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TRANSCRIPT
Elements of Water Security
Gordon Young President International Association of Hydrological Sciences
American Association for the Advancement of Science
Water Security in Canada
Vancouver, 17 February 2012 (evening panel discussion)
Global Precipitation changes 1990 - 2090
The Climate Moisture Index, representing
climatically-induced water variability
Elements of water security
Diverse uses of water • Human well-being – health, food security
• Economic development (energy, industry)
• Social development
• Water to sustain ecosystems
Water as a threat • Floods
• Droughts
• Pollution
Basic Human Well-
being – water for
health and food security
Ataturk dam, Euphrates River, Turkey
18
4
85
21
12
6
55
38
29
20
4
11
4
58
1
90
0
43
0
2108
0
200
400
600
800
1,000
1,200
1,400
1,600
1,800
2,000 C
am
ero
on
Nig
eria
Eth
iopia
Ke
nya
Ta
nza
nia
Ug
an
da
Bu
rkin
a F
aso
Gh
an
a
Se
ne
ga
l
Alg
eri
a
Eg
yp
t
Mo
rocco
Wo
rld
Ave
rag
e
Ele
c. co
nsu
mp
tio
n (
kW
h/y
r)/C
ap
ita
500 kWh/capita/year minimum consumption
for reasonable quality of life
Energy use per person in Africa kWh/cap/year
United States consumption – 12000kWh/capita/yr
The Energy Linkage
Social development
- The need for education
- The effects of lack of drinking water and
sanitation on education
Water for natural ecosystems
Ex
trem
e h
yd
rolo
gic
al v
ari
ab
ilit
y:
flo
od
s an
d d
rou
gh
ts
FLOODS
AND
DROUGHTS
Water as a threat: • Floods from the land
• Storm surges, tsunamis from oceans
OXYGEN STARVED ZONES
Regions of stress
Non-sustainable use
Canada – elements of water security in a land of snow and ice
• Ice-jam floods
• Global warming more pronounced in high latitudes and high altitudes
• Permafrost retreat
• Mountains as water towers of snow and ice
• The effects of shorter winters
• The effects of glacier retreat
River ice jams
Polar ice cover Sept 2001 Sept 2007
1 10 05 1 12 05 1 02 06 1 04 06 1 06 06 1 07 06
Permafrost thaw
Ice roads – the effects of early
break-up
Western Canada
Annual Precipitation Annual Snowfall
Rockies in winter
Average change (days/yr) in snow
cover duration in the second half (Feb.-Jul.) of the snow year over the period 1972-2000.
Derived from the
NOAA weekly satellite snow cover dataset
The importance of mountains as ‘Water Towers’
High inter-annual variability in precipitation
Athabasca (photo: D Latimer)
Peyto Glacier 2001
Annual Bow River (above Banff) Basin yield with glacier wastage and storage super-imposed
-100
0
100
200
300
400
500
600
700
800
900
1000
1100
1200
1300
1400
1500
1600
17001
95
2
19
54
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86
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88
19
90
19
92
yie
ld (
x10
6m
3)
1970, high wastage/yield proportion (13.2%)
Annual Bow River Yield
Annual Glacier Wastage Yield
Average yield ~ 1250
7 Highest wastage/yield
ratio years
7 Lowest flow years
Observed monthly hydrograph for Bow River above Banff 1969-1972 with modelled
wastage flow super-imposed
0
100
200
300
400
500
1969 1970 1971 1972
Mo
nth
ly Y
ield
(m
3x1
06)
Bow River Basin yield
Glacier Wastage
Thank You