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CE 308 -
HYDROLOGY
ENGR. ANJI LAGRADA
HYDROLOGY
The science of water. It is the
science that deals with the
occurrence, circulation and
distribution of water of the earth
and earth's atmosphere
SOME TERMINOLOGIES
• WATER CYCLE – describes the continuous movement of water on, above and
below the earth surface
• EVAPORATION – transformation of water from liquid to gas, it moves from the
ground or bodies of water into the overlying atmosphere
• EVAPOTRANSPIRATION – water transpired from plants and evaporated from
the soil
• CONDENSATION –tansformation of water vapor in the air that cools down and
turns back into liquid watcer
• PRECIPITATION – transformation of water (in the form of rain, snow, hail or
sleet) falls from clouds in the sky.
SOME TERMINOLOGIES
• AQUIFER – a water-bearing rock that readily transmits water to wells and
springs
• INFILTRATION – movement of water into the ground from the surface
• RUNOFF – variety of ways by which water moves across the land. As it flows,
water may infiltrate into the ground, evaporate into the air, and become stored in
lakes or reservoir, or be extracted for agricultural uses or other human uses
• SUBSURFACE FLOW – flow of water underground, it can return into the surface
or seep into the ocean
TYPES OF PRECIPITATION
• DRIZZLE - a very light, usually uniform, precipitation consisting of numerous
minute droplets with diameters in excess of 0.1 mm but smaller than 0.5 mm.
• RAIN -. precipitation consisting of water drops larger than 0.5 mm. It can be
classified as light rain when the intensity is smaller than 2.5 mm/hr, moderate
when it is between 2.5 and 7.5 mm/hr, and heavy when it exceeds 7.5 mm/hr
• SNOW - precipitation in the form mainly of branched hexagonal or star-like ice
crystals, resulting from direct reverse sublimation of the atmospheric water vapor
• SLEET - (North American usage) is precipitation consisting of transparent pellets or
grains of ice, formed as a result of the passage of raindrops through a layer of
colder air near the ground. In British usage the word sleet refers to precipitation
consisting of melting snow or a mixture of snow and rain.
TYPES OF PRECIPITATION
• GLAZE - also known as freezing rain; an ice deposited by drizzle or rain on cold
surfaces.
• SNOW PELLETS- also called granular snow or graupel; a form of precipitation
consisting of white, opaque, small grains with diameters between roughly 0.5 and
5 mm.
• HAIL - consists of balls or irregular chunks of ice with diameters between 5 and
50 mm, or even larger. These lumps of ice can be transparent, or they can consist
of concentric layers of clear and opaque ice
• DEW - consists of moisture in the form of liquid drops on the ground surface and
on the vegetation and other surface elements, as a result of direct condensation of
atmospheric water vapor.
RAINFALL CHARACTERISTICS
INTENSITY
DURATION
DEPTH
TYPES OF RAIN GAUGES
GRADUATED
RAIN GAUGE
TIPPING
BUCKET RAIN
GAUGE
WEIGHING
PRECIPITATION
GAUGE
OPTICAL RAIN
GAUGE
ACOUSTIC
RAIN GAUGE
DELINEATION OF
WATERSHED
WATER BALANCE EQUATION:
where:
P – precipitation
R - river runoff
G - ground water
ET - evapotranspiration
EXAMPLE #1:
(Delineation of
Watershed)
The volume of atmospheric water per month is
12,900km3. The evapotranspiration from land is
28,000 km3 per year and river runoff is 50,000 km3
per year. Estimate the storage volume of the
catchment.
RAINDROP
DROP TERMINAL VELOCITY
EQUATION:
From fluid mechanics, the force balance is:
D 0.2 0.4 0.6 0.8 1.0 2.0 3.0 4.0 5.0
Cd 4.2 1.66 1.07 0.815 0.671 0.517 0.503 0.559 0.66
Drag Coefficient table
The force balance for a raindrop is:
Fd = Fg – Fb
where:
𝐹𝑑 – drag force
𝐹𝑔 – gravity force
𝐹𝑏 – buoyancy force
EXAMPLE #1:
(Raindrop)
What is the terminal velocity for the light rain with a
drop size of 0.6mm at sea level.
Ans. : 2.4708m/s
PRECIPITATION
DATA:
THEISSEN POLYGON METHOD:
where:
Ai – area within assigned gauges
Ri – rainfall within assigned
gauges
A – total area
R – average rainfall for catchment
EXAMPLE #1:
(Precipitation
Data)
In the given catchment figure as shown, the theissen
polygon with the rainfall depths recorded by gauge
A, B, and C as 10mm, 8mm, and 9mm. The
corresponding polygon areas are 5.1km2, 3.2km2,
and 5.3km2. Compute the average rainfall depth
express in mm.
