Academic literature on the topic 'Osobni͡ak N.V'
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Journal articles on the topic "Osobni͡ak N.V"
Li, Chi-Kwong, and Yiu-Tung Poon. "Diagonals and Partial Diagonals of Sum of Matrices." Canadian Journal of Mathematics 54, no. 3 (2002): 571–94. http://dx.doi.org/10.4153/cjm-2002-020-1.
Full textKhemmani, Varanoot, and Supachoke Isariyapalakul. "The Multiresolving Sets of Graphs with Prescribed Multisimilar Equivalence Classes." International Journal of Mathematics and Mathematical Sciences 2018 (August 1, 2018): 1–6. http://dx.doi.org/10.1155/2018/8978193.
Full textChen, Xiaodong, Meijin Xu, and Yanjun Liu. "Spanning 3-Ended Trees in Almost Claw-Free Graphs." Discrete Dynamics in Nature and Society 2015 (2015): 1–5. http://dx.doi.org/10.1155/2015/476182.
Full textAssaf, David, and Ester Samuel-Cahn. "The secretary problem: minimizing the expected rank with I.I.D. random variables." Advances in Applied Probability 28, no. 3 (1996): 828–52. http://dx.doi.org/10.2307/1428183.
Full textAssaf, David, and Ester Samuel-Cahn. "The secretary problem: minimizing the expected rank with I.I.D. random variables." Advances in Applied Probability 28, no. 03 (1996): 828–52. http://dx.doi.org/10.1017/s0001867800046516.
Full textTokarčíková, Katarína, Beáta Bolerázska, Tomáš Elexa, and Štefan Hauks. "Laboratórna dynamika akútneho infarktu myokardu / Laboratory Dynamics of Acute Myocardial Infarction." Laboratórna Diagnostika XXVII, no. 2/2022 (2022): 188–95. https://doi.org/10.5281/zenodo.7224731.
Full textSayi, Robi Nugraha, Lyra Yulianti, and Syafrizal Sy. "DIMENSI METRIK DARI GRAF Wn + Cn, UNTUK n 2 f3; 4g." Jurnal Matematika UNAND 7, no. 2 (2018): 165. http://dx.doi.org/10.25077/jmu.7.2.165-169.2018.
Full textLong, Mary C., Vincent Escuyer, and William B. Parker. "Identification and Characterization of a Unique Adenosine Kinase from Mycobacterium tuberculosis." Journal of Bacteriology 185, no. 22 (2003): 6548–55. http://dx.doi.org/10.1128/jb.185.22.6548-6555.2003.
Full textLukan, Norbert. "Cytokínová búrka v ére kovidovej / Cytokine storm in the covid era." Laboratórna Diagnostika XXVII, no. 2/2022 (2022): 32–33. https://doi.org/10.5281/zenodo.7319282.
Full textBalla, Ján. "Vzdelávanie, školenie a hodnotenie kompetencií POC testovania v primárnej starostlivosti / Education, training, and assessment of POC testing competencies in primary care." Laboratórna Diagnostika XXVII, no. 2/2022 (2022): 24–26. https://doi.org/10.5281/zenodo.7233838.
Full textBook chapters on the topic "Osobni͡ak N.V"
"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. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-60.
Full text"National Drought Mitigation Center for the forty-eight contiguous states in the United States demon strated that severe and extreme drought affected more than 25 per cent of the country in twenty-seven o of ft7h5e0p ,0 a 0 st 0omnie2h (1 u , n9d4r2e , d50y0 ea k rs m . 2 T ) h o is rrm ep orrees . ents an area con D tr raosutg to htf lo s o el ddso , m hu rrre ic su an lt ess , inansdtrtuoc rn tu ardaol es d . a m Fo argteh , e s in e reasons, the quantification of impacts and the pro vision of disaster relief are far more difficult tasks for A fif lttyho ye uagrhsaT go an , n c ehill’s book was written m drought than they are for other natural hazards. recognising the li omnasteotloogf ists continue to strug o g re le twhiatnhtEommeerdgetnocydem al a in ngagweirtsh , ifm or paecxtasm th p a le t , ar aerestm ru ocrteu ra alccaunsd p cr oiltiecry ia ) m fo ak redresclcaor ntinue tdor ou d g eb hat te a nd th e sc ie bnatsiissts (i a . ned ., lcoocm al m ise udn , i ca re ti sopno nd an in dgttroa ns th peosre ta t e io v n en ts c ha bnynerless , to p ri rnog acc Second, the ab in se gnacneeonfdatopraecdirsoeugahntd . universally vdird in in k g in