tes ncatio of greeougas. let's o is wole bunch of odel m hci, image

e's nteionagros indfentens witherent clate mde d sorth ad lne all ht twe're ju ooking at spr id onpixel on a tthose nuerat ar dayrises

the terates fm 2 re celsius ore t 7 orashn wn h ceae ikee spagttiagor ovious asonssrtof ly me ies yost the consensus too much inthisorthese solutions but what s deceivingis your e

ye, is drawn to the out liars going up and there's this number of a simations that have gdalittle by por stedy asid wh'sre lifoiar dn e fit wousur pritioar a omac riod78th 1d s. 1994somimwe lly geormaeaut eem ket does ha of ithns

here's again thisuor li yer iwouno toeltollfor moree nooo odel for hat thisiw i think the's some cedily about this. tha little ha to see but thiis a funny global projecti wre t mai ndof jstroll it outand it bemea rectangle - any a thhtihas ade i becseey t tr t he'tqu, 30 degreerth 6eeh ort tothe a is ringal

the ea inking thn in oars al henortpcific h. atwhy ogt uch in. 'rdetfle o e opifichigh. what's appening in these ate mulations s ho btrocal igorer less, ae stngtheninon the heand ifyoul in setle yomight m ened bec ilooks a or etwa eoefnoh.

ne. ere we juste snario 's poset arnamand his t mahated, is snevaand ishe raiofaril rsperiod surroundi 20ro90 u can sering he wer evatns o a e tiwe ch 0in is a grs

wose 0 ent thcpact it's not the sow th changes thhydro graph a you heard this morni. so this is octor hrough seber the aggravateded sira r off. more in he wter period, and less in the prg f yb ad tis that i e asystem wehad he lefedt

inall ge w st onch ia raining o 9ou f ove. ank ahaabh eche s ss e ain wainhrgho some watingut y htorasww ing o unof imdiaty h od iags a y stemat i ws a ua wheiteoftays ipio d oi1o987 ood whead vigh sn ve thee coernebond tha usthe blin

cafoia. xtthe dlth annexon pase. ana- we ys talk abousea leverise and i hea cuple of orders f magnitude ofesmas his morning anone of h was more ke hiswe ts i the mrv mate te hge n sea eu eot d

or undea evf se m t dotoo much but heit's couple wh htand storenoaybe

toa f ds e th this i83 iangoa. wet's gn neo. hohe tueevel record. in the pay da, t'snojust sea lel risbut the fact that whe fre wtefloods. this is te level that ic street water auge in sacramen. darn this thing. ay. those are tdes. mostly summeri, b tharfds u an seyu know thwar evels geut e merthere s acal rihennsewhich

a istofevieillangto co we act is sort fhing coontlleo equent and otal r. i don't tound like he on quirerw count,u tkeootelsandok at s nhis is ope coasnw tooa cordoted te umber mei smu wherwe includ idnd s, mis 30ceimets or hh year period. notee ft abo. li more tan one foot.

the are ceedg ove a vel that appensless tha once yearand ou can see, over timhow often those get exceeded. i n'go into filiee re t's go o the next one. yosed m c- sug ihipod you kn thpogmag cle program csind ha ay tste of rnia i- ndful ace wrkecaus yo, have th arad ually a rich cic coitn e hp

thti inin nebraska, guys. any way, california ity elot of different wa. do we have anybody from nebraska here? the magnitude of the impacts of climate change going back to the different emission change, get much worst f the gbal greenhouse loading takes ts higher rather than lor route. and the greenhouse loading in thatmosphere, which i should have sd earlier is a big problem not only because of it's physics, but because o

it's longevity. co 2 has a lifetime of more than a hundred ears some what we do is compound n the atmosphere and that's wy the analogy was this b bge. we can't change it rapidly. it does ot rain out. this thing is there for generations. next ne. it's already happening. there's no doubt in the climate commities mind. the precipitation of course, is an enormous issue for you guys but i don't think yur ever going to see with a big degree of confidence a projection you can believe. you're going to have to live as yor cmus a

t you nt otact that is gointo gt wme and s levels are going g higher. you can count on t fact that lot of these s are oing

the tus o hat,somes havregnaorcstal, not n b meing alifni va not totay uated m nog this s asolv prlem. um gap s watokwh's gog n cera, et cete.

but in fact the earth response

to climate s not oing tomake too much difference ntil about the mdle part of the century between allthose scenar through 2050 a clatmodelis sort ofalimatmodel no atter whatyou do with it. in fact if you top all co2 emissions today. fossil fuelis thereason it's increasing becausfossilmeans it's tored in the ground and w we're putng it in the air and burning it. it's recycleby the ecosyst and so foh. if wstoed verything tda 's stitethere's anoer half degree and full degree of warming inte syst bec the earth is not ina bce. that's why we're warming uh f s of

tch isogcd monk a is d thaa soro obsessivguy hungp o s u're hng up n 21. itean thesvel willop isi t 200. e waa ebaton hmuch siafoh. as ast h is aa wk o urselve

mn and pple n e le o y

eyea gd sta w m i inthe ls acup of his i tho ould riey his morninseation,d that utityonverse almingnd we're fy prmac,e loupo chngad gs ave r anoapt a woked t lim chs in1990 at mt ok touhe pusought aeoardrkops onhe imatns r he tu. we reatd xeise a decaten panel cme anoon

how srt plannin global warming. was pragmaticd the liciesweradopted unously. i r myagency runs thgamut in terms of political areas. veryliberal areas ike santa monica to quite conrvative to parts forange countyand veral aeas troughout our enti seice aea. was never partisan but what we nd to o as an issue. i find i intereg this is interesting b in utiliti issues, it'more hoare yu epared. tend to gt ur water wee cky because we have iversified water upply.

four ajor soues i sther california and becau their from dict thigh droe logical arwe tend to not ve them dry a the same time it's one of our primary areas or dfenses, we get colorado okaykay, nthcalifornia, and local in our sout californiaregion thatupplies almost half the water we use d then thugh one ofour member ancies city of os angeles he east sis a this yeais it's becomg depress ingly clear and 07' is shaping up tt al f heare well