That part of atmospheric moisture that falls on the earth surface
PRECIPITATION
what are the 10 types of precipitation?
Water droplets in clouds are formed by nucleation of vapor on aerosols, then go through many condensation evaporation cycles as they circulate in the cloud, until they aggregate into large enough drops to fall through the cloud base.
SUBLIMATION NUCLEI
a process of artificially nucleating clouds to induce precipitation
CLOUD SEEDING
is a common nucleating agent and is spread from aircraft in which a silver iodide solution is evaporated with a propane flame to produce particles.
SILVER IODINE
___________ and ___________are known to co-exist in the atmosphere at sub-freezing temperatures.
ICE CRYSTALS and WATER DROPLETS
_________ of water droplets as a result of their coming in contact through the action on them of air movement and
gravitational pull.
COALESENCE
air is drawn upwards by convective action, such as in the center of a thunderstorm cell
CONVECTIVE PRECIPITATION
where warm air is lifted over cooler air by frontal passage
FRONTAL PRECIPITATION
which an air mass rises to pass over a mountain range
OROGRAPHIC PRECIPITATION
what are the 4 types of precipitation?
the simplest method of determining areal average rainfall which involves averaging the rainfall depths recorded at a number of gages
ARITHMETIC AVERAGE
This method is satisfactory if the gages are uniformly distributed over the area and the individual gage measurements do not vary greatly about the mean.
ARITHMETIC AVERAGE
Assumes that at any point in the watershed the rainfall is the same as that at the nearest gage so the depth recorded at a given gage is applied
out to a distance halfway to the next station in any direction.
THIESSEN METHOD
The relative weights for each gage are determined from the corresponding areas of application in a Thiessen polygon network, the boundaries of the polygons being formed by the ____________.
PERPENDICULAR BISECTORS OF THE LINES JOINING ADJACENT GAGES.
ISOHYETAL METHOD
The gaging networks in the Philippines
3 types of estimation of Areal Precipitation
a. ARITHMETIC AVERAGE
b. THIESSAN METHOD
c. ISOHYETAL METHOD
2 types of rainfall adjustments
A. Estimation of Missing Rainfall Data
B. Adjustment of Rainfall due to Changes in Locations
Complete measured precipitation data are important to many problems in hydrologic analysis and design but there are missing values
ESTIMATION OF MISSING RAINFALL DATA
type of Estimation of Missing Rainfall Data that is preferrable for relatively flat areas
STATION-AVERAGE METHOD
ADJUSTMENT OF RAINFALL DUE TO CHANGES IN LOCATION
is the method that is used to check for an
inconsistency in a gaged record.
DOUBLE-MASS CURVE ANALYSIS
is a graph of the cumulative catch at the rain gage of interest versus the cumulative catch of one or more gages in the regions that have been subjected to similar hydrometeorological occurrences and are known to be consistent
DOUBLE-MASS CURVE