학술논문


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'학술논문' 에서 검색결과 27,045건 | 목록 1~20
h it Drought igohccausrsw in el v is i rt a normal l as ulao ll wya ra ll i , re ncfla im curring featur ll a a ti rcearse . g I im t e is s . e I of climate; severity levels) and the vulnerability of society to the aberration, atteom cc puorrsariyniesveanrt. esTuh lt e o na fttuhrealoecvceunrtre (i n .e c . e , m of etpeeorrsoilso te g n ic tallad rg ro e-usgch al t e ) m rai annfe al nltafreeaatsu in r contr . Meaonfythpe ast to eocp li lmeaatseara id nid ty , i s which is sociate th re estorc ic ctuerdtao per­ disruptions in the global circulation pattern of the dr rence lo owftah tm er oesp is helrie td . e E , xipfoasnuy re th tiongd , ro th uagthtwvearc ie asnsd pa o t ia to ll yaa lt nedrm Pl oaoiurngs ht wedo if f f ic N ith most of Auo lt rythv is A ua m li esri ic f a ri , caa , nIdn ng droug d A ia u , s C tra h l ina, ht in So ia u ; th tthheey Great drought occurrence. Vulnerability, on the other hand, B east A ha si vae , d is e m de otgerrampihniecd ch bayrascotceira is l ti fcasc , to treschsnuoclhogays , ppoop li u cy la , ti aonnd , rTerhgaizo il, wes is nfsacpt erc tern Euro em e p iv heads is beyspme, anoyrttohehae both the vaes te arsn Uni region uarlplauns te odfS tates, social behaviour. These factors change over time, and nature of d re w la attievre . r th es upsonvsue ln teoratbhielsie ty c h is a n li gkeesl . yStuobs increase or decrease in cussed in mdo ro re ugdh et t a , il a la cthearriancttehriisstc ic hatph te art . will be dis­ isdaemne ti c re agl io in n w in il tlenhsaiv ty e , did ff uerraetn io tneefqfu ec etnst , d ev ro eungihfttshe in ytahree in D th reouagm ht oiusn th teocfonpsreeqcu ip ein ta cteioonfarencae tu iv readl re odvuecrt io anntcehra is ntg ic esd , because societal char , acatned ri st sipcas tia w l il c l ha hraavce ­ leexntg en th d , e d al tpheoru io gdhoofth ti emrec , li u m su a a ti l c ly faacs to erasso ( nsuocrhm as orheigihnvdu is lcnuesrsab . th ilHe it ow sye to ev ac derro , umg uch can be d tions fhrto , m an mdasnuybs one reeqgue to ntlecshsaepnt societal te ional and edrisscw ip il ­ l w ar mepoefr te a n tures, high winds, and low relative humidity) linary perspectives. th oerledv and a c ss aoncisaitgendi fi w ca it nht ly it aigngrm av aantyertehgeiosnesveo ri f ty thoeftphre in criapeanlt. Dr iny sseeaassoonugohfto is c als on, occu c r ur o re rneclea , teddeltaoysthienttihmeinsg ta r ( t i. e o ., f Because drought affects so many economic and social p th ri encriapianlsc ( rio . p e. , grroaw in tfh al lstraegnecse ) aonf rains in relation to intensity d , n the effectiveness of a se vca to ri rest , yscoofreds is coifpld in ef eisn . it Iinonasdhda it vieonb , ebeencaduesveeldorpoeudgbhyte cl viemna ts ti ) c . T ch haursa , c te eraicsh ti cs d ro aungdhtimypeaacruimsbuenr iq oufe ra iinn fa it lsltohcecug rs lo w be it , h in vaa ry l ing frequency in nearly all regions of Magalhaes ts. For example, developed and ltdyepvees lo opfinegc on coomuinctrs