VARIAÇÕES SOBRE OS HOMENS AS PALAVRAS UNEM E DIVIDEM OS HOMENS CORTAM-SE E CONSTROEM-SE RELAÇÕES COM PALAVRAS PODEM SER DESTRUÍDAS ESSAS RELAÇÕES NA FORMA ORAL OU ESCRITA PODEM SER PALAVRAS GESTUAIS OU VISUAIS LÊ-SE MAIS NAS PALAVRAS DE UM HOMEM SOBRE O QUE ELE É DO QUE NAS SUAS ACÇÕES AS PALAVRAS E GESTOS SÃO INTENÇÕES MOMENTÂNEAS NÃO O DEFINEM OS SEUS DISCURSOS, EXPRESSÕES ESCRITAS NO TEMPO JÁ O DEFINEM ALGUNS QUEREM SER ACEITES POR OUTROS (CONCEITO ALIENÍGENA PARA ALGUNS) OUTROS QUE CONSIDERAM SEUS SUPERIORES,SEUS IGUAIS, SEUS SEGUIDORES CEGOS PARA SE APROXIMAREM DESTES SERES USAM O INGLÊS COMO LINGUAGEM UNIVERSAL OU O CHINÊS OU OUTRA LÍNGUA DESPREZANDO A SUA LÍNGUA MATERNA POIS QUEREM QUE OS OUTROS OS TOMEM A SÉRIO QUEREM SER FUTUROS CÉSARES, FUTUROS ÁTILAS, VOLTAIRES E SÓCRATES PRESENCIAIS OU HIPOTÉTICOS POETAS É FÁCIL MANIPULAR OS HOMENS COM PALAVRAS FÁCIL É TAMBÉM AFASTÁ-LOS OU APROXIMÁ-LOS
Mais fácil ainda, usando convenções e sinais, apelando às suas necessidades estéticas e de ordem. As plavrs pdem sr ldas na desrdem, na maioria dos cérebros,mas não apelam à leitura.
The mélange behaves as a weak, granular ice shelf whose rheology varies seasonally. Sea ice growth in winter stiffens the mélange matrix by binding iceberg clasts together, ultimately preventing the calving of full-glacier-thickness icebergs (the dominant style of calving) and enabling a several kilometer terminus advance. Each summer the mélange weakens and the terminus retreats. The mélange remains strong enough, however, to be largely unaffected by ocean currents (except during calving events) and to influence the timing and sequence of calving events. Furthermore, motion of the mélange is highly episodic: between calving events, including the entire winter, it is pushed down fjord by the advancing terminus (at ∼40 m d−1), whereas during calving events it can move in excess of 50 × 103 m d−1 for more than 10 min. By influencing the timing of calving events, the mélange contributes to the glacier's several kilometer seasonal advance and retreat; the associated geometric changes of the terminus area affect glacier flow. Furthermore, a force balance analysis shows that large-scale calving is only possible from a terminus that is near floatation, especially in the presence of a resistive ice mélange. The net annual retreat of the glacier is therefore limited by its proximity to floatation, potentially providing a physical mechanism for a previously described near-floatation criterion for calving. Versuchsanstalt für Wasserbau, Hydrologie und Glaziologie
June 2009 accepted 17 September published 21 January 2010, as times goes by
Solar cycle 23,ended in 2008, lasted longer than previous cycles, with a prolonged phase of low activity that scientists had difficulty explaining.
The new NCAR analysis suggests that one reason for the long cycle could be changes in the Sun's conveyor belt. Just as Earth's global ocean circulation transports water and heat around the planet, the Sun has a conveyor belt in which plasma flows along the surface toward the poles, sinks, and returns toward the equator, transporting magnetic flux along the way.
The key for explaining the long duration of cycle 23 with our dynamo model is the observation of an unusually long conveyor belt during this cycle," Dikpati says. "Conveyor belt theory indicates that shorter belts, such as observed in cycle 22, should be more common in the Sun."
Recent measurements gathered and analyzed by Ulrich and colleagues show that in solar cycle 23, the poleward flow extended all the way to the poles, while in previous solar cycles the flow turned back toward the equator at about 60 degrees latitude. Furthermore, as a result of mass conservation, the return flow was slower in cycle 23 than in previous cycles.
In their paper, Dikpati, Gilman, and de Toma used simulations to model how the solar plasma conveyor belt affected the solar cycle. The authors found that the longer conveyor belt and slower return flow could have caused the longer duration of cycle