Academic literature on the topic 'Hôpitaux Décès'

"eppeirsocdeenst . oTfhtehequm as oir -e glm ob aarlkesd ca lEeN se SaO warm ture (SST) patterns associated wistuhr fa E ce Ntaenmdpceorlad ­ R bution of rainfall as a functio SO that sta ogpees le w of skEiNaSnOdcHaanlpoefr te tn1b9e9no5i ) d . efBEeNcS au Ose st tah te e ( eea .g., influence these rainfall patterns appear consistently in more before typical ENSO-ntified a season r o ly rfmoarnryecreencten de tcsa tu d d es ie , s P -ar kee .g r ., anHdsF iu o n ll ganadnd19N9e1wseilnlc1e9t8h3ereepc is oogdneith io ansiomfp th oer ta e n ar tlyprsetdarg el easteodfdarodu ev gehltospcionmgm EN en ScOe, late Idne in nt eitfe ic eanttihonc entury. However, one of th ic e t ive m value. precipitation relatio onfs hip tshepsreo vid ceo ain limitations sntsh is etecnlte are E st NiSnO di -­ E ac NcS or O d -in b g as teod th s e ea h so is ntaolr ic parlerdeicco ti rodn , EsN ch SeOmeissaicst iv tehaot, fce ation that seasonal meteorological drought in quite its warm or cold phases only about half the tim ienux se te fnuslisvkei ll a r ( e i. aes , ionftthheehg is lo to bre ic m al aryecboerdp , reEdN ic S ta O b -l reelw at i e th d S co in ld ce 1e9p0 is 0 o , dteh er yeeahrasv , e b ac eceonrtdhiinrg ty w to a rm th aendSnoiunteh te e e rn n . idtnryth con he aepspedroa it prie on r a ia s s ). occu te Fsiegaursroeat2 leas ns, .3 whsth7o5wsp ere p e th rocse recip entre of the time Osc itatio gi nondse , fiacn it dsJSoonue il s l at ( i1o9n87 In ) dex-based criterion of Ropelewski and are strongly associated with the warm or cold phase equa th to errinalPOas . c The cif il ilca tio clos se n a su Iendreex la tio (S n O sh I i ) pbaentdw ee cne nt trhaelo tu freEsNiSnOth -e i t . reo ., piw ca alrm ea sotrPcaoclid fi c s . eaAlstuhro face tempera­ d rface temperature anomaly may not occur consistently with every wuagrhmdorroucgoh ld tFu ig r u in durin re ggm2.4o all . s t su Ioffptr he twentieth century is illustrated in ENSO episode as appropriate, these regions do have a dr ch E ec N ip SiO ta ti eopn is owdeerse , sbku il tfun ll oytportehdeircw ta ibslee , tch le aanr -l n y or i m de anltsie fi aesdo na ilncco re nadsie ti d o ns p . r T ob haebliiln it k y wi o th fEdN ri SeOr-r th es eouotuigrm ht p ce e s . H re odw ic etv io enw managed r, ecvroouplsdm on ulsytbbeeppolsasnitbeldeaabnoduwtahtaelrfcba il n it ybedifso tr rim bu al tiisoend by ca ery year. s condi ltciuolnaatl in ognptrheecisptiattaet io onfEpN ro SbOa . ­ m ho awneyvedrr , ouEgNhSt-Op ro is nenortegtihoensonAlsy is disc . The farce to la r u ssed tiv in el f y lu ebnec lo in w g , T hi h st uosripcrae ll c y ip o it bas ti eornvepdr edic recent shif ttison in sctahnebperobb as aebd il iptuyredliysto ri n ­ g at a m in ossipnhu er nedesryssttaenmditnhg ro oufgch li m EN ate S O as satucdoiueps le h d as olceedan to -." In Droughts. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-40.

