PLANETARY BOUNDARY LAYER STRUCTURE IN THE MONSOON TROUGH REGION
DOI:
https://doi.org/10.54302/mausam.v45i3.2118Keywords:
PBL, Monsoon trough, Lapse rate, MixED layer, l nversion MonsoonAbstract
A ~IUt ly of PbllWIHI") lt cundury l.nycr (PUll in the lIIunsllun llflllgh !"l'l:illll ha:oo h! 't'11 Carrl,'t11l1l1
based on MONTDl EX 1989 pilot experiment d ata PilI. structure over land !>hllw'IO lAid l' , pati,11 lIn,1 tem poral
variatums. TIlrCCtypes of PRL- .'IOha llu\oli convective . monsoon ~11111 111) convective boundaryl a yers haw been obv-rved
. Ch ar act eri st ic features :I!I:"Ul"i:JI~lt wilh Jill"t'relll types of POL have been iJe- l\lilit... 1and p rcscnr c..t in th e p:Jlll'r.
With the help of observe...1rill ,structure over-eastern. ceutral and wcsrcm M'11m suf llu' ll1tlll~ IHn tmullii. ;1111"'1111'1has
h«'11 made to develop "PlIl '(" e ro s e-sec tio ns of PUL UH'r Ind o -G a ngetic plains llu rilli' act ive. wcuk ,lilt' bren k
monsoon co nd itio n s.
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