ie yss tem al s i , kea , ndth in e y cl eiam rs attihcadt if ofeetreanl. c e ( s19b8e8 tw ) eheanvef iv v e iv c id olnysp ec o u in ti tveeddoruotug th heta id peporlooagcihceasltdaik ff eenretnoce define it also reflect regional and and ccurred in northe s (Wilhite 1992). Impacts also timin 1g9o8f3r , ai nno fa ti lnlg an d th iemcpraic ti tcsaalstliB nk ra azgielsb . ebtew tw ee enen19t7h9esdo if cfieert al spcaotn ia tlelxytaonfdd ro te umgphot. raA ll y u , ni dveep rs eanldd in e g fi ni o ti nonthoef dur D at riooung , hitntseenvse it r y it , y a is nddegpeeongdreanpthin ca olto ex nl t y en tonof the dGrloaung tz h t ( 1i9s 85 an ) cuonnrcelau listic expectation. Wilhite and specific dro a should reflect a regio dneadltbhia as tdse in fi cnei ti w on at serofsudp ro p u ly g h is twmaatdeerbsyuphpu li m ug ahnt ac etp iv is i o ti d es e , anbdutveag ls e o ta t o io nntohneadreem gi aonnd ’ s s larg D el eyfianiftu io nncst io onfdorfocu li gmhat ti ccan re gbiemcea . tegorised broadly wi es. The soc th ie ty it , s ec f o ar n -o re mayc , hianngcdhiaem ra pca te crtiss , t ic msao ke fdirtos ug ef hfte , ctaslo nviron onngaGs la enittzh er 19c8o5n ). c ep Ctoun al c ep otruaol pe dreaftiinoin ti aolns ( W ar i e lh it oefatnhde not M im an pyo ss piebo le p , letociodn en si t d if eyradnrdomq ent uugahntt if dty if o . ficult, though dictionary t be largely atdheesccro ip ntc io enptyopfe , d generally defining of th ro e ug p h he t, naonmdetnhouns . the boundarie a F re orgeenxearm ic pilne , thseo ir frneaatlu it rya , l or the compone dnrpohu ysical t. Tghhet ri h ev as e nt b . oFtihg ur ae1n .3 atiu ll ruasl tra atn es d th saotc , iianlE 19 n 9 cy 6 c ) lo dpeefd in ia e sk associated wsodfroCulg im ht a te as a ‘a nndeW xt eeantdheedrp (S e c ri hondei -d er atrh eg e io enveinsta ( p i. reo ., dupc ro tboafbb il o it tyho th feoc re i g th iodnr ’ osuegxhptos fo urrean to yrseelaasto iv n e , taoytehaer , stoar ti sste ic vaelramluyletairysea -r omfedaenfifcoirenatre ra giinofn all currence at various These types of definitions are useful for furthering ’
Book
Droughts ISBN: 9781315830896
tth ra rdoeugphropbo le omrss ; top ra o g st e -; h w ar avteesrtelroosssieosn in ofth th eefsio el idl; aan nd d form Th a e ti omnajionrK tr eannysapoarrtestohfem re o g is io tu nraelim nl oannsdofoonrarlaw in i fall ma D ny roou th gehrt , prhoocw es esveesro , fisentvhie ro nmmae jo n r tal degradation. systems. The direction and speed of these winds al nsdotchua lt tuh ra alspbreoednucatsisvo it c y ia ; te sh dow rt iatghesanonfuaelndaetfu ic riatls disaster affect the pat nergy, fo o in d , aagn ri d ­ T ov weortdhies ti rnecgti te m rn osnsoofotnhaelcwoinn vective processes inland. water; famine; and devastating impacts on many other Both converg oeno , vnearmKee ly nynaoardn th sdaynsd te m so sua th re ecaosm ter m lie osn . n se a c ti toon rs a / lsesrovciicoeescotnhoamt ic fo d rm ev eilnotpem gr e al components of torial eastern Africa during the oatuhteurmpna rt asndofsepq ri unag ­ sdursotu ai gnhatb le