695 resultados para Chuanxi Plateau, China
Resumo:
In the last decade, the presence of China in Latin America has been characterized by a model of economic cooperation based on pragmatic principles of complementarity and mutual benefits. Latin America is presented as a “paradise” of natural resources and expanding markets, while China stands as the main financier and investor in the region. In this scenario, particularly since 2009, Ecuador has become one of the top recipients of Chinese funding and investment, mainly in strategic sectors such as energy and infrastructure. The presence of China in the country has been the subject of extensive discussions about the true benefits and costs behind its model of economic cooperation.
Resumo:
This paper states that even though the Antarctic Treaty is a remarkable instrument for peaceful collaboration and scientific research, it is, basically, a by-product of the Cold War that reaffirms a particular status quo. This paper explores whether the ATS will meet the needs of an emerging world order. Particularly, the paper evaluates the ATS in the face of new global challenges, both internal and external to the Antarctic Treaty System (ATS) itself, as well as power shifting processes on a world scale, climate change and the changing interests of new states. China is a key component in understanding this issue because its Antarctic engagement is entering a new phase one that challenges current multilateral provisions. China’s Antarctic program will be analyzed within the framework of International Relations approaches and theories.
Resumo:
Formando parte importante del conjunto de los países en vías de desarrollo, América Latina y el Caribe constituyen una fuerza relevante en el actual escenario internacional. Las nuevas circunstancias traen renovadas oportunidades de desarrollo para las relaciones sino-latinoamericanas y no-caribeñas. La elaboración por parte del Gobierno chino del Documento sobre la Política hacia América Latina y el Caribe tiene como propósito manifestar con mayor claridad los objetivos de la política china hacia la región, plantear los principios rectores de la cooperación en las diversas áreas durante un determinado período del futuro y promover el continuo desarrollo sano, estable e integral de las relaciones sino-latinoamericanas y sino-caribeñas.
Resumo:
Los Jefes de Estado y de Gobierno y los Representantes Especiales de Brasil, China, así como Costa Rica, Cuba, Ecuador, Antigua y Barbuda, también miembros del Cuarteto de CELAC – y Argentina, Bolivia, Chile, Colombia, Guyana, México, Paraguay, Perú, Surinam, Uruguay y Venezuela, realizamos una reunión en Brasilia, el 17 de julio de 2014, bajo el tema “Igualdad y Beneficio Mutuo, Cooperación Recíproca y Desarrollo Común”, emiten una declaración conjunta reconociendo que el mundo está experimentando por un proceso de globalización económica y cambio político y que nuestros países tienen un rol clave que desempeñar contribuyendo a la paz, la estabilidad, el crecimiento inclusivo y el desarrollo sostenible, la prosperidad y para la forja de un mundo multipolar.
Resumo:
This CEPS Special Report gives an overview of China’s perceptions of the EU and the protection of Chinese investments in Europe since the outbreak of the European sovereign debt crisis, especially since the more concrete talks in late 2011 on possible financial support from China. Although the top leadership of the communist party of China (CPC) changed in its recent handover, the perceptions described in this paper are likely to remain the same, just as the main tenets of China’s foreign policy are unlikely to change in the near future. The report argues that while the EU’s image has suffered greatly from the sovereign debt crisis and the way it has been handled, there is room to improve China’s view of Europe and for the EU to maintain a relatively strong negotiation position towards China.
Resumo:
The influence on the summer flow over Asia of both the orographic and thermal forcing of the Tibetan Plateau is investigated using a sequence of idealised experiments with a global primitive equation model. The zonally averaged flow is prescribed and both realistic and idealised orography and heating are used. There is some similarity between the responses to the two forcings when applied separately. The upper tropospheric Tibetan anticyclone is predominantly forced by the heating but also weakly by the orography. Below this, both forcings tend to give air descending in an equatorward anticyclonic circulation down the isentropes to the west and rising in a similar poleward circulation to the east. However the heating-only response has a strong ascending southwesterly flow that is guided around the south and south-east of the orography when it is included. On the northern side, the westerly flow over the orography gives ascent on the upslope and descent on the downslope. It is found that heating over the Plateau leads to a potential vorticity (PV) minimum and that if it is sufficiently strong the flow is unstable, producing a quasi-biweekly oscillation. During this oscillation the Tibetan anticyclone changes between a single centre over the southwestern side of the Plateau and a split/double structure with centres over China and the Middle East. These characteristics are similar to observed variability in the region. Associated with this quasi-biweekly oscillation are significant variations in the strength of the ascent over the Plateau and the Rossby wave pattern over the North Pacific. The origin of the variability is instability associated with the zonally extended potential vorticity PV minimum on a θ-surface, as proposed by Hsu and Plumb (2000). This minimum is due to the tendency to reduce the PV above the heating over the Plateau and to advection by the consequent anticyclone of high PV around from the east and low PV to the west. The deep convection to the south and southeast of the Plateau tends to suppress the quasi-biweekly oscillation because the low PV produced above it acts to reduce the meridional PV gradient reversal. The occurrence of the oscillation depends on the relative magnitude of the heating in the two regions.