundwater Risk Index – Normalization Scheme (SA)  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 Country Minimum - Maximum Normalization (GRI original) Z -Score Standardization Indicization (divide by largest) Score Ranking Quantile Rank Score Ranking Quantile Rank Score Ranking Quantile Rank Israel and PT 68.1 1 75th or higher 2.4 1 75th or higher 47.4 1 75th or higher Qatar 66 2 75th or higher 2.3 2 75th or higher 41.6 2 75th or higher UAE 56.4 3 75th or higher 1.7 3 75th or higher 40 3 75th or higher Kuwait 55.8 4 75th or higher 1.4 4 75th or higher 20.9 4 75th or higher Oman 44.2 8 50th to 74th 0.7 5 (+3) 50th to 74th 20.3 5 (+3) 50th to 74th Jordan 44.8 7 50th to 74th 0.6 6 (+1) 50th to 74th 20.2 6 (+1) 50th to 74th Morocco 47.3 5 50th to 74th 0.4 7 (-2) 50th to 74th 16.1 7 (-2) 50th to 74th Lebanon 46.5 6 50th to 74th 0.1 9 (-3) 25th to 49th 6.9 10 (-4) 25th to 49th Tunisia 42.5 9 25th to 49th 0.3 8 (+1) 50th to 74th 13.1 8 (+1) 50th to 74th Saudi Arabia 36.9 10 25th to 49th 0 10 25th to 49th 9 9 25th to 49th Egypt 36.2 11 25th to 49th -0.3 11 25th to 49th 1.7 11 25th to 49th Algeria 33.5 12 25th to 49th -0.6 12 25th to 49th -1.5 12 25th to 49th Syria 32.6 13 24th or lower -0.8 13 24th or lower -8.7 14 (-1) 24th or lower Yemen 28.9 15 24th or lower -1 14 (+1) 24th or lower -7 13 (+2) 24th or lower Libya 29.8 14 24th or lower -1.1 15 (-1) 24th or lower -12.4 15 (-1) 24th or lower Iraq 25.6 16 24th or lower -1.3 16 24th or lower -16.3 16 24th or lower
  • 45. Groundwater Risk Index – Aggregation Method (SA)  Run GRI using the following aggregation methods: Additive Arithmetic Aggregation 1 𝑛 𝑞 𝑐 Multiplicative Geometric Aggregation (𝑞 𝑐 )1/𝑛 Country Weighted Arithmetic Mean (GRIoriginal) Weighted Geometric Mean Score Rank Quantile Rank Score Rank Quantile Rank Israel and PT 68.1 1 75th or higher 65.2 1 75th or higher UAE 56.4 3 75th or higher 44.3 2 (-1) 75th or higher Qatar 66 2 75th or higher 33.2 7 (+5) 50th to 74th Lebanon 46.5 6 50th to 74th 43.7 3 (-3) 75th or higher Kuwait 56 4 75th or higher 32.4 9 (+5) 25th to 49th Morocco 47.3 5 50th to 74th 40.7 4 (-1) 75th or higher Jordan 44.8 7 50th to 74th 36.5 5 (-2) 50th to 74th Tunisia 42.5 9 25th to 49th 34.9 6 (-3) 50th to 74th Oman 44.2 8 50th to 74th 33.2 8 50th to 74th Egypt 36.2 11 25th to 49th 29.4 10 (-1) 25th to 49th Saudi Arabia 36.9 10 25th to 49th 22.5 13 (+3) 24th or lower Algeria 33.5 12 25th to 49th 24.9 12 25th to 49th Syria 32.6 13 24th or lower 25.3 11 (-2) 25th to 49th Yemen 28.9 15 24th or lower 22.5 14 (-1) 24th or lower Libya 29.8 14 24th or lower 17.6 15 (+1) 24th or lower Iraq 25.6 16 24th or lower 17.1 16 24th or lower
  • 46. Groundwater Risk Index – Sensitivity Analysis 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 34 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
  • 47. Study comparison of groundwater storage capacity in the Arabian Aquifer System, Nubian Aquifer System, and Northwestern Sahara Aquifer system.
  • 48. Country WTD (meters) WTD+GWSC (meters) Δ Algeria 48.11 48.22 0.22% Egypt 67.99 68.31 0.47% Iraq 17.47 16.90 -3.26% Israel 34.67 35.10 1.23% Jordan 32.01 31.85 -0.51% Kuwait 20.23 20.54 1.54% Lebanon 35.77 34.89 -2.45% Libya 47.69 47.83 0.31% Morocco 53.36 53.98 1.16% Oman 25.42 24.00 -5.59% Saudi Arabia 30.53 30.79 0.85% Syria 22.52 22.52 0.02% Tunisia 34.89 34.77 -0.33% United Arab Emirates 21.96 22.25 1.33% Yemen 52.06 51.16 -1.73%
  • 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”
  • 54.
