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  1. Porpora, Douglas
    In: Routledge Handbook of Critical Terrorism Studies; (2016) S. 80-89
    Buch
  2. Achieng', Shirley ; Oando, Samwel
    In: Contemporary Reflections on Critical Terrorism Studies ; page 53-68 ; ISBN 9781003266709; (2023)
    Buch
  3. Rodrigues, Inês Nascimento
    In: Contemporary Reflections on Critical Terrorism Studies ; page 227-244 ; ISBN 9781003266709; (2023)
    Buch
  4. Martini, Alice ; Schweiger, Elisabeth
    In: Contemporary Reflections on Critical Terrorism Studies ; page 142-157 ; ISBN 9781003266709; (2023)
    Buch
  5. Schmid, Julian
    In: Contemporary Reflections on Critical Terrorism Studies ; page 245-259 ; ISBN 9781003266709; (2023)
    Buch
  6. Dixit, Priya
    In: Contemporary Reflections on Critical Terrorism Studies ; page 124-141 ; ISBN 9781003266709; (2023)
    Buch
  7. Jackson, Richard
    In: Critical Terrorism Studies at Ten ; page 161-173 ; ISBN 9780429454844; (2020)
    Buch
  8. Pettinger, Tom
    In: Bringing Normativity into Critical Terrorism Studies ; page 86-109 ; ISBN 9781003098362; (2020)
    Buch
  9. Lindahl, Sondre
    In: Bringing Normativity into Critical Terrorism Studies ; page 48-67 ; ISBN 9781003098362; (2020)
    Buch
  10. Lindahl, Sondre
    In: A Critical Theory of Counterterrorism ; page 87-110 ; ISBN 9781351121279; (2018)
    Buch
  11. Jackson, Richard
    In: Terrorism and Policy Relevance ; page 119-125 ; ISBN 9781315179513; (2018)
    Buch
  12. Carr, Casey Douglas
    In: Assessing the War on Terror ; page 234-252 ; ISBN 9781315469171; (2017)
    Buch
  13. a (o m ft oeunnti ) n an cdom th p e arison to som inten duration of tehenodrrmyaplero io r d. avTeh ra ugse , b cu y l ti a v lt aetr io in ngprtahcet ic cerso . p, genotype, planting date, and m th u es sesid ty ef iann it d io ndsu . raM ti eotneoarroelotghieca key characteristics of Agriculture is usually the first economic sector to phe t be considered as region spe lcid fi rcosuignh ce ttdheefiantim tio onss ­ abreeao ff f e te c n te dqub ic ykd ly roduegph le ttbeedc , aeusspeec so ia illlymiofis th tu erepesruipopdl ie osftsaotm io ric cendaoerfen diti ini c ti l o im on astethraetgriemseu lt dienpe deficiencies of precipi­ moisture deficiency is associated with high tempera­ on the ns differentiate me n te doernotl . ogFiocraledxraomupglhet , tduurreisngan th dewgirnodwyincgon se d a it sioonnsi . s T cr h it e ic a ti l m in in tgheofdertaeirnm fa i l ­ llm es asgn th abna si ssom of e th sepencu if m ie bderthorfesdhao ys l with precipitation nation of impacts. Crop or forage yields may be nor­ (e.g., itude of the deficiency over so dmreap th e e ri rod th o an f ti t m he etm im al eloyr ( i a .e b . o , vceo in ncoirdm in aglwdiu th ri n cr g i ti acadlrpohueg no hltog if icraalinsfta ag ll esi ) saOsrm ga unc fo h r Britain, fifteen days, none of which received and effective (i.e., low intensity and high soil infil­ in thos iz aeats0. rieogni215 on 93m6m ]) . oSfupcrh ec a ip idteaftiinoint io [B n ri is ti suhnrReaailn is ftailcl trat H io yndrroaltoeg ). ical droughts are associated with the effects c se oam so mno al n . an M d os etxst where precipitation distributi m en e d te eodropleorg io ic daslw dr i o th uoguhttrd ai enff in al oln is of periods of precipitation shortfall on surface or sub­ relate actual precipitation depa itio a n re slsaukre fa cleevw els a , tegr ro su upnpdlwya ( tie .e r) ., rsa tr th ea emrftlhoawn , rweistehrvpor ir eca ip nid ­ a ti mmoeun sc tasleosn . H monthly, seasonal, wa rtteurreyse ar t , ooraavnen ra ugaeltHay ti dornolsohgo ic rt aflald ls r o ( uDgrhatcsuapreetusaul. al1 ly 98o0u , t K of le pmheaSse1o9r8l7a ) g . are Aegqruiaclu ly lt uvraarliuam ble a . n