MODULE 1 Flashcards

1
Q

is the science that deals with the motion of liquids in relation to disciplines such as fluid mechanics and fluid dynamics.

A

HYDRAULICS

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2
Q

is the science that deals with the
occurrence, circulation and distribution of water of the earth and earth’s atmosphere.
it is concerned with the water in streams and lakes, rainfall and snowfall, snow and ice on the land and water occurring below the earth’s surface in the pores of the soil and rocks.

A

Hydrology

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3
Q

The most abundant substance on earth, the principal constituent of all living things, and a major force constantly shaping the surface of the earth.

A

Water

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4
Q

The planet earth is called as the

A

Water planet.

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5
Q

The earth’s ability to support life is facilitated by the existence of water in its three states, as it serves as a climate stabilizer by absorbing and releasing energy
during transitions between these phases.

A

WATER

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6
Q

the water transfer cycle, which
occurs continuously in nature.

This is a conceptual model of how water moves
around between the earth and atmosphere in
different states as a gas, liquid or solid.

A

Hydrologic Cycle

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7
Q

PHASES OF HYDROLOGIC CYCLE

A

Evaporation
Transpiration
Evapotranspiration
Precipitation
Infiltration
Runoff

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8
Q

the transfer of water from the surface of the earth to the atmosphere.

A

Evaporation

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9
Q

the process of water vapor being emitted by plant leaves.

A

Transpiration

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10
Q

the total evaporation.

A

Evapotranspiration

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11
Q

the result when tiny condensation particles grow too large.

A

Precipitation

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12
Q

the flow of water from the ground surface into the ground.

A

Infiltration

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13
Q

the quantity of water discharged in surface streams.

A

Runoff

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14
Q

the direct conversion from solid state to vapor state.

A

Sublimation

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15
Q

the primary form of atmospheric moisture.

A

Water Vapor

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16
Q

the transition process from the vapor state to the liquid state.

A

Condensation

17
Q

the water cycle is in balance, and the amount of precipitation falling will slowly soak into the ground and eventually reach the rivers.

A

WATER BALANCE

18
Q

The hydrological cycle is a good example-the total amount of water is the same, with virtually no water added to or lost from the cycle.

A

A CLOSED SYSTEM

19
Q

Human activities have the potential to lead to
changes in this balance which will have knock on
impacts.
Paving, compacting soils, and altering the nature of
the vegetation (including deforestation).

A

HUMAN INPUTS

20
Q

Air temperature, precipitation, soil moisture, and evapotranspiration are related through the balance of incoming and outgoing energy, in combination with water at the earth’s surface.

A

ENERGY AND WATER BALANCE

21
Q

can be established for any of earth’s surface by calculating the total precipitation input and
the total of various outputs.

A

water balance

22
Q

allows an examination of
the hydrologic cycle for any period of time.

A

water-balance approach

23
Q

a method by which we can
account for the hydrologic cycle of a specific area,
with emphasis on plants and soil moisture.

A

water balance

24
Q

defined by the general hydrologic equation, which is basically a statement of the law of conservation of mass as applied to the hydrologic cycle.

A

water balance

25
Q

WATER BALANCE EQUATION

A

∆S = I – O

where:
I = inflow
O = outflow
∆S = change in storage

26
Q

WATER BALANCE EQUATION

A

P − Q − E = dS/dt

where:
P = precipitation [mm/a-1]
Q = discharge [mm/a-1]
E = evaporation [mm/a-1]
dS/dt (∆S) = storage changes per time step [mm/a-1]

27
Q

Water balances are usually calculated for a specific
area, which is called______________ (also called as drainage basin, discharge area, precipitation area, and watershed).

A

catchment area

28
Q

defined as the area upstream from a certain point in the water course that contributes to flow when precipitation falls. The size of the catchment depends on where this point is located in the stream and its topography or altitude situation.

A

catchment

29
Q

The area of the catchment is determined by the__________________

A

water divide

30
Q

estimates the amount of water in each
component of the water cycle.

A

Water budget

31
Q

WATER BUDGET COMPONENTS
*water inflow

A
  • Precipitation
  • Surface water flow into basin
  • Imported water
  • Ground water inflow
32
Q

WATER BUDGET COMPONENTS
*Water Outflow

A
  • Evaporation
  • Evapotranspiration
  • Surface water outflow
  • Exported water
  • Ground water outflow
33
Q

WATER BUDGET COMPONENTS
*Change in Water Storage

A
  • Snow pack
  • Unsaturated soil zone
  • Streams, rivers, reservoirs
  • Aquifers