ML092640166

From kanterella
Revision as of 08:01, 25 August 2018 by StriderTol (talk | contribs) (Created page by program invented by StriderTol)
(diff) ← Older revision | Latest revision (diff) | Newer revision → (diff)
Jump to navigation Jump to search
2009/08/28-Meteorological Fundamentals
ML092640166
Person / Time
Site: Indian Point  Entergy icon.png
Issue date: 08/28/2009
From:
Atomic Safety and Licensing Board Panel
To:
SECY RAS
References
50-247-LR, 50-286-LR, ASLBP 07-858-03-LR-BD01, RAS 284
Download: ML092640166 (16)


Text

"MC Obrempora", lad, an a Snapshot refers to a projection based on a initial set of conditions, persisted without change.L e.g., "straight line" Gaussian.Spatial refers to the ability to represent impacts on the plume after release from site.21 e.g., plume bending to follow river valley, sea breeze circulation.

k Temporal refers to the ability of model to reflect input data changes over time.e.g., change in release rate; meteorology.

U

  • SAII(A 100 t 4 47 Absorbed 3 I 20 EnryDsrbto I~~~~ Sinc th etblnevre safnto f A Tim of day Clu cover 0Surae oe" Veeain/ eet/Bdiso ae" Ura hea island--there~~00 isa0nqa itiuino nryars h earth, .casn difrne ntm ertr*n rsue Wete as we kno it is lagl th resul of thse dif rne ine eg itiuin O' V o d -Horizonta wid r0rae ydfeecsi oa prsurs bot loa and global.0 Win flw frmhge rsue*i asst oe prssr ai masses Sic th itiuino i assvres owns Lo e sufc wind tyia at night.0 Becus ofsraefitowidsed eeal inceas with height.. S *Grdin deed on sufc etueadtrblnei

~0 -S t- Sa 0 -I~~ Th tmeatur of thoetlyrofteamshr (toosphre geeal inrae wit decreasin hegh I Thi grdin is knw as th atoshei las rae On aveage the amspei las rat is abu +65 per kio ee of elevation Tyial reere to as0 del- in nucea poe co m nt By covnin las rat is alay th hihe elevtio te prtr les th lo e elvto tempeatur

  • ,4 A t-1 S SS S S 4k..- ý 0 '1 i t JLAI.6 Seosph I Ovral laps rate thrug thrpshrspstv LL I I .height) 0 ie. poiie wit decreasin I nheloerkiomte, aps rat vaie wit th al Thra grdet are cratd reulin in thermal curet an turbulence

-I 0topei stbiit is an ine of th amun of- -

A" Stblt I Untal Atmopher Poitv las rat (iceae wit derasn hegt Wame buyn ai nea sufc rises 0 Stbl Atophr N e g ti v l a s r at ( d c e a e Wit de c r a s n h e g h Littl or no vetia curn s di 00vo difso Motl at niht als knw as I er f --10 -u-- Stblt on DS s I ~ Cosie paclo irijce int th atmsper by a o resr m o i e o u y n o ce r s u e G a i n Parcel ~ ~ ~ dosntmxwt surrounding 0ai P a c e w il e x a n o r c o t a tA r P r e as th0 resr o i surudn th parcel

  • 0 0c0a0ng0es If prcelis ess ens tha G avtioaFrc th sur u dn air th pac lHgh P e s r wil rise~.As~~~~~~ th0aclepnso contracts, it 0em eaur n fiyoftSo Knw astedy daai laps rat Th atophr temperature*Is als changin as aucino th mesue atmospheri laps rate As such th pace movmen is a fucto of the mesue atopei lapse rate mesuedatmsr c lapse rae s tegratrth are 0 deg 5 s Shw her is a iuton-e prssr inrese wit 5 egS derasn hegh 10 deg Pace of ai rie slngA acliei