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Artykuły w czasopismach na temat "ET AND HT"
Moret, C. "Autorécepteur sérotoninergique et antidépresseurs". Psychiatry and Psychobiology 5, nr 3 (1990): 195–99. http://dx.doi.org/10.1017/s0767399x00003497.
Pełny tekst źródłaLenka, Abhishek, Ketaki Swapnil Bhalsing, Ketan Ramakant Jhunjhunwala, Vijay Chandran i Pramod Kumar Pal. "Are Patients with Limb and Head Tremor a Clinically Distinct Subtype of Essential Tremor?" Canadian Journal of Neurological Sciences / Journal Canadien des Sciences Neurologiques 42, nr 3 (10.04.2015): 181–86. http://dx.doi.org/10.1017/cjn.2015.23.
Pełny tekst źródłaYang, B. C., W. W. Nichols, D. L. Lawson i J. L. Mehta. "5-Hydroxytryptamine potentiates vasoconstrictor effect of endothelin-1". American Journal of Physiology-Heart and Circulatory Physiology 262, nr 4 (1.04.1992): H931—H936. http://dx.doi.org/10.1152/ajpheart.1992.262.4.h931.
Pełny tekst źródłaDumas, Catherine. "Comedias et comédies au Grand Siècle : adaptation et désaveux". Horizons/Théâtre, nr 3 (31.12.2013): 34–45. http://dx.doi.org/10.4000/ht.3109.
Pełny tekst źródłaXu, Tao, Kangying Cao, Changwei Wang i Shiwei Yin. "The effect of asymmetric external reorganization energy on electron and hole transport in organic semiconductors". Physical Chemistry Chemical Physics 23, nr 28 (2021): 15236–44. http://dx.doi.org/10.1039/d0cp06686a.
Pełny tekst źródłaBhaskaran, Subha, Jeremy Zaluski i Amy Banes-Berceli. "Molecular interactions of serotonin (5-HT) and endothelin-1 in vascular smooth muscle cells: in vitro and ex vivo analyses". American Journal of Physiology-Cell Physiology 306, nr 2 (15.01.2014): C143—C151. http://dx.doi.org/10.1152/ajpcell.00247.2013.
Pełny tekst źródłaCalame, Claude. "La tragédie grecque comme performance musicale et rituelle : voix et danses chorales". Horizons/Théâtre, nr 8-9 (1.01.2017): 10–26. http://dx.doi.org/10.4000/ht.741.
Pełny tekst źródłaLeón-González, Antonio J., Prudencio Sáez-Martínez, Juan M. Jiménez-Vacas, Vicente Herrero-Aguayo, Antonio J. Montero-Hidalgo, Enrique Gómez-Gómez, Andrés Madrona i in. "Comparative Cytotoxic Activity of Hydroxytyrosol and Its Semisynthetic Lipophilic Derivatives in Prostate Cancer Cells". Antioxidants 10, nr 9 (25.08.2021): 1348. http://dx.doi.org/10.3390/antiox10091348.
Pełny tekst źródłaRemaud, Sylvie, i Barbara Demeneix. "Les hormones thyroïdiennes régulent le destin des cellules souches neurales". Biologie Aujourd'hui 213, nr 1-2 (2019): 7–16. http://dx.doi.org/10.1051/jbio/2019007.
Pełny tekst źródłaGiona, Fiorina, Marica Laurino, Luciana Teofili, Sara Capodimonti, Maurizio Martini, Giovanna Palumbo, Maria Luisa Moleti i in. "Primary Trombocythemia in Children and Adolescents Includes Different Subtypes Compared to Adult Essential Thrombocythemia". Blood 124, nr 21 (6.12.2014): 1865. http://dx.doi.org/10.1182/blood.v124.21.1865.1865.
Pełny tekst źródłaRozprawy doktorskie na temat "ET AND HT"
MIQUEL, MARIE-CHRISTINE. "Caracteristique biochimique et moleculaire des recepteurs serotoninergiques 5-ht#3 et 5-ht#1a dans le systeme nerveux central". Paris 6, 1991. http://www.theses.fr/1991PA066242.
Pełny tekst źródłaTournois-Hirzel, Claire. "Récepteur 5-HT 2B murin : voies de transduction et isoformes". Paris 5, 2000. http://www.theses.fr/2000PA05P626.
Pełny tekst źródłaRAMPILLON-GARCIA, VALERIE. "Conception et synthese d'antagonistes des recepteurs serotoninergiques 5-ht#3". Paris 6, 1994. http://www.theses.fr/1994PA066432.
Pełny tekst źródłaYANG, DONGLAI. "Conception et synthese d'antagonistes des recepteurs serotoninergiques 5-ht#3". Paris 11, 1994. http://www.theses.fr/1994PA112136.
Pełny tekst źródłaJouha, Jabrane. "Conception, synthèse et évaluation biologique de nouveaux ligands sérotoninergiques 5-HT₇". Thesis, Orléans, 2017. http://www.theses.fr/2017ORLE2013/document.
