An implementation of the reservoir operations model of Garcia et al. (2016), which seeks to answer the question "what is the impact of reservoir operations policy on the reliability of water supply for a growing city?".
References
Garcia, M., Portney, K., and Islam, S. (2016). A
question driven socio-hydrological modeling process, Hydrol. Earth Syst.
Sci., 20:73-92, doi:10.5194/hess-20-73-2016.
Clone of Clone of Clone of Reservoir operations model
An implementation of the reservoir operations model of Garcia et al. (2016), which seeks to answer the question "what is the impact of reservoir operations policy on the reliability of water supply for a growing city?".
References
Garcia, M., Portney, K., and Islam, S. (2016). A
question driven socio-hydrological modeling process, Hydrol. Earth Syst.
Sci., 20:73-92, doi:10.5194/hess-20-73-2016.
Clone of Clone of Reservoir operations model
An implementation of the reservoir operations model of Garcia et al. (2016), which seeks to answer the question "what is the impact of reservoir operations policy on the reliability of water supply for a growing city?".
References
Garcia, M., Portney, K., and Islam, S. (2016). A
question driven socio-hydrological modeling process, Hydrol. Earth Syst.
Sci., 20:73-92, doi:10.5194/hess-20-73-2016.
Clone of Clone of Reservoir operations model
An implementation of the reservoir operations model of Garcia et al. (2016), which seeks to answer the question "what is the impact of reservoir operations policy on the reliability of water supply for a growing city?".
References
Garcia, M., Portney, K., and Islam, S. (2016). A
question driven socio-hydrological modeling process, Hydrol. Earth Syst.
Sci., 20:73-92, doi:10.5194/hess-20-73-2016.
Clone of Clone of Reservoir operations model
Clone of The Hydrologic Cycle
A simple reservoir model for Lake Cachuma in the Santa Ynez valley in Santa Barbara County.
Clone of Lake Cachuma Water Balance
An implementation of the reservoir operations model of Garcia et al. (2016), which seeks to answer the question "what is the impact of reservoir operations policy on the reliability of water supply for a growing city?".
References
Garcia, M., Portney, K., and Islam, S. (2016). A
question driven socio-hydrological modeling process, Hydrol. Earth Syst.
Sci., 20:73-92, doi:10.5194/hess-20-73-2016.
Clone of Clone of Reservoir operations model
An implementation of the reservoir operations model of Garcia et al. (2016), which seeks to answer the question "what is the impact of reservoir operations policy on the reliability of water supply for a growing city?".
References
Garcia, M., Portney, K., and Islam, S. (2016). A
question driven socio-hydrological modeling process, Hydrol. Earth Syst.
Sci., 20:73-92, doi:10.5194/hess-20-73-2016.
Clone of Clone of Reservoir operations model
An implementation of the reservoir operations model of Garcia et al. (2016), which seeks to answer the question "what is the impact of reservoir operations policy on the reliability of water supply for a growing city?".
References
Garcia, M., Portney, K., and Islam, S. (2016). A
question driven socio-hydrological modeling process, Hydrol. Earth Syst.
Sci., 20:73-92, doi:10.5194/hess-20-73-2016.
Clone of Clone of Reservoir operations model
An implementation of the reservoir operations model of Garcia et al. (2016), which seeks to answer the question "what is the impact of reservoir operations policy on the reliability of water supply for a growing city?".
References
Garcia, M., Portney, K., and Islam, S. (2016). A
question driven socio-hydrological modeling process, Hydrol. Earth Syst.
Sci., 20:73-92, doi:10.5194/hess-20-73-2016.
Clone of Reservoir operations model
An implementation of the reservoir operations model of Garcia et al. (2016), which seeks to answer the question "what is the impact of reservoir operations policy on the reliability of water supply for a growing city?".
References
Garcia, M., Portney, K., and Islam, S. (2016). A
question driven socio-hydrological modeling process, Hydrol. Earth Syst.
Sci., 20:73-92, doi:10.5194/hess-20-73-2016.
Clone of Clone of Reservoir operations model
An implementation of the reservoir operations model of Garcia et al. (2016), which seeks to answer the question "what is the impact of reservoir operations policy on the reliability of water supply for a growing city?".
References
Garcia, M., Portney, K., and Islam, S. (2016). A
question driven socio-hydrological modeling process, Hydrol. Earth Syst.
Sci., 20:73-92, doi:10.5194/hess-20-73-2016.
Clone of Clone of Reservoir operations model
very important
go with the flow
reservoir model
Clone of Global Hydrological Cycle
This model uses simple functions (converters, cosine) to simulate the water balance inside a reservoir.
