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Climate change and Hydrological impact
modeling: achievements and challenges
气候变化与水资源模拟 : 进展与挑战
Dept of Geosciences, University of OsloChongyu Xu http://folk.uio.no/chongyux/
Chongyu Xu 许崇育University of Oslo
Chong-yu Xu
Lecture at
许崇育挪威奥斯陆大学
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Where can you find me?
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If you have the following problems
Too much water – flood
Too little water – drought
Pollution
Erosion
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Issues in catchment management
• Water resources management– Water supply, hydropower– Irrigation and drainage– Social, economic, environmental
• Flood management– Flood forecasting, risk analysis,
damage analyses– Planning of protective and
controlling structures (dams, dikes, gates)
– Optimization of the reservoir system (maximize the profit)
– Dam break scenarios
• Water quality management– Waste water purification & outlets– Reservoirs– Toxic and harmful releases– Eutrophication
• Watershed erosion management– Agricultural & forestry practices– Ecosystem conservation
• Sediment management– Reservoirs,– Morphological changes– Dredging
• Land use management– Urban development,– Agriculture & forestry practices– Re-settlement– Infrastructure planning– Social, cultural, and economic
interests
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• Catchment management is to find best solution and balance between:
– Water available (quantity, quality)– Water demand (quantity, quality)– Water transportation/delivety/use efficiency– Others
• Water logging and salinization, flooding, etc.• erosion and sediment load, etc.
• Sustainable management means that the solution we made and the balance we achieved have no negative effect to our next generations.
Catchment managementhydrologic view
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Climate system:Precipitation, temperature, etc
Hydrologic system:Watershed, streams, etc
Water availability
Reservoirs: Water control
Regulatory requirements
Natural system requirements
Human requirements
Water control
Water supply & allocation
Climate model
Hydrological model
Water managementModel
Hydraulic constructions: dam, reservoirs, etc
Components of catchment management systems
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Application of hydrologic models
DESIGN OPERATION MANAGEMENT RESEARCH &TEACHING
Dams & reservoirs design water yield capacity, failure
Floods frequency mapping
Urbanization storm drains flood plains channel alterations
Irrigation & drainage water yield diversions
Water resources assessment
Land-use change
Climate change
Point nonpointPollution
Groundwater recharge
Flow forecasting
Reservoir control
Urban storm draincontrol
University training
Industrial training
Research
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• Background
– Climate will change (or has been changing) due to greenhouse effect,
– Availability and variability of regional water resources will be affected,
– GCMs have been used as the only available tool for modeling future climate evolution,
– There are gaps between GCMs ability and hydrology need.
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What a GCM looks like?
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• Inputs: Main forcings or boundary conditions:1 Solar radiation
2 Atmospheric composition
(gases, H2O, CO2, O3, and aerosols)
3 Surface characteristics (albedo, roughness,…)
Inputs and outputs of climate models
• Outputs: climatologic and hydrologic variables:1 Temperature, pressure,
wind,
2 Humidity, cloudness, precipitation,
3 Runoff, evapotranspiration, soil moisture
Accuracy
declines
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What a hydrological model looks like?
Lumped model
Semi-distributed
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What a hydrological model looks like?
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Spatial mismatch between GCM and hydrological models
Dept of Geosciences, University of OsloChongyu Xu http://folk.uio.no/chongyux/
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GCMs ability increases
Hydrological importance increases
Gaps between GCM ability and Gaps between GCM ability and hydrological demandhydrological demand
Better Simulated
WorkingVariable
mismatch
Wind speedTemperatureAir pressure
PrecipitationCloudiness
Humidity
RunoffSoil moistureEvaporation
VerticalScale
mismatch500 hPa 800 hPa
EarthSurface
SpatialScales
mismatch
Global300*300 Km
Regional50*50 Km
Local0-50 Km
TemporalScales
mismatch
Meanannual
Meanmonthly
Daily orshorter
Ability
Gaps
Less-wellSimulated
Not-wellSimulated
New models
Macro-scale hydrological
models
Statistical downscaling
Dynamic & statistical
downscaling
Bucket – SVAT
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LWBM
Routing
MLHM
CHM
CHM
Hydrologic modeling
Deltachange
Deltachange
Deltachange
Regional Climate scenario
Wat
er r
eso
urc
es s
cen
ario
s
RCM
RCM
Statistical downscaling
Dynamic downscaling
RCMDynamic downscaling
Dynamic downscaling
Hypothetic
Downscaling
Hydrological modeling under changing Hydrological modeling under changing climateclimate
Emissionscenarios
GCM
GCM
Dept of Geosciences, University of OsloChongyu Xu http://folk.uio.no/chongyux/
Signature (unit, name, etc.)Landuse Change
Assessment of climate change impact on water resources management
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• My work in modeling– Development and application of
hydrological models• Global and continental scales water
balance modeling• Catchment scale water balance
modeling• Hillslope and local scales physically
based storm-runoff modeling
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Average annual runoff in China.
Average annual runoff in Northern Europe.
Global Mean annual runoff
Example results of Global water balance model
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Example results of catchment modeling – subtropical catchments
Subtropical monsoon catchments in Southern China
Modeled actual evapotranspiration
Modeled soil moisture
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Example results of storm floods modelling
Model structure:•Fully distributed•DEM and GIS supported•Physically-based differential equations:
Overland flow - St. Venant equations Channel routing - kinematic wave and
Manning’s equation Groundwater flow - continuity equation and
Darcy’s law
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Thank you!
http://folk.uio.no/chongyux/
Dept of Geosciences, University of OsloChongyu Xu http://folk.uio.no/chongyux/
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许崇育教授简历
• 许崇育 , 博士 , 教授 . 挪威奥斯陆大学地球科学系– 主要从事的研究领域 :
• 不同气候区域和不同时空尺度的水文模型的建立和应用• 水文模型参数估计和不确定性检验方法的研究• 流域蒸发能力和区域实际蒸发计算方法的研究• 气候变化及其对水资源与水环境的影响的研究
– 获奖 , 荣誉及兼职 :• 世界气象组织杰出青年科学家奖• 中科院海外评审专家• 南京大学城市与资源系兼职教授• 武汉大学水文与水资源系兼职教授• 中科院海外杰出人才• 中国科学院北京地理资源所兼职教授• 国际水文科学杂志编委
个人网页 : http://folk.uio.no/chongyux/
奥斯陆大学