7. Convection is an area of strong (precipitation) echo above melting layer. For
Convection
, do one of the following:
• Enable
Convection
to be able to define criteria to determine whether precipitation is
convective or large scale, and only the latter is corrected.
• In the first box, type the threshold (in dBZ). Determine this value using the
intensity of convection in your locale.
Typically a value of 35 ... 40 dBZ is appropriate for most locations in mid
latitudes, 20 dBZ in cool climates.
• In the second box, type the convective top height (how much above melting layer
it should be, in km) in the next box.
This is typically 1 ... 2 km (0.6 ... 1.2 mi) to allow some clearance above the bright
band.
The suitable value for threshold height depends of the accuracy of the melting
level height estimate. The smaller the value, the more often pixels are considered
convective.
• Disable
Convection
to have all precipitation corrected with the above given profile.
More information
‣
Configuring Map Projections (page 19)
‣
‣
‣
Associating Products with Tasks (page 17)
3.17.5 SRI Profile Correction Example
This example shows the profile correction in a typical situation with bright band at 3 km
(1.9 mi), gradient below the bright band (in rain) 3 dBZ/km (4.8 dBZ/mi) and above the
bright band (in snow) 10 dBZ/km (16.1 dBZ/mi). Radar is located at height of 0 km (0 mi)
and the reference height is at 1 km (0.6 mi). Full power half beam width is 1°.
The correction is calculated for 2 elevations, 1.0° (in black) and 2.0° (in grey). Note that the
correction is negative near the radar where measurement it made below the reference
height and that the curves have different shapes since the bright band is filling the Gaussian
beam only partially.
Chapter 3 – Configuring IRIS Products
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Summary of Contents for IRIS
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