An Overview of North Slope Hydrology and Potential Response to Climate Change
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Transcript of An Overview of North Slope Hydrology and Potential Response to Climate Change
An Overview of North Slope Hydrology and Potential
Response to Climate Change
Presented by:
Amy Tidwell, PhD
Water and Environmental Research Center
University of Alaska Fairbanks
Wildlife Response to Environmental Arctic Change
(WildREACH)
17-18 November 2008
Outline
• Introduction to the Arctic hydrologic cycle
• General water balance approach
• Discussion of seasonal hydrologic features in the Arctic
• Hydrologic response to climate change
– Scenario I: Increasing air temperature
– Scenario II: Increasing air temperature with increasing precipitation
• Panel discussion
Winter Spring Summer Fall
Seasonally frozen ground
Permafrost
Rainfall (PR)
Evapotranspiration
Ps=snow, PR=rain, Es=sublimation, ET=evapotranspiration, R=surface runoff,
Ssoil=soil moisture storage, and Ssurface=surface water storage
Snow accumulation
Ssurface + Ssoil
Output
InputPRPs
(PS + PR) - (ES + ET) - R = ∆ (Ssurface + Ssoil)
Water Balance:
Es ET
Sublimation (Es) Sublimation
SnowSnow (Ps)
Water Balance Terms
12.0 11.5 9.5
24.1 26.2
8.5
17.8 14.0
6.1
8.05.7
7.4
10.0 17.9
3.4
0
10
20
30
40
50
60
70
80
Imnavait Upper Kuparuk Putuligayuk
(1985-2003) (1996-2002) (1999-2007)
Basin
Ave
rag
e D
epth
(cm
)
Storage Change
Summer Runoff
Snow Runoff
ET
Rainfall
SWE
Water Balance Terms for Selected Arctic Basins
Data sources: Kane et al., 2000; Kane et al., 2004;
Kane et al., 2008.
Map from WERC/UAF
Water Balance Terms
0%
10%
20%
30%
40%
50%
60%
70%
80%
90%
100%
Imnavait Upper Kuparuk Putuligayuk
(1985-2003) (1996-2002) (1999-2007)
Basin
Ave
rag
e D
epth
(cm
)
Storage Change
Summer Runoff
Snow Runoff
ET
Rainfall
SWE
Winter Spring Summer Fall
Seasonally frozen ground
Permafrost
Ps=snow, PR=rain, Es=sublimation, ET=evapotranspiration, R=surface runoff,
Ssoil=soil moisture storage, and Ssurface=surface water storage
Snow accumulation
Ssurface + Ssoil
Output
InputPRPs
(PS + PR) - (ES + ET) - R = ∆ (Ssurface + Ssoil)
Water Balance:
Es ETA
IDC
B
G
F
H
JE
Act
ive
La
yer
Th
ickn
ess
Rainfall (PR)
EvapotranspirationSublimation (Es) Sublimation
SnowSnow (Ps)
Imnavait Creek
Drainage Area = 2.2 km2
0
0.5
1
1.5
2
2.5
3
3.5
4
14-Apr 13-Jun 12-Aug 11-Oct
Dis
char
ge
(m3/
s)
2001 Discharge;SWE=14.2 cm;Psumm=20.4 cm
2002 Discharge;SWE=12.6 cm;Psumm=30.3 cm
Upper Kuparuk River at Dalton Highway
Drainage Area = 142 km2
0
20
40
60
80
100
120
140
14-Apr 13-Jun 12-Aug 11-Oct
Dis
char
ge
(m3/
s)
2001 Discharge;SWE=11.7 cm;Psumm=22.2 cm
2002 Discharge;SWE=10.5 cm;Psumm=29.4 cm
Putuligayuk River at Spine Road
Drainage Area = 471 km2
0
10
20
30
40
50
60
70
80
14-Apr 13-Jun 12-Aug 11-Oct
Dis
char
ge
(m3/
s)
2001 Discharge;SWE=8.4 cm;Psumm=7.5 cm
2002 Discharge;SWE=9.4 cm;Psumm=13.7 cm
Hydrographs for Selected Basins
and Years
Kane, D.L. and Hinzman, L.D., 2008. Climate data from the
North Slope Hydrology Research project. University of Alaska
Fairbanks, Water and Environmental Research Center. URL:
http://www.uaf.edu/water/projects/NorthSlope/. Fairbanks,
Alaska, variously paged. November, 2008.