im spoacc io ts e co li nnogm er icfd or e ve se lo v p er n al t . ySeoam rs e ment can , of th aenrd th ensoe seas efore w na inncoens. ofHon wever, Kenya is largely u ds durin ogr th th eeasso te urtlhye /s ronu /n th o rt ehaesr te nrd ly erm th oensdooom na i­ l m be enatchsite ra vteedg ie wsitfhooructopprio ng pewrip th la n su n c in hgda ro nudghm ts a . naTghee ­ w so innsd , sryesstpe ectively. The patterns of n th esummomnesroosnea a­ l m str aajtoerg ie csommpuosnt en in ts c lu odfesdurcohugdhitsam st o er n it m or a in na g g , edm ia egn ­ t low levels, m by scao re m p si lgenxif to ic paong tl ryapmho ic dailfipeadt , teersnpse . cially at ndo ro si usg , hptrepdriecpta io re n d , neefsfs ic p ie o n li tce ie asr . ly warning systems, and i m nte I on rTsh CZ oeomni sp mhaerrkis al wind c t sy nhsoer th co tems n . evTaeh st regreez ly n ce a nd ofstohueth lo ewa -s lteev rl eyl has Tahdids re rsesve ie dwfoo ur fkperyeddirco ta ubgih li ttyi ss oufesK , ennaymaenlyd : rought n ov o e rt rhh ea adnsdun south of the eq ounaetotrh er feoflo lo re m , and often lags behind it by thr w e in igg ra ttheese to five • • d so ycniaom ec ic osnaonmdicc auses weeks. ITC imp ; acts, including the recent p ow at itn er gnstoantZhe is veexriy st edn if cfeu se oaftc th oemlpolw ex letvoep ls oignra Keny d many large inland water bodies, pwhhiiccaal , • p in rteedg ic ra ta te b d il i g ty lo pbraolsepfefcotrst ; satnod address such problems; poo ft neenntisntirnod th u e ce se bao so th n al zomniaglraa ti nodnm ov eerr idional com h ­ • challenges to drought prediction in Kenya. zonal compo Kenya. The A as tsloacnitaitce / dCwoint en ng hot / hteof in th fl euxI Zaire bTao CZ, si fnms, ofsotrw ex whic ehsatm er p li lees , fhraosmbe th en e
Book
Droughts ISBN: 9781315830896
t lo wnegn -t tieertmhicnecnrteuarsyei ( nFp ig re u c re ip i 2 ta .6 ti ) o , n , btuhtebpe ro ca buasbe il it oyfoafm ev o id deenl ce priosjn ec ottioynest conclusive. Some coupled climate ddirfofu er gehntt , f m or eatshueretdwo in paeb ri sood lu s. teArasiinm fa illlaraim nc oruen as ts e , iinst im opbae ct on drought in in sdoim ca e te patrh ts atofatnheaw nt ohrrlodpiosg li ekneilcyA ra u in sfta ra ll l ia f o in rtahegl iven state of evident in the twenty-first century. This can 1996b). ast twenty-five EyN ea S rs O ( N is ic hsoelelnseotvaelr . p ar aitstee rn fr somd ire cchtalnyge fo s rc iend th beyacthm an ogsepsheirn ic gcrierecnuh la otu io sne fou Inndf the N gases and other pollutants, possible changes in the affect th oertcro op hoerrtehntAm tl ualn ti tic, new evidence has been behaviour of ENSO (for which the evidence is Allen 1997). P ic o a te lnatn ia dlem xt arn at nruoaplicvaalrioac ti e ons in SS echanisms for asnuc ( hSu va tt roTn that iati aonndsd co ir netcrtadiincftloureyncaetporfesweanrtm ), in ogrm on er etlhye be su ca rf uasceeowfattheerN are orb th ei nAgtf la onutn ic d ( s G ea r ot szunre fa rceeta te l. m1p9e9r8a ) tu . rVe ar biin at vioolnvsinignr in al is ceraenac , gse. In th iv ein in graanine