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<br /> <br /><::'~Q. <br />\~\>~ <br /><2.+ (.\).. <br />1/IG..~ <br />, f- :;)-'--\: L\ t <br />( l r' <br />LA 0\ ~ j <br />We) (V..... <br /> <br />ii..: <br />r=:-- <br />L- <br />L <br /> <br />. ~ <br />!-_-- <br />!: <br /> <br />f- <br />i <br /> <br />, <br />J ~ <br />, <br /> <br />i: <br />r--- <br /> <br />!- <br />!' <br /> <br />, <br />i- <br /> <br />,- <br />. <br /> <br />! <br /> <br />'- <br />.- <br />i- - <br />i:- <br />~ _i_ <br /> <br />L <br />!o <br />:-:- <br /> <br />-~ .. <br /> <br />3rv~~i~g a~d :!c~k (~982) ~ot on~y n3d the ~enefit ot se~~al rawinsonde <br /> <br />~~~~ b~= c~so ~cj s2~e~li~e d2~a to clarify ~~e kata~atic or split-front <br /> <br />f:.rs:- des~ribed <br /> <br />..Jj- :-!~les (:i962). <br /> <br />sc~ematic model from <br /> <br />Figure 14 is e <br /> <br />3ro~~i~g ~~~ Mc~k desc~~bi~g a kata~atic fro~t. <br /> <br />Note ?art~~ularily the <br /> <br />- - . <br />relB.:.:.ve <br /> <br />~- . <br />l.oC=.::J..O!: <br /> <br />the warm <br /> <br />cold =ront, <br /> <br />f:-cnt, <br /> <br />0= C1e <br /> <br />s~rface <br /> <br />the u::mer <br /> <br />co:'li <br /> <br />=rG~t a~~ ~he Sh field. Since b8th the British Isles and California lie on <br /> <br />the e2st side of t~e'At~arrtic and Pacific Oceans, respectively, this <br /> <br />st:Qges~s <br /> <br />!:ne <br /> <br />DossibE~tv <br />~ . '" <br /> <br />that each area experiences similar synoptic <br /> <br />~ea=~er Datte~~s. <br /> <br />--,~ se~~lOL c detai:ed ti~e-height analysis of ~he passage of a <br /> <br />ka~~~a~ic frc~t based S~ 5E~ 3-~ourly rawinso~de data ~~l: ~e presented. <br /> <br />.~~ Ly~a~~cs of t"e airf~o~ 2,-C the ~~crophysical processes in the shallow, <br /> <br />5~3~~e c~cg~apiic ~:C~~ ~allo~ing the passage of the upper level front <br /> <br />~l~~ ~e ~rese~~eG. <br /> <br />Fig~re 152-= is a ~~ce-heigh~ cross-sec~io~a: analysis of Sheridan <br /> <br />ra^~csGcie da~a fey r.r:e stern: on lL Yeoruarv 1983. <br /> <br />A nu~~e~ of feat~res <br /> <br />a~e re~e2~e1 !; eac~ figure: <br /> <br />the ~ropopause (TROP), the upper level front <br /> <br />(T~- !:""; <br />- ....--- _:, <br /> <br />near 3.5 k~ and the ~arm =ror.t (WF). <br /> <br />staY!.e lave~ <br /> <br />(SL1 <br /> <br />5~~!aCe cold fron~ could be ide~tifieri. <br /> <br />A~ead of the ULF ~he cloud tops <br /> <br />~e~e 9 tc iQ kG ~ith te~~erctures near -550C. Following passage of the ULF <br /> <br />. - c:c~~ tC?5 drcpped dra~Etically to ~3.5 k~ with temperatures of -5 to <br /> <br />~he 21:i~4~e 0= ~he TROP was well defiLec cn all soundings and <br /> <br />Ye~a~~eQ ne~~ee~ lO and 1: km. <br /> <br />Behind the ULF the air was neutrally <br /> <br />~~cyaLt a~c very dry. <br /> <br />Co~seq~e~tly, T only a~pears to have decreased a <br /> <br />~~~,. a3o~~t ~hile tte j l~~es rose ~.e. tilted drc~atically Epward. The <br /> <br />38 <br /> <br />'-,-~ <br />~:-~ . <br />-~t - <br />-,1 <br />,{ <br />I <br />I <br />'I <br />I <br />i <br />t <br />1 <br />1 <br />I <br />I <br />t <br />. <br />I <br />-I <br />I <br />I <br />.1 <br />I <br />! <br />i <br />f <br />i <br />, <br />j <br />! <br />i <br /> <br />No <br />