tell me when to go
jesus christ wore dreads, so shake em!
mofukas in tah atmosphere be shakin them dreads, classic late spring baroclinic steelo goin dizzown.
real deezy late winter spring seaseezy goin down. why? thank that coooooold pool smokin dubs round tha north pole. mad potential vorticity jus’ waitin to crack a bottle an make north dakota wobble. apologia word socrates. example:
ery’ octopussay droppin off tha centa swirl iz sum a dat mad tropo droppin. when that shiyat goes down, hoes be bumpin heads tryin ta get in yo house. that cold pool supplies mad potential vorticitay. when tha uppa level IPV getz supaimpozed on tha lowa IPV we getz mad cyclone deeeeevelopment
when that tropo be droppin in we got hella goodies in front o this mofucka.
every term in tha isentropic potential vorticitay equation be greata than zero. stabilitay, friction an tiltin. gimme sum diabatic ass heatin an friction to hit me with tha cyclone developmtizzle.
that blue drop offshor a tha bay iz that lil shorty thats hollerin. to tha right, stretchin, convection, latent heat release, and cylonic spizzin like daven rims. convectin action warms them cloudz by releasin latent heat. hometown on my face forty five in my lap. warmin getz tha expansion. thanks to that hyposometric equation, minus rho g deezee this moves air out tha column. thats divergence. dee u dee x plus dee v dee y. makes it rain on them hos.
what?
letz look at that from tha full ass perspectiv. excuse my propa language i’m thinkin science. hyphy in tha house tho. california license plates ridin through the ATL.
we can undastand thiz shiyat froma sea leva perspective dis way. all yall gangstas know low sea level pressa means chronic straightlines and droppin stupid doo doo dum aiyeeer aiyeeers.
sea leva pressa be given by horizonta advection ( minus U dee u dee x minus V dee v dee y) plus boundary laya pumpin minus uppa leva divergence minus latent heatin. so muthafuckin what. heyers what.
baroclinic instabilitay (mad temperature gradient (blue versus red in tha above image) makes a rossby wave. thanks to IPV conservation this shiyat starts as MJO based convection and getz bounced norte to sud and back a bunch. all kindz a crazy shiyat happenz ova tha pacific. dukes of hazard doors in compton we call em suicides. el nino la nina pda blah blah. anyways the up an down droppin makes waves. rossby waves yo. as this shiyat rolls inland an tha disturbance deepens into a consolidated pressa system an hooks up wit tha polar an subtropic jet (OH BY THA MUTHA FUCKIN WAY. BITCHES THAT BE TALKING ABOUT SUBTROPICAL JETS MOST A THA TIME DONT KNOW SHIT. mad difference between subtropical tap (hits wit a clap) and subtropical jets (bout as good as tha Mets). NWS talks bout that subtropical tap, fools mix it up an think bout tha jet. no. that shit is tha SOUTH BRANCH O THA POLAR JET!) back to SLP. as that SLP dropz, the pressa gradient one ova minus rho grad p startz spinnin circulation around tha low. lil bit o boundary laya pumpin makes upper leva divergence increase fasta, an tha low deepens (gets low, to tha flo beyotch!). air goin up makes cloudz an we get the above discussed shiyat. precip ensuez. latent heatin keeps warmin shit, mass keeps bouncin outta that mofucka an SLP keeps droppin. now we got a $$ low. in front, warm air advection (why stormz be warm comin in) as tha low passes we get cold air advection (cold ass bluebird days with sticky icky pow shreddilationation). warm an cold air be gettin wrapped up like rubbas. this cause thizz dancin an changez up tha temperature gradients and thermal windz. az tha low pumpz tha brakez an slowz down behind tha max divergence tobecontinued
problem iz she’z chillin out an stallin offsho. ruc 6hr to 30 hr got tha low in tha same damn place! now whoz got tha party out der? ain’ no party like a offshore buoy HELL NO. move in beeyotch!
probly lookin bout 4-8 inches o sticky icky from this first wizzave.
real good shot to peep iz tha theta heightz from u of u
mmmmhmmm
