SWAT Hydrological Model for Assessing Climate Change Impact on Water Resources - PowerPoint PPT Presentation

1 / 24
About This Presentation
Title:

SWAT Hydrological Model for Assessing Climate Change Impact on Water Resources

Description:

SWAT Hydrological Model for Assessing Climate Change Impact on Water Resources – PowerPoint PPT presentation

Number of Views:2102
Avg rating:1.0/5.0
Slides: 25
Provided by: sand81
Category:

less

Transcript and Presenter's Notes

Title: SWAT Hydrological Model for Assessing Climate Change Impact on Water Resources


1
SWAT Hydrological Model for Assessing Climate
Change Impact on Water Resources
  • Sandhya Rao

2
SWAT (Soil and Water Assessment Tool) - Model
  • Features
  • Physically based
  • Distributed model
  • Continuous time model (long term yield model)
  • Uses readily available data
  • Used for long term impact studies

3
SWAT System and Processes Modeled
  • Weather
  • Hydrology
  • Sedimentation
  • Plant Growth
  • Nutrient Cycling
  • Pesticide Dynamics
  • Management
  • Bacteria
  • Land phase of the hydrological cycle
  • Water, sediment, pesticide loading to the main
    channel in each subbasin
  • Routing (water) phase of the hydrological cycle
  • Movement of water, sediment, pesticide loading
    through the channel network of the watershed to
    the outlet

4
SWAT Strengths
  • Upland Processes Comprehensive Hydrologic
    Balance
  • Physically-Based Inputs
  • Plant Growth Rotations, Crop Yields
  • Nutrient Cycling in Soil
  • Land Management BMP Tillage, Irrigation,
    Fertilizer, Pesticides, Grazing, Rotations,
    Subsurface Drainage, Urban-Lawn Chemicals, Street
    Sweeping
  • Channel Processes
  • Flexible Watershed Configuration
  • Water TransferIrrigation Diversions
  • Sediment Deposition/Scour
  • Nutrient/Pesticide Transport
  • Pond, Wetland and Reservoir Impacts

SWAT variable comparable to stream flow is
calculated as sum of Direct surface runoff,
Lateral flow (subsurface runoff) from soil
profile, GW flow from shallow aquifer
5
Crop Growth Simulation
  • Crop cover / vegetation cover determines
  • Transpiration (LAI)
  • Interception ? Surface runoff (soil cover)
  • Soil erosion (soil cover)
  • Additional water consumption (aET) due to
    irrigation
  • Nutrient uptake (biomass production)
  • Indirect impact on water quality due to farming
    practice (i.e. fertilization, pesticide
    application
  • a generic crop growth model, one model simulates
    many crops
  • The crops are differentiated by different
    parameter values
  • Phenological development of the crop is based on
  • daily heat unit accumulation
  • Potential biomass increase, leaf-area index
    (LAI), plant size, water use and plant-growth
    constraints due to water, temperature, aeration
    and radiation

useful for evaluating some agronomic adaptations
to climate change, such as changes in planting
dates, modifying rotations (i.e., switching
cultivars and crop species), changing irrigation
practices, and changing tillage operations
6
Application Impact of Climate Change on water
resources - India
  • Initial National Communication of India to UNFCCC
  • For Ministry of Environment and Forests
  • To quantify the impact of the climate change on
    the water resources of India, Identify Hotspots,
    Identify Adaptation Coping strategies
  • 12 river basins modelled
  • Flood and drought analyses have been performed

7
Tools Used
  • Modelling SWAT (Soil and Water Assessment Tool)
    model used - provides opportunity for scenario
    generation
  • GIS framework acts as a pre-processor for the
    distributed modelling and is also a powerful tool
    for visualization of the outputs/results in terms
    of V A

8
Data Used for Modeling
  • Digital Elevation Model 1km grid, generated
    using 1250,000 topographic map
  • Land use Global data, 12M USGS
  • Soil Global data, 15M FAO
  • Drainage 1250,000
  • Weather Data generated in transient experiments
    by the Hadley Centre for Climate Prediction
    U.K. at a resolution of 0.44 X 0.44 latitude by
    longitude grid points obtained from IITM, Pune
  • HadRM2 IS92a IPCC Scenario
  • 20 years current and 20 years GHG

9
River Basins Modeled
10
Layers
  • DEM
  • Delineated Basins
  • Landuse
  • Soil
  • Weather

11
Impact studied
  • Impact on annual water availability
  • Impact on seasonal water availability
  • Impact on inter annual water availability
  • Regional Variability of Water availability

