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@PhDThesis{Guarnieri:2005:EsOrIn,
               author = "Guarnieri, Fernando Lu{\'{\i}}s",
                title = "Estudo da origem interplanet{\'a}ria e solar de eventos de 
                         atividade auroral cont{\'{\i}}nua e de longa 
                         dura{\c{c}}{\~a}o",
               school = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                 year = "2005",
              address = "S{\~a}o Jos{\'e} dos Campos",
                month = "2005-02-22",
             keywords = "geof{\'{\i}}sica espacial, atividade auroral, eletrojeto 
                         auroral, auroras, vento solar, buracos coronais, tempo do 
                         espa{\c{c}}o, ondas magnetohidrodin{\^a}micas, space geophysics, 
                         auroral activity, auroral electrojets, auroras, solar wind, 
                         coronal holes, space weather, magnetohydrodinamic waves.",
             abstract = "Esta tese consistiu no estudo das causas solares e 
                         interplanet{\'a}rias e das conseq{\"u}{\^e}ncias geoefetivas de 
                         14 eventos HILDCAAs ocorridos entre os anos de 1998 e 2001. Estes 
                         eventos foram usados por seguirem rigidamente os crit{\'e}rios de 
                         sele{\c{c}}{\~a}o para este tipo de fen{\^o}meno. No meio 
                         interplanet{\'a}rio os HILDCAAs est{\~a}o associados a feixes 
                         r{\'a}pidos ricos em flutua{\c{c}}{\~o}es alfv{\'e}nicas. No 
                         Sol, estes feixes t{\^e}m origem em buracos coronais, que foram 
                         relacionados {\`a} ocorr{\^e}ncia de cada um dos eventos. Dados 
                         de campo magn{\'e}tico do meio interplanet{\'a}rio e do 
                         {\'{\i}}ndice AE tiveram suas periodicidades analisadas por 
                         t{\'e}cnicas cl{\'a}ssicas, como espectro de pot{\^e}ncia, e 
                         tamb{\'e}m por t{\'e}cnicas modernas, como Multitaper e 
                         Wavelets. As an{\'a}lises de periodicidades mostraram que esses 
                         eventos s{\~a}o altamente complexos e suas componentes de 
                         freq{\"u}{\^e}ncia s{\~a}o numerosas e vari{\'a}veis de evento 
                         para evento. A an{\'a}lise por wavelets foi a que se mostrou mais 
                         eficiente para an{\'a}lise deste tipo de sinal, e indicou que 
                         flutua{\c{c}}{\~o}es de longo per{\'{\i}}odo de Bz (maiores 
                         que 64 minutos) foram as que resultaram em maior atividade do 
                         {\'{\i}}ndice AE. A an{\'a}lise por multi-resolu{\c{c}}{\~a}o 
                         mostrou que, pela filtragem das altas freq{\"u}{\^e}ncias, 
                         {\'e} poss{\'{\i}}vel obter uma elevada correla{\c{c}}{\~a}o 
                         entre Bz e AE. Na ionosfera auroral, os HILDCAAs foram estudados a 
                         partir de imagens do instrumento UVI, a bordo do sat{\'e}lite 
                         POLAR. Estas imagens de emiss{\~a}o de part{\'{\i}}culas 
                         mostraram pela primeira vez a intensidade e 
                         distribui{\c{c}}{\~a}o da emiss{\~a}o durante estes 
                         fen{\^o}menos. As formas aurorais durante HILDCAAs s{\~a}o 
                         brandas e bem distribu{\'{\i}}das ao longo de toda a oval 
                         auroral e algumas vezes cobrindo toda a calota polar. Foi 
                         investigado se os eventos HILDCAAs eram ou n{\~a}o uma forma 
                         cont{\'{\i}}nua de sub-tempestades. Os resultados mostraram que 
                         a atividade cont{\'{\i}}nua dos eletrojatos aurorais n{\~a}o 
                         correspondem {\`a} sub-tempestades, embora elas possam ocorrer 
                         esporadicamente durante os HILDCAAs. Foi desenvolvido um 
                         m{\'e}todo para quantifica{\c{c}}{\~a}o da emiss{\~a}o auroral 
                         a partir das imagens do POLAR/UVI. Estas medidas, al{\'e}m de 
                         fornecerem a taxa de emiss{\~a}o de part{\'{\i}}culas para 
                         eventos HILDCAAs, mostraram que o efeito integrado desta 
                         emiss{\~a}o ao longo de v{\'a}rios dias pode ser maior do que 
                         durante algumas tempestades geomagn{\'e}ticas intensas. A 
                         an{\'a}lise de el{\'e}trons na faixa de 40-400 KeV mostrou que 
                         durante eventos HILDCAAs ocorre uma inje{\c{c}}{\~a}o 
                         cont{\'{\i}}nua de killer electrons em {\'o}rbitas 
                         pr{\'o}ximas {\`a} Terra (entre L=2 e L=4) por um 
                         per{\'{\i}}odo de v{\'a}rios dias. O efeito integrado destas 
                         inje{\c{c}}{\~o}es de el{\'e}trons pode ser altamente danoso 
                         para equipamentos e sensores embarcados em sat{\'e}lites em 
                         {\'o}rbitas nestas regi{\~o}es, justificando assim a necessidade 
                         de estudos, como o desenvolvido na presente Tese, da variabilidade 
                         do Clima Espacial durante a ocorr{\^e}ncia de eventos HILDCAAs. 
