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Статті в журналах з теми "C.U.T. di Bari"
Tasia, Winda, Rina Zuraida, and Yopi Yopi. "Isolasi Bakteri Pendegradasi Xilan dan Manan dari Perairan Indonesia." Jurnal Pascapanen dan Bioteknologi Kelautan dan Perikanan 11, no. 1 (June 8, 2016): 101. http://dx.doi.org/10.15578/jpbkp.v11i1.283.
Повний текст джерелаRadhitya W, Theresia Vania, and Meilanny Budiarti Santoso. "PENGENDALIAN EMOSI PADA REMAJA PELAKU TINDAK KRIMINAL DI LEMBAGA PEMASYARAKATAN KHUSUS ANAK (LPKA) BANDUNG." Focus : Jurnal Pekerjaan Sosial 2, no. 2 (February 12, 2020): 219. http://dx.doi.org/10.24198/focus.v2i2.26251.
Повний текст джерелаMuhammad Khairulanwar Abd. Ghani and Mohd Tarmizi Hasrah. "REKONSTRUKSI DALAMAN DIALEK BALING PURBA." RENTAS: Jurnal Bahasa, Sastera dan Budaya 3, no. 1 (July 16, 2024): 209–32. http://dx.doi.org/10.32890/rentas2024.3.10.
Повний текст джерелаSutresna, I. Made Agus Atseriyawan Hadi, Anak Agung Putu Putra, and Ni Made Suryati. "Balinese Phonology Ungasan Dialect Generative Phonology Study." Kalangwan Jurnal Pendidikan Agama, Bahasa dan Sastra 13, no. 2 (September 30, 2023): 99–108. http://dx.doi.org/10.25078/kalangwan.v13i2.2599.
Повний текст джерелаLukmanulhakim, Ady Setiawan, and Andini Linarsih. "Inovasi Media Pembelajaran Berbasis Augmented Reality Hewan Khas Kalimantan Barat Arwana Red Bagi Anak Usia Dini 5-6 Tahun." Jurnal Pelita PAUD 7, no. 2 (June 30, 2023): 396–400. http://dx.doi.org/10.33222/pelitapaud.v7i2.3059.
Повний текст джерелаSyawaludin, Muhammad, Aminuyati Aminuyati, Hadi Wiyono, Venny Karolina, and Thomy Sastra Atmaja. "Efektivitas Model Pembelajaran Outdoor Study dalam Meningkatkan Hasil Belajar Siswa pada Pembelajaran IPS di Tingkat Sekolah Menengah Pertama." EDUKATIF : JURNAL ILMU PENDIDIKAN 5, no. 1 (February 18, 2023): 328–34. http://dx.doi.org/10.31004/edukatif.v5i1.4243.
Повний текст джерелаLubis, Novita Sari, Ayu Diana, and Marnida Yusfiani. "Hanpen Fish Cake, Rough Flathead (Grammoplites scaber) Diversification Product." Jurnal Pertanian Tropik 7, no. 1 (April 25, 2020): 126–35. http://dx.doi.org/10.32734/jpt.v7i1.3840.
Повний текст джерелаMufidah, Ainin Nur, Hammis Syafaq, and Ana Toni Roby Candra Yudha. "INTEGRATED ECONOMIC EMPOWERMENT: EVIDENCE IN THE RELIGIOUS AREA OF GUSDUR'S TOMB." Jurnal Ekonomi Syariah Teori dan Terapan 8, no. 6 (December 5, 2021): 785. http://dx.doi.org/10.20473/vol8iss20216pp785-796.
Повний текст джерелаWahab, Wahab. "ANALISIS PENGARUH FDR, NPF, TINGKAT BAGI HASIL, KUALITAS JASA DAN ATRIBUT PRODUK ISLAM TERHADAP TINGKAT PEMBIAYAAN MUDHARABAH PADA BANK UMUM SYARI’AH DI SEMARANG." Economica: Jurnal Ekonomi Islam 5, no. 2 (May 3, 2016): 107. http://dx.doi.org/10.21580/economica.2014.5.2.772.
Повний текст джерелаKumalasari, Intan, and Zizke Rusella. "RISIKO KEJADIAN ASFIKSIA NEONATORUM PADA PERSALINAN KALA II MEMANJANG, AIR KETUBAN BERCAMPUR MEKONIUM DAN USIA IBU." JURNAL KEPERAWATAN SUAKA INSAN (JKSI) 7, no. 2 (July 13, 2022): 91–97. http://dx.doi.org/10.51143/jksi.v7i2.325.
Повний текст джерелаДисертації з теми "C.U.T. di Bari"
Rizzi, Marco. "C o l t i v a r e i l p a r c o p u b b l i c o. Produzione e distribuzione alimentare lungo la ferrovia a Lisbona | Il caso di Marvila." Master's thesis, 2020. http://hdl.handle.net/11144/4775.
