precipitation I Flashcards

1
Q

what are some factors to consider when using a rain gauge?

A
  • height matters because the wind profile changes near the ground
  • color matters: dark surfaces heat up and cause evaporation
  • wind matters: wind deforms the pressure field around the rain gauges
  • methods matter: wind protection, instantaneous measurements and tipping bucket
  • location matters: no object should be closet than 2 times its height to the rain gauge
  • people matter
  • timing matters: frequent measurements keeps evaporation losses low
  • technology matters: fails and doesn’t detect errors
  • size matters: less inspections if large
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2
Q

what is a lysimeter?

A

device that records the amount of precipitation an area receives and the amount of water that drains the soil
–> weighing lysimeters can measure the precise amount of water that falls on them

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3
Q

what is the relative humidity equation?

A

RH= actual vapor pressure/saturation vapor pressure x 100%

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4
Q

what is the dew point?

A

temperature that you would have to cool air to reach saturation line and cause condensation

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5
Q

what happens when a point is in undersaturated and supersaturated location in the saturation vapor pressure curve?

A

undersaturated (under line): no cloud
supersaturated (over the line): air is not capable of holding that much water in it so it will condensate (clouds) or rain

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6
Q

what are the two types of uplifts?

A
  • convective uplift: in a small cell, uplift of air until it cools and turns into clouds
  • frontal/advective lift: water/air comes from elsewhere, either warmer air pushing upwards or cold air coming from below (pushing warm air up -> cooling)
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7
Q

what is an adiabatic lapse rate? and what are the dry and moist adiabatic lapse rates?

A

how much colder it gets with increasing height
dry adiabatic lapse rate: 10 degrees per thousand meters
moist adiabatic: 6 degrees per thousand meters

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8
Q

why is the moist adiabatic lapse rate slower than the dry adiabatic lapse rate?

A

because there is condensation which requires energy

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9
Q

what is orographic precipitation?

A

driven by height, usually on one side of the mountain
- moist adiabatic lapse rate going up one side and dry on the way down so warmer on the other side

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10
Q

where does it rain the most?

A
  • mountain ranges on the wind side where moist air is pushed against
  • coastal regions
  • tropics because its warmer so air can hold more vapor
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11
Q

factors in distribution of precipitation?

A
  • temperature
  • seasonality
  • topography
  • distance from ocean
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12
Q

how do raindrops form?

A

water vapor gas gathers onto tiny airborne particle called a condensation nuclei -> collide with each other and grow -> once they are heavy enough, they fall

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13
Q

what are the airborne particles in rain droplets from?

A

dust, aerosols or salt

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14
Q

what are the types of precipitation?

A
  • rain (0.5 - 5 mm diameter)
  • drizzle (0.5 mm diameter)
  • showers (vary in intensity)
  • snow (when water vapor turns to ice without turning into liquid first)
  • hail (when water droplets freeze in high, very cold clouds -> get bigger as they are coated with more layers or banging into each other)
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15
Q

where do we need more rain gauges?

A
  • mountainous regions (orographic effects)
  • tropics (small scale convective precipitation)
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16
Q

what are methods of spatial interpolation?

A
  • arithmetic averages
  • thiessen method -> polygons assigned to every point that is closest to the point
  • isohyets: contour lines of equal rainfall depth
  • kriging: computerized isohyet map
17
Q

what is a rainfall hyetograph?

A

graphical representation of the distribution of rainfall over time