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Hydrology Engineering
Lecture 6 1 2 3 4 5 6 IR HERMONO S. BUDINETRO, M. ENG Part of the lecture was from ibu Purwanti Sri Pudyastuti
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HYDROLOGI General HYDROLOGI HYDROMETRI CLIMATOLOGY RAINFALL
AWLR, Peil scal RAINFALL ARR, ORR EROSIFITAS WATER LEVEL POINT RAINFALL Observation Current meter SEDIMEN TRANSPORT Observation RATING CURVE AREAL RAINFALL Analisa frekuensi DESIGN RAINFALL RIVER DISCHARGE Sintetis Frequency Analysis DESIGN DISCHARGE Maximum discharge (at maximum water level) Minimum discharge (at dry season) and Design discharge (design flood) and Water availibility
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CLIMATOLOGY the scientific study of climate
The incidence and distribution of water in an area depends on the climate, topography and geology. Climate is mostly influenced by geographical location in the earth's surface. In general, the climate has an influence on the lives of humans and animals, and plants, .
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Climate influence on Soil, Plants and Animals / Humans
Factor Soil Plant Animal/Human Temperatur Good for the separation of organic substances and thus facilitate the dissolution of the mineral soil Good for the growth and maturation of the fruit. Accelerate water loss, or evaporation. Influencing the decrease / increase in body temperature Humidity Retard the drying. Good for decay and facilitate dissolution of organic materials Good for growth. Reduce evaporation. Affect heat loss, pushing their skin disorders, make humans uncomfortable Wind velocity Erodes the open land, and encourage drying Accelerate evaporation. Help pollination. Encouraging heat loss Sun shine raising the temperature arrange photosynthesis Can burn the skin, the skin surface temperature increase Rainfall Peeling and washing land Agglomerate clay/soil Water is important for plants, dissolving nutrients Affect health, it could bring the danger of flooding Agglomerate= meggumpalkan
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Climatic factors that are important for hydrological analysis are:
humidity, temperature, radiation, wind, and precipitation. Topography is closely related to the level surface of the earth, the mountains, rivers, lakes, swamps, geological structure of the local soil and forms / types of the earth's surface (land use) that will directly affect the level / large runoff (coefficient run- off) ,
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Climatological station
Climatic conditions of a region obtained from Climatological Station, Rain fall depth, The amount of time the sun is shining and the amount of solar radiation, Velocity and direction of wind Humidity Temperatur maximum and mininimum Evaporation Changes in the water table of the groundwater.
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CLIMATOLOGY STATTION 1. Rainfall 2. Humidity 3. Temperatur
Ordinary Rainfall Recorder = ORR Automatic Rainfall Recorder = ARR. 1. Rainfall 2. Humidity psychrometer, hair hygrometer or hygro thermograph. 3. Temperatur Thermometer maximum and Thermometer minimum 4. Sun shine the length of sun shine “Campbell Stokes Recorder” (glass ball) Sun shine calories “Actinograph” 5. Velocity & direction of wind Anemometer 6. Evaporation Pan Evaporation
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Lay – Out Climatology station
ARR ORR 1,0 m gate 10 m 6 m 2,5 m 3,0 m 2,0 m measuring device for solar heat sunshine recorder Pan evaporasi tank for water storage home instrument with the door a north facing measuring device for wind speed and direction house of supporting devices for ARR pagar transparan Lay – Out Climatology station
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ARR = Automatic rainfall recorder
THERMOMETER ARR = Automatic rainfall recorder THERMOHYGROGRAPH Temperature & humidity ORR = ordinary rainfall recorder SUNSHINE “Campbell Stokes Recorder” the length of sun shine ACTINOGRAPH Sun shine calories ANEMOMETER Velocity & direction of wind PAN EVAPORASI
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Rain recorder is 2 (two) types: Ordinary Rainfall Recorder = ORR” and
Automatic Rainfall Recorder = ARR. ARR must always be accompanied by the ORR. which is used as a calibration total daily rainfall. ARR = Automatic rainfall recorder ORR = ordinary rainfall recorder
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THERMOHYGROGRAPH Temperature & humidity
The temperature was recorded with a thermometer, placed in an open box protected from rain and direct sunlight, The thermometer usually together with air humidity recording device. Observations were made using the maximum and minimum thermometers, which will provide information on the maximum and minimum temperatures at a certain period. In Indonesia, the minimum temperature occurred at around 4:30 AM and the maximum temperature at 13,00.PM. The higher the elevation of the ground surface of the sea level, the lower the air temperature, the change range from 6.50 C to rise 1000 m. Variations in air temperature also depends on the intensity of sunlight, the pattern of ocean currents, wind, and plants. THERMOMETER Maximum & minimum
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Humidity The air easily absorb moisture, thus forming air humidity. The amount of water vapor that is absorbed depends on the air temperature and water. The higher the temperature, the more water vapor that can be held. If there is an energy source that can vaporize this water into the air, the evaporation will continue until the air becomes saturated with water vapor, so that it can no longer absorb water vapor, resulting in a balance. In these conditions the water molecules will put pressure on the system at a certain temperature, known as the "saturated vapor pressure" or es. Value es varies according to the surrounding temperature. To measure humidity used psychrometer, a hair hygrometer or hygrothermograph. In relation to the science of hydrology, the amount of humidity will affect the prevalence of cloud that will turn into rain. THERMOHYGROGRAPH Temperature & humidity
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Sun Shine The measurement a long sun shines with devices "Campbell Stokes Recorder" placed on brick masonry. This device consists of a solid glass ball with a diameter of 4 inches (= 10.1 cm) attached to the sunken field, diameter and placement so that sunlight passing through the glass ball with a sharp focus on the field of concave, in case the sun will burn the paper placed on the sunken field. Of combustion in the paper can be known a long the sun shines every day. SUNSHINE “Campbell Stokes Recorder” the length of sun shine ACTINOGRAPH Sun shine calories
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Purwanti Sri Pudyastuti
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Evaporation Evaporation measurements is used the Pan Evaporation (next lecture) PAN EVAPORASI
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The velocity and direction of wind
The wind is moving air, to have the direction and speed. Wind direction is expressed in 16 majors compass and comes with directions that states the degree to north. Wind speed expressed in miles / hour, kilometers / hour, meters / second, or knots (1 knot = km / h). Wind speed and direction are usually measured by the anemometer and wind direction. Anemometer commonly used is the type of dish that consists of 3 or 4 cup that rotates around the vertical axis. Anemometer installed at a height of 2 m above the ground. ANEMOMETER Velocity & direction of wind
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