Повний текст джерелаЧастини книг з теми "C.U.T. di Bari"
"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, 84. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-60.
Повний текст джерела"a in ff teec ra tcm tio o n re srbey al ist dictions into glob ian ic se m l at r m ti ondg elling of ocean-atmosphere model to a new equilibrium (e.g., Figure 2.5). This give a direct forecast of o th seph th e e ri sce ci S rc ST anom precipitat u io la n ti o (e n . gma ., o ly Jdpiee ls re new t a to l. lciibrrciuul oc m ati eoannsm ta o te deilnu tu n r ti nldirtivreesacahg es lo b a al atmospheric 1994). output . toWd in ri dvesttrhee ss ofc ie ela ds are taken fro m (n e th airs ) meoqdueil imp A ro lt vheom ug ehn ts t h in estehedsekv il elloofppmreendtisc ti hnagvEeNrSeO su -l rteelda te idnw et h al. 1994). This is a n fo m rm o del again and so on (Ji SSTs, their greatest contribution has been in diag sep earrea te t he c om at pmoonsepnhtes re ofantdheoocfeacnouaprleedhamnodd le e d ll in agsn ev oesri , ngsotm he ecroeu se p a le rc d ocean-climate h has in a d tm ic o at sepdhetrhee sy psotteemn . t ia Hlofw or a cl timmoastpehm er o ic demltohdaetlhacsan th ebeadavasnttaatgee -o of-f th sey -s a te rmt . g lo TbhaelaCpapnle ic aatn io dnsZeobf ia kENESNOSOSSSTSTprperdeidcitc io ti nosns -h aev .g e ., b e th en e p el reem di ecn ti tns. g Al w te o rn rl a d ti w ve id ly e , it prm ec aiyp it j at au us itonbeatnodm atically u a stati o st tihcearlt in seZdi as the b hat f m ur btahbewre asis f si g ( nCia fi noerse ta tta is l t . ic cant prog 1a9l9f4o ) r . ecH ast ress requi orwseovfemr, a ize yield model (e.g., Barnett et al. 1993). of es the in it clsueseim on s thre Feorufsu ef r u th lerrev in ie f w or smoaf ti o se n a , stohneal re fo ad re ecras is t in d g ir : ecPtaeldmteoro oc f th etahnee mea ic an annunalac nnual d at y m cl oesp ( c i. yec ., lecionuptlhiengmboe dels. In heric fields inst tewaedenotchleusf io ul nla (1 n9d98A ) n . derson (1994), Davey (1996), and Carson sainnof their the cmeatlh ie e s ) oc heaas ni tcu rn aendd out be exceedingly difficult." In Droughts, 60–62. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-42.
Повний текст джерела"T cu im rre e n tl Sycahleeasd ) qu aas rte wreeldlaatst he thLeammounltt -i D na oth io e n rt aylEIaR rt I h , odtrhoeurgm ht ajporrem di ocd ti eolnprw ob il llem re s q . u T ir hee the resolution of hOabvseearnva im to p ry o rt oafntCcooluupm le bdiamoUdneilvecrosm ity p . onTehnet, sea lt ehfo fo urgthsp ex hteernes , io onntaogfloorbeaclasdto in mga , in boatnhdth th eseeaorcee dva saonlnacn es diantcm lu odse m in acn lu ydeodf ( t C he a rs toyn pe 1s9o 98 f ) m . ethods discussed above are uomciesamnatacnhdbaettmwoesepnhtehree . fl Fuo xe rsmaatntyhearbeoaus, n d th atr io ie nsoofftthhee rep F li o ca rtE in NgSaOn , d c , ur in re nstom co eupclaesdesm , oidmep ls roav re in cgapoanb le thoefo of frtehaelsie st iwcillalnrde -q suuirrfeacse ig coupling may be ess eenatd ia dli . tiA on ll tshue cc ecsusrroefnetmgpein ri ecraalt / isotn at i o st ficcaolumpe le th dom ds o . dFeo ls rirnesptlain ca ctee , a model parameterisatio nificant improvements in the SST anomaly patterns in the equatorial Pacific that th ry elraeyqeu rs ir , ecd lo m ud osd , erlad im inasp ti oonf , saun rf dacceonpv ro ecce ti sosn es, bound have many characteristics in common with observed to a quick solution, but, ro g v iv eemnetnhtesiam re p o li rktealny . N to onye ie o ld flEeN ss SsO uc cceosm sf puolsiin te tsh . eCm ur orreentdim ffi ocduelltspa ro re blceomnso id ferreapblliy imp Iatcsthoofud ld ronuogthbte , they are worth pursuing. ce of the p ca hteirnigcc th ir ecuslpae ti c o if n ic peav tt oelruntsioinnoafgtihve en SESNTSaOndepaitsm od oes . tehxe prospects for im forgotten, however, that not all of However, it is precisely this problem that must be no ctlufsuilv ly eluynodnersse ta a n so pnraolvteidmde ro sc uag le hst . p A re l dictions reside solved. Just as the ‘average’ daily weather is rarely of climate variabilit d y , th th eem re u l is ti aanmnpulaelteo th doeucgahdawles