Use of X-band differential reflectivity measurements to study shallow arctic mixed-phase clouds

Mariko Oue, Michele Galletti, Johannes Verlinde, Alexander Ryzhkov, Yinghui Lu

Research output: Contribution to journalArticle

13 Citations (Scopus)

Abstract

Microphysical processes in shallow Arctic precipitation clouds are illustrated using measurements of differential reflectivity ZDR from the U.S. Department of Energy Atmospheric Radiation Measurement Program polarimetric X-band radar deployed in Barrow, Alaska. X-band hemispheric range height indicator scans used in conjunction with Ka-band radar and lidar measurements revealed prolonged periods dominated by vapor depositional, riming, and/or aggregation growth. In each case, ice precipitation fell through at least one liquid-cloud layer in a seeder-feeder situation before reaching the surface.Along period of sustained low radar reflectivity ZH (,0-5 dBZ) and high ZDR (6-7.5 dB) throughout the depth of the cloud and subcloud layer, coinciding with observations of large pristine dendrites at the surface, suggests vapor depositional growth of large dendrites at low number concentrations. In contrast, ZDR values decreased to 2-3 dB in the mean profile when surface precipitation was dominated by aggregates or rimed dendrites. Small but consistent differences in zenith Ka-band radar Doppler velocity and lidar depolarization measurements were found between aggregation- and riming-dominated periods. The clean Arctic environment can enhance ZDR signals relative to more complex midlatitude cases, producing higher values.

Original languageEnglish (US)
Pages (from-to)403-424
Number of pages22
JournalJournal of Applied Meteorology and Climatology
Volume55
Issue number2
DOIs
StatePublished - Jan 1 2016

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reflectivity
radar
lidar
arctic environment
Doppler radar
ice
liquid
energy
programme
radiation
indicator

All Science Journal Classification (ASJC) codes

  • Atmospheric Science

Cite this

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abstract = "Microphysical processes in shallow Arctic precipitation clouds are illustrated using measurements of differential reflectivity ZDR from the U.S. Department of Energy Atmospheric Radiation Measurement Program polarimetric X-band radar deployed in Barrow, Alaska. X-band hemispheric range height indicator scans used in conjunction with Ka-band radar and lidar measurements revealed prolonged periods dominated by vapor depositional, riming, and/or aggregation growth. In each case, ice precipitation fell through at least one liquid-cloud layer in a seeder-feeder situation before reaching the surface.Along period of sustained low radar reflectivity ZH (,0-5 dBZ) and high ZDR (6-7.5 dB) throughout the depth of the cloud and subcloud layer, coinciding with observations of large pristine dendrites at the surface, suggests vapor depositional growth of large dendrites at low number concentrations. In contrast, ZDR values decreased to 2-3 dB in the mean profile when surface precipitation was dominated by aggregates or rimed dendrites. Small but consistent differences in zenith Ka-band radar Doppler velocity and lidar depolarization measurements were found between aggregation- and riming-dominated periods. The clean Arctic environment can enhance ZDR signals relative to more complex midlatitude cases, producing higher values.",
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Use of X-band differential reflectivity measurements to study shallow arctic mixed-phase clouds. / Oue, Mariko; Galletti, Michele; Verlinde, Johannes; Ryzhkov, Alexander; Lu, Yinghui.

In: Journal of Applied Meteorology and Climatology, Vol. 55, No. 2, 01.01.2016, p. 403-424.

Research output: Contribution to journalArticle

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