982 resultados para north central China


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The aim of the thesis is to analyze traffic flows and its development from North European companies` point of view to China and Russia using data from logistics questionnaire. Selected North European companies are large Finnish and Swedish companies. The questionnaire was sent via email to the target group. The study is based on the answers got from respondent companies from years 2006, 2009 and 2010. In the thesis Finnish Talouselämä newspaper and Swedish Affärsdata are used as a database to find the target companies for the survey. Respondents were most often logistics managers in companies. In the beginning of the thesis concepts of transportation logistics is presented, including container types, trade terms, axel loads in roads and in railways. Also there is information about warehousing types and terminals. After that, general information of Chinese and Russian transportation logistics is presented. Chinese and Russian issues are discussed in two sections. In both of them it is analyzed economic development, freight transport and trade balance. Some practical examples of factory inaugurations in China and Russia are presented that Finnish and Swedish companies have completed. In freight transport section different transportation modes, logistics outsourcing and problems of transportation logistics is discussed. The results of the thesis show that transportation flows between Europe and China is changing. Freight traffic from China to European countries will strengthen even more from the current base. When it comes to Russia and Europe, traffic flows seem to be changing from eastbound traffic to westbound traffic. It means that in the future it is expected more freight traffic from Russia to Europe. Some probable reasons for that are recent factory establishments in Russia and company interviews support also this observation. Effects of the economic recession are mainly seen in the lower transportation amounts in 2009.

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Integrated Ocean Drilling Program (IODP) Site U1313, located at the northern boundary of the subtropical gyre in the central North Atlantic, lies within the southern part of the ice-rafted debris belt. Seventy-three palynological samples were studied from an uninterrupted interval ca. 726–603 ka (upper Marine Isotope Stage [MIS] 18 through lower MIS 15) to resolve conflicting paleoceanographic interpretations. Glacial stages were characterized by high productivity surface waters reflecting a southward shift of the Arctic Front. Sea surface salinities (SSSs) and sea surface temperatures (SSTs) were obtained by transfer functions using the Modern Analogue Technique. The lowest SSTs of 9ºC (±1.3) and 10ºC (±1.3) were recorded in glacial MIS 16 and MIS 18 respectively. However, these reconstructions are influenced by abundant heterotrophic taxa and may reflect elevated nutrient levels rather than lowered temperatures. Reworked palynomorphs uniquely indicate a Cretaceous as well as Paleozoic provenance for the first Heinrich-like events.

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Previous research has shown that site-specific nitrogen (N) fertilizer recommendations based on an assessment of a soil’s N supply (mineral N testing) and the crop’s N status (sap nitrate analysis) can help to decrease excessive N inputs for winter wheat on the North China Plain. However, the costs to derive such recommendations based on multiple sampling of a single field hamper the use of this approach at the on-farm level. In this study low-altitude aerial true-color photographs were used to examine the relationship between image-derived reflectance values and soil–plant data in an on-station experiment. Treatments comprised a conventional N treatment (typical farmers’ practice), an optimum N treatment (N application based on soil–plant testing) and six treatments without N (one to six cropping seasons without any N fertilizer input). Normalized intensities of the red, green and blue color bands on the photographs were highly correlated with total N concentrations, SPAD readings and stem sap nitrate of winter wheat. The results indicate the potential of aerial photography to determine in combination with on site soil–plant testing the optimum N fertilizer rate for larger fields and to thereby decrease the costs for N need assessments.

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Durante los últimos diez años, la cooperación militar entre China y Rusia ha buscado proteger los intereses nacionales de ambos Estados, los cuales se encuentran estrechamente relacionados con las dinámicas en materia de seguridad de Asia Central.

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El escenario internacional, antes desfavorable a sus intereses, ha dado un giro a favor del antiguo Imperio del Medio. Si bien el siglo XX estuvo marcado por el fin de la monarquía milenaria, las guerras con sus vecinos Japón, Corea y Rusia, o las cruentas guerras civiles, y con ello tuvo que asimilar cambios para los cuales esta inmensa nación no estaba preparada, el fin de siglo -bajo la conducción de Deng Xiao Ping desde 1978- sirvió para reconducir al país por la vía de la estabilidad y la prosperidad. De este modo, el comienzo del siglo XXI ha sido excepcional y ha marcado un paso de enorme crecimiento y transformación tecnológica y científica.

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El interés de la presente monografía es evaluar las implicaciones geopolíticas que ha tenido la política exterior energética China dentro la región de Asia Central. De esta manera, se analiza el papel de los recursos energéticos en las dinámicas geopolíticas que se están dando en la región centroasiática, al igual que la influencia de grandes potencias en esta zona. Así, teniendo en cuenta la teoría geopolítica de Saúl Bernard Cohen se sostiene que el acercamiento de China, a través de su política exterior energética, ha ayudado a transformar a Asia Central en un shatterbelt debido a su intención de ejercer influencia y control sobre los recursos de la región.

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Este estudio de caso se centra en los esfuerzos de China por reanudar los Six Party Talks o Diálogos a Seis Bandas que son considerados como la opción más viable para tratar la situación nuclear en la península coreana.