"After the mid-1970s, the low values of the SOI were hnaovteab cc eoemnp th aeniceadsebybedfrooruegthhtastats im wei . despread as would itm hese apparent changes demand so mAet th st eud ve yryolfea th st e , sta p ti lsitciactailom ns e th fo ordsseoarso cl niaml at peremdo ic dteilosn . , whether with The strength of the relationshi Nino-Southern Oscillation and ps Aubse tr taw li eaennctlhiemaE te l ----- t eo (1 ro 9l9o3 gic va fsoyrs ri te a m tio sns fo mrecaln im s ecast schemes atthe at i a re prted is icrteiloan ti , vealnyds em ismep ve le ratlodd if efveerleonpt different organisations -s eorm gi engg . ov Seor , n m in e n th teagfeuntcu ie re s , , ----- d so is m tr eibpurtiivnagtef or oercgaasn ts is fao ti rodnrsou -g hwti . llTbhe is p se re em pa sriln ik g and lead to confusion, since the systems and forecast eslywtio ll differ. In the past, such confusion has at times led consumers to doubt the credibility of the forecasts; such doubts will continue to arise. strategies to deal with an increas W ing e m nu u m st bdeerv is oef A (p uosttern al tiiaalilsy to cboenn fl eifcittin fr g o ) mftohreecparsetds ict oafb il d it ryopurgohvti , deidf ibsyntohteoEvleN rc ionmo-eS , oAuutshte ra rln ia Owsicli lllcao ti notn in . uIefttho is bceha su ll bejnegcet to th South eeerxnceO ss climate variability produced by El Nino- tive aspects o sc fitlh la etipohnew no it m ho euntong ’ asin in in fl guefn ro ce m . the posi­ Beth Lavery provided the drought time series for FTihgeurSeO3I . 1 v . alCua es rs tfeonr Frederiksen p the figures we rroevipdreodviFdiegdurbey3t . h3e . Bureau of Meteorology’s National Climate Centre." In Droughts. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-56.

"m of ona itoring is therefore an important component as US$5,while the importin real-ti nmyedm ro oungih to t rin p g re p m ar eetdhnoedsssuss tr eadt eg iines. Ke TnhyeatbiamgesofasmhaiigzheadsurU in S g $ 2a0dw ro g price fo it uhg in htapsepra io rdtihse so sa mmee ­ d n (d eip sc eunsdselda rg aeb ly ovoen ). th Seom raingauge network design three months. Such drought industries omftuwsotb to eisnucclhudreedc or sdas te l h li atvee -d enro iv t ed e rece be erna in cfaanltl me libr eas te ti t m ho a ds have discouraged. rainfall es d fo te r s , pob in utt8dFiiangannocsiiasl , prreesdoiucrtcieosn , faonrdddrroouugghhttpm re opnairteodrn in es g s , t to hreingg lo bmaettih mates in Kenya. Other drought moni­ are limited in Kenya. Kenya has, however, 3 Efficient lccoloi ds de mmm at uenc pend ic eanttiroeson (e . cgl . i , mEaN te SpO ro ducts from invested heavily in meteorological training, edu­ for the collection, dis n facilities ar feo re re ca qsutisr ) e . d9cTa im tio e n ly , an a d va bia la si bcilfia ty c ilit o ie f s. drought products and ndeattwa/ o in rk fo irsm ation. Th seemaivnaaitliaobn le , acnodmem xc uhnaincgae ti oonfm ser e v te ic oerso lo fr g o ic m al g se lo rv bia ce lsc in li mtahtee re cgeinotn re s r el Myaonny4pRreespeaarrecdh nes nsoatndadeeaq rl uyaw te arfnoirng an syesftfeem ct . ive drought tdhreo ug d h ev tea lo dpve is d o ri w es orflrdo . m Su th cehcp li r m od at uectcsenitnrcelsudoefadcrto io ungsh . t pr ios ce re s q se usira ed to understand the complex ENSO advisories and global circulation data. very limi R te edso in urK ce esnyfaon . rdm th e e te ir orsoolcoigoieccaolnroem se iacrcihntaerre ­ S tim uc e h . iTnh fo erm in a st t a io ll n a ti is onsoomfetth im eensewnoitntaecrcneestsifbalceilo it ny5D re rqouu ir geht sp m ec oinailtoe ri qnugiyp diagnosis, and predic at the Kenya Meteorological Department will facilities including s ment and high techno t lo io gny 10 A sig nne if diu ca cnattleyd im an pdrowveellt -h iinsfoprrm ob eldem pu . blic is likely to 6 p Sk uitle le rs d , hwuhm ich are limit peedciianlK in esnty ru a m . ents and com­ rceastp io onndanbdetttrearin to in agnyofntehweppoulbilciyc, / mmeatnhaogdesr . s , Eadnud ­ tHhue ma mnulrte id so iasn ci prleisnoaurryc es di a m re e n required in handling policy makers is an important component of any ological conc uerpctessof fo drrohuagnhdtliansg io n th seo ba f s ic drm ou e ghts. drought preparedness strategy. This has not been However, they need speci re available in Ke tneyoa r­ . coopm tim pl u ex mmiunl ti K di esncy ip a l , ineasrpyed ci raolu ly ghitn in ltiegrhatc ti oofnst . he ecfofm ec p ti o vely address the co amltprlaeixn in mgutlo ti d b is eciapb li lneatroy 11 iSnttrruocdtuuc ra ed laadnjeuw st m di e m nt eno si fon th ientW he orrledgiB on ansk in ce haist7M ba iss ic mcahnaeln le ts that could be required to address the discourages government subsidy, which has been a mation n ag henm ge esntofadn ro dugahbtupsree pa orfeddnreo ss ave u . ght infor­ pmraojvoirdipnogst-bdarso ic u gh fo toedmeirng en tchye re dlr ie ofug st hrta -t setg ri yckfeonrpdo ro li u ti gch al t , in afnod rm baete io nnohbasse rved in some cases when region. The method was adopted during the citizens, dono rs o , ther gai b ns e en byu se sdom fo ereicnodn iv oim du ic al , A dr cotuognht28ofJ1 an 9u9a6r -y 71b9y9i7n . v W ok iitnhgou th teem Pu e b rg li ecnSceycfuoro it dyh general public. Inansdomoe th ecrasseast , tdhreouegxh pe tnasdeviosfortiheesrceolm ie mfoadnid ti es g ov in e rn t m he e nt dr souubgsh id t-ys tr o ic n k en b asi rce gi foonosd , cmo av memboedein ti eas bu an sed through hoarding of essential including provision for subsidised seed prices when aft aerrkertecweiitvh in in gaidnffeow int rmm rod a o ti n u th ci sng at thhiekm ed bpa ri cckes to the the rains started, the impacts of the 1996-7 experience drought with oinn that one countr . yEw ve il n l dro Iutgm ht aywobueldcohnacvleubdeeedntvheartyadle th va osutg at h in K g. enya has cdoounnotrrsyhatvoebeexepn known to caon fe ti wnumepornetshssi , ngso th maetm an i tt ieneteu rm nd in eirs te th ri ealod ff iiscaes te orfm th aenapgreem sid eenntt, co a m nd ­ fmuinndisma fo l prices boyrtgu th ar e a ir n te gerianigntrheesye rv weis ll p at r ov viedreyvm id aenyreo le th va enrtm se in citsotrearliadl ro su ubgchotm in m fo it rtm ee ast io th nattoptrhoe ­ export pr ricgerafionra im b p ag oro ts f m in aiczaese is o so f m dr e o ti umgehstsa . s T lo hweiann te irnm te in girsa te te r d ia lna co tu m ra mlitdtiesea , stK er epnryeapadroeedsnensostphoa li vcey." In Droughts. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-65.

"n ar eegattaikveenco to rr e im la p ti loynsa , p th hy essieca ‘ ltelliencko nnectio key va between ntphaet te lo rn ca s l ’ w (1 a9s7o2n ). tFhoellpoowiinntgosfoemmeeirngc in on gcilsusc iv oentw ai onrekdbiynoLtahm er bsm Gl aapnstzrioeatblael . a1n9d9t1h ) e . widely distributed one (e.g., see (e.g., by Berlage and DeBoer 1960), Professor Jacob pressure f an pdr ec wiapsi ta atiW on a , l ke te r m produced teleconnection Bjerknes at the University of California at Los modes of interannual blcel im to a te idve perature, and surface Angeles made the key step forward by demonstrating nise today, including the South anerrita if nbyi li tthyethlaatrgweestre scale that the atmospheric teleconnection patterns were North Atlantic O Oscillation and c o th g e ­ p eq a u rt atoof ri aalcPoaucp if liecdOmco ea dneaonfdinttheer ac gtlioobnalbaettmwo ee sp nhteh re e was Inaba le d d to it icoanr ry to scb illation. (Bjerknes 1966, 1969, and 1972). It is now clear that of fortunate circu omuste ing a first-rate scientist, Walker other parts of the global ocean also participate in the the art of statistics htaahn is work because of a confluence Southern Oscillation, manifested through changes in matical tool of the ob d se cdeesv . e F lo ir pset, shortly beforehand, sea surface