surface water balance (2)

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Surface Water Balance Surface Water Balance (2) (2)

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Surface Water Balance (2). Review of last lecture Components of global water cycle. Ocean water Land soil moisture, rivers, snow cover, ice sheet and glaciers Sea ice Atmosphere water vapor, clouds, precipitation Water in biosphere (including human beings). Surface water balance. - PowerPoint PPT Presentation

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Page 1: Surface Water Balance (2)

Surface Water Balance (2)Surface Water Balance (2)

Page 2: Surface Water Balance (2)

Review of last lectureReview of last lectureComponents of global water cycleComponents of global water cycle

• Ocean water• Land soil moisture, rivers, snow cover, ice sheet and

glaciers• Sea ice• Atmosphere water vapor, clouds, precipitation• Water in biosphere (including human beings)

Page 3: Surface Water Balance (2)

Surface water balanceSurface water balance

dS/dt

Precipitation (P)

Evaportranspiration (E)

Runoff (Rs)

Irrigation (I)

Infiltration (Rg)

The changing rate of soil moisture S

dS/dt = P - E - Rs - Rg + I

Page 4: Surface Water Balance (2)

Evaporation from bare soil (Eb)

EvaportranspirationEvaportranspiration• Is equivalent to latent heat flux • Has four components: E = Eb + Ei + Es + TR

Evaporation from inception storage

(Ei)

Transpiration (TR)

Snow sublimation (Es)

Page 5: Surface Water Balance (2)

Reference evaportranspirationReference evaportranspiration• A large number of more or less empirical methods have

been developed over the last 50 years by numerous scientists and specialists worldwide to estimate evapotranspiration from different climatic variables. Relationships were often subject to rigorous local calibrations and proved to have limited global validity. Testing the accuracy of the methods under a new set of conditions is laborious, time-consuming and costly, and yet evapotranspiration data are frequently needed at short notice for project planning or irrigation scheduling design.

• To meet this need, the Food and Agriculture Organization (FAO) of the United Nations developed and published four methods for calculating a reference evaportranspiration: the Blaney-Criddle, radiation, modified Penman and pan evaporation methods.

Page 6: Surface Water Balance (2)

Evaluation of the four methodsEvaluation of the four methods • The Penman methods may require local

calibration of the wind function to achieve satisfactory results.

• The radiation methods show good results in humid climates where the aerodynamic term is relatively small, but performance in arid conditions is erratic and tends to underestimate evapotranspiration.

• Temperature methods remain empirical and require local calibration in order to achieve satisfactory results. A possible exception is the 1985 Hargreaves' method which has shown reasonable ETo results with a global validity.

Page 7: Surface Water Balance (2)

Evaluation of the four methods (cont)Evaluation of the four methods (cont) • Pan evapotranspiration methods clearly reflect the

shortcomings of predicting crop evapotranspiration from open water evaporation. The methods are susceptible to the microclimatic conditions under which the pans are operating and the rigour of station maintenance. Their performance proves erratic.

• The relatively accurate and consistent performance of the Penman-Monteith approach in both arid and humid climates has been indicated in many studies.

Page 8: Surface Water Balance (2)

Penman-Monteith equationPenman-Monteith equation

where Rn is the net radiation, G is the soil heat flux, (es - ea) represents the vapour pressure deficit of the air, a is the mean air density at constant pressure, cp is the specific heat of the air, represents the slope of the saturation vapour pressure temperature relationship, is the psychrometric constant, and rs and ra are the (bulk) surface and aerodynamic resistances.

Page 9: Surface Water Balance (2)

Soil moistureSoil moisture• Typically expressed as ‘volumetric soil water content’ S = Vwater / Vsoil

• Increases with depth• Complicated to measure

Root zone

Intermediate zone

Ground water

Page 10: Surface Water Balance (2)

Soil moisure regimesSoil moisure regimes

Page 11: Surface Water Balance (2)

US Soil moisture mapUS Soil moisture map

Page 12: Surface Water Balance (2)

Palmer drought severity index (PDSI)Palmer drought severity index (PDSI)• was developed by Wayne Palmer in the 1960s

and uses temperature and rainfall information in a model to determine dryness of soil moisture.

• is most effective in determining long term drought (a matter of several months) and is not as good with short-term forecasts (a matter of weeks).

• It uses a 0 as normal, and drought is shown in terms of minus numbers; for example, minus 2 is moderate drought, minus 3 is severe drought, and minus 4 is extreme drought.

Page 13: Surface Water Balance (2)

PSDI for US in August 2012PSDI for US in August 2012

Page 14: Surface Water Balance (2)

Change of PDSI in the last 100 yearsChange of PDSI in the last 100 years

Page 15: Surface Water Balance (2)

DesertificationDesertification

• Caused mainly be human activities and climate change

• Is one of the most significant global environmental problems

• About a billion people are under threat

Page 16: Surface Water Balance (2)

Global desertification vulnerabilityGlobal desertification vulnerability

Page 17: Surface Water Balance (2)

Infiltration - Darcy’s lawInfiltration - Darcy’s law• The infiltration flux

where • Y is wetting front soil suction head • h0 is the depth of ponded water above the ground surface• K is the hydraulic conductivity• L is the total depth of subsurface ground in question.

Rg

Page 18: Surface Water Balance (2)

Surface water balanceSurface water balance

dS/dt

Precipitation (P)

Evaportranspiration (E=Eb+Ei+Es+TR)

Penman-Monteith eq

Runoff (Rs)

Irrigation (I)

Infiltration (Rg Darcy’s law)

The changing rate of soil moisture S

dS/dt = P - E - Rs - Rg + I

(PDSI, desertification)