evapotranspiration III Flashcards

1
Q

what is evapotranspiration?

A

combined loss of water vapor from within the leaves of plants and evaporation of liquid water from water surfaces, bare soil and vegetative surfaces

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2
Q

what are the 5 ways we determine evapotranspiration?

A
  • lysimeter measurements
  • inflow-outflow measurements
  • micrometereological measurements (eddy covariance method)
  • study of groundwater fluctuations
  • ET equations
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3
Q

what is lysimetry?

A
  • mainly used in agricultutal environments
  • crop of interest grown under natural conditions in an isolated tank in large field of same crop
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4
Q

what are the disadvantages of lysimetry?

A

difficult and expensive to construct, requires careful operation and maintenance and primarily for research

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5
Q

what is an eddy flux tower?

A

directly measures how much CO2 or H20 vapor blows in and out of a site in wind gust (vertically)

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6
Q

what are the disadvantages of meteorological techniques to determining evapotranspiration?

A
  • expensive
  • requires air to be turbulent
  • requires flat terrain and homogenous underlying vegetation
  • when data acquisition fails, gap-filling the data is difficult
  • difficult to separate ecosystem components directly
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7
Q

what is potential evapotranspiration?

A

ET that would occur if there was an adequate soil-moisture supply at all times, takes into account local weather conditions and energy status

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8
Q

what is actual ET?

A

actual evaporation rate from any surface under prevailing conditions of moisture availability and radiative input

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9
Q

what is pan evaporation?

A

evaporation from a US Class-A evaporation pan

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10
Q

what is reference crop ET?

A

ET that would take place under strictly prescribed biologic and surface moisture conditions

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11
Q

what is the focus of the blaney-criddle method to measure ET?

A

air temperature

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12
Q

what does the FAO recommend for the Blaney-Criddle equation?

A
  • using site latitude and the literature to identify p for a given month
  • use air temperature data from an entire month
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13
Q

what is the thornthwaite model for evaluating ET?

A

uses annual heat index, mostly applicable to arid areas like central and eastern US

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14
Q

what is the Penman-Monteith model for evaluating ET?

A

considers the vegetation canopy as one isothermal leaf

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15
Q

what is the hargreaves method for evaluating ET?

A

estimates grass reference ET, uses air temperature and humidity

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16
Q

what is the Hamon equation for evaluating ET?

A

uses temperature and saturated vapor pressure

17
Q

what are the four types of equations to compute ET and an example for each?

A
  • equations using mean daily air temperature (thornthwaite)
  • equations using daily air temperature and solar radiation (jensseen Hafse)
  • equations using mean daily air temperature and humidity (Hamon)
  • complex equations (penman)
18
Q

when is P-ET negative?

A

in dry conditions