The primary aim of this paper is to elucidae economic and spatial impacts of the Sino-Pan-Pacific economic relationships on China. Specffically, it explores the following questions: what is the historical Process of e...The primary aim of this paper is to elucidae economic and spatial impacts of the Sino-Pan-Pacific economic relationships on China. Specffically, it explores the following questions: what is the historical Process of economic cooperation between the two economies? What is the Position of inter-trade between China and Pan-Pacific countries in China's total international trade? What is the position of Pan-pacific countrys' direct investment in China? And what is the potential subsequent meaning of favorable location choice of sevral major investment countries in China?展开更多
The three-dimensional structure of precipitation on a seasonal scale in the Asian-Pacific's three monsoon regions is investigated based on the tropical rainfall measurement mission (TRMM) data. The results show tha...The three-dimensional structure of precipitation on a seasonal scale in the Asian-Pacific's three monsoon regions is investigated based on the tropical rainfall measurement mission (TRMM) data. The results show that: (1) The maximum seasonal variation of the relative proportional difference of convective precipitation and stratiform rain occurs in the East Asian monsoon region, the second occurs in the Indian monsoon region, and the minimum is in the northwest Pacific monsoon region. In both the northwest Pacific mon soon region and the Indian monsoon region, the convective rain is proportionately larger than stratiform rain in all four seasons. (2) Cloud ice reaches its maximum at around 9 km. Cloud water's maximum range is between 3 and 4 km. The large value area of precipitation ice is mainly between 4 and 9 km. The precipi tation water particle is concentrated mostly below 4 km. The largest content is from the ground to 2 km. (3) The most remarkable variance of the content of cloud ice in the Indian monsoon region occurs from spring to winter, and the content of cloud water in the northwest Pacific is always higher than that in the other two regions. (4) The latent heat profile has a similar double-peak structure. The first peak is at 4 km and the second peak is at 2 km. In autumn and winter, the latent heat is higher in the northwest Pacific than in other two regions. In all three regions, the release of the latent heat is higher in summer and autumn than in spring and winter.展开更多
TheThe Regional Conference on Asian Pacific Countries of the IGU was held from August 13 to 19,1990 at Beijing,on the premises of Peking University.It was the first of such event of the Union to take place in China.Th...TheThe Regional Conference on Asian Pacific Countries of the IGU was held from August 13 to 19,1990 at Beijing,on the premises of Peking University.It was the first of such event of the Union to take place in China.The Conference was attended by 1017 geographers from 40 countries of six continents(Asia 788,Europe 125,North America 74,Oceania 15,Latin America 7,Africa 3),with the larger delegations from:U.S.A.(45),South Korea(44),Japan(31),France(18),Italy(17),FRG(16),Canada(16),U.S.S.R.(13),Australia(10),Spain(9),U.K.(8)and India(8).China composed the majority,and Taipei sent a sizable delegation of 15,the rest of the participating countries sent 1-4 delegates each.The organizing committee of the Conference included the executive committee members of the Geographical Society of China and members of China Committee for the IGU.Profs.Huang Bingwei and Wu Chuanjun were responsible for all the activities organized during the Conference.展开更多
The Coupled Model Intercomparison Project (CMIP) is an international community-based infrastructure that supports climate model intercomparison, climate variability, climate prediction, and climate projection. Impro...The Coupled Model Intercomparison Project (CMIP) is an international community-based infrastructure that supports climate model intercomparison, climate variability, climate prediction, and climate projection. Improving the performance of climate models over East Asia and the western North Pacific has been a challenge for the climate-modeling community. In this paper, we provide a synthesis robustness analysis of the climate models participating in CMIP-Phase 5 (CMIP5). The strengths and weaknesses of the CMIP5 models are assessed from the perspective of climate mean state, interannual variability, past climate change during the mid-Pliocene (MP) and the last millennium, and climate projection. The added values of regional climate models relative to the driving global climate models are also assessed. Although an encouraging increase in credibility and an improvement in the simulation of mean states, interannual variability, and past climate changes are visible in the progression from CMIP3 to CMIPS, some previously noticed biases such as the ridge position of the western North Pacific subtropical high and the associated rainfall bias are still evident in CMIP5 models. Weaknesses are also evident in simulations of the interannual amplitude, such as El Nino- Southern Oscillation (ENSO)-monsoon relationships. Coupled models generally show better results than standalone atmospheric models in simulating both mean states and interannual variability. Multi-model intercomparison indicates significant uncertainties in the future projection of climate change, although precipitation increases consistently across models constrained by the Clausius-Clapeyron relation. Regional ocean-atmosphere coupled models are recommended for the dynamical downscaling of climate change oroiections over the East Asia-western North Pacific domain.展开更多