Winter Spring Summer Fall
Seasonally frozen ground
Permafrost
Snow accumulation
Ssurface + Ssoil
Output
InputA
IDC
B
G
F
H
JE
Es ET
PRPs
Act
ive
La
yer
Th
ickn
ess
Rainfall (PR)
EvapotranspirationSublimation (Es) Sublimation
SnowSnow (Ps)
Winter Spring Summer Fall
Seasonally frozen ground
Permafrost
↓ Winter energy flux from ground to atmosphere
Enhanced active layer development
↑ Soil storage capacity (settlement?)
Geomorphic and vegetation changes
↑ Temperature only
↑ Summer energy flux from atmosphere to ground
↑ Potential for mid-winter melt and ice in snow
↑ Evapotranspiration
↓ Soil moisture (no ↑ precipitation)
Ssurface + Ssoil
Output
Input
Snow accumulation
Ps
A
IDC
B
G
F
H
JD
Es ET
PR
Act
ive
La
yer
Th
ickn
ess
Rainfall (PR)
EvapotranspirationSublimation (Es) Sublimation
SnowSnow (Ps)
Winter Spring Summer Fall
Seasonally frozen ground
Permafrost
Snow accumulation
↓ Winter energy flux from ground to atmosphere
Enhanced active layer development
↑ Soil storage capacity (settlement?)
Geomorphic and vegetation changes
↑ Temperature, ↑ Precipitation
↑ Summer energy flux from atmosphere to ground
↑ Potential for mid-winter melt and ice in snow
↑ Evapotranspiration
Soil moisture change unknown
?Ssurface + Ssoil
Output
InputA
IDC
B
G
F
H
E
Es ET
PR
Act
ive
La
yer
Th
ickn
ess
Rainfall (PR)
EvapotranspirationSublimation (Es) Sublimation
SnowSnow (Ps)
J
References
• Bowling, L.C., D.L. Kane, R.E. Gieck, and L.D. Hinzman, 2003. “The role of surface storage in a low-gradient Arctic watershed.” Water Resources Research, 39(4), 1087.
• Hinzman, L.D. and others, 2005. “Evidence and implications of recent climate change in Northern Alaska and other arctic regions.” Climatic Change, 72: 251-298.
• Kane, D.L., 1997. “The Impact of Hydrologic Perturbations on Arctic Ecosystems Induced by Climate Change.” In Global Change and Arctic Terrestrial Systems, Eds. Oechel, Callaghan, Gilmanov, Holten, Maxwell, Molau, and Sveinbjornsson.
• Kane, D.L., L.D. Hinzman, J.P. McNamara, Z. Zhang, and C.S. Benson, 2000. “An Overview of a Nested Watershed Study in Arctic Alaska.” Nordic Hydrology, 31: 245-266.
• Kane, D.L., R.E. Gieck, and L.D. Hinzman, 2008. “Water Balance for a Low-Gradient Watershed in Northern Alaska.” Proceedings, Ninth International Conference on Permafrost, Fairbanks, AK.
• Kane, D.L. and D. Yang (eds), 2004. Northern Research Basins Water Balance. International Association of Hydrological Sciences. IAHS Publication 290. Wallingford, UK, 271pp.
• McNamara, J.P., D.L. Kane, and L.D. Hinzman, 1998. “An analysis of streamflow hydrology in the Kuparuk River Basin, Arctic Alaska: a nested watershed approach.” Journal of Hydrology, 206: 39-57.
• Woo, M.K., D.L. Kane, S.K. Carey, and D. Yang, 2008. “Progress in Permafrost Hydrology in the New Millennium.” Permafrost and Periglacial Processes, 19: 237-254.
• Woo, M.K., and X.J. Guan, 2006. “Hydrological Connectivity and Seasonal Storage Change of Tundra Ponds in a Polar Oasis Environment, Canadian High Arctic.” Permafrost and Periglacial Processes, 17: 309-323.
Hydrology Panel
Doug Kane, Water and Environmental Research Center, UAF
Matthew Sturm, Cold Regions Research and Engineering Laboratory
Amy Tidwell, Water and Environmental Research Center, UAF
Larry Hinzman, International Arctic Research Center, UAF
Anna Liljedahl, International Arctic Research Center, UAF