Jakob Larson - Summer Research - 2015

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Model Inputs (Outflows) *(P + Previous Year’s Storage) – ET = ΔS Temperature Radiation
Equation • Inputs = Outputs + (change in) S • P + Q(in) + GW(in) = E + Q(out) + GW(out) + (change in) S • P – E + Q(in) –Q(out) + GW(in) –GW(out) + (change in) S • P – ET = (change in) S Q = Discharge/Flow GW = Groundwater *At large scales, Q and GW become negligible P = Precipitation ET = Evapotranspiration S = Storage
Page 1 and 2: “Quantifying the Impact of Multi-
Page 3 and 4: 0.589 2.2 0.01 0.001 Global Water A
Page 5 and 6: http://www.ritholtz.com/blog/2014/0
Page 7 and 8: Controls On Precipitation El Nino 1
Page 9 and 10: Research Questions • If Californi
Page 11: Model Inputs (Inflows) Precipitatio
Page 16 and 17: Agricultural (and crop) Water Usage
Page 18 and 19: How Much Water Do These Crops Use?
Page 20 and 21: Calculated (weighted) Kc Values for
Page 22 and 23: Barley/Oats/Wheat Maize, grain Cott
Page 24 and 25: 700.50 600.50 500.50 Water Used (bi
Page 26 and 27: Money Saved in Irrigation If Substi
Page 28 and 29: Acknowledgements • Dr. Hillary Je
Page 30 and 31: Controls on California’s Water Su
Page 32 and 33: El Nino: A Positive Precipitation C

Jakob Larson - Summer Research - 2015

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