Variable

Unit

Formula

Tmax

˚C

Tmin

˚C

Taverage = (Tmax + Tmin)/2

˚C

Taverage

˚C

Δ

Altitude

m

γ

U2

m/s

(1 + 0.34 U2)

Δ/(Δ + γ (1 + 0.34 U2))

γ/(Δ + γ (1 + 0.34 U2))

(900/(Taverage + 273)) × U2

Vapor Pressure Deficit (VPD)

Tmax

˚C

eo (Tmax)

KPa

Tmin

˚C

eo (Tmin)

KPa

Saturation vapor pressure: es = [eo (Tmax) + (eo (Tmin)]/2

KPa

ea derived from air moisture

RHmax

%

e˚ (Tmin) × RHmax/100

KPa

RHmin

%

e˚ (Tmax) × RHmin/100

KPa

ea: average value

KPa

Saturation vapour pressure deficit (es − ea) KPa

Radiation

Latitude

Day

Ra

MJ∙m–2∙day–1

Month

N

Hour

n

Hour

n/N

if Rs is not given: Rs = (0.25 + 0.5 n/N) × Ra

MJ∙m–2∙day–1

Rso = [0.75 + 2 (altitude)/100000] × Ra

MJ∙m–2∙day–1

Rs/Rso

MJ∙m–2∙day–1

Rns = 0.77 Rs

MJ∙m–2∙day–1

Tmax

MJ∙m–2∙day–1

Δ Tmax. K4

MJ.m–2.day–1

Tmin

MJ∙m–2∙day–1

Δ Tmin. K4

MJ.m–2.day–1

(Δ Tmax, K4 + Δ Tmin. K4)/2

MJ∙m–2∙day–1

ea

KPa

(0.34 – 0.14 ea1/2)

Rs/Rso

(1.35 Rs/Rso – 0.35)

Rnl = (Δ Tmax. K4 + Δ Tmin. K4)/2 × (0.34 – 0.14 ea1/2) × (1.35 Rs/Rso – 0.35)

MJ∙m–2∙day–1

Rn = Rns – Rnl

MJ∙m–2∙day–1

Tmois

MJ∙m–2∙day–1

G

MJ∙m–2∙day–1

Tmois–1

MJ∙m–2∙day–1

G month = 0.14 (T month – T month – 1)

MJ∙m–2∙day–1

Rn – G

MJ∙m–2∙day–1

0.408 (Rn – G)

MJ∙m–2∙day–1

Reference evapotranspiration

Δ/(Δ + γ) (1 + 0.34 U2) × 0.408 (Rn – G)

mm/day

[γ/(Δ + γ) (1 + 0.34 U2)] × (900/(Taverage + 273)) × U2 × (es-ea)

mm/day

mm/day