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  • 72. 2003 WECG Food S. Gov GWR GWSC 2004 WECG Food S. Gov GWR GWSC 2005 WECG Food S. Gov GWR GWSC WECG - -0.03 -0.07 0.11 -0.17 WECG - -0.04 -0.08 0.11 -0.24 WECG - -0.04 -0.04 0.11 -0.18 Food S. -0.03 - 0.45 0.04 -0.03 Food S. -0.04 - 0.41 0.04 -0.10 Food S. -0.04 - 0.33 0.02 -0.06 Gov -0.07 0.45 - 0.00 -0.08 Gov -0.08 0.41 - 0.01 -0.08 Gov -0.04 0.33 - 0.01 -0.13 GWR 0.11 0.04 0.00 - 0.02 GWR 0.11 0.04 0.01 - 0.02 GWR 0.11 0.02 0.01 - 0.08 GWSC -0.17 -0.03 -0.08 0.02 - GWSC -0.24 -0.10 -0.08 0.02 - GWSC -0.18 -0.06 -0.13 0.08 - 2006 WECG Food S. Gov GWR GWSC 2007 WECG Food S. Gov GWR GWSC 2008 WECG Food S. Gov GWR GWSC WECG - -0.06 -0.03 0.11 -0.02 WECG - -0.06 -0.03 0.10 0.02 WECG - -0.09 0.01 0.11 0.17 Food S. -0.06 - 0.28 0.02 -0.23 Food S. -0.06 - 0.33 0.00 -0.15 Food S. -0.09 - 0.35 0.00 0.01 Gov -0.03 0.28 - 0.01 -0.22 Gov -0.03 0.33 - 0.00 -0.21 Gov 0.01 0.35 - -0.01 0.05 GWR 0.11 0.02 0.01 - 0.05 GWR 0.10 0.00 0.00 - -0.01 GWR 0.11 0.00 -0.01 - -0.01 GWSC -0.02 -0.23 -0.22 0.05 - GWSC 0.02 -0.15 -0.21 -0.01 - GWSC 0.17 0.01 0.05 -0.01 - 2009 WECG Food S. Gov GWR GWSC 2010 WECG Food S. Gov GWR GWSC 2011 WECG Food S. Gov GWR GWSC WECG - -0.06 -0.08 0.10 0.14 WECG - -0.04 -0.02 0.10 0.13 WECG - -0.04 0.00 0.09 0.15 Food S. -0.06 - 0.36 0.00 0.08 Food S. -0.04 - 0.37 -0.02 0.00 Food S. -0.04 - 0.40 -0.03 0.11 Gov -0.08 0.36 - -0.03 0.10 Gov -0.02 0.37 - -0.03 -0.06 Gov 0.00 0.40 - 0.00 0.04 GWR 0.10 0.00 -0.03 - -0.02 GWR 0.10 -0.02 -0.03 - -0.07 GWR 0.09 -0.03 0.00 - -0.04 GWSC 0.14 0.08 0.10 -0.02 - GWSC 0.13 0.00 -0.06 -0.07 - GWSC 0.15 0.11 0.04 -0.04 - 2012 WECG Food S. Gov GWR GWSC 2013 WECG Food S. Gov GWR GWSC 2014 WECG Food S. Gov GWR GWSC WECG - 0.04 0.05 0.10 0.06 WECG - -0.02 0.10 0.10 0.04 WECG - -0.01 0.05 0.09 0.02 Food S. 0.04 - 0.28 0.00 0.13 Food S. -0.02 - 0.23 -0.01 0.17 Food S. -0.01 - 0.29 -0.01 0.20 Gov 0.05 0.28 - -0.01 0.14 Gov 0.10 0.23 - -0.01 0.16 Gov 0.05 0.29 - -0.01 0.16 GWR 0.10 0.00 -0.01 - -0.02 GWR 0.10 -0.01 -0.01 - 0.00 GWR 0.09 -0.01 -0.01 - 0.01 GWSC 0.06 0.13 0.14 -0.02 - GWSC 0.04 0.17 0.16 0.00 - GWSC 0.02 0.20 0.16 0.01 - 12 Year Average WECG Food S. Gov GWR GWSC WECG - -0.04 -0.01 0.10 0.01 Food S. -0.04 - 0.34 0.00 0.01 Gov -0.01 0.34 - -0.01 -0.01 GWR 0.10 0.00 -0.01 - 0.00 GWSC 0.01 0.01 -0.01 0.00 -

Editor's Notes

  1. 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)
  2. 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.
  3. 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
  4. 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.
  5. 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
  6. 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
  7. The research questions that I’m tackling are the following: Paraphrase slides
  8. The proposed research questions translate into the following objectives, Then read the slides
  9. 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
  10. So in our groundwater assessment we aim at filling that gap by quantifying groundwater reserves on one hand and groundwater storage change on another
  11. 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
  12. 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
  13. 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.
  14. 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
  15. 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
  16. 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…
  17. Refer to slide
  18. The development of an index involves the following main stages Refer to slide
  19. 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.
  20. 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.
  21. 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.
  22. 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.
  23. 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
  24. 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.
  25. 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.
  26. 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).
  27. 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.