precipitation Flashcards

1
Q

rain

A

liquid water droplets between 0.5-0.7 mm diameter

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2
Q

drizzle

A

rain subset with droplets of less than 0.5 mm

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3
Q

sleet

A

freezing raindrops, combination of snow and rain

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4
Q

snow

A

complex ice crystals agglomerated

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5
Q

hail

A

balls of ice between 5-125mm diameter

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6
Q

conditions for precipitation formation

A

for formation:
- air must cool to dew point
-condensation nuclei must be present
- droplets must grow
For sustaining:
-continuous import of water

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7
Q

dew point

A

temperature at which air mass is saturated by water vapor (reach 100% relative humidity)

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8
Q

airmass

A

mass of air with relative homogenous temperature and density

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9
Q

convective lifting

A

air warmer than surrounding is less dense -> will rise

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10
Q

frontal lifting

A

cold front meeting hot front will cause hot air to rise as fronts migrates

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11
Q

orographic lifting

A

air forced to rise because of physical presence of mountains

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12
Q

condensation nuclei

A

small particles/ aerosols upon which water vapor attaches to initiate condensation

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13
Q

condensation

A

process driving change from water vapor to liquid water

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14
Q

tipping bucket rain gauge functioning

A

count small increment of rain collected
How:
-rain falls via funnel into container divided in 2 equal part
- when specified amount of rain has drained into a part -> bucket tilt

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15
Q

problem of tipping bucket gauge

A

undercatch of precipitation because:
-wind turbulence
-evaporation loss
-wetting loss
-rain splash effect

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16
Q

typical climate station will record:

A

wind speed & direction
rainfall
relative humidity & temperature
radiation

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17
Q

Snow variables

A

amount & distribution of snow

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18
Q

liquid water content

A

unfroze water existing in snowpack

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19
Q

relative density

A

ratio of snowpack to water density

20
Q

SWE

A

height of water that would be on ground if snowpack melted in place

21
Q

Snowmelt dynamic (3 phases)

A

1.Warming phase = cold snowpack require energy to rain temperature to 0 Celsius
2.Ripening = warm snowpack gains additional energy inputs and retain initial meltwater (until water holding capacity is exceeded)
3.Output = continued input of energy to melt remaining snow and ice AND water leaving by base of snowpack

22
Q

snow course

A

when multiple measurement of snow depth&SWE are made on path between 2 fixed points

23
Q

Measuring snowfall as SWE

A

weighing bucket gauge -> heated tipping bucket
snow pillow -> weight of snow forcing fluid in panel into pressure transducer

24
Q

measuring snow on the ground

A

with ruler
with snow surveys
with ultrasonic depth sensor -> continuous record of depth

25
Q

rainfall hyetograph

A

plot of rainfall depth/intensity as function of time

26
Q

cumulative rainfall hyetograph

A

plot of summation of rainfall increments as function of time

27
Q

rainfall intensity

A

plot of depth of rainfall per unit time

28
Q

how to compare rainfall event using:

A

duration
average rainfall intensity
max rainfall intensity
magnitude (total rainfall amount)

29
Q

Method for Estimating rainfall over larger area

A

Arithmetic
Thiessen polygon
Isohyetal
Inverse distance weighting

30
Q

Problems of arithmetic method

A

gages must be inside watershed
need uniformly distribution
need not too large outliers

31
Q

Problem of isohyetal method

A

value of delineation varies depend on density of gauge

32
Q

Issues converting snow into SWE

A

-time lag from precipitation to melting
-snowmelt enter watershed where it melts -> not where it falls

33
Q

Interception

A

fraction of gross precipitation that wets & adheres to above ground object, doesn’t reach the ground and returns to atmo with evaporation

34
Q

Gross precipitation

A

measured above canopy or in a clearing

35
Q

Throughfall

A

precip reaching surface directly or via canopy drip

36
Q

stemflow

A

water reaching surface by running along trunks and stems

37
Q

total interception loss

A

sum of all canopy interception and losses

38
Q

Why is interception critical

A

-significant water source for evapo
-strongly influence runoff
-canopy drips increase local erosion

39
Q

Issues measuring interception

A

Spatially variable (diff vegetation, wind, etc.)
Temporally variable (begin VS end of storm)

40
Q

Interception by vegetation hierarchy

A

conifer
broadleaves & tropical forest
Soybean, corn, wheat (grasses)

41
Q

Factors affecting interception

A

vegetation type
duration
precipitation intensity
wind
precipitation type (snow VS rain)
precipitation frequency

42
Q

depression storage

A

precip retained in ground surface depressioin

43
Q

detention storage

A

short-term storage depleted via flow away

44
Q

retention storage

A

long-term storage depleted via evaporation

45
Q

wetlands

A

transitional system between terrestrial and aquatic system where water table is at/near surface

46
Q

criteria for wetlands to meet:

A

-hydrophytic vegetation
-hydric soils
-hydrologic conditions (saturated substrate some time during growing period)