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La década de 1950 fue determinante en el establecimiento y póstumo desarrollo del sistema de política exterior de la República Popular China. Al respecto, es de vital importancia realizar un análisis exhaustivo sobre esta primera etapa en donde actores externos a la nación tuvieron un papel determinante. Se busca, entonces, analizar la incidencia que tuvo el discurso de Estados Unidos en la política exterior China a través de un profundo análisis cualitativo que tendrá como base elementos propios de la historiografía. Mediante aproximaciones constructivistas, se pretende demostrar que las creencias pre-existentes de ambos actores (así como la intersubjetividad entre los mismos), determinó la identidad construida a través de la percepción mutua. Lo anterior, impulsó las relaciones predominantemente agresivas entre Estados Unidos y la China Maoísta de principios de la Guerra Fría.

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La cooperación Sur-Sur (CSS) emerge y se consolida ante los constantes cuestionamientos en torno a la cooperación tradicional Norte-Sur. China, a la cabeza de los donantes emergentes “del Sur”, surge como un actor prometedor. Su fuerte dinamismo está cambiando las reglas de juego del sistema internacional de cooperación. Sin embargo, mucho se cuestiona su ayuda como reproductora de las falencias de la cooperación tradicional. Así, China ejemplifica las contradicciones en las que ha caído la CSS: por un lado, las oportunidades de reconfiguración del sistema internacional, y por otro, los desafíos que deberá superar para convertirse en un verdadero modelo alternativo de cooperación y desarrollo en el mundo.

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The text shows the heterogeneous views of various Latin American countries, like Mexico, Brazil, Argentina, Chile, Colombia and Venezuela, in terms of their analyses of and studies about foreign policy. This paper aims to make clear the different images that China generates as a rising power in the world economy, particularly as a major trade partner of these countries. The goal of this article is to provide elements for analysis about policy coordination vis-àvis China. The central argument states that there should be coordination between regional integration strategies and foreign policies in relation to China. However, these heterogeneous visions can work against that goal as well.

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This paper analyzes the People’s Republic of China economic and political ascendance in the 21st century, focusing on the evolution of its sui géneris economic development model and its significance for the relationship between China and the developing countries of the peripheral ‘Global South.’ The objective of this article is to analyze the relationship between China and Latin America in the 21st century, characterizing it as a new Center-periphery global power network based on trade and investment, which is often referred to as the ‘Asian Consensus’. The article will give special attention to the Brazilian case.

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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.

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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.

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Predictability of the western North Pacific (WNP) summer climate associated with different El Niño–Southern Oscillation (ENSO) phases is investigated in this study based on the 1-month lead retrospective forecasts of five state-of-the-art coupled models from ENSEMBLES. During the period from 1960 to 2005, the models well capture the WNP summer climate anomalies during most of years in different ENSO phases except the La Niña decaying summers. In the El Niño developing, El Niño decaying and La Niña developing summers, the prediction skills are high for the WNP summer monsoon index (WNPMI), with the prediction correlation larger than 0.7. The high prediction skills of the lower-tropospheric circulation during these phases are found mainly over the tropical western Pacific Ocean, South China Sea and subtropical WNP. These good predictions correspond well to their close teleconnection with ENSO and the high prediction skills of tropical SSTs. By contrast, for the La Niña decaying summers, the prediction skills are considerably low with the prediction correlation for the WNPMI near to zero and low prediction skills around the Philippines and subtropical WNP. These poor predictions relate to the weak summer anomalies of the WNPMI during the La Niña decaying years and no significant connections between the WNP lower-tropospheric circulation anomalies and the SSTs over the tropical central and eastern Pacific Ocean in observations. However, the models tend to predict an apparent anomalous cyclone over the WNP during the La Niña decaying years, indicating a linearity of the circulation response over WNP in the models prediction in comparison with that during the El Niño decaying years which differs from observations. In addition, the models show considerable capability in describing the WNP summer anomalies during the ENSO neutral summers. These anomalies are related to the positive feedback between the WNP lower-tropospheric circulation and the local SSTs. The models can capture this positive feedback but with some uncertainties from different ensemble members during the ENSO neutral summers.

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Identifying predictability and the corresponding sources for the western North Pacific (WNP) summer climate in the case of non-stationary teleconnections during recent decades benefits for further improvements of long-range prediction on the WNP and East Asian summers. In the past few decades, pronounced increases on the summer sea surface temperature (SST) and associated interannual variability are observed over the tropical Indian Ocean and eastern Pacific around the late 1970s and over the Maritime Continent and western–central Pacific around the early 1990s. These increases are associated with significant enhancements of the interannual variability for the lower-tropospheric wind over the WNP. In this study, we further assess interdecadal changes on the seasonal prediction of the WNP summer anomalies, using May-start retrospective forecasts from the ENSEMBLES multi-model project in the period 1960–2005. It is found that prediction of the WNP summer anomalies exhibits an interdecadal shift with higher prediction skills since the late 1970s, particularly after the early 1990s. Improvements of the prediction skills for SSTs after the late 1970s are mainly found around tropical Indian Ocean and the WNP. The better prediction of the WNP after the late 1970s may arise mainly from the improvement of the SST prediction around the tropical eastern Indian Ocean. The close teleconnections between the tropical eastern Indian Ocean and WNP summer variability work both in the model predictions and observations. After the early 1990s, on the other hand, the improvements are detected mainly around the South China Sea and Philippines for the lower-tropospheric zonal wind and precipitation anomalies, associating with a better description of the SST anomalies around the Maritime Continent. A dipole SST pattern over the Maritime Continent and the central equatorial Pacific Ocean is closely related to the WNP summer anomalies after the early 1990s. This teleconnection mode is quite predictable, which is realistically reproduced by the models, presenting more predictable signals to the WNP summer climate after the early 1990s.