latter situation, given no or little Arctic regions have also long been su ifnaclrl, eassuemdm te enrdseoniclymtooisdtruoruegdhetf . icFir ts o m ca nam in o tr d ig euh in as gbeeveindefnocuendofthaatchoausplse ig dnioscpeeacnt -ed. Recently, ‘meteorological drought’ perspective, comb ficant aptom te onstp ia hletroeseyxspteecm te a d ti cianlc ly re raesd es u c in e p th oepu ra la in ti f o al n l , dseufc ic hiecnhcayng in eesdcw ou it lhda sc ff a e le cst ( t D he e lw cl o im rth at eeto al f . E 19 urope on multidecadal time at which society becomes stressed by the atshsroecsihao te ld dvCahra ia ntg io et al. (1997) have 9 id 7 e ) n . tIin fi e th dedtercoapdiaclaltiAmte la sncta ic le , p ag o r li itciuclatlutreanl si aonnds ( hRyodd ro dlaog1i9c9a5l ). droughts, leading to n so o m rt ehancnsodn in tr soautdhipto ro le pio ca flSA ST tl aann ti ocm , aallitehsoubg et hwteheenrethies pro Fgirna ally, the pr oversy about this dipole (Enfield and framew mom rk enh ec aessa sa m ev o io nugsliy ts m ob ejn ec ti t o iv neesdanWiM nte O r na CtL io InPaSldMeacyaedral1v9a9 ri 7 a ) ti . onSsuicnh ra vianrfiaaltlio in nsboctohulndor be linked to information and pr rey to th Africa and to the d dic t e io nnh . anTcheesaendacptr iv oim tie ostewcillilm li antke nor O th neaasgtlBorbaazlils , caallteh , o th uegrhetihseallsaottaemraprleeneovt id setn ro cnegt . hat V se O rv SeTsewvreoruaglhAtfm ric oanni to co ri unngtrc ie esn . tr T es hea lr IeRaIdyan se dtP up R O to ­ sdyesctaedmalcaanndsloom ng eetr im -sc easle co v n ar fioaubn ility in the climate more tho i u ll gahltsoiswboerikngtogw iv aerndtto hese objectives. Much climate s d the interannual climate data information and isnetaesgornaatli ng p re h d is itcotriiocnaslW tro apridca ( l1w9 ig 9n7a ) l . id Feonrtiifnystaanscte ro , nFgo lland et al. (1991) and within the context of how drought forecasts could be may be lin eksetdAtforivcaarniarta io in nfsaliln . T th h m ey u lt sipdeeccualdaatl signal in used, especially in developing countries (Frederick H. circu e global ther e m th oahtaltihniesM of . th Seesmeaizszsiu , epsearrseonda is lccuosm se mdu in nidceatta io il n f , o1r9n9o7r ) t . hSA ev f e ri rcaallsaotm io enlah ti aosn of the oceans. The thermohaline circu­ in Hulme et al. (1992a and 1992b). Here clima­ the Soouftthhtee he rnNpoortHtehnetrinalH to e m change the temperature of tologists, hydrologists, economists, and sociologists ti emisphere is opch ea e n re soocne an msurle ti la dteicvaedtaolscoacm ie e t al toig ss eutehserthtaotm id aeyntairfiysesoonmceero ea f so th nea bl cyom sk p il lfeuxlienvmeer scales (Sc cre , as leasr ge in -s ca hlesinge tr loe po asnpthhrraonpdogReanm ic anekfufte ty 1994). H eric aerosols, m cts o st rleyl at iend ow to ­ drought forecasts become possible. Northern the the A se dviasrciu at
Book
Droughts ISBN: 9781315830896
Book
Chemotherapy Regimens and Cancer Care ISBN: 9780429090233
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[검색어] Ow, C. P. C.
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