%0 Journal Article %@holdercode {isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S} %@nexthigherunit 8JMKD3MGPCW/3EUPEJL %@nexthigherunit 8JMKD3MGPCW/43SKC35 %@resumeid %@resumeid 8JMKD3MGP5W/3C9JJ53 %@resumeid 8JMKD3MGP5W/3C9JJ7M %@archivingpolicy denypublisher denyfinaldraft %@usergroup administrator %@usergroup deicy %3 Santos e Silva et al (2009).pdf %X The rainfall field estimated by an S-band radar was evaluated with rain gauges network measurements during the Tropical Rainfall Measuring Mission and Large-Scale Biosphere¡VAtmosphere Experiment in Amazonia (TRMM-LBA), then the daily variability associated with the presence (absence) of the South Atlantic convergence zone (SACZ) were studied. The results showed the high spatial variability of the rainfall over southwest (SW) Amazonia and suggest that local mechanisms (topography and/or local circulations induced by contrast of vegetation) may be associated with heavy rainfall episodes; moreover, it was possible to observe the squall line influence on the diurnal and semidiurnal cycles. Copyright ÆÉ 2009 Royal Meteorological Society. %@mirrorrepository sid.inpe.br/mtc-m18@80/2008/03.17.15.17.24 %8 apr-jun %N 2 %T Diurnal and semidiurnal rainfall cycles during the rain season in SW Amazonia, observed via rain gauges andestimated using S-band radar %@secondarytype PRE PI %K S-POL radar, Amazon basin, TRMM-LBA. %@group CPT-CPT-INPE-MCT-BR %@group DMD-CPT-INPE-MCT-BR %@group DMD-CPT-INPE-MCT-BR %@e-mailaddress deicy@cptec.inpe.br %@secondarykey INPE--PRE/ %@secondarymark B1_GEOCIÊNCIAS %@issn 1530-261X %2 sid.inpe.br/mtc-m18@80/2009/07.28.17.24.26 %@affiliation Instituto Nacional de Pesquisas Espaciais (INPE) %@affiliation Instituto Nacional de Pesquisas Espaciais (INPE) %@affiliation Instituto Nacional de Pesquisas Espaciais (INPE) %B Atmospheric Science Letters %P 87-93 %4 sid.inpe.br/mtc-m18@80/2009/07.28.17.24 %D 2009 %V 10 %@doi 10.1002/asl.214 %A Silva, Claudio Moisés Santos e, %A Gielow, Ralf, %A Freitas, Saulo Ribeiro de, %@dissemination WEBSCI; PORTALCAPES. %@area MET