ca dloeo ce bpsteuravleda , idthteo ‘ ucnadneornsitcaanl’ diEnNgS th Oan id aeauissefm ul orceonastcroun ct e2x .1 is c t ) e nc aend -e th .g e . , sien the time series o vidence for its for prediction. To reach their full potential, coupled distributions of rai cnuflaalrl ( cFhiagnugrees2i . n2ftrhae in f p al rlob (F ab ig il uir ty eim nd oidveildsun al eepdas to t E be N S ab O le etpoisroedpe li scaa te ndt he th eeivroleuv ti ooln vi nogfnoefw co duep velopments in data an ). Very recently, extratropical atmospheric and ocean interactions. There is lesdommeoedveildsehnacveeosftd ar etaeld ys t is oaonpdeinn the accuracy The most optimistic expectation is that once that may have a somewhat c ad d a if lfv er aern ia t t io unpstihnisEN fie S ld O . cEoNuSpO le , d th m ey odw el i s ll bheavaeb le cotnoqhueelrped id etnhtei fy chaanld le npg re edio ct ftmheeasiun red by the ocean s character, as other modes of climate variability. This may include Zhang te ertananl. ua1l99 ti 7 m , eFoslc la al neusr fa ( cKeleteemmapne ra et tures, from links between ENSO and the climate system not yet are now beginning to fin ddeatanlu . m1b9e9r8 ) o . M al. od1e9 ll 9e6 rs , m dis ocdoevlesremdaiyntahiediimnpienrv fe ecsttiogbaste io rv nast io onfaplodsastiab . lIemcplriomvaetdem ab e il cih ty anoin sm th seinde th ca edN al otrothmaun lt d i tropic f potential modes that link ocean basins, such as ENSO-and Barnett 1996). There is adlescoad ev aalltiPm ac eifsiccaf le o r ( vari related variations of SST in the tropical North Atlantic, ENSO links to rainfall may come an id dengcoed th ep aetnsLoam ti e f rece In n tl aydddiistc io u n ss etdoboycE ea n n fi -e altdmaonsdphMea re y er c o ( u1p9l9 in 7 g ). , new nointutdheeo se fcE ul N ar S O va riitas bility in the str ding generations of models need to include realistic land-southern Europe (R eolpfe -le wes .g k . i , a in ndneonrg Ha th th lp e e rn an dAfm ri acga/ rae tm ali oss ti pchm er oedeclosuopflitnhge . la Snudch su rifm ac peroavnedmie ts ntvsegientvao ti lovneaThheeadp , r m ed aiyctaalbsio lity of ENS rt 1987). and adequate descriptions based on observed data of in Northern Hevm ar iyspohnerdeecOa sp d , rail on ntgiem ( e to s Ba c a ls a a le fse , w e sp se eacs ia oln ly strheep re isne it nitaal tio ve nge in ta t m io ondesltsa te is . c W ur orrekn tl oynbleainndg -s m ur afiancleym 19 e9a5n ) s . (i I . n e ., additio meda et al. driven by the development of coupled models for over several cdheacnagdenes , sis ) n ec a th u lso e la r ‘ itvnyfpairciaalbio li rty in the climate climate change projection over the next century conditional ENSO probability l u fo ernecceassetsxsi . m pe Fpcolteeds ’ e values (Dickinson et al. 1996). the Gulf Coast of the United States shows reaxaam sonal Significant advances in coupled model-based ENSO signal for both the first and second half s o tro p n le, f th g e." In Droughts, 65. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-45.
Повний текст джерела"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, 96. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-65.
Повний текст джерела"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, 56. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-39.
Повний текст джерела"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, 57–58. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-40.
Повний текст джерелаТези доповідей конференцій з теми "C.U.T. di Bari"
Maretto, Marco, Vicente Mas, Eva Alvarez, Barbara Gherri, Carlos Gomez, Maria Rosaria Guarini, Anthea Chiovitti, and Gianluca Emmi. "A multidisciplinary approach to urban fabrics analysis. The historical centre of Valencia." In 24th ISUF 2017 - City and Territory in the Globalization Age. Valencia: Universitat Politècnica València, 2017. http://dx.doi.org/10.4995/isuf2017.2017.5674.
Повний текст джерелаFulantelli, Giovanni, Lidia Scifo, and Davide Taibi. "THE ECOLOGICAL SYSTEMS THEORY OF HUMAN DEVELOPMENT TO EXPLORE THE STUDENT-SOCIAL MEDIA INTERACTION." In eLSE 2021. ADL Romania, 2021. http://dx.doi.org/10.12753/2066-026x-21-019.
Повний текст джерела