gemwear te gre , nacnydm so edfiocratlh . s T up h p es li eesc , ha ernascu te r r in is g ti cs sao fe f a it bsoeupttewdh definition of drought adds to the confusion drought have hindered the development of accurate, mu dsetgb re eeeotf her or reg s io ev nerai ty n . oRtneaald is rto ic uag lly h , tdeexfiisntistiaonnds , oiffd it roduogehst , a re nld ia , bl uel , tiamnadtetliym , el tyhee st fiom rm ate u s la o ti fon se voefr it dyraonudgh im tpcaocn ts T th haitshiasvoenbeeeenxpdle an d at iaopnplfiocrattihoens ( coor re im spoafcdt) efsipne it ciio fi ncs . ting Heanzcayrd pl aenvsenbtysm ha ovsetbgeoevnerrnam nk eend ts b . y Bryant (1991) faincaalty io se ndsm tud o y re , th vaenl op 1e5d0 . W de iflihniitte io annsdiGn la th n e tz ir (1 c 9 la 8 ss 5 i ) roannk th in egb is assiusmomftah ri esierdcihnarTaacb te le ri s1t . i1c . sKaenydhiamzp ar adctcsh . aTrh ac is ddeeffiinne it idornosug are annudmemraonuys , mmoarney ex diost. noAtl th ad oeuqguhatteh ly etoefritsh ti ecsdu eg se re defoorftsheivsee ri v ty al , ulaetn io g n th inocf lu edveenatn , e to xtparlesasrieoanlp ar oel ic a y rb m i akers h . t T in hemteharneisnhgofludlstefromrsde fo cl ras ri c n ie gntd is rtosuagnhdteefxfteecn ts t, , tlootnagl -l toesrsm of im li p fe a , ctt , otsauldedceonnnoem ss i , calnod ss , oscoccu ia r lteox am sp pelceitfriacryim in pam ct o s st inc as keesy (i e . ceo ., ntohm ey ic ar seecn to orts ) l . i nk FeodrA re lntcheouogfhatshseocriaattiendgshoafzatrhdesvfao ri rou th s ir htayz -a orndesihnazTaarbdlse . pmeor cent , owfnho at r m is atlhperesc ig ip niitfa ic ti aonnceovoefraatphe re ri sohdolodfo th fr7e5ep1r .1 ova id re essuabnjeicnttievge, rattheedoavsesreaslslm ra ennktiosfuh se afzualrdb ec cahuas ra eci tsee spe nctihas ll yormmio sl reea ? d A in gdeffo in r i ti looncao ti fon th sisw ty it phewa ou st lrdonbgetBee ri csatu ic sseoafntdhetihne te nrse it lya , t io dnusrhaitp io s n , baen tw desepna tia hlaezxatredns. t s ty ta p as eos na olfcporm ob ploenm ent of annual precipitation. These of drought events and the magnitude of associated init n io d n in s g an odftthheelcsaocn are kceopft th beytrheo su c se lt f o or fmau la m ti insgunddeefr icm og pean ct t s , a d rg ruom ug ehntt , ra hnokwsevveerry , h th ig aht . t O ot naelc lo asnsmoafke li fe aaop th p e ly rtshce ie dne ti fsitnsito io rndiin sc a ip clt in oenssiw de il rlateivoenntguiavle ly n n to ee dhotwo associated with drought in this case is significantly assessments of impact in u m al uld ti rpoluegh ec tosn it oum ations (e.g., d ov ro e u rr gah te t d . isLo ra srseoifnl if meo th sattsies tt d in ir gesc . t ly T h as esorcain at keidngwib th yrderlo ie ufgphrtogdreacm la m ra e ti s o ) n . s or revocations for eli igcibsie li cttyortso , dBrroyuagnhtt. atT tr h ib is uitses in a lo pspsroopfr ia li tfeesb in ecceau th se eporfim fa a m ry inceautsoe spre Tahdi rd ov , er draoluag rg hetrigmepoagcrtaspha ic re a nonstruct of famine in recent decades has been civil war or that result from other natural haz laradrse . aFtohraneudraamla and political strife, both of which heighten vulnerability to recent analysis of drought occurrence by x th aemp ( lUeg , eassdS) fa yrsotu em ght. mine s . anDdrocu an ghbteeavesnitgsnid fi icsarnutptnaftouord al p tr riogdguecrtifoonr." In Droughts. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-26.
Full text"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.
Full textConference papers on the topic "Osobni͡ak N.V"
Kováčová Holevová, Bibiána. "PRACOVNÉ CIELE V KONTEXTE ĎALŠÍCH CIEĽOV SÚČASNÝCH MLADÝCH ĽUDÍ NA SLOVENSKU." In PSYCHOLÓGIA PRÁCE A ORGANIZÁCIE 2023. Vydavateľstvo ŠafárikPress, Univerzita Pavla Jozefa Šafárika v Košiciach, 2023. http://dx.doi.org/10.33542/ppo-0265-7-18.
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