                         ABSTRACT: In this thesis a study about the solar and 
                         interplanetary causes and the geoefective consequences of 14 
                         HILDCAA events occurred between 1998 and 2001 was performed. These 
                         events were chosen by following strictly the selection criteria 
                         for this kind of phenomena. In the interplanetary medium, HILDCAAs 
                         are associated with high speed solar wind streams, wich are 
                         frequently embedded with alfv{\'e}nic fluctuations. At the Sun, 
                         these high speed streams are originated in coronal holes. For each 
                         one of the selected events we have found the most probable coronal 
                         hole from where emanated the high speed stream. Interplanetary 
                         magnetic field and AE index were analyzed to find their 
                         periodicities. Classic techniques, such as power spectrum, and 
                         also modern techniques, as Multitaper and Wavelets, were used. 
                         These analysis show that these events are highly complex and their 
                         frequency components are numerous and variable from one event to 
                         another. The Wavelet analysis is the most favorable technique to 
                         analyze these data. It was found that long period Bz fluctuations 
                         (longer than 64 minutes) resulted in the most significant part of 
                         the AE activity. The Multi- resolution analysis found that, 
                         eliminating the high frequencies in both Bz and AE, a high 
                         correlation can be found between them. In the auroral ionosphere, 
                         HILDCAAs were studied using the UVI instrument onboard POLAR 
                         satellite. These images show, for the first time, the intensity 
                         and distribution of the emission during these events. Auroral 
                         shapes during HILDCAAs were only moderate and well distributed 
                         along the whole auroral oval, and sometimes covering the whole 
                         polar cap. It was investigated whether HILDCAAs are a continuous 
                         form of substorms. The results showed that the continuous activity 
                         observed in auroral electrojects do not correspond to substorm 
                         expansion phases, although some substorms can occur sporadically 
                         during HILDCAAs. A new method was developed to quantify the 
                         auroral emission based in the POLAR/UVI images. These 
                         measurements, besides providing the particle emission rate during 
                         HILDCAAs, showed that the time integrated effect of this emission 
                         during several days can be greater than the values observed during 
                         some intense geomagnetic storms. The electrons in the range 
                         between 40-400 KeV (killer electrons) observed during HILDCAA 
                         events presented continuous injections in orbits close to the 
                         Earth (between L=2 and L=4), lasting for several days. The time 
                         integrated effects of these injections in the geostationary orbits 
                         can be highly harmful to equipments and sensors onboard satellites 
                         orbiting these regions. These effects justify the development of 
                         studies on Space Weather variability during HILDCAA occurrences, 
                         as performed in this Thesis.",
            committee = "Sobral, Jos{\'e} Humberto Andrade (presidente) and Alarcon, 
                         Walter Dem{\'e}trio Gonzalez (orientador) and Alves, Maria 
                         Virg{\'{\i}}nia and Alarcon, Al{\'{\i}}cia Luiza Cl{\'u}a de 
                         Gonzalez and Tsurutani, Bruce T. and Ferreira, Jos{\'e} 
                         Leonardo",
           copyholder = "SID/SCD",
         englishtitle = "A study of the interplanetary and solar origin of high intensity 
                         long duration and continuous auroral activity events",
             language = "pt",
                pages = "316",
                  ibi = "6qtX3pFwXQZ3r59YD7/FUaBo",
                  url = "http://urlib.net/ibi/6qtX3pFwXQZ3r59YD7/FUaBo",
           targetfile = "paginadeacesso.html",
        urlaccessdate = "20 maio 2024"
}


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