poster draft 2 - the conference exchange€¦ · poster draft 2.pptx author: joe finlon created...

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A Comparison of X.band Polariza4on Parameters with In.Situ Cloud & W.band Radar Measurements in the Comma Head of A Winter Cyclone Joseph A. Finlon 1 , David M. Plummer 1 , Robert M. Rauber 1 , Greg M. McFarquhar 1 , Brian F. JeweN 1 , Kevin R. Knupp 2 , David Leon 3 1 Department of Atmospheric Sciences, University of Illinois at Urbana.Champaign, 2 Atmospheric Science, University of Alabama, Huntsville, 3 University of Wyoming Atmospheric Science 1. Objec4ves Analyze the ver4cal change of dual.polariza4on parameters (from ground.based radar) within the 22 February 2010 cyclone during the Profiling of Winter Storms (PLOWS) field campaign. Relate these findings to coincident in.situ cloud microphysical measurements. 2. Data Both the Mobile Alabama X.band (MAX) Doppler Radar and the W.band Wyoming Cloud Radar (WCR) profiled the comma head region of a cyclone as the NSF/NCAR C.130 aircra\ made ver4cally stacked passes along the same azimuthal angle as the MAX RHI radar scans. Fig. 1 The MAX radar measured reflec4vity (Z) and radial velocity, as well as the correla4on coefficient hv ) and differen4al reflec4vity (Z dr ). Fig. 2 The two.dimensional cloud (2D.C, above) and precipita4on (2D.P) probes captured par4cle size and shape along with other variables. Fig. 3 WSR.88D regional radar for 0045 UTC 22 February 2010. The MAX radar loca4on (pink triangle) is shown, with the black line outlining the scanning direc4on and flight path of the MAX and C.130, respec4vely. 4. Dual.Polariza4on Measurements S N 5(a) Fig. 4 (a) WCR reflec4vity cross sec4on for the same path as (b.d) MAX RHI variables. Pink dot in RHI scans denote the loca4on of the C.130 aircra\, with average values of Z, ρ hv , and Z dr as the aircra\ flew toward/away from the MAX radar. Same as in Fig. 5 but at a different aircra\ al4tude. 5. Microphysical Measurements 4 4.5 5 5.5 6 6.5 7 7.5 8 Al(tude [km] Fig. 6 2D.C par4cle images taken at four specified al4tudes, with a notable shi\ in crystal size and composi4on at lower al4tudes. 1.6mm Z [dBZ] ρ hv Z dr [dB] Fig. 7 Plots of (a) size distribu4ons, (b) concentra4on, (c) IWC, (d) median mass diameter, and (e) mass.weighted area ra4o for four different al4tudes within the cyclone. Increasing par4cle size deeper within the cloud support par4cle growth by aggrega4on as in Fig. 6. Current work is examining linkage between area ra4o and Z dr data on a point.by. point basis. 3. Methodology Reflec4vity and dual.polariza4on variables from the MAX were averaged at specific C.130 al4tudes during 4mes when the aircra\ was close to the X.band radar. 2D.C images, as well as size distribu4ons and corresponding bulk parameters determined from 2DC/2DP probes, were used when the C.130 was in the view sampled by the MAX RHI scans. 6. Conclusions Dual.pol measurements of ρ hv and Z dr are consistent with more uniformity in par4cle shape and larger par4cle size deeper within the cloud, respec4vely. Corresponding probe data suggests that growth by aggrega4on is occurring during the par4cle’s descent (no liquid water is present at these levels for riming to occur). Uniqueness of coincident ground. and air.based measurements of the same cyclone region give further insight into the MAX radar’s dual.pol values. Acknowledgements This research is funded by grant NSF.AGS.0833828 . Thanks to the University of Alabama in Huntsville for data collec4on through the use of the MAX radar. Contact [email protected] www.joefinlon.me Al4tude [km] Time [UTC] Distance [km] 20 40 60 80 Sensi4vity of WCR makes it beNer able to detect weak echoes. C.130 flight track Reflec4vity [dBZ e ] 20 40 60 80 Distance [km] Time [UTC] C.130 encountering merging of ice par4cles deeper within the cloud. (b) (c) (d) Distance from Radar [km] Al4tude [km] Z avg = .14.8 dBZ ρ hv,avg = 0.48 Z dr,avg = 1.4 dB 4(a) (b) (c) Z avg = .3.9 dBZ ρ hv,avg = 0.86 (d) Z dr,avg = 2.9 dB S N Distance from Radar [km] Higher values indicate par4cles fairly uniform in size and shape. Higher values are consistent with larger, more dense crystals. MAX Radar (01:05 UTC) MAX Radar (02:35 UTC) Growing size suggests aggrega4on of crystals is occurring. LiNle increase in par4cle concentra4on Al4tude [km] N [# liter .1 ] Increasing IWC IWC [g m .3 ] Increasing par4cle size Al4tude [km] D mm [μm] Mass.weighted Area Ra4o General trend consistent with more circular par4cles (except for lowest al4tude) Higher concentra4ons of larger par4cles deeper within cloud. D max [μm] N(D) [cm .4 ]