Ans. : 9.1397mm
THANK YOU
ENGR. ANJI LAGRADA

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Prelim-Presentation-Module-1.pptx

  • 2. HYDROLOGY The science of water. It is the science that deals with the occurrence, circulation and distribution of water of the earth and earth's atmosphere
  • 3. SOME TERMINOLOGIES • WATER CYCLE – describes the continuous movement of water on, above and below the earth surface • EVAPORATION – transformation of water from liquid to gas, it moves from the ground or bodies of water into the overlying atmosphere • EVAPOTRANSPIRATION – water transpired from plants and evaporated from the soil • CONDENSATION –tansformation of water vapor in the air that cools down and turns back into liquid watcer • PRECIPITATION – transformation of water (in the form of rain, snow, hail or sleet) falls from clouds in the sky.
  • 4. SOME TERMINOLOGIES • AQUIFER – a water-bearing rock that readily transmits water to wells and springs • INFILTRATION – movement of water into the ground from the surface • RUNOFF – variety of ways by which water moves across the land. As it flows, water may infiltrate into the ground, evaporate into the air, and become stored in lakes or reservoir, or be extracted for agricultural uses or other human uses • SUBSURFACE FLOW – flow of water underground, it can return into the surface or seep into the ocean
  • 5. TYPES OF PRECIPITATION • DRIZZLE - a very light, usually uniform, precipitation consisting of numerous minute droplets with diameters in excess of 0.1 mm but smaller than 0.5 mm. • RAIN -. precipitation consisting of water drops larger than 0.5 mm. It can be classified as light rain when the intensity is smaller than 2.5 mm/hr, moderate when it is between 2.5 and 7.5 mm/hr, and heavy when it exceeds 7.5 mm/hr • SNOW - precipitation in the form mainly of branched hexagonal or star-like ice crystals, resulting from direct reverse sublimation of the atmospheric water vapor • SLEET - (North American usage) is precipitation consisting of transparent pellets or grains of ice, formed as a result of the passage of raindrops through a layer of colder air near the ground. In British usage the word sleet refers to precipitation consisting of melting snow or a mixture of snow and rain.
  • 6. TYPES OF PRECIPITATION • GLAZE - also known as freezing rain; an ice deposited by drizzle or rain on cold surfaces. • SNOW PELLETS- also called granular snow or graupel; a form of precipitation consisting of white, opaque, small grains with diameters between roughly 0.5 and 5 mm. • HAIL - consists of balls or irregular chunks of ice with diameters between 5 and 50 mm, or even larger. These lumps of ice can be transparent, or they can consist of concentric layers of clear and opaque ice • DEW - consists of moisture in the form of liquid drops on the ground surface and on the vegetation and other surface elements, as a result of direct condensation of atmospheric water vapor.
  • 8. TYPES OF RAIN GAUGES GRADUATED RAIN GAUGE TIPPING BUCKET RAIN GAUGE WEIGHING PRECIPITATION GAUGE OPTICAL RAIN GAUGE ACOUSTIC RAIN GAUGE
  • 9. DELINEATION OF WATERSHED WATER BALANCE EQUATION: where: P – precipitation R - river runoff G - ground water ET - evapotranspiration
  • 10. EXAMPLE #1: (Delineation of Watershed) The volume of atmospheric water per month is 12,900km3. The evapotranspiration from land is 28,000 km3 per year and river runoff is 50,000 km3 per year. Estimate the storage volume of the catchment.
  • 11. RAINDROP DROP TERMINAL VELOCITY EQUATION: From fluid mechanics, the force balance is: D 0.2 0.4 0.6 0.8 1.0 2.0 3.0 4.0 5.0 Cd 4.2 1.66 1.07 0.815 0.671 0.517 0.503 0.559 0.66 Drag Coefficient table The force balance for a raindrop is: Fd = Fg – Fb where: 𝐹𝑑 – drag force 𝐹𝑔 – gravity force 𝐹𝑏 – buoyancy force
  • 12. EXAMPLE #1: (Raindrop) What is the terminal velocity for the light rain with a drop size of 0.6mm at sea level. Ans. : 2.4708m/s
  • 13. PRECIPITATION DATA: THEISSEN POLYGON METHOD: where: Ai – area within assigned gauges Ri – rainfall within assigned gauges A – total area R – average rainfall for catchment
  • 14. EXAMPLE #1: (Precipitation Data) In the given catchment figure as shown, the theissen polygon with the rainfall depths recorded by gauge A, B, and C as 10mm, 8mm, and 9mm. The corresponding polygon areas are 5.1km2, 3.2km2, and 5.3km2. Compute the average rainfall depth express in mm. Ans. : 9.1397mm