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HYDROMETEROLOGY (LESSON 2.1)

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TYPES, FORM, AND VARIATION OF PRECIPITATION

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HYDROMETEROLOGY (LESSON 2.1)
 

HYDROMETEROLOGY (LESSON 2.1)Version en ligne

TYPES, FORM, AND VARIATION OF PRECIPITATION

par Grace Balahay
1

it is a product of the condensation of water vapor in the atmosphere that falls in the surface due to gravity • It is also considered as “input” water in the surface water balance

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2

is an imaginary sample volume of air, assigning them in a thermodynamic or fluid process.

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3

is the most important climatic element in the Philippines.

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4

receive the greatest amount of rainfall

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5

receives the least amount of rain.

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6

can be referred as “thermal convection” and this precipitation is in a form of llocal whirling thunderstorms which usually occurred in the tropics.

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7

sometimes called as cyclonic precipitation •Caused by the conflict between two air masses of different temperatures and densities

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8

When two air masses of different temperatures and densities clash, a front will be formed whether a cold of warm fronts

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9

when a cold air mass moves into an area occupied by a warmer air mass.

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10

bring a quick drop in temperature, gusty winds, and heavy precipitation, often in the form of thunderstorms or intense rain.

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11

occurs when a warm air mass advances over a retreating cold air mass. • Weather Impact: bring gradual warming and extended periods of light rain or drizzle, often followed by warmer, more humid air

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12

forms when a cold front overtakes a warm front, lifting the warm air aloft.

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13

lead to complex weather patterns and prolonged precipitation, as seen in mid-latitude cyclones

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14

These fronts bring varied weather, from light rain to more intense precipitation, depending on the temperature of the advancing air

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15

forms when two air masses meet but neither advances, remaining relatively still.

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16

These fronts lead to long-lasting periods of cloudiness and precipitation, which can result in flooding if rain persists over a region

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17

the rise of warm air is due to the topographic barriers like mountains as it cannot move horizontally.

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18

most observed, drops larger than drizzle (> 0.5 mm). if the smaller drops, in contrary to drizzle, are widely separated

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19

a fairly uniform precipitation composed exclusively of fine drops very close together. It somehow appears to float while following air currents, but unlike fog droplets, it falls to the ground.

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20

precipitation of snow crystals that are mostly branched in the form of six-pointed stars.

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21

can be termed as ice pellets, which is a transparent or translucent pellet of ice, which are round and irregular hard grains consists of frozen raindrops, or largely melted then refrozen snowflakes.

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22

precipitation in the form of small balls or other pieces of ice falling separately or frozen together in irregular lumps. They are usually larger than 5 mm in diameter and associated with thunderstorms. Sizes 25 mm and larger indicate a severe thunderstorm.

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23

very small, white, and opaque grains of ice and it is basically a frozen drizzle.

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24

also known as snow pellets, with diameter smaller than 5 mm, and characterized as white, opaque grains of ice that are round or conical in shape.

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25

falling crystals in a form of needles, column, or plates. It is also called “diamond dust” due to direct formation of ice as the ice crystals appear like a fog with individual water particles and the shape of the individual ice crystals causes the light pillar optical effect above the light source.

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26

a thin coating of ice that forms when a supercooled liquid precipitation like freezing rain or drizzles fall into objects with temperature below or slightly above freezing

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27

Water falls to the ground either directly through gaps in canopy, or indirectly having dripped off leaves, stems or branches

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28

Rainfall that is intercepted by stems and branches and acts like a funnel that flows down the trunk into the soil in a much smaller area

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29

water loss while sitting on the canopy prior to indirect through fall or stemflow due to evaporation

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30

water gain by the turbulent mixing of air as it passes over a rough canopy which promotes rapid deposition of condensing water

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