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  1. Dieser Titel kann aus lizenzrechtlichen Gründen nur im Campusnetz oder nach Anmeldung angezeigt werden!
    academicJournal
  2. Jeu as nte -A A u fr g ic uasnt. T lo h w ese in tropospheric jetstr ea le mvc el l , u de antdhew su e b st t ro A pi f c ri aclan ea st m er ildy -, deve s. These fast-moving upper pre Spoa lo re pdendes th srpoou li gch ie s s . ound early warning and disaster ltehveeltw ra inn cieties in sdpsoh rt avoeffamr-o re is atcuhrien , g m im opmaecn ts tuwm it , hproelslpuetcatnttso , reeflfyorh ts e , a w vi h ly icohndp ev o e st l -o dpiisnagstceorurnetlr ie ie fsa , ned sp reech ia alb ly ilA ita fr tiicoan , a an tm dop sp es htesr , ic to dgyentahm er ic w s. ith many other aspects of the tdo is atshtee rs s . evIen re imm ake them m creas peadc ts vuo ln fed ra ro o u re ghatn bility doafnmdsooo re th vulnerable Tropical cyclones have both direct and indirect severe consequences of natural disasters c iet eyrn to a tu t r led to th haeliam ss poacc ia ts t ed onwK ith entyhaensrtarionn fa gll. w T in hdes , doic re ecatniwmapvaecst , saanrdefdoerc la N ra attiuornalofDtihsea st 1e9r90Rseadsuc th ti eon In t ( eIrD na N ti D on R a ) l D by e ca th deeaen xc yescsyicvleonperew cip e ith it iant io th netw ha etstoec rn cu Irnw di haennO th ceeaenffeex ct tsenodfpUrnoim te odteNdaitsiaosn te s. rpTrheevemna ti joonraonbd je cptrievpearoefdInD es NsD th R ro iusgthocolv im er atK ol eongyiac . a l It sh hit the Keny arneccoorod uld be as s t . shTohwen th o a ted ind tino th cayt rect ecflto he fe nce ts ahvaaosileafavbe le rcdo ev n e ce ny dama lo rgp te e, in dgc in otuen rn tr aiteiso , ntaol re adcu ti coen , l os esspo ecially in the cyclone, however, occur when the cyclone is far from often as so acnid at esdocw io it ehconnaotm ur iacld di issa ru st petrisofn li , few , hpircohpea rt ryet it hserceegn io tr n e , butthsetrie ll bayt tra in cttesrtfhee ri n re g g io wniatlh wi tnhdes to n w or a m rd aslh at etlip tu tdoess hi tfhtattheap re o st p -d re is vaaslteenrt re iln ie f and . r T eh haeb se il it cao ti uolnd circ Culloas ti e on patterns of the many developing general ciin rc te urlaac ti t o io nnsohvaevrerbeegeinonoabl winds. the regi soenrvaendd between the cou A n tr n ies the extra-includin egw . th d e im feuntsuiroen re to cu rnraetnucrealocflidm ro at uegh variability, tsryosp te ic masl , wmeiadtlhaetr it u sy dsetewmesstle ik r e li etsh , e N fr oorn th ta lAatn la dntb ic lo coksicn il g ­ tchuerrternatdigtlioobnaallcsopn ac cee -r t n im aebopuattttehrenspootfengtlioablacths, a n is geth in e T la e ti l climate, Ke l o ec n o , nenae st Atlantic pat nyan rai cntfiaolnlsanhdavEeNaSltseor ns b , eeanndobEsuerravse ia dpbaetttw erns. inclu O, quasi-biennial oscillati eoenn , h cl u im madt ing the space-time ch an eaecvteinvtis ti etsh . roSuug ch h e im nv piarcoanrm ac e te nrtiasltidces gr oafdaetx io tre ts are currently subj nembey intraseasonal wave, and so forth. The influence of the of many studies and debates, as reflected in the 19 c9t5sw co a m te prlebxod topographical patterns and the large inland Intergovernmental Pane inland wat ieersbiosdv ie e s ry insc ig lu n