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HYDROMETEOROLOGY (LESSON 2.3A)

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HYDROMETEOROLOGY (LESSON 2.3A)

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EVAPORATION AND EVAPOTRANSPIRATION

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Grace Balahay
Grace Balahay
United States

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HYDROMETEOROLOGY (LESSON 2.3A)
 

HYDROMETEOROLOGY (LESSON 2.3A)Online version

EVAPORATION AND EVAPOTRANSPIRATION

by Grace Balahay
1

is the transferal of liquid water into a gaseous state and its diffusion into the atmosphere

Written answer

2

evaporation may be a minor component of hydrologic cycle due to little available energy

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3

abundant available energy and has a potential to become part of the water balance

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4

Evaporation is a cooling process in that the latent heat of vaporization (at about ______ of evaporated water) must be provided by the water body

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5

is a function of the differences in vapor pressure at the water surface (ew) and in the atmosphere (actual; ea)

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6

aids in removing the evaporated water vapor from the zone of evaporation and consequently creates greater scope for evaporation.

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7

is a function of the size of the water surface. For large water bodies high-speed turbulent winds are needed to cause maximum rate of evaporation

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8

is the evaporation that occurs above a body of water such as a lake, stream or the oceans.

Written answer

9

is that which occurs over the land’s surface, or would occur if the water supply were unrestricted

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10

This occurs when a soil is wet and what evaporation is able to happen occurs without a lack of water supply.

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11

is that which actually occurs (i.e., if there is not much available water it will be less than potential)

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12

are water-containing pans which are exposed to the atmosphere and the loss of water by evaporation measured in them at regular intervals.

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13

• The simplest of the three analytical methods and is also the least reliable • It involves writing the hydrological continuity equation for the lake and determining the evaporation from a knowledge or estimation of other variables • Thus, considering the daily average values for a lake, the continuity equation is written as

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14

• It is an application of the law of conservation of energy. • The energy available for evaporation is determined by considering the incoming energy, outgoing energy and energy stored in the water body over a known time interval.

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15

bases primarily on the concept of the turbulent transfer of water vapor (by eddy motion) from an evaporating surface to the atmosphere. - based on the concepts of discontinuous and continuous mixing at the air-liquid surface

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