Principles and Processes of Hydrology 1 Flashcards

1
Q

What is the water balance equation?

A

(P-E) + Uk + Ui + Q + deltaS = 0

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2
Q

What are the 4 fundamental laws that form the basis of hydrology?

A
  1. Conservation of mass
  2. Newtons law of motion
  3. laws of thermodynamics
  4. Fick’s law of diffusion
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3
Q

Dimension

A

The ratio of the magnitude of the quantity (of water) to the magnitude of a standard unit of measurement.

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4
Q

Dimension of Force

A

[F] in Newton

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5
Q

Dimension of Mass

A

[M] in kilograms

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6
Q

Dimension of Length

A

[L] in meters

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7
Q

Dimension of Time

A

[T] in seconds

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8
Q

Dimension of Temperature

A

[Theta] in Kelvin

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9
Q

Integers

A

[Mâ] where a is the integer

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10
Q

How are units of Mass and units of Force related by Newtons 2nd law?

A

[F] = [M A] = [M L T^-2]

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11
Q

Dimension of Energy (what it equals)

A

[E] = [F L]

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12
Q

Dimensionless quantities

A

Quantities obtained by counting, denoted as [1]

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13
Q

Units

A

The arbitrary standards in which magnitudes of quantities are expressed.
(Expresses the ratio of the magnitude of a quantity to the magnitude of an arbitrary standard)

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14
Q

Systeme International (SI)

A

The international standard for science (the metric system)

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15
Q

The density of water

A

1000 kg/m^3

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16
Q

An equation that is dimensionally homogenous

A

An equation that is describing a physical relation that has the same dimensions on both sides of the equal sign.

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17
Q

What are the 3 modes of energy exchange?

A
  1. Latent heat
  2. Sensible heat
  3. Electromagnetic radiation
18
Q

What is an f(x) of the weight of the overlying atmosphere?

A

Pressure

19
Q

Saturation vapor pressure e^*

A

The maximum vapor pressure, the greatest amount of water that the atmosphere can hold. Can be estimated as an f(x) of temperature.

20
Q

Equation for e*

A

611 * exp(17.27*T / T- 273.3) (For a horizontal liquid surface)

21
Q

Estimate of the atmospheric pressure

A

1000 mb

22
Q

Amount of water vapor in percentage of total atmospheric volume

A

0-4%

23
Q

Range of vapor pressure in mb

A

0-40mb

24
Q

Saturation

A

Condition where air is holding as much water as possible. At maximum capacity, it precipitates. Changes with temperature and pressure.

25
Q

Absolute humidity

A

Ratio of mass H20/volume of air (in g/m^3).

26
Q

Specific humidity

A

Ratio of mass H20/mass of total air (in g/kg)

27
Q

Specific humidity mixing ratio

A

Ratio of mass H20/mass of DRY air (in g/kg)

28
Q

Relative humidity

A

A ratio measuring the percentage of saturation of actual H20 vapor/maximum H20 vapor. Changes with temperature and pressure.

29
Q

What change in temperature leads to a lower relative humidity if all else remains constant?

A

An increase in temperature

30
Q

Dew point

A

The temperature to which air must cool for condensation to occur (saturation).

31
Q

Precipitable water

A

The amount of water vapor in a column of the atmosphere extending from surface to top of atmosphere. Dimensions are [L] and it represents the depth of water that would result from the complete condensation and precipitation of all water vapor above a particular location.

32
Q

Evaporation

A

The change of state from liquid to gas

33
Q

Transpiration

A

Vapor loss form stomata in plant leaves

34
Q

Evapotranspiration

A

Net transfer (loss) of water vapor from wet surfaces and vegetation into the atmosphere.

35
Q

Vapor exchange

A

Dry air of temperature Ta lies above a horizontal water surface with the temperature Ts. Some water molecules have sufficient energy to enter the air above. The number of those molecules increases as Ts increases.

36
Q

e(a)

A

A steady state vapor pressure at specific given wind and temperature conditions. And f(x) of Ta and wind speed.

37
Q

Evaporation rate is proportional to ______

A

e*s - ea

38
Q

Controlling factors for evapotranspiration

A
  1. water
  2. energy
  3. vapor pressure
  4. wind
  5. vegetation
39
Q

If e*s > ea

A

Evaporation is occurring

40
Q

If e*s < ea

A

Water is condensing on the surface

41
Q

If e*s = ea

A

Neither condensation nor evaporation is occurring

42
Q

Latent Heat of vaporization

A

The quantity of heat energy that must be absorbed to break the hydrogen bonds when evaporation takes place. The same quantity is released when when bonds are reformed and condensation occurs.