12
Annual mean water balance for Control and GHG
climate scenarios in different river basins
13
Percent change in mean annual water balance for
Control and GHG climate scenarios
14
Trend in Precipitation, Runoff and
Evapotranspiration for Control and GHG Climate
Scenarios
  • Increase in precipitation in Mahanadi, Brahmani,
    Ganga, Godavari, and Cauvery, for the GHG
    scenario
  • the corresponding total runoff for all these
    basins has not necessarily increased
  • Cauvery and Ganga show decrease in total runoff.
    This may be due to increase in evapotranspiration
    on account of increased temperatures or variation
    in the distribution of the rainfall
  • In the remaining basins decrease in precipitation
    has been expected
  • The resultant total runoff has decreased in
    majority of the cases but for Narmada and Tapi

15
Vulnerability Assessment Drought Flood
  • Soil Moisture Index to monitor drought severity
  • focuses on the agricultural drought where
    severity implies cumulative water deficiency
  • weekly information has been derived using daily
    SWAT outputs to incorporate the spatial
    variability
  • Daily outflow discharge taken from the SWAT
    output
  • Maximum daily peak discharge has been identified
    for each year and for each sub-basin
  • analysis performed to identify those basins where
    flooding conditions may deteriorate in the GHG
    scenario
  • two vulnerable river systems Mahanadi and
    Brahmani

16
Vulnerability Assessment Procedure
  • Palmer Drought Severity Index (PDSI) widely used
    index
  • incorporates information on rainfall, land-use,
    and soil properties in a lumped manner
  • PDSI value
  • below 0.0 indicates the beginning of drought
    situation
  • A value below -3.0 as sever drought condition
  • Soil Moisture Index to monitor drought severity
    using SWAT
  • output to incorporate the spatial variability

17
Drought Analysis
  • Krishna Subbasins with maximum Monsoon Non
    monsoon events in Control GHG Scenario

18
Spatial and temporal distribution of drought
conditions
  • graduated colour depicts spatial variability of
    concurrent severity of drought, number of
    sub-basins where severe concurrent conditions
    prevailed in that year
  • size of the green dot reveals the number of
    drought weeks experienced in each sub-basin over
    the 20 years
  • Sabarmati and Mahi, sever drought conditions in
    comparison to control scenario
  • Mahanadi and Brahmani , the drought conditions
    seem to improve in the GHG scenario

19
Flood Analysis
Mahanadi River Basin
  • Annual maximum daily peak discharges for two
    sub-basins of Mahanadi and Brahmani river basins
    for Control and GHG scenarios

Brahmani River Basin
20
Spatial Distribution - Mahanadi River Basin
  • spatial distribution of annual maximum daily peak
    for 19th year as a sample year for control
    scenario
  • and 20 year bar charts for control and GHG
    scenarios for each of the sub-basins of the
    Mahanadi River

21
Key Findings
  • Under the GHG scenario the conditions may
    deteriorate in terms of severity of droughts in
    some parts of the country and enhanced intensity
    of floods in other parts
  • there is a general overall reduction in the
    quantity of the available runoff under the GHG
    scenario
  • Luni with the west flowing rivers Kutch
    Saurastra which occupies about one fourths of the
    area of Gujarat and 60 percent of the area of
    Rajasthan shall have acute physical water scarce
    conditions
  • River basins of Mahi, Pennar, Sabarmati, Krishna
    and Tapi shall face constant water scarcities and
    the water shortage conditions
  • River basins belonging to Cauvery, Ganga, and
    Narmada shall experience seasonal or regular
    water stressed conditions
  • River basins belonging to Godavari, Brahmani and
    Mahanadi shall have rare water shortages and if
    exist are only confined to few locations

22
Uncertainties
  • Uncertainties in Climate Simulation
  • Assumptions and Coarseness of the Data
  • One GCM and one IPCC scenario used
  • Landuse has been coarse
  • detailed data on the agricultural land use and
    the cropping pattern has not been used
  • Soil type and profile has also been scanty
  • Water bodies including reservoirs were not
    incorporated due to lack of data on their
    capacities and the operation rules

23
Future Improvements
  • Use HadRM3 simulation daily
  • Use more SRES scenarios
  • Incorporate man made interventions like
    reservoirs, dams etc
  • Identify hotspots with respect to drought,
    floods, incorporating socioeconomic and other
    desired parameters
  • Pilot level flood zone mapping for river basin
  • Integration of the results from water sector with
    other sectors to formulate coping strategies

24
Thank You
Write a Comment
User Comments (0)
About PowerShow.com