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Page 1: Poster draft 2 - the Conference Exchange€¦ · Poster draft 2.pptx Author: Joe Finlon Created Date: 9/17/2013 5:18:11 PM

A"Comparison"of"X.band"Polariza4on"Parameters"with"In.Situ"Cloud"&"W.band"Radar"Measurements"in"the"Comma"Head"of"A"Winter"Cyclone"

Joseph"A."Finlon1,"David"M."Plummer1,"Robert"M."Rauber1,"Greg"M."McFarquhar1,"Brian"F."JeweN1,"Kevin"R."Knupp2,"David"Leon3"

1Department"of"Atmospheric"Sciences,"University"of"Illinois"at"Urbana.Champaign,"2Atmospheric"Science,"University"of"Alabama,"Huntsville,"3University"of"Wyoming"Atmospheric"Science""1.  Objec4ves"

• Analyze" the" ver4cal" change" of" dual.polariza4on"parameters"(from"ground.based"radar)"within"the"22"February"2010"cyclone"during"the"Profiling"of"Winter"Storms"(PLOWS)"field"campaign."• Relate" these" findings" to" coincident" in.situ" cloud"microphysical"measurements."

2.  Data"Both"the"Mobile"Alabama"X.band"(MAX)"Doppler"Radar"and"the"W.band"Wyoming"Cloud"Radar"(WCR)"profiled"the"comma"head"region"of"a"cyclone"as"the"NSF/NCAR"C.130"aircra\"made"ver4cally"stacked"passes"along"the"same"azimuthal"angle"as"the"MAX"RHI"radar"scans."

Fig." 1" The" MAX" radar" measured"reflec4vity" (Z)" and" radial" velocity,"a s" we l l" a s" the" co r re l a4on"coefficient" (ρhv)" and" differen4al"reflec4vity"(Zdr)."

Fig." 2" The" two.dimensional" cloud"(2D.C," above)" and" precipita4on"(2D.P)" probes" captured" par4cle"size" and" shape" along" with" other"variables."

Fig." 3" WSR.88D" regional" radar" for"0045" UTC" 22" February" 2010." The"MAX"radar"loca4on"(pink"triangle)"is"shown,"with" the"black" line"outlining"the" scanning" direc4on" and" flight"path" of" the" MAX" and" C.130,"respec4vely."

""

4."Dual.Polariza4on"Measurements"

S" N"

5(a)%

Fig."4"(a)"WCR"reflec4vity"cross"sec4on"for"the"same"path"as"(b.d)"MAX"RHI"variables."Pink"dot"in"RHI"scans"denote"the"loca4on"of"the"C.130"aircra\,"with"average"values"of"Z,"ρhv,"and"Zdr"as"the"aircra\"flew"toward/away"from"the"MAX"radar."Same"as"in"Fig."5 "but"at"a"different"aircra\"al4tude."