d if eicL an ak teinViKce to nryiaa . , w Th h e ic h la h rg aess in c d ie inctaitfe ic d ‘d aisssceesrsnm ib elnet inf olfoncC lim lim a ate Change (IPCC) an area of about 70,000 km2 and is the second largest the recent climate trends l ’ u . eInPcCeCof te change, which freshwater lake in the world. The complex topo­ ever, that no conclusive evidence ( 1h9u9m5a ) nnaoctteid vi , tiheosw in ­ K gr i a li p m hical patterns include Mt. Kenya, Mt. human-can be derived fo anjaro, and the Great Rift Valley with its accurate inmdeutcheoddscf li omrattheed ch et aencgte io nsiagnnd al s a tt urn ib ti ult io mnoroercaltitm en a d te anptroccheasisnesofcamnobuentoab in ta s i . n D ed e ta fr i o ls of the regional natural/anthropoge f Anyamba 1992, Fremming 1970, manOdg al F lo in 1d9 la 9 te 3 r , acn ha dng ac e cu si rgan te a ls cla im re atanv ic a ilab ( lhe, u m to agne -t ihnedrucweid th ) ad celq im ua attee 1966. tch li e m si ast . ecSheavnegrees , icnocnes lu eddqau ta e n for testing various hypo­ patterns of extreme clim iantge ces ecvheanntgseosf in htuhmeasnp -a icned -u ti c m ed e like drought, would cDorm ou pgohntenatnsdoofthnear tu erxatl reme climate events are normal h ca ig ll hlfiogrhtceld ea brym th it eigIaPtC io C n . and adaptation policies, as iam nd pacco ts m m of onthpehseenon me n in atew ra o n rl nduwaildceliemvaetreyvyaeraira . b T ili htey men Gtlaolbadlegcroandcae ti ronnapbrooucte ss heusmaannd -i nsduusc ta eidn ab ein li vtiyr on o ­ f m an idn im ad al eqiuna the de atural disasters, however, te drou v g el hotpesdhoccokunatbrs ie osrbw er hserheaveef fi b ci aernettniaetsurlaeld re to so u een Conference th rc ees vita on o rga Enlnivstao ir t most o io nnmeonfs ocioecon t the anUdn it oemd ic Naat ctivi­ Sustain iaobn le s
    In: Droughts ; page 84-84 ; ISBN 9781315830896; (2016)
    Buch
  3. IPnad lm ex e r (P Darlomuegrh1t Sev United States, an 9d6t5hea ri n ty dI1n9d6e8x , aAnldl Crop Moisture et al. 1987). On the other hand, it is indeed ra e Yield Moistur eey In 1d9e8x4 ) ( Jionsetheetedv ro er uygyhetanr. oFttooreexxiasmtipnlea , pFo ig rt uiroen1o .5 f th il e lu ssetrcao te usnttrrieesfo in r al. 1991 hat in tiinve th ly enU ew ) in the Philip ni tienddeSxtatth es atisistpgia ne he iSnstiaanngndid elsew anrcdriezaesd in h g ere. Pr epcopAu ipit la re ri ltay ­ tdhreouU gh ntitiesdofSttean te g s, retahteerp th er acnen1t0agpeerarceeanta . f T fe hcu te s d , th beyI1n9d9e5x ) . (SPI), developed by McKee et al. (1993 ation governments of these larger countries are more drough Atisdiisncculsusd io ed nionfc se li v m er aatliccihnadpitceerssfionrtm hi osnvio to r a in ngdaec st caubsltio sh meedda to dealing with water shortages and have in Part III (Monitoring and e lume actively. For n sm ianlf le ra rsc tr ouucn tu tr riees, toitriesspmoonrde , l a ik lb el eyit th re a -t n lo igqiuceasl ) . inFdo ic reas , csoemepOalriid so ap noo ( f1s9 ev 8e5raarl ly p op wualranr in mge te te ocrh o­ ­ tuhseuael ntire coun ). scale ly anroem gi aoln ie asltrpyhm en aoymbeenaaff -e cttheedysrienscueltdrfo ro u m gh ltasrgae re -dur A at n io o n th . eDrrdoiusg ti hntgsuu is shuian ll gyrfeeqau tu ir reeaomfidnr im ou ugmhtof is t its that become es ta