Precipitation Analysis Flashcards

1
Q

Types of precipitation

A

Depends on the mechanism of lifting

-Orographic (due to topography)
-Convective (due to convection)
-Cyclonic (due to cyclones)

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2
Q

Lifting due to topography

A
  1. Warm ocean - evaporation
  2. Prevailing winds
  3. Ascent up mountain - rain
  4. Descent down mountain - lee-side downdraft - rain shadow
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3
Q

Congestive precipitation

A
  1. The air near ground gets heated and mixing
  2. The air mass starts ascending
    - if the temp lapse rate of the air mass is smaller than that of one of the surrounding air, the vertical motion continues (INSTABILITY)
  3. Condensation to precipitation
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4
Q

Dry adiabatic lapse rate

A

Lifting a dry air mass without heat exchange. Temperature decreases due to expansion

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5
Q

Moist adiabatic lapse rate

A

Lifting a moist air mass without heat exchange. Temperature decreases due to expansion but not as fast as that of the dry air mass

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6
Q

Ambient temperature lapse rate

A

The surrounding air temperature also decreases with height. This is measured by air balloons

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7
Q

Cyclone genesis

A

-air flow due to pressure gradient (high to low)
-deflection by Coriolis force
-resulting in a rotating motion
-twisting temp distribution

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8
Q

Rain gauges (TBR) - factors that affect accuracy

A
  • location
  • strong winds
  • field animal activities
  • human activities
  • unreliable in heavy rainfall
  • ‘point’ measurement
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9
Q

Weather radars

A

-uses reflected EM energy
-related to rainfall intensity (radar equation)
-can reveal spatial coverage by rotational scanning
-composes images with multiple radars

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10
Q

Cons of weather radars

A

-not as accurate
-complex algorithm to calibrate before use
-large errors
-expensive to build/maintain

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11
Q

Mass curves

A

-used due to rainfall being affected by non meteorological factors -> consistency needs to be checked
-plots of cumulative values of time dependant observations

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12
Q

Measurements

A
  • Depth (R) : mm
  • Intensity ( I) : mm/h
  • Duration (D) : mins, hours or days
  • Areal Extent (A) : km2, miles2
    -Frequency (n) : occurrences out of N years
  • Return period (T): one in T years
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13
Q

Intensity

A

Measured as depth/time
-higher intensity causes less water infiltrated and therefore more surface runoff
-higher intensity can cause more damage

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14
Q

Areal extent

A

-connective precipitation tends to be localised and sporadic whereas cyclonic precipitation often covers large areas with smooth distribution
-> discontinuation
-> should be a reduction factor when use point rainfall

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