Pełny tekst źródłaSerotonin-activated cell-surface receptor 5-HT₇ is the most recently discovered 5-HT receptor. Intensive studies of structure-activity relationships have been pursued by several research groups, including our laboratory, and have resulted in the publication in the literature of an impressive number of potential ligands 5-HT₇. In this context, the main purpose of this thesis is to design four distinct classes of ligands. First, we were interested in the preparation of 2,4-diaminopyrido[2,3-d]pyrimidinique and 2,4-diaminopyrimidinique ligands. Subsequently, we developed a third family of compounds built on a pyridine scaffold, from one of the most interesting current 5-HT₇ selective agonists, via an effective multistep strategy. The last part of this thesis was devoted to developing an original and rapid method for the synthesis of polysubstituted tetrahydro-1,6-naphthyridines starting from the 3-vinyl-1,2,4-triazines platforms via a domino addition sequence of aza-Michael and intramolecular inverse-electron-demand Diels-Alder cyclization
Langlois, Xavier. "Etude de l' expression et de l' adressage des récepteurs 5-HT 1A et 5 HT-1B/1D Bêta de la sérotonine à l' aide d' anticorps spécifiques". Paris 5, 1996. http://www.theses.fr/1996PA05P604.
Pełny tekst źródłaSchohn, Hervé. "Purification et caractérisation des protéines entérocytaires impliquées dans l'absorption de la vitamine B12 (récepteur du facteur intrinsèque et transcobalamine) dans l'intestin mature et fœtal". Nancy 1, 1990. http://www.theses.fr/1990NAN10399.
Pełny tekst źródłaMassot, Olivier. "5-HT-moduline : un nouveau peptide endogène interagissant spécifiquement avec les récepteurs sérotoninergiques de type 5-HT 1B/1D, purification, identification, caractérisation biochimique et fonctionnelle". Paris 5, 1994. http://www.theses.fr/1994PA05P614.
Pełny tekst źródłaLaumonier, Mickaël. "Mélange de magmas à HP-HT : contraintes expérimentales et application au magmatisme d'arc". Phd thesis, Université d'Orléans, 2013. http://tel.archives-ouvertes.fr/tel-00859628.
Pełny tekst źródłaRIAD, MUSTAPHA. "Les recepteurs 5-ht#1#a et 5-ht#3 de la serotonine - nouvelles approches pour l'etude de leurs implications fonctionnelles dans des cellules en culture". Paris 6, 1994. http://www.theses.fr/1994PA066686.
Pełny tekst źródłaKsiążki na temat "ET AND HT"
Designråd, Dansk, red. Et bomaerke for HT: The spirit of a trademark. Copenhagen: Dansk Designråd, 1985.
Znajdź pełny tekst źródłaCaron, Daniel J. Web HT.0: Pour une société informée : la pertinence numérique et ses défis pour les sociétés démocratiques au XXIe siècle. Paris: Hermann, 2011.
Znajdź pełny tekst źródłaWeb HT.0: Pour une société informée : la pertinence numérique et ses défis pour les sociétés démocratiques au XXIe siècle. Paris: Hermann, 2011.
Znajdź pełny tekst źródłaCzęści książek na temat "ET AND HT"
Micevski, B. "Faunistics, Ecology, Structure and Energetics of the Ornithocenosis in Macedonian Oak Ecosystem (Quercetum Trojanae Em Et Ht.) in the Np Galičica (Macedonia, Yugoslavia)". W Responses of Forest Ecosystems to Environmental Changes, 983–84. Dordrecht: Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-2866-7_253.
Pełny tekst źródłaAnderson, Garnet L., i Ross L. Prentice. "Understanding the Effects of Menopausal Hormone Therapy: Using the Women’s Health Initiative Randomized Trials and Observational Study to Improve Inference". W Causality and Psychopathology. Oxford University Press, 2011. http://dx.doi.org/10.1093/oso/9780199754649.003.0009.
Pełny tekst źródła"tor, and R13 and R14 divider ratio can be set up and adjust the output voltage to reach high voltage accu-ra tc o yr . Ind a Rd 1 d3 it i ao n nd , Ra 1 n4 R dC iv i cd i er r iti oco cn an eb c et e s det b ue p ed en th ae d j cu a st t ht o hd e eo u a tn p du t t vh o el ta r ge e tr o ca e vh o il g hg v eo l t te a rg m ei a nc a u - of TL cn o n tt u pR ro ri t ou n lc - en ri ate ti ct o te r le tor, and R13 an sp d roR o1 r d en r oit u i ns1 id v tep tra tac". W Network Security and Communication Engineering, 181–82. CRC Press, 2015. http://dx.doi.org/10.1201/b18660-40.
