Hare Irrigation Project Reconstruction

CROPWAT Climate & Crop Water Requirement

A transparent reconstruction of crop-water demand for the Hare Irrigation Project using FAO CROPWAT climate procedures, modern climate and SWAT checks, and a direct comparison with the FAO-based water-demand methodology used in the original 1995 Hare design.

Purpose and method

How the Crop Water Requirement Analysis Works

Crop water requirement is estimated by first defining the atmospheric demand for water through reference evapotranspiration (ETo), then adjusting ETo for the characteristics and growth stage of each crop using the crop coefficient (Kc). Rainfall that is effectively stored in the crop root zone reduces the amount that must be supplied by irrigation. The remaining net irrigation requirement is increased to account for conveyance, field and application losses before the scheme diversion requirement is established.

1

Climate & ETo

Temperature, humidity, wind and sunshine/radiation define reference evapotranspiration.

FAO Penman–Monteith → ETo
2

Crop Coefficient

Kc varies through the initial, development, mid-season and late-season crop stages.

ETc = Kc × ETo
3

Effective Rainfall

Only the portion of rainfall that becomes available within the crop root zone is credited.

Pe = effective rainfall
4

Net Irrigation Requirement

The natural rainfall contribution is subtracted from crop evapotranspiration.

NIR = ETc − Pe
5

Gross Requirement

Losses in conveyance, distribution and field application are included to determine diversion demand.

GIR = NIR ÷ irrigation efficiency
6

Scheme Demand

Crop areas and planting calendars are combined to obtain monthly and peak scheme discharge.

Demand → canal discharge & scheduling
Climate reference

FAO CROPWAT Online Climate Data

Historic climate information for the Hare/Arba Minch area was obtained from FAO CROPWAT Online at approximately 6.03°N, 37.56°E and 1239 m elevation. The historic climatic normal refers to 1961–1990 and provides an independent reference against which the reconstructed climate and evapotranspiration analysis can be checked.

Historic annual rainfall
811 mm
FAO / CRU 1961–1990 climate normal
Historic annual ETo
1622 mm
FAO reference evapotranspiration
Location
6.03°N, 37.56°E
Elevation 1239 m
Monthly data

Monthly Climate Table

MonthRainfall
(mm/month)
Wet DaysTmin
(°C)
Tmax
(°C)
Tmean
(°C)
RH
(%)
Sunshine
(%)
Wind
(m/s)
ETo
(mm/month)
ETo
(mm/day)
Jan242.713.831.022.441.580.21.21454.7
Feb223.615.031.623.341.680.71.21425.1
Mar705.516.031.423.747.873.21.61685.4
Apr13511.316.529.923.259.463.91.31414.7
May1289.916.728.322.566.064.41.31354.4
Jun538.616.427.421.964.759.91.31234.1
Jul427.816.226.421.365.651.61.31193.8
Aug468.416.226.921.565.156.91.31274.1
Sep947.416.128.122.162.164.51.21324.4
Oct1166.815.628.622.164.464.71.21324.3
Nov605.714.029.321.658.572.41.01254.2
Dec213.413.030.121.549.782.31.01334.3
Annual81181.1—1622—

Source: FAO CROPWAT Online / AQUASTAT Climate Information Tool; historic climate normal 1961–1990, CRU CL 2.0.

Model cross-check

CROPWAT Online vs SWAT

The FAO historical climate normal and the SWAT simulation serve different purposes. The FAO value is a long-term climate reference, whereas the SWAT result represents the mean annual behaviour of the recent model simulation period. They should therefore be compared as independent checks rather than treated as observations from the same years.