in b li asthm ed o sp ahnedr ic p er csiirsctulfaotr io n p er piaotdtse rn osftcoontthirneueemfoonr th msotnothbsecoormeyeeasrtsa . bl T is hheedmbaugt then cwaon mo Fnrtohms, sae as p o la nns, n o in r longer. drought impacts is closely related t nitude of teristics of drought ghapveerssp er eicotu iv sei , mtphle ic astp io a n ti s a . lNcahtairoancs ­ tohnesedtuorfattihoenporfectihpei ta etv io e n nt . shTohre ta g fi e o , tih ts eitn im te ing of the should know the probability that drought may simul­ dr ve-year ( n1s9i7 ty 9 , -a 8n3d ) r ta enge io onuss ly w a it f h fe in cttah ll eiorrbsoervdee ra rs l m an aj dordcervoep lo -p procdounctiinng ­ y th eiosusge ht in northeast Brazil is a good case in point. In gencies if such an event were to occur. Likewise, it is du arrisngirn ie tsh th oefcyleaas rs, 1979 and 1980 were both drought important for governments to know the chances of a sonal rain e fa lplritnocsiipcaslernasieny ( i s .e e . a , so a significant deficiency regional drought simultaneously affecting agricultura tals were slightl n y ) . a b In ov 1e9n8o1r , m th ael, sbeuat ­ pnreoad rb uyctn iv aittiyonisnotnhew ir hocm ou tnhte ry yaarsew de e p ll e n as deandtjafcoernftooodrltdhreo ug te hmt. po Irnal 19 d 8 is 2 tr , ib tuhtei on ra in re fa slul lte to d t al isnwaegrrei cu ble tu lo ral supplies. In some inst normal, but the temporal distribution of precipitatio wnfdrroomugnhetam rb i y ti gnaattiioonnss , tr iagtneagny ces, a nation’s primary was conducive to crop development. Agricultural drought may have signif o ic ri nmgatyhebel ik to e li ihmopoodrtthfaotodaw im e p re a ct fsow llo e w re e d le ss bya dv th er ese. mTohset se ant regional impa sefvoeurre ‘d drroouugghhtt ’ yyeeaa rs r w fo oord ld w su ipdpelioers . inLtihkeewpirs in e, citphaelgorcac in u -r e re xnpcoer ti onfgdnrco ts ugohntm (1 a9t8 ic 3 ) ago ri fcu th lt e u ra plre im vi poaucststw (M en atgya -f lih ve years, with dra­ such as occurred during the ENSO event of 1a9t8 ions, aes et al. 1988). (Glantz et al. 1987, Glantz e2-3 cha D ra rco te urg is httiscs. al T so hedair ffer in terms of their spatial nificantly alter a developing cou tnatlr . y’ 1s9a9c1c ) e , ssmtaoy fo si ogd ­ e sh viofltve fr ogm ra dsueaalsloyn , a to ndser as affect ea esgoino . nIsnoefdb lar m ge ayrxism ev uem re idnrt ought from donor governments. as Brazil, China, India, the Unit ceodunS tr tiaetse , e n su si cthy
    In: Droughts ; page 43-44 ; ISBN 9781315830896; (2016)
    Buch
  4. In: Children Reading Pictures ; page 178-203 ; ISBN 9780203005156; (2004)
    Buch
  5. Baynham, Mike
    In: The Routledge Handbook of Migration and Language; (2017) S. 431-447
    Buch
  6. Pavlic, Breda, [Ed.]. ; Uranga, Raul R., [Ed.]. ; et al.
    2021
    Online E-Book
  7. Pavlic, Breda, [Ed.]. ; Uranga, Raul R., [Ed.]. ; et al.
    2019
    Online E-Book
  8. Pavlic, Breda ; Raul R Uranga ; et al.
    2019
    Online E-Book
  9. Mukherjee-Reed, Ananya
    2008
    Online E-Book
  10. Ananya Mukherjee Reed
    2008
    Online E-Book
  11. In: The Companion to British History, Routledge; (2001)
    Online E-Book
  12. PhD, Melissa Farley
    2003
    Online E-Book
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