Clone of Clone of Water balance in a reservoir
A 'leaky bucket' soil moisture model, based on Guswa et al. (2002). Rain falls as discrete events. The mean depth and frequency of rainfall events are determined by total monthly rainfall and number of rain days. A portion of the rainfall is intercepted by vegetation and evaporates before reaching the soil. The remaining rainfall (throughflow) either infiltrates the soil or, if the soil has insufficient capacity, runs off immediately. Soil water exceeding the field capacity is lost by sub-surface leakage, at a rate determined by the degree of soil saturation. Degree of soil saturation also limits rates of soil evaporation and vegetation transpiration. The partitioning between evaporation and transpiration is influenced by fractional area covered by vegetation.
Reference:
Guswa, A.J., Celia, M.A., Rodriguez-Iturbe, I. (2002) Models of soil
moisture dynamics in ecohydrology: a comparative study. Water Resources
Research 38, 5-1 - 5-15.
Soil moisture sub-model
A 'leaky bucket' soil moisture model, based on Guswa et al. (2002). Rain falls as discrete events. The mean depth and frequency of rainfall events are determined by total monthly rainfall and number of rain days. A portion of the rainfall is intercepted by vegetation and evaporates before reaching the soil. The remaining rainfall (throughflow) either infiltrates the soil or, if the soil has insufficient capacity, runs off immediately. Soil water exceeding the field capacity is lost by sub-surface leakage, at a rate determined by the degree of soil saturation. Degree of soil saturation also limits rates of soil evaporation and vegetation transpiration. The partitioning between evaporation and transpiration is influenced by fractional area covered by vegetation.
Reference:
Guswa, A.J., Celia, M.A., Rodriguez-Iturbe, I. (2002) Models of soil
moisture dynamics in ecohydrology: a comparative study. Water Resources
Research 38, 5-1 - 5-15.
Clone of Soil moisture sub-model
A 'leaky bucket' soil moisture model, based on Guswa et al. (2002). Rain falls as discrete events. The mean depth and frequency of rainfall events are determined by total monthly rainfall and number of rain days. A portion of the rainfall is intercepted by vegetation and evaporates before reaching the soil. The remaining rainfall (throughflow) either infiltrates the soil or, if the soil has insufficient capacity, runs off immediately. Soil water exceeding the field capacity is lost by sub-surface leakage, at a rate determined by the degree of soil saturation. Degree of soil saturation also limits rates of soil evaporation and vegetation transpiration. The partitioning between evaporation and transpiration is influenced by fractional area covered by vegetation.
Reference:
Guswa, A.J., Celia, M.A., Rodriguez-Iturbe, I. (2002) Models of soil
moisture dynamics in ecohydrology: a comparative study. Water Resources
Research 38, 5-1 - 5-15.
Clone of Soil moisture sub-model
A 'leaky bucket' soil moisture model, based on Guswa et al. (2002). Rain falls as discrete events. The mean depth and frequency of rainfall events are determined by total monthly rainfall and number of rain days. A portion of the rainfall is intercepted by vegetation and evaporates before reaching the soil. The remaining rainfall (throughflow) either infiltrates the soil or, if the soil has insufficient capacity, runs off immediately. Soil water exceeding the field capacity is lost by sub-surface leakage, at a rate determined by the degree of soil saturation. Degree of soil saturation also limits rates of soil evaporation and vegetation transpiration. The partitioning between evaporation and transpiration is influenced by fractional area covered by vegetation.
Reference:
Guswa, A.J., Celia, M.A., Rodriguez-Iturbe, I. (2002) Models of soil
moisture dynamics in ecohydrology: a comparative study. Water Resources
Research 38, 5-1 - 5-15.
Clone of Soil moisture sub-model
This model uses simple functions (converters, cosine) to simulate the water balance inside a reservoir.
Clone of Water balance in a reservoir
This model uses simple functions (converters, cosine) to simulate the water balance inside a reservoir.
Clone of Water balance in a reservoir
A 'leaky bucket' soil moisture model, based on Guswa et al. (2002). Rain falls as discrete events. The mean depth and frequency of rainfall events are determined by total monthly rainfall and number of rain days. A portion of the rainfall is intercepted by vegetation and evaporates before reaching the soil. The remaining rainfall (throughflow) either infiltrates the soil or, if the soil has insufficient capacity, runs off immediately. Soil water exceeding the field capacity is lost by sub-surface leakage, at a rate determined by the degree of soil saturation. Degree of soil saturation also limits rates of soil evaporation and vegetation transpiration. The partitioning between evaporation and transpiration is influenced by fractional area covered by vegetation.
Reference:
Guswa, A.J., Celia, M.A., Rodriguez-Iturbe, I. (2002) Models of soil
moisture dynamics in ecohydrology: a comparative study. Water Resources
Research 38, 5-1 - 5-15.
Clone of Soil moisture sub-model
