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Nonprecipitating Phenomena Seen by the S-PolKa Radar Nonprecipitating Phenomena Seen by the S-PolKa Radar

Nonprecipitating Phenomena Seen by the S-PolKa Radar - PowerPoint Presentation

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Nonprecipitating Phenomena Seen by the S-PolKa Radar - PPT Presentation

In AMIE ARM Science Team Meeting Washington DC 14 March 2012 R Houze University of Washington Summary Non precipitation features seen by SPolKa in AMIE Humidity Cumulus organization Cirrostratus amp altocumulus layers ID: 368907

humidity smart polka kazr smart humidity kazr polka nonprecipitating clouds cumulus ice pool cold layer moist anvil active zdr

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Presentation Transcript

Slide1

Nonprecipitating Phenomena Seen by the S-PolKa Radar

In AMIE

ARM Science Team Meeting, Washington DC, 14 March 2012

R. Houze

University of WashingtonSlide2

Summary

Non-

precipitation features seen by S-PolKa in AMIEHumidity Cumulus organizationCirrostratus & altocumulus layersAnvils of deep convection Slide3

Humidity gradient layers and nonprecipitating cloudsSlide4

Bragg scattering shows nonprecipitating cumulus in the moist layer

dBZρhvZDR

“Mantle Echoes” Knight and Miller (1998)Slide5

Long lines of cumulusSlide6

Lines of cumulus parallel to windSlide7

Slightly active moist layer

Clouds

building at cold pool boundariesSlide8

graupel

small ice

large non-melting ice

h

eavy

rain

m

elting

ice

Hydrometeor identificationSlide9

An anvil example

Doppler velocityHydrometeor typeSlide10

A stratiform region anvil seen by

bothS-PolKa and KAZRSlide11

Dual-wavelength humidity profilesSlide12

End

This research was sponsored by DOE ARM grant #DE

-SC0001164/ER-64752Slide13

ExtrasSlide14

S

KaNCAR S-PolKa

RadarSlide15

Examples of Humidity Features and Nonprecipitating Clouds Seen by S-PolKaSlide16

Humidity gradient rings and nonprecipitating cloudsSlide17

Nonprecipitating clouds and virgaSlide18

Cold pool examples seen in differential reflectivity (ZDR)Slide19

Humidity rings and anvil cloudSlide20

The “worm echo”Slide21

Upper-level cloud over KAZRSlide22

Slightly active moist layer

Clouds building at cold pool boundariesSlide23

More ExtrasSlide24

Gan KAZR and SMART-RKAZR

SMART-R24Generally agree well above 3-km heightSMART-R low level (1-3km) APBelow 1-km SMART-R ground clutter? Slide25

Gan KAZR and SMART-RKAZR

SMART-R25Note: color scale is different between two radarsZtop difference is about 1~2 kmSMART-R Ze is about 8 dB too high (Courtney), this has not been corrected yetSlide26

Rain over area scanned by S-PolKa