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Integrated lidar backscatter: Quantifying the occurrence of supercooled water and specular reflection Robin Hogan and Anthony Illingworth Enhanced algorithm for supercooled water detection (Hogan et al. 2003, QJ in press) Specular reflection could be a problem for nadir-pointing EarthCARE lidar: how common is it?

Robin Hogan and Anthony Illingworth

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Integrated lidar backscatter: Quantifying the occurrence of supercooled water and specular reflection. Robin Hogan and Anthony Illingworth Enhanced algorithm for supercooled water detection (Hogan et al. 2003, QJ in press) - PowerPoint PPT Presentation

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Page 1: Robin Hogan and Anthony Illingworth

Integrated lidar backscatter:Quantifying the occurrence

of supercooled water andspecular reflection

Robin Hogan and Anthony Illingworth

• Enhanced algorithm for supercooled water detection (Hogan et al. 2003, QJ in press)

• Specular reflection could be a problem for nadir-pointing EarthCARE lidar: how common is it?

Page 2: Robin Hogan and Anthony Illingworth

Introduction

• The integrated backscatter through a cloud of optical depth of is approximately (Platt 1973):

– k is the extinction/backscatter ratio (18.75 sr for droplets) is the multiple scattering factor (~0.7 for the CT75K)

• For large optical depth it reduces to (2k)-1

• If z1 and z2 encompass the 300 m around the strongest echo in a profile, we can identify thin liquid water layers with greater than, say, 0.7

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Page 3: Robin Hogan and Anthony Illingworth
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Results for lidar 5° from zenith

• Chilbolton 2000– Occurrence of supercooled layers with > 0.7

Page 6: Robin Hogan and Anthony Illingworth

Results for zenith pointing lidar

• Chilbolton 1999– Enhanced occurrence between -10 and -20°C

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Supercooled water in models

• A year of data from the Met Office and ECMWF– Easy to calculate occurrence of supercooled water with > 0.7

Page 8: Robin Hogan and Anthony Illingworth

Specular reflection

• Specular reflection from planar crystals can occur within 1° from zenith or nadir– Enhanced backscatter with no accompanying increase in

extinction: very low k – Integrated backscatter in ice can exceed the asymptote

corresponding to optically thick liquid cloud (recall ~(2k)-1)

• To quantify, require lidar to be precisely at zenith: 20 days of data obtained so far at Chilbolton– Algorithm calculates integrated backscatter from 2 km up– Specular reflection deemed to occur if this integral is more than

1.05 times the asymptote for liquid water– Excess above this value is attributed to pixels with highest – But allowance made for common scenario of liquid above ice

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Results

• Around 23% of ice cloudy profiles affected– Specular reflection in 20% of

cloudy pixels at 4 km– Big problem for interpreting

backscatter measurements

• Must analyse more data– Use model for temperature:

specular reflection only for plates between -9 and -23°C?

– Problem solved with a high spectral resolution lidar?