temperature and the overlying atmos­ also a very ab rvational dscriaepnicdelsy . aWsaalkm er atwhaes ­ phe B ri ycctih rc e u la la ti toen. 1970s and early 1980s, climate o st fat ti hse ti cIsnd (W ian alM ker le1 99 m7a ) t . h H em av aitn ic giatn ak ewn ho understood scientists were able to document the relationships gained the oppo ertteuonrio ty lo tgoicc al Departme th netijnob19o0f3h , e h ad ehRyap sm ot uhsesso is neda nd byCaB rp je ernktneers 19 in 8 2, mwoh re odd is e c ta uisls ed (e . tgh . e , m re aqtuhierm ed ata ic a la l rg oepesrta aff capab alreryoofupteh rf is orsm tu idniges, m w an h u ic ahlT So hue th ceorunplO ed sco il cleaa ti n o -n a / tEmlosNpihneoreasvaaricao ti uopnlecdenstyrsetdemo ) n . W ve a ry lk p er raw ct ais able to t m io ankseoanmeax jo te rne si f v fo e rt d a to ta so se lv ts e . tShoeE th NeSeO qu a ( t E or l ia NlP in ac o i / f S ic oiustnhoew rn co Omsm cil oln at liyon re ), f er a r ed p h to ra saesA ra n in oftah ll e , rkaencaalcp ti rvoib ty le m th aotfh pr aed dicting Indian monsoon coined in planning documents for the international by the earl yyfyaecatrosrowfasthtehattwietnh sta taidejru te t st dbe in c om th eep1 os 8s7i0 bl s e . Tmreonpti . caDlO ur cienagntG he lo b 1 al 98A0tsmoasnpdh er 1e99 (T 0s OGaAs ) ereix es p er o i­ flsaurfgfe ic -s ie cnatlence li amr-agtleob va arl ia d ti aotnas . to de hsccre ib n e tu raynd to agnaatlh ys eereom ur p iri ucnadl, e m rs o ta dned ll iinngg , aonfdtthheeo re p ti hcyaslicsa tu l di m es e c in hcarneiassm ed s 192 T3heansdtu1d9 ie 2s4 , bWyaW lk a e lker and others (e.g., Walker aad ss voacnicae te sdinwiutnhdEeN rs S ta O n . diAngdettealielceodndnie sc c u ti sosn io pnao tt ferrencsen in trge lo la b ti aol) nsshuirp fa s ce exp is re te s d su rbeertawnedenB li lsasrg1e9 -s 3c2a ) le s h ( o i. w e. e , d n that the TOGA era (1985-94) can be found in Trenberth patterns -in particular, tphaettIen rn d s ia n an sdum re m gional rain efaarl -l et aTl. h1e 99 i8deanntd if i A ca ll tainone ta o l. f 19 so 9m6. e of the physical v ra aitn io fa nlal. l W ev a id lk eenrc ’s erfeosreatrhcehepxrio st veindceedo th feefr monso an ir osrtgaonbisseorn ­ m rev ec it h a anism ed conne l c is t e io dnsi nt aesrseosct iated with patterns. in A W se a ri lekser’ osENfp SO has st ruedciiepsi ta w ti i o th n g re te alte ly -glo more wHoerbcaal-ls le cda le tpk did no hi tsattthee rn hav Soofuitnh terannual climate variability. complete data sets (e.g., Kiladis and Diaz 1989; expected because, efotrhe re a im e p rn acOt scillatio sons th tahtartemma ig n. htI in unh itia nc alveel ly ar b , e h th einsrReocpoenlfeiw rm sk eida se nvde ra Hlao lp f e th rt et1e9 le 8c6o , nn 1e9c8t7 io , ns ansdu gg 1e9s9 te 2 d ) c so o o rr n e la ptr io ec nispib ta et t w io enenwtehaekepnreed ss uarbeopuatt te th rn esta im nd e m th oene ­ cboynW ne acltkieornsa . ndRootphee le rs w , saknidaindde nt H ifi aeldpeardt di ( t 1 io 9n8a7ltaen le-were discovered. Th y 1989) attempted to improve the usefulness of tele d ­ taitmtehemomsitdodf le thoefetah rl eec tw or ernetliae ti tohncsesnttruernyg , th beuntebdyag th a a in tcdooncnuemce ti notn patterns y work ha ing regions foorfstehaesognlaolbcelitm ha att , eipnreaddidcittiioonnb to y fille Adc in ru c w ia alspaap rt hyosfictahleepxipcltaunrdebteheantfro em rg aoitn ten atio ed . to be a m ls e o re lhyadshroew la itn io gnssh ta itp is stiw ca ilthEN EN SO SO -p rtehca ip t it w at eiroenhliignhklsy , t te hleecSoonuntehcetrinonOp sc aitltleartn io s. n A ju rsetvaisewaonfk fo nrow th leedogbesaeb rv oeudticdoennstiisftieendttfhreom se aespoin so sdaend to reegpiiosn od seo . f T th h e ey g p lo a b rt eicw ul haerr ly physical explanation precipitation was associated with ENSO in at least 75 e." In Droughts. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-39.