Pełny tekst źródła"some of the n ev oetr , aliltd is rovuegrsy tr ht ocn le g ENS s in arKfernoymOFeivgeunrta are as ess ( 4 F . i socia 5 gure t e ed awn4d . it 5h4 ). . E5HfoNtwShO at T ou hte chance of any year being d . exte tnhdeincgouonvte ry r , a o ll rpaanry ts droofuK gh en troofuaghpta -r f t re ya, are ailceu through so la re r la se ti avseoln y low (Ogallo 1989). t inte Trh an envuuallne ra ra in bfia li l ty of the country to high degrees of liom ng el -y ra n an gdep ef rfeedcitc iv levad ri raobu il g it hythm ig ohnliitgohrtisng the need for components of dis ti aosn te , rapnrdepeaa re rl dyne warning , ss strat d eg as ia gcn ru o c sis, devastating impacts of the droughts in ies. Th ia elttaotg io et nheerf fo writtsh th th at eap re osct-odm is m as o te nrirnelm ie afnayndd ev re K h enya, co elo apbiin li g tchoeunm tr o ie sst , raerceenhtig ( h1l9 ig 9h6t -e 7 d ) in the nsidered one of the worst d in ro rueghnte , xwt section, using cent ye haircsh . has been aEnxoammapllieesso ar f e th g e iv etn im ienF se ig ri uersesof4 . t6heansde asonal rainfall specific locations. It is evident from the 4 . f 7 ig for some ures that". W Droughts, 86–87. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-62.
Pełny tekst źródła"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 ’." W Droughts, 38–39. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-27.
Pełny tekst źródła"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". W Droughts, 43–44. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-31.
Pełny tekst źródła"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". W Droughts, 65. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-45.
Pełny tekst źródła"te a c ri hanbiiq li ues draw on many aspects of recorded past cast skill is that the statistical techniques generally cao ss r o re cliaattie ty d w in i th thEeNS cl O im . aItne system, not just those perform poorly in northern spring, with cross forecasts o , nanaunmd be mruo lt fipo le ad li dnieta io r n to simple linear validated anomaly correlations <0.6 for forecasts even operational use. These ttohoelrssitn at c i sti rceagl re to ss oilosn -a braes ed just one season ahead and <0.3 for forecasts two antianalogs (Livezey lude analogs an idnd se aam so pnesdapheerasd is . te S n im ce p l ( eapceorm sis btiennacte io onfo th fepeSrS si Tss te , nocrethaenidrCClain mate Normals ( OaC nd N ) B a ( r H ns utaonng 19 e8t8a ), l . O1p9 ti 9m4a ) l , tcilm im eao to fltohgeyy ), easrh . ow just as much, or more, skill at this l P in re eio se n n ic d al Correlation Analysis (CCA) (Barnett and Even if the statistically based SST forecasts were War adrda is ocrrfiemr in 1a9n8t7a ) n , a ly asnids (M eig a e ry novnecatnodrSatnoarleyy si s19a8n5d , p th earn fe -c pte , rf heocwtreevlear ti , o n th sh e ip hsisbteotrw ic eaelnrS ec SoTrda no sh moaw li sesla es nsd -d beav se e d lo ponndnFeoulrlaalndne1 tw 99 o 1). More complex methods precipitation even for regions with a strong ENSO skill scor eedso (e f . g o . p , er Lao ti nognaertksal. ha1v9e also recently been influence. In such regions, precipitation anomalies these tools has been mar lgpirneacl ip in it 9a7 ti ) o . nIn fo general, the typically show a consistent ENSO relationship in 75-much more skilful in parts of the t h tr eopeixc tr raetcrao sts using 80 per cent of the ENSO episodes this century. How et al. 1993). In the extratropics, statist s ic a (e l .g p . i , cWsba ut ever, even the best performing statistical SST pre offer little encouragement for more reliable m dr e o th uogd rd s b di e c tw tio enen sc ohbes mes have ht Pacific SST oefrv0e .8 d -0 a .9 ndcp ro re sds-ivca te li for two se d d ate aso t n ro dspa ic caolr re e la atsitoen rn s p cu re r d re ic nttiosn ta steexocfepEtNwShOenoursw ed it h in EcNoS nj Ounfcotrieocnasw ts i th (e . tgh . e , n co orrrtehleartn io nsuomfm th er e through fall. Thus if th hee ad an ionmtahleysB ta atrin st sitcoanldarnodu gh Stmp it rhe di 1c9 ti 9o6n ) . t ha Wter el nao te w s to fo cEuNsSoOn , m th ieghotbr served SST igs iv 0 e . n8irnegs io tr noanlgpE re N ci SpO ita tyieoanrsw , w ith e a in ndpatrh ti ecuplraerd . iction of central and eastern Pacific SST pitation eawsio th na abn ly o m ex a p ly ecctotrorem la atk io e such year nps re odfi0 ct . i6o -n 0 s . 7ofdpurreicnig icsorcro el nastiisosn -o i v .e e . r , a in ll aybeo ar ustwhialllfboefsau ll byse ta a n rs t . iaT ll hyeleasvse ; rtahgies tent with experience (Barnston and Smith". W Droughts, 59. Routledge, 2016. http://dx.doi.org/10.4324/9781315830896-41.
Pełny tekst źródłaStreszczenia konferencji na temat "ET AND HT"
Jin, W., T. Atkinson, G. Neupane, T. McLing, C. Doughty, N. Spycher, P. Dobson i R. Smith. "Influence of Mechanical Deformation and Mineral Dissolution/precipitation on Reservoir Thermal Energy Storage". W 56th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2022. http://dx.doi.org/10.56952/arma-2022-2068.
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