5."Microphysical"Measurements"

4"4.5"5"

5.5"6"

6.5"7"

7.5"8"

Al(tud

e%[km]%

Fig." 6" 2D.C" par4cle" images" taken" at" four"specified" al4tudes," with" a" notable" shi\" in"crystal"size"and"composi4on"at"lower"al4tudes."

1.6mm"

Z"[dBZ]"ρhv"

Zdr "[dB]"

Fig."7"Plots"of"(a)"size"distribu4ons,"(b)"concentra4on,"(c)"IWC,"(d)"median"mass"diameter,"and"(e)"mass.weighted"area"ra4o" for" four"different"al4tudes"within" the" cyclone." Increasing"par4cle" size"deeper"within" the" cloud" support"par4cle"growth"by"aggrega4on"as" in"Fig."6."Current"work" is"examining" linkage"between"area"ra4o"and"Zdr"data"on"a"point.by.point"basis."

3.  Methodology"• Reflec4vity" and" dual.polariza4on" variables" from" the"MAX"were"averaged"at"specific"C.130"al4tudes"during"4mes" when" the" aircra\" was" close" to" the" X.band"radar."•  2D.C" images," as" well" as" size" distribu4ons" and"corresponding" bulk" parameters" determined" from"2DC/2DP"probes,"were"used"when" the"C.130"was" in"the"view"sampled"by"the"MAX"RHI"scans."

6.  Conclusions"• Dual.pol" measurements" of""ρhv" and" Zdr" are" consistent"with" more" uniformity" in"par4cle" shape" and" larger"par4cle" size" deeper" within"the"cloud,"respec4vely."•  Corresponding" probe" data"suggests" that" growth" by"aggrega4on" is" occurring"during"the"par4cle’s"descent"(no"liquid"water"is"present"at"these" levels" for" riming" to"occur)."• Uniqueness" of" coincident"ground." and" a i r .based"measurements" of" the" same"cyclone" region" give" further"insight" into" the"MAX" radar’s"dual.pol"values."

Acknowledgements""

This" research" is" funded" by"grant" NSF.AGS.0833828."Thanks" to" the" University" of"Alabama"in"Huntsville"for"data"collec4on" through" the" use" of"the"MAX"radar."

Contact""

[email protected]"www.joefinlon.me"

Al4tud

e"[km]"

Time"[UTC]"

Distance"[km]"20" 40" 60" 80"

Sensi4vity"of"WCR"makes"it"beNer"able"to"detect"weak"echoes."C.130"flight"track"

Reflec4vity"[dBZe ]"

20" 40" 60" 80"Distance"[km]"

Time"[UTC]"

C.130" encountering" merging" of" ice"par4cles"deeper"within"the"cloud."

(b)%

(c)%

(d)%

Distance"from"Radar"[km]"

Al4tud

e"[km]"

Zavg"=".14.8"dBZ"

ρhv,avg="0.48"

Zdr,avg"="1.4"dB"

4(a)%

(b)%

(c)%

Zavg"=".3.9"dBZ"

ρhv,avg="0.86"

(d)%

Zdr,avg"="2.9"dB"

S" N"Distance"from"Radar"[km]"

Higher"values"indicate"par4cles"fairly"uniform"in"size"and"shape."

Higher"values"are"consistent"with"larger,"more"dense"crystals."

MAX Radar (01:05 UTC) MAX Radar (02:35 UTC)

Growing"size"suggests"aggrega4on"of"crystals"is"occurring."

LiNle"increase"in"par4cle"concentra4on"

Al4tud

e"[km]"

N"[#"liter.1]"

Increasing"IWC"

IWC"[g"m.3]"

Increasing"par4cle"size"

Al4tud

e"[km]"

Dmm"[μm]" Mass.weighted"Area"Ra4o"

General"trend"consistent"with"more"circular"

par4cles"(except"for"

lowest"al4tude)"

Higher"concentra4ons"of"

larger"par4cles"deeper"within"

cloud."

Dmax"[μm]"

N(D)"[cm

.4]"