The Shanghai Cooperation Organization(SCO)has withstood storms to create a cooperative platform in Central Asia that conforms to the trend of the times,meets regional needs,and serves its member states’interests.SCO...The Shanghai Cooperation Organization(SCO)has withstood storms to create a cooperative platform in Central Asia that conforms to the trend of the times,meets regional needs,and serves its member states’interests.SCO’s commitment to innovative thinking,security cooperation and regional coordination has contributed to regional stability and development and to gaining experience for establishing regional and global order.China-Russia cooperation,efforts by the“Shanghai Five,”relations among member states,and external pressure have been the main driving forces supporting a huge increase in trade in the past 20 years.For regional development and stability and a greater role in global governance,the SCO should continue taking the long-term perspective in planning and policy.展开更多
The interactions among the Asian-Pacific monsoon subsystems have significant impacts on the climatic regimes in the monsoon region and even the whole world. Based on the domestic and foreign related research, an analy...The interactions among the Asian-Pacific monsoon subsystems have significant impacts on the climatic regimes in the monsoon region and even the whole world. Based on the domestic and foreign related research, an analysis is made of four different teleconnection modes found in the Asian-Pacific monsoon region, which reveal clearly the interactions among the Indian summer monsoon (ISM), the East Asian summer monsoon (EASM), and the western North Pacific summer monsoon (WNPSM). The results show that: (1) In the period of the Asian monsoon onset, the date of ISM onset is two weeks earlier than the beginning of the Meiyu over the Yangtze River Basin, and a teleconnection mode is set up from the southwestern India via the Bay of Bengal (BOB) to the Yangtze River Basin and southern Japan, i.e., the "southern" teleconnection of the Asian summer monsoon. (2) In the Asian monsoon culmination period, the precipitation of the Yangtze River Basin is influenced significantly by the WNPSM through their teleconnection relationship, and is negatively related to the WNPSM rainfall, that is, when the WNPSM is weaker than normal, the precipitation of the Yangtze River Basin is more than normal. (3) In contrast to the rainfall over the Yangtze River Basin, the precipitation of northern China (from the 4th pentad of July to the 3rd pentad of August) is positively related to the WNPSM. When the WNPSM is stronger than normal, the position of the western Pacific subtropical high (WPSH) becomes farther northeast than normal, the anomalous northeastward water vapor transport along the southwestern flank of WPSH is converged over northern China, providing adequate moisture for more rainfalls than normal there. (4) The summer rainfall in northern China has also a positive correlation with the ISM. During the peak period of ISM, a teleconnection pattern is formed from Northwest India via the Tibetan Plateau to northern China, i.e., the "northern" teleconnection of the Asian summer monsoon. The above four kinds of teleconnections reflect the links among the Asian monsoon subsystems of ISM, EASM, and WNPSM during the northward advancing march of the Asian summer monsoons.展开更多
The current East Asian regional cooperation framework is a complex system with multiple fields,levels,and players.In terms of social network theory and analysis,the East Asian regional cooperation framework can be def...The current East Asian regional cooperation framework is a complex system with multiple fields,levels,and players.In terms of social network theory and analysis,the East Asian regional cooperation framework can be defined as an affiliation network of cooperative mechanisms and players.Combing through the process of East Asian regional cooperation and constructing an East Asian regional cooperation network on the basis of the affiliation network model shows that the network has distinct characteristics in terms of cooperation mechanisms,cooperation entities,inter-entity relations,and the interaction of various fields of cooperation.These characteristics are apparent in concentrated form in the dynamics and limitations of East Asian regional cooperation networks.Describing and analyzing the structure and characteristics of the regional cooperation network of the Association of Southeast Asian Nations(ASEAN)can help us conduct a comprehensive examination of the current regional cooperation framework,grasp the developmental prospects of East Asian regional cooperation,and provide reference material for China's path choice in the process of future regional cooperation.展开更多
The boreal summer intraseasonal oscillation(BSISO) is simulated by the Climate System Model(CSM) developed at the Chinese Academy of Meteorological Sciences(CAMS), China Meteorological Administration. Firstly, the res...The boreal summer intraseasonal oscillation(BSISO) is simulated by the Climate System Model(CSM) developed at the Chinese Academy of Meteorological Sciences(CAMS), China Meteorological Administration. Firstly, the results indicate that this new model is able to reasonably simulate the annual cycle and seasonal mean of the precipitation, as well as the vertical shear of large-scale zonal wind in the tropics. The model also reproduces the eastward and northward propagating oscillation signals similar to those found in observations. The simulation of BSISO is generally in agreement with the observations in terms of variance center, periodicity, and propagation, with the exception that the magnitude of BSISO anomalous convections are underestimated during both its eastward propagation along the equator and its northward propagation over the Asian–Pacific summer monsoon region. Our preliminary evaluation of the simulated BSISO by CAMS-CSM suggests that this new model has the capability, to a certain extent, to capture the BSISO features, including its propagation zonally along the equator and meridionally over the Asian monsoon region.展开更多
文摘The primary aim of this paper is to elucidae economic and spatial impacts of the Sino-Pan-Pacific economic relationships on China. Specffically, it explores the following questions: what is the historical Process of economic cooperation between the two economies? What is the Position of inter-trade between China and Pan-Pacific countries in China's total international trade? What is the position of Pan-pacific countrys' direct investment in China? And what is the potential subsequent meaning of favorable location choice of sevral major investment countries in China?