perceptions of these conditions tdhreo ug o h cc ts u . rrM en e c te eoroof lo g m ic e a te lod ro ro lo uggihctasl re asnudltfargorm ic u p lt ruerca i­ l m on etperoercoilpoigtiacta io lddrroouugghhttto li n a ks various characteristics of pitation deficiencies; agricultural droughts are largely and potential nesvhaopro ta tr gaenss , gdriifcfuelrteun ra cles im bpea tw cts, focusing the result of soil moisture deficiencies. More time deficits, and piration (ET), seoeinlawca tu te arlien la o ps th es erbceo fo mrpeopnreenctispio ta fttihoenhdyedfr ic oileongciiceasla sy re s te d m et e (e c . tge . d , cdheapreancd te ern is tto ic nsop re fvoa rt i h li . ngAw plant’s demand for water is reservoirs, groundwater). As a result, impacts are out growth, and s t he ofphtyhse ic al sp eeactih fi ecrcpolnadnitt , i ons, biological of phase with those in other economic sectors. Also, the soil. and biological p it rsopsetratg ie esooffw riv a e te rs r ) i n is hoyfd te ro nlougsiecdalfo st rom ra ugletispy le st eam nd s ( ceo .g m ., preets in er gvopiu rs r­ , dorfocu ro gphst sh Aonu ld opaecrcaotu ional definition of agricultural poses (e.g., power generation, flood control, irri­ example, adted fi icfifeen re tnstub st natge fo srotfhe cr voap riable susceptibility gation, recreation), further complicating the sequence stage wil soil moisture idneavneleoaprm ly egnrt. o w Fo th r a in n d th q es ueansttiofriacgae ti osnyso te f m im sepsaccatlsa . te Csodm ur pientg it idornoufg or htw , aatnedrrseoq il u ir m em oi lsthuarveeliist tle su impact on final crop yield if top-conflicts between water users increase significantly. moisture en ctosn . ti Hnouw es e , v ffi ear ci , einft th teodm ef e ic eiten early growth The frequency and severity of hydrological drought result. substantial yie c ld y o lo fsss ub m so aiyli ( s19o6f6 te ) n de dfeifniendedaadtrotuhgehtr iv yeerarbaassionnescian le . whW ic hhiptphlee the The impacts of drought are crop specific because a ru gngo re ff g . atLeow ru -n fl oofwfifsre less than the long-term average betw m ee onstcrw op ea s. thPelra -s netn in s g it idvaetepshaenndolm og aitcuarla ti s o ta ngepserv io a d ry stfiomremapney ri osd tr efaam lls s . bIefqu th eenca ie cstuhaalvfelobweefnordea te srem le icnteeddahlisgohv te a m ry p between crops and locations. A period of hydrological drought lioswc on a si cdeerrtead in tothbreesihnop ld ro , gr th es esn . d se rnysic ti ovnedi era g ti roonts ur wt hmeasy tr ecsositnhca id teocw cu it rhsiancarsis ti occailatw io enatw stage for one he it r h -b Hio li w ty e v th ear, ttm he usntubmebeexrco ee fddeadystoanddeftihneelaevheyldorfop lo rgoibcaa ­ l c ca ri n ti coafltesn ta rgeedu fo crea th neotrh is ekro cr fodpr . o A cr gorp ic while missing a drought period is somewhat arbitrary. These criteria ught ium lt pua ra cltpolnancn ro in pgs will Tvhaeryibm et p w ac etesnso tr f e am hy sda ro nldog ri ivcearl ba dsr in osu . ght in an
    In: Droughts ; page 41-41 ; ISBN 9781315830896; (2016)
    Buch
  14. 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
    In: Droughts ; page 66-66 ; ISBN 9781315830896; (2016)
    Buch
  15. In: CAD Principles for Architectural Design ; page 228-228 ; ISBN 9781315042794; (2013)
    Buch
  16. Wang, Kefei ; Huang, Libo ; et al.
    2018
    Buch
  17. Heath-Kelly, Charlotte
    In: Routledge Handbook of Critical Terrorism Studies; (2016) S. 287-297
    Buch
  18. Fitzgerald, James
    In: Routledge Handbook of Critical Terrorism Studies; (2016) S. 49-59
    Buch
  19. Toros, Harmonie
    In: Routledge Handbook of Critical Terrorism Studies; (2016) S. 70-79
    Buch
  20. Trompf, Garry W. ; Kim, David W. ; et al.
    2019
    Buch
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