http://www.iisc.ernet.in/
Hydrologic model with landscape dynamics for drought monitoring
http://wgbis.ces.iisc.ernet.in/energy/
1Energy and Wetlands Research Group, Centre for Ecological Sciences [CES],
2Centre for Sustainable Technologies, 3Centre for infrastructure, Sustainable Transportation and Urban Planning (CiSTUP),
Indian Institute of Science, Bangalore – 560012, India.
*Corresponding author:
cestvr@ces.iisc.ernet.in

RESULTS AND DISCUSSIONS

Figure 6 depicts the land use based on the classification of remote sensing data of 2010 and land use statistics are listed in table 3. Sharavathi river basin has a total forest cover of 33.7% followed by forest plantations (22%), and agriculture (14 %). The overall classification accuracy is 91.51% with kappa of 0.90. Figure 7 depicts sub basin wise hydro-meteorological parameters such as net rainfall, runoff, infiltration, ground water recharge, and evapotranspiration.


Figure 6: Land use 2010

Table 3: Land use 2010

Land use Area Ha Percent
Urban 2937.248 0.97%
Water 21017.41 6.91%
Agriculture 42803.92 14.07%
Open lands 3443.096 1.13%
Moist Deciduous Forest 42954.99 14.12%
Evergreen to Semi Evergreen forest 59711.55 19.62%
Scrub/Grassland 27592.47 9.07%
Acacia/Eucalyptus 41290.43 13.57%
Teak/Bamboo 25922.35 8.52%
Coconut/Arecanut 36595.8 12.03%
Dry Deciduous 0 0.00%
Total Area 304269.3


Figure7: Hydro-meteorological parameters (all units in Million litres)

The hydrological parameters together contribute to the water supply. The demand given in Figure 8 is estimated as a function of crop water, domestic and livestock water demand, and losses such as evapotranspiration. Water demand is higher in sub-basins with higher human population coupled with agriculture and horticultural activities.


Figure 8: Parameters contributing to the demand

Figure 9 illustrates the water balance in each basin considering water availability and the requirement in each basin. The coastal sub basins experiences water stress, due to higher water demand


Figure 9: Water Balance

Figure 10 groups the basins depending on the availability of water in streams as A, B, C or D. This also highlight the linkages of water availability with the land use as basins with higher cover of forests with native vegetation have water availability all 12 months or A type streams catering all demand (agriculture, domestic, horticulture and livestock), while the basins where large scale landuse changes also witness water scarcity evident from the presence of C or D type streams.


Figure 10: Flow regime

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Citation : Vinay S, Bharath S, Bharath H Aithal, and  Ramachandra T V, Hydrologic model with landscape dynamics for drought monitoring,  Joint International Workshop of ISPRS VIII/1 and WG IV/4 on Geospatial Data for Disaster and Risk Reduction, November 21-22, 2013.
* Corresponding Author :
Dr. T.V. Ramachandra
Energy & Wetlands Research Group, Centre for Ecological Sciences, Indian Institute of Science, Bangalore – 560 012, India.
Tel : +91-80-2293 3099/2293 3503 [extn - 107],      Fax : 91-80-23601428 / 23600085 / 23600683 [CES-TVR]
E-mail : cestvr@ces.iisc.ernet.in, energy@ces.iisc.ernet.in,     Web : http://wgbis.ces.iisc.ernet.in/energy, http://ces.iisc.ernet.in/grass
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