Precipitation Analysis Flashcards
Types of precipitation
Depends on the mechanism of lifting
-Orographic (due to topography)
-Convective (due to convection)
-Cyclonic (due to cyclones)
Lifting due to topography
- Warm ocean - evaporation
- Prevailing winds
- Ascent up mountain - rain
- Descent down mountain - lee-side downdraft - rain shadow
Congestive precipitation
- The air near ground gets heated and mixing
- 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) - Condensation to precipitation
Dry adiabatic lapse rate
Lifting a dry air mass without heat exchange. Temperature decreases due to expansion
Moist adiabatic lapse rate
Lifting a moist air mass without heat exchange. Temperature decreases due to expansion but not as fast as that of the dry air mass
Ambient temperature lapse rate
The surrounding air temperature also decreases with height. This is measured by air balloons
Cyclone genesis
-air flow due to pressure gradient (high to low)
-deflection by Coriolis force
-resulting in a rotating motion
-twisting temp distribution
Rain gauges (TBR) - factors that affect accuracy
- location
- strong winds
- field animal activities
- human activities
- unreliable in heavy rainfall
- ‘point’ measurement
Weather radars
-uses reflected EM energy
-related to rainfall intensity (radar equation)
-can reveal spatial coverage by rotational scanning
-composes images with multiple radars
Cons of weather radars
-not as accurate
-complex algorithm to calibrate before use
-large errors
-expensive to build/maintain
Mass curves
-used due to rainfall being affected by non meteorological factors -> consistency needs to be checked
-plots of cumulative values of time dependant observations
Measurements
- 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
Intensity
Measured as depth/time
-higher intensity causes less water infiltrated and therefore more surface runoff
-higher intensity can cause more damage
Areal extent
-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