hydrology Flashcards

(68 cards)

1
Q

are formed when
raindrops are carried
upward by thunderstorm
updrafts into extremely cold
areas of the atmosphere
and freeze.

A

Hail

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2
Q

is a liquid precipitation
falling from the sky. Rain
occurs when air rises into the
upper atmosphere and cools.
The cool temperatures cause
water vapor to condense into
water droplets, which fall
from the clouds as rain.

A

Rain

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3
Q

is like a mix of rain and snow, it starts as a snowflake but melts into raindrops as it falls through a layer of warm air

A

Sleet

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4
Q

is precipitation
that forms when water
vapor freezes. It is ice
crystals that form in the
cold clouds.

A

Snow

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5
Q

Rapid upward movement of warm
air causes short, intense rainfall,
often with thunderstorms or hail.

A

Convective Storms

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6
Q

Moist air rises over mountains, leading
to heavy rain on the windward side and
drier conditions on the leeward side

A

Orographic Storms

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7
Q

Large low-pressure systems bring
widespread, prolonged rainfall

A

Cyclonic Storms

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8
Q

Intense storms over warm oceans
produce heavy rain, strong winds, and
storm surges

A

Hurricanes or Tropical Cyclones

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9
Q

Liquid water drops

A

rain

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10
Q

ice crystals

A

snow

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11
Q

small ice pelletes

A

sleet

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12
Q

large ice balls

A

hail

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13
Q

rain that turns to ice on surface

A

freezing rain

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14
Q

light, tiny water drops

A

drizzle

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15
Q

soft ice balls formed on snowflakes

A

graupel

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16
Q

How much water
has fallen over a
period of time.

A

depth

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17
Q

Refers to the length
of time rainfall
occurs

A

duration

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18
Q

Ratio of the total
amount of rain falling
during a period of time

A

intensity

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19
Q

Graphical representation
between rainfall intensity
and time

A

hyetography

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20
Q
  • Also known as Station Rainfall
    it refers to the rainfall data of a station
  • Daily, weekly, monthly, seasonal, or annual rainfall
A

point rainfall

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21
Q

Rainfall is expressed in terms of
the _______ to which rainwater
would stand on an area, if all the
rain were collected on it.

A

depth

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22
Q

what to plant in certain areas, where and when to plant, when
to harvest

A

agriculture

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23
Q

how and when to irrigate

A

horticulture/viticulture

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24
Q

design drainage systems and prevent water-related issues in
buildings

A

engineering

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25
An instrument to measure rainfall rate in a certain period of time. It catches and represents the precipitation falling on a respective surrounding area.
rain gauge
26
This type of rain gauge is an ordinary rain gauge
non-recording
27
This type of rain gauge gives automatic rainfall records without any bottle reading.
recording
28
WEIGHING BUCKET TYPE TIPPING BUCKET TYPE FLOATING TYPE
recording rain gauge
29
availability of continuous record of previous rainfall
continuity
30
rainfall data of previous year should be consistent with the present environmental condition.
consistency
31
If the normal precipitation at each of the selected stations is within 10% of that station with missing data.
arithmetic-mean method
32
If the normal precipitation/rainfall at any of the selected stations is more than 10% of that station with missing records. Consists of weighing the precipitation at the various stations by the ratios of normal annual precipitations.
normal ratio method
33
calculated by taking an average of the values that are obtained from several observation points or stations within the region.
arithmetical-mean method
34
method assigns weightage to stations based on proximity, superior to the arithmetic-mean method. It’s effective for outside catchment stations and easy to calculate for fixed networks.
thiessen-mean method
35
entails drawing isohyets derived from precipitation data of different stations and then taking an average precipitation by integrating over the areas which correspond to these lines
isohyetal method
36
A test for consistency of record or for rain gauge inconsistency.
double-mass analysis
37
The process by which water in the ground surface enters the soil Depending on how saturated the ground is, the water can continue downwards to replenish water tables and aquifers
infiltration
38
Infiltration is dependent on the condition of the land surface (cracked, crusted, compacted etc.)
surface entry
39
Infiltration rates are greatly influenced by factors like temperature, wind, freezing/thawing cycles, soil moisture condition, seasonal fluctuations, and the intensity and duration of rainfall.
climate and weather condition
40
The amount and rate of water movement through the soil are determined by the size and arrangement of soil particles.
soil texture and structure
41
Sand: Silt: Clay:
high infiltration rate moderate infiltration rate low infiltration rate
42
Saturated soils exhibit higher water content, preventing infiltration and can even increase surface runoff and erosion
soil saturation
43
Steeper slopes generally experience faster runoff and reduced infiltration rates, as water moves downslope quickly. On the other hand, soft slopes allow greater infiltration rates because they make it easier for water to disperse and seep into the soil.
slope of the land
44
- Roads and concrete pavements produce an impermeable layer that prevents infiltration. - Decreasing vegetation due to farming, tree-cutting, and animal grazing will lower permeability.
human activities
45
Increased evapotranspiration rates have the potential to lower soil moisture content, which can accelerate infiltration rates because drier soils initially take up water more easily. Lower evapotranspiration rates can cause a lower infiltration rate because of decreased pore space availability and possible surface sealing.
evapotranspiration
46
Measure infiltration over a large area Provides understanding of infiltration variability of the area Used in agricultural assessments and hydrological studies
areal measurement
47
Measure infiltration of a specific point in the soil Easy to perform Used in site-specific studies
Point Measurement
48
- the speed at which water enters the soil
infiltration rate
49
- device used to measure the water infiltration into the soil
infiltrometer
50
uses a single ring driven in the ground where water is poured at a certain depth. The decrease in water over time reflects the infiltration rate
single ring infiltrometer
51
uses two concentric rings into the ground. The inner ring is driven into the ground and an outer ring follows to help the flow of water
double ring infiltrometer
52
capacity decreases with time and ultimately reaches a constant rate
horton's equation
53
an alternative approach to developing a more approximate physical theory that has an exact analytical solution.
green-ampt model
54
1. The soil under consideration is homogenous and stable, implying that macropores and preferential migration pathways should not be considered. 2.The supply of ponded water at the surface is not limited. 3. A distinct and precisely definable wetting front exists, and as water continues to infiltrates, the wetting front advances at the same rate with depth 4. The capillary suction just below the wetting front is uniform throughout the profile and constant in time during the infiltration event. 5. The soil is uniformly saturated above the wetting front, and the volumetric water contents remain constant above and below the advancing wetting front
five principal assumptions of G-A Method
55
Case 1: i f The rainfall intensity is greater than the infiltration rate and runoff can occur
3 cases of g-a model
56
is the amount of time that has passed from the start of rainfall to the occurrence of ponds in the observed area. _____ is usually utilized to determine the intensity of rainfall.
ponding time
57
principles behind the flow in open channels
leonardo da vinci
58
rainfall is the only source of water for rivers and springs in 15th century
bernard palissy
59
water came from precipitation
aristotle
60
who came up with water cycle
leonardo da vinci and bernard palissy
61
pioneers of modern hydrology
a. pierre perrault b. marriot c. hally
62
water balance equation and catchment area method
pierre perrault
63
first to measure evaporation in mediterranian
marriot
64
the study of origin, circulation, and distribution of water
scientific hydrology or simply hydrology
65
engineering application
applied or engineering hydrology
66
occurrence and distribution of water in surface
surface water hydrology
67
occurrence and distribution of water beneath the surface
groundwater hydrology
68
essential tool for planning of hydraulic structures such as dams
hydrology