ParameterFAO CROPWAT historicSWAT simulationInterpretation
Annual precipitation811 mm/yr1665.5 mm/yrDifferent climatic periods, datasets and spatial representation.
Reference ETo / PET1622 mm/yr1570.7 mm/yrClose magnitude; difference ≈ 3.2%.
Actual ET—928.9 mm/yrSWAT realized evapotranspiration.
Surface runoff—267.63 mm/yrDirect runoff contribution.
Lateral flow—250.62 mm/yrSubsurface lateral flow component.
Groundwater return flow—182.06 mm/yrBaseflow contribution to streamflow.
Important distinction. CROPWAT reports reference evapotranspiration (ETo), whereas SWAT reports potential evapotranspiration (PET) according to the PET method selected in the SWAT model. Their close annual magnitudes provide a useful consistency check, but the two variables should not be described as mathematically identical without confirming the SWAT PET method.
Historical reconstruction

Comparison with the 1995 Hare Irrigation Design

1995 ORIGINAL DESIGN

FAO 1977 / Modified Penman Approach

The original Hare report estimated irrigation demand using FAO crop-water-requirement procedures available at the time. Reference evapotranspiration was estimated with a modified Penman method, and crop evapotranspiration was obtained by applying crop coefficients through four crop-development stages.

2026 RECONSTRUCTION

FAO CROPWAT 8.0 / Penman–Monteith

The reconstruction repeats the same physical water-balance logic using modern CROPWAT procedures, updated climate information, current crop/land-use evidence and independent checks from SWAT. This allows the 1995 engineering assumptions to be tested rather than simply reproduced.

Component Hare 1995 design Current CROPWAT reconstruction Purpose of comparison
Reference ET method Modified Penman FAO Penman–Monteith in CROPWAT Check whether modern ETo magnitude and seasonality support the historical estimate.
Crop evapotranspiration ETc derived from ETo and crop coefficient Kc ETc = Kc × ETo Retain the same physical basis while updating input data.
Crop stages Initial, development, mid-season and late-season Same four-stage FAO crop-development framework Compare Kc curves, planting dates and crop calendars.
Net irrigation requirement NIR = ETc − Pe, with effective-storage considerations NIR determined from ETc and effective rainfall in CROPWAT Compare the irrigation depth actually required at field level.
1995 efficiencies Ec 80%; Ea 70%; Ef 80%; Ep = Ec × Ea × Ef Efficiency assumptions to be tested against the reconstructed system Assess how conveyance and field losses affect gross demand.
Special 1995 assumption ETc reduced by 20% because of the local humid/lake-and-tree environment Not imposed automatically; modern climate data and model outputs are used to test the assumption Determine whether the historical adjustment remains justified.
Scheme output Monthly diversion requirement and irrigation discharge Monthly CWR, NIR, GIR, peak demand and required discharge Directly compare the resulting design demand and canal capacity.
Historical note. The 1995 Hare report did not use CROPWAT 8.0. It used the FAO procedures then available, principally FAO 1977 crop-water-requirement guidance with a modified Penman ETo calculation. The present exercise is therefore a methodological reconstruction and comparison, not a rerun of an identical software model.
Comparison objective. Once the current crop runs are complete, this section will show crop-by-crop and month-by-month differences in ETo, ETc, effective rainfall, NIR, gross irrigation requirement and peak scheme discharge. The historical values will be retained as the baseline and the modern results will be presented alongside them without forcing agreement.
Figures

CROPWAT Project Image Gallery

The figures below summarize the historic climate reference, the CROPWAT–SWAT cross-check, and the crop-water-requirement workflow. Use the forward/back controls to browse, or enlarge any image for full-screen viewing.

Next analysis

Crop Water Requirement Runs

The next stage is to run the reconstructed crop pattern through CROPWAT. For each crop we will document the planting date, stage lengths, crop coefficients, rooting depth and soil parameters, then calculate crop evapotranspiration, effective rainfall and irrigation requirement.

1. Crop inputs

Crop type, planting date, Kc values, growth stages and rooting depth.

2. Rainfall & soil

Effective rainfall method, available soil water and irrigation scheduling assumptions.

3. CWR outputs

Monthly ETc, effective rainfall and net irrigation requirement for each crop.

4. Scheme demand

Gross requirement, peak demand, discharge and comparison with the canal supply limit.