基金The National Natural Science Foundation of China under contract No.41275060the National Key Basic Research Program of China under contract No.2014CB953903+2 种基金the National Basic Research Program of China under contract No.2011CB403500the Fundamental Re-search Funds for the Central Universities of China under contract No.13lgjc03the National Natural Science Foundation of China under contract No.41275145
文摘The three-dimensional structure of precipitation on a seasonal scale in the Asian-Pacific's three monsoon regions is investigated based on the tropical rainfall measurement mission (TRMM) data. The results show that: (1) The maximum seasonal variation of the relative proportional difference of convective precipitation and stratiform rain occurs in the East Asian monsoon region, the second occurs in the Indian monsoon region, and the minimum is in the northwest Pacific monsoon region. In both the northwest Pacific mon soon region and the Indian monsoon region, the convective rain is proportionately larger than stratiform rain in all four seasons. (2) Cloud ice reaches its maximum at around 9 km. Cloud water's maximum range is between 3 and 4 km. The large value area of precipitation ice is mainly between 4 and 9 km. The precipi tation water particle is concentrated mostly below 4 km. The largest content is from the ground to 2 km. (3) The most remarkable variance of the content of cloud ice in the Indian monsoon region occurs from spring to winter, and the content of cloud water in the northwest Pacific is always higher than that in the other two regions. (4) The latent heat profile has a similar double-peak structure. The first peak is at 4 km and the second peak is at 2 km. In autumn and winter, the latent heat is higher in the northwest Pacific than in other two regions. In all three regions, the release of the latent heat is higher in summer and autumn than in spring and winter.
文摘TheThe Regional Conference on Asian Pacific Countries of the IGU was held from August 13 to 19,1990 at Beijing,on the premises of Peking University.It was the first of such event of the Union to take place in China.The Conference was attended by 1017 geographers from 40 countries of six continents(Asia 788,Europe 125,North America 74,Oceania 15,Latin America 7,Africa 3),with the larger delegations from:U.S.A.(45),South Korea(44),Japan(31),France(18),Italy(17),FRG(16),Canada(16),U.S.S.R.(13),Australia(10),Spain(9),U.K.(8)and India(8).China composed the majority,and Taipei sent a sizable delegation of 15,the rest of the participating countries sent 1-4 delegates each.The organizing committee of the Conference included the executive committee members of the Geographical Society of China and members of China Committee for the IGU.Profs.Huang Bingwei and Wu Chuanjun were responsible for all the activities organized during the Conference.
基金This work is jointly supported by the National Natural Science Foundation of China (41420104006 and 41330423), and by the R&D Special Fund for Public Welfare Industry (Meteorology) (GYHY201506012).
文摘The Coupled Model Intercomparison Project (CMIP) is an international community-based infrastructure that supports climate model intercomparison, climate variability, climate prediction, and climate projection. Improving the performance of climate models over East Asia and the western North Pacific has been a challenge for the climate-modeling community. In this paper, we provide a synthesis robustness analysis of the climate models participating in CMIP-Phase 5 (CMIP5). The strengths and weaknesses of the CMIP5 models are assessed from the perspective of climate mean state, interannual variability, past climate change during the mid-Pliocene (MP) and the last millennium, and climate projection. The added values of regional climate models relative to the driving global climate models are also assessed. Although an encouraging increase in credibility and an improvement in the simulation of mean states, interannual variability, and past climate changes are visible in the progression from CMIP3 to CMIPS, some previously noticed biases such as the ridge position of the western North Pacific subtropical high and the associated rainfall bias are still evident in CMIP5 models. Weaknesses are also evident in simulations of the interannual amplitude, such as El Nino- Southern Oscillation (ENSO)-monsoon relationships. Coupled models generally show better results than standalone atmospheric models in simulating both mean states and interannual variability. Multi-model intercomparison indicates significant uncertainties in the future projection of climate change, although precipitation increases consistently across models constrained by the Clausius-Clapeyron relation. Regional ocean-atmosphere coupled models are recommended for the dynamical downscaling of climate change oroiections over the East Asia-western North Pacific domain.
