LEADER 00828nam a2200253 i 4500 001 991001791189707536 005 20020502204239.0 008 950105s1986 it ||| | ita 035 $ab10910384-39ule_inst 035 $aLE02377019$9ExL 040 $aDip.to Studi Storici$bita 082 0 $a746.4 100 1 $aBussagli, Mario$034070 245 13$aLa seta in Italia /$cMario Bussagli 260 $aRoma :$bEditalia,$c1986 300 $a300 p. :$bill. ;$c33 cm. 650 4$aSeta$xStoria 650 4$aTessuti d'arte 907 $a.b10910384$b21-09-06$c28-06-02 912 $a991001791189707536 945 $aLE023 746 BUS 1 1$g1$i2023000017500$lle023$o-$pE0.00$q-$rn$so $t0$u1$v0$w1$x0$y.i11014696$z28-06-02 996 $aSeta in Italia$9445242 997 $aUNISALENTO 998 $ale023$b01-01-95$cm$da $e-$fita$git $h3$i1 LEADER 03539oam 2200541Ia 450 001 9910695336503321 005 20231115164535.0 035 $a(CKB)5470000002369387 035 $a(OCoLC)52259345 035 $a(EXLCZ)995470000002369387 100 $a20030516d2001 ua 0 101 0 $aeng 135 $aurmn|---||||| 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 10$aRelationships between El Nino-southern oscillation and the Arctic oscillation $ea climate-weather link 210 1$a[Camp Springs, Md.] :$c[NOAA, National Weather Service, National Centers for Environmental Prediction, Climate Prediction Center],$d[2001] 215 $a1 electronic text $cHTML file 225 1 $aNCEP/Climate Prediction Center atlas 300 $a"By Y.P. Zhou, R.W. Higgins, and H.-K. Kim."--HTML index page. 300 $a"July 2001." 320 $aIncludes bibliographical references. 330 $a"Time series representing two of the climate systems' most leading variability in northern hemisphere, namely the El Nino-Southern Oscillation (ENSO) and the Arctic Oscillation (AO), together with 50 years of observed daily mean surface air temperature, precipitation over the conterminous United States, as well as circulation fields from NCEP/NCAR CDAS/Reanalysis are used to investigate the climate impact of ENSO and AO and their combined effects. Composites of ENSO only (El Nino, neutral, La Nina) phase, AO only (high, neutral, low) phase, and their nine combinations are constructed for US temperature, precipitation and the circulation fields for each 12 running season. The results show that both ENSO and AO have profound impact on US temperature and precipitation in winter. In general, the low index phase of AO resembles that of La Nina and high index phase of AO resembles El Nino. Therefore, during (C, AO- ) and (W, AO+), enhanced impact on temperature and precipitation anomalous field is expected. For example, while it is normally warmer and drier in the northern states, cooler and wetter in the southern states during El Nino years, the high index phase of AO provides much warmer winter for large areas of US from northern border to central and northeast than the low index phase of AO in the same phase of ENSO. The AO impact on precipitation is less well organized but the impact exists through out the year in the south and east coastal area, as well as the Tennessee and Ohio valley. These composites provide useful tools to support the 6-10 day, monthly and seasonal forecasts in the Climate Prediction Center." 606 $aNorth Atlantic oscillation$vObservations 606 $aSouthern oscillation$vObservations 606 $aWeather forecasting$vAtlases 606 $aOcean-atmosphere interaction$vObservations 606 $aClimatic changes$vObservations 607 $aEl Nin?o Current$vObservations 608 $aAtlases.$2lcgft 615 0$aNorth Atlantic oscillation 615 0$aSouthern oscillation 615 0$aWeather forecasting 615 0$aOcean-atmosphere interaction 615 0$aClimatic changes 700 $aZhou$b Y. P$01383625 701 $aHiggins$b R. Wayne$01382553 701 $aKim$b H. K$01383626 712 02$aClimate Prediction Center (U.S.) 801 0$bOLA 801 1$bOLA 801 2$bOCLCQ 801 2$bGPO 906 $aBOOK 912 $a9910695336503321 996 $aRelationships between El Nino-southern oscillation and the Arctic oscillation$93428685 997 $aUNINA