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The

potential

evapotranspiration

concept

was

first

introduced

in

the

late

1940s

and

50s

by

Penman

and

it

is

defined

as

"

the

amount

of

water

transpired

in

a

given

time

by

a

short

green

crop

,

completely

shading

the

ground

,

of

uniform

height

and

with

adequate

water

status

in

the

soil

profile

".

Note

that

in

the

definition

of

potential

evapotranspiration

,

the

evapotranspiration

rate

is

not

related

to

a

specific

crop

.

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Q: What is the potential evapotranspiration ratio?
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Climate ratio is used to describe the moisture side of climate. It compares the precipitation (P) with the potential evapotranspiration (Ep) for a region. One way to do this is to express the relationship between them as a ratio using the formula: Climate ratio = P / Ep When the potential evaporation is greater than yearly precipitation, this ratio is less than 1. When precipitation is greater than evapotranspiration, the ratio is greater than 1. P: precipitation (in mm) or the amount of moisture available for evapotranspiration, evapotranspiration is the combined process of evaporation and plant respiration. Ep: potential evapotranspiration (in mm) or the amount of moisture needed for evapotranspiration. This value increases as temperature and plant life increase. The climate ratios are used to determine climate type: P/Ep: Less than 0.4: arid climate 0.4 - 0.8: semiarid climate 0.8 - 1.2: subhumid climate Greater than 1.2: humid climate Source: NOAA


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