文摘The Shanghai Cooperation Organization(SCO)has withstood storms to create a cooperative platform in Central Asia that conforms to the trend of the times,meets regional needs,and serves its member states’interests.SCO’s commitment to innovative thinking,security cooperation and regional coordination has contributed to regional stability and development and to gaining experience for establishing regional and global order.China-Russia cooperation,efforts by the“Shanghai Five,”relations among member states,and external pressure have been the main driving forces supporting a huge increase in trade in the past 20 years.For regional development and stability and a greater role in global governance,the SCO should continue taking the long-term perspective in planning and policy.
基金Supported by the National Science and Technology Support Program (2007BAC03A01)the National Plan on Key Basic Research and Development (2006CB403604).
文摘The interactions among the Asian-Pacific monsoon subsystems have significant impacts on the climatic regimes in the monsoon region and even the whole world. Based on the domestic and foreign related research, an analysis is made of four different teleconnection modes found in the Asian-Pacific monsoon region, which reveal clearly the interactions among the Indian summer monsoon (ISM), the East Asian summer monsoon (EASM), and the western North Pacific summer monsoon (WNPSM). The results show that: (1) In the period of the Asian monsoon onset, the date of ISM onset is two weeks earlier than the beginning of the Meiyu over the Yangtze River Basin, and a teleconnection mode is set up from the southwestern India via the Bay of Bengal (BOB) to the Yangtze River Basin and southern Japan, i.e., the "southern" teleconnection of the Asian summer monsoon. (2) In the Asian monsoon culmination period, the precipitation of the Yangtze River Basin is influenced significantly by the WNPSM through their teleconnection relationship, and is negatively related to the WNPSM rainfall, that is, when the WNPSM is weaker than normal, the precipitation of the Yangtze River Basin is more than normal. (3) In contrast to the rainfall over the Yangtze River Basin, the precipitation of northern China (from the 4th pentad of July to the 3rd pentad of August) is positively related to the WNPSM. When the WNPSM is stronger than normal, the position of the western Pacific subtropical high (WPSH) becomes farther northeast than normal, the anomalous northeastward water vapor transport along the southwestern flank of WPSH is converged over northern China, providing adequate moisture for more rainfalls than normal there. (4) The summer rainfall in northern China has also a positive correlation with the ISM. During the peak period of ISM, a teleconnection pattern is formed from Northwest India via the Tibetan Plateau to northern China, i.e., the "northern" teleconnection of the Asian summer monsoon. The above four kinds of teleconnections reflect the links among the Asian monsoon subsystems of ISM, EASM, and WNPSM during the northward advancing march of the Asian summer monsoons.
文摘The current East Asian regional cooperation framework is a complex system with multiple fields,levels,and players.In terms of social network theory and analysis,the East Asian regional cooperation framework can be defined as an affiliation network of cooperative mechanisms and players.Combing through the process of East Asian regional cooperation and constructing an East Asian regional cooperation network on the basis of the affiliation network model shows that the network has distinct characteristics in terms of cooperation mechanisms,cooperation entities,inter-entity relations,and the interaction of various fields of cooperation.These characteristics are apparent in concentrated form in the dynamics and limitations of East Asian regional cooperation networks.Describing and analyzing the structure and characteristics of the regional cooperation network of the Association of Southeast Asian Nations(ASEAN)can help us conduct a comprehensive examination of the current regional cooperation framework,grasp the developmental prospects of East Asian regional cooperation,and provide reference material for China's path choice in the process of future regional cooperation.
基金Supported by the National Key Research and Development Program(2016YFA0601504)National Basic Research and Development(973)Program of China(2015CB453203)+1 种基金National Natural Science Foundation of China(41675068)Basic Research Funds of the Chinese Academy of Meteorological Sciences(2015Z002)
文摘The boreal summer intraseasonal oscillation(BSISO) is simulated by the Climate System Model(CSM) developed at the Chinese Academy of Meteorological Sciences(CAMS), China Meteorological Administration. Firstly, the results indicate that this new model is able to reasonably simulate the annual cycle and seasonal mean of the precipitation, as well as the vertical shear of large-scale zonal wind in the tropics. The model also reproduces the eastward and northward propagating oscillation signals similar to those found in observations. The simulation of BSISO is generally in agreement with the observations in terms of variance center, periodicity, and propagation, with the exception that the magnitude of BSISO anomalous convections are underestimated during both its eastward propagation along the equator and its northward propagation over the Asian–Pacific summer monsoon region. Our preliminary evaluation of the simulated BSISO by CAMS-CSM suggests that this new model has the capability, to a certain extent, to capture the BSISO features, including its propagation zonally along the equator and meridionally over the Asian monsoon region.