Lec 3: Precipitation I Flashcards

1
Q

What factors affect rain gauge (pluviometer) readings and why? (9)

A

Height: Wind profile changes near ground

Color: Dark surfaces heat up and cause evaporation

Wind: deforms pressure field around gauge, causes under-measurements

Methods: wind protection & instantaneous, automated measurements increase measured quantity and reduce evaporation losses

Location: to avoid wind effects, no object should be closer than 2 times its height to the rain gauge (buildings, trees)

People: observation errors

Timing: Frequent measurements keep
evaporation losses low
* In dry regions, rain alerts may help
identify when measurements are
needed

Technology: better technology = better measurements, but technology can fail or not detect certain errors

Size: larger gauge = less inspections required, but evaporation can become significant after longer periods

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2
Q

Describe gadgets that account for or prevent evaporation

A

Tipping bucket rain gauge
Gauge that draws water level live

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3
Q

How accurate are rain/snow gauge in cold climates? Why? What are some solutions

A
  • very innacurate
  • wind and snow drift are very prevalent. frequent, high-quality measurement difficult due to hard to reach locations and difficult conditions
  • heated gauges that melt the snow that falls in the gauge (but this may increase evaporation)
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4
Q

What does a lysimeter do and how?

A

they measure the amount of actual evapotranspiration which is released by plants

how:
- By recording the amount of
precipitation that an area receives and the amount of water that drains the
soil, the amount of water lost to evapotranspiration can be calculated.

  • Weighing lysimeters measure the precise
    amount (weight) of water that falls on them
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5
Q

What is relative humidity?
What is it an indicator of?

A

RH is the ratio of actual (partial) vapor pressure to saturation vapor pressure (at a given temperature), in %

RH is a good indicator for likelihood of rain,
but doesn’t say anything about amount of water vapor in air

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6
Q

What is saturation temperature? What is another name for it?

A

the temperature at which water condenses
aka dew point

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7
Q

Describe the saturation vapour pressure curve

A

Relationship between temperature and pressure. Curve represents relative pressure needed at a given temperature to reach saturation.

Above curve = supersaturated
Below curve = undersaturated

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8
Q

What is absolute humidity?

A

Absolute humidity is mass of water per unit of air

e.g. mass water per mass air OR mass water per volume air

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9
Q

What is the relationship between absolute and relative humidity?

A

Absolute humidity is higher at higher levels of relative humidity

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10
Q

Describe the two types of adjective (or frontal) uplift

A

cold front
- cold air advances into warm air
- steep boundary between air masses, warm air rises quickly
- showers and thunderstorms, clears quickly

-warm front
- warm air moves over cold air
- more gradual boundary, warm air rises slowly
- shield of steady rain or snow

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11
Q

How does convective uplift cause precipitation?

A

Convective uplift occurs when air near the ground is warmed by the sun and begins to rise. Air rises and cools, forming clouds and precipitation.

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12
Q

What is the adiabatic lapse rate?
How does it differ for dry and wet air?

A

the rate at which the temperature of an air parcel changes in response to the compression or expansion associated with elevation change

The adiabatic lapse rate for a saturated parcel is lower than that for an unsaturated parcel.

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13
Q

What is orographic precipitation?

A

Precipitation which is caused by hills or mountain ranges deflecting the moisture-laden air masses upward, causing them to cool, reach the dew point and precipitate their moisture on the windward side of the mountain.

The air that goes down the leeward side is warm and dry. As the air descends, its pressure increases, which makes its temperature go up.

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14
Q

What are some local names for orographic precipitation/cloud formation?

A

Foehn winds, Chinook

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15
Q

Where does it rain most?

A
  • mountain ranges
  • coastal regions
  • equator
  • India
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16
Q

What factors affect the global distribution of precipitation?

A
  • Temperature
  • Global atmospheric circulation patterns (seasonality)
  • Topography (orographic rain)
  • Distance to ocean (source of water)
17
Q

How do raindrops form?

A
  • condensation nuclei attract water vapor gas and form cloud droplets (one million times smaller than a raindrop)
  • “favoured droplets” with stronger nuclei attract airborne water molecules and grow, at the expense of other droplets
18
Q

How does rain form?

A
  • Raindrops form around condensation nuclei (salt crystals, dust, aerosols)
  • Updraughts move drops; they collide with others and grow
  • When they are heavy enough, they fall as rain or snow
19
Q

give examples of condensation nuclei

A

salt crystals, dust, aerosols

20
Q

Name 5 types of precipitation

A
  • rain
  • drizzle
  • showers
  • snow
  • hail
21
Q

Describe rain

A
  • Rain droplet diameter: 0.5 - 5mm
  • Rain normally falls from nimbostratus or
    altostratus clouds
22
Q

Describe drizzle

A
  • droplets smaller than for rain (less than 0.5mm)
  • fall from stratus clouds or fog
23
Q

Describe showers

A
  • Showers are precipitation that varies in intensity
  • Generally falling from cumulonimbus or large cumulus clouds
24
Q

Describe snow

A
  • Snow forms when water vapor turns to ice without first condensing into a liquid
  • Snow flakes are composed of microscopic water crystals that cluster together in groups of 50 or more
  • When the temperature is low enough (say, minus 40 degrees), snow can fall from clear blue skies
25
Q

Describe hail

how can they grow bigger?

A
  • Hail is formed when water droplets freeze in high, very cold clouds

can grow bigger:
* as they are coated with successive layers of ice
- when they are pushed up and down through the atmosphere by strong updraughts and downdraughts.
- when they bang into each other
and stick, forming conglomerate hailstones.

26
Q

How big is the standard error due to gauge spacing? What is this error due to?

A

10-20%, or more
There aren’t enough gauges to do a proper assessment, so we average measurements from a network of gauges

27
Q

What are some methods of spatial interpolation?

A
  • Arithmetic averages
  • Thiessen method
  • Isohyets
  • Kriging
28
Q

What are isohyets?

A

contour lines of equal rainfall depth

29
Q

What is a rainfall hyetograph?

A

A hyetograph is a graphical representation of the distribution of rainfall over time

30
Q

What are important rainfall characteristics (5)

A

► Magnitude
* Amount of precipitation: depth mm
► Duration
* How long it rains: time
► Intensity
* Magnitude/duration: mm/time
► Frequency
* How often it rains
► Combination of these
* Frequency-duration-return period
(statistics)

31
Q

What are the pros and cons of remote precipitation measurements?

How are they measured?

A

pros: Great for measuring the spatial distribution of events

cons: difficult to calibrate (e.g. they detect rain or snow in the air, but is it actually falling?