robin hogan ewan o’connor the instrument synergy/ target categorization product

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Robin Hogan Ewan O’Connor The Instrument Synergy/ Target Categorization product

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Robin HoganEwan O’Connor

The Instrument Synergy/Target Categorization

product

The Instrument synergy/Target categorization

product • Makes multi-sensor data much easier to use:

– Combines radar, lidar, model, raingauge and -wave radiometer– Identical formatIdentical format for each site (based around NetCDF)

• Performs common pre-processing tasks:– Interpolation on to the same grid– Ingest model data (many algorithms need temperature & wind)– Correct radar for attenuationattenuation (gas and liquid)

• Provides essential extra information:– Random and systematic measurement errorsmeasurement errors– Instrument sensitivitysensitivity– Categorization of targets: droplets/ice/aerosol/insectsdroplets/ice/aerosol/insects etc. – Data quality flags:Data quality flags: when are the observations unreliable?

Ice

Liqu

idRai

n

Aeros

ol

Inse

cts

Target categorization• Combining radar, lidar and model allows the type of cloud

(or other target) to be identified• From this can calculate cloud fraction in each model gridbox

Melting layer identification

• Look within 5ºC of Tw=0ºC isotherm in model– Melting layer is where

greatest divergence in radar Doppler velocity

Z v

Classification

Divergence

Melting ice

Model variables• T, q, p, u and v taken

from model or sonde:– To correct for radar gas

attenuation: T, q, p (but saturated where cloud observed)

– To correct for radar liquid attenuation: estimate LWC profile using scaled adiabatic method (T, p, LWP)

• Subsequent algorithms:– E.g. IWC method requires

temperature– Cloud fraction on model grid

requires advection speed

Radar sensitivity• Z_sensitivity variable is estimated as a function of height each day, using the Z distribution– Includes range-squared

law, mean gas attenuation and ground clutter

– Used for iwc_sensitivity and to modify model cloud fraction

• Code tries to avoid erroneous Z values below the real radar sensitivity

• Also calculated:– Z_bias: calibration

accuracy– Z_error: random error

Incorrect Z_sensitivity!

A day of Z values

Example fromUS ARM site:Need todistinguishinsects fromcloud

Now applied to ARM data

Ice

LiquidRainAerosol Insects

• Currently use two of the four modes (robust + rain) as others can have artefacts that lead to erroneous cloud fraction

• Recently use simple merging of ceilometer and micropulse lidar