为了提高机载嵌入式系统软件开发效率,快速生成软件原型,同时提升机载嵌入式系统软件的可移植性,研究了基于Wind River Hypervisor的机载嵌入式系统虚拟化技术,对Wind River Hypervisor架构进行了剖析,阐述了hyperkernel的内部结构,指明...为了提高机载嵌入式系统软件开发效率,快速生成软件原型,同时提升机载嵌入式系统软件的可移植性,研究了基于Wind River Hypervisor的机载嵌入式系统虚拟化技术,对Wind River Hypervisor架构进行了剖析,阐述了hyperkernel的内部结构,指明了Wind River Hypervisor中不同类型线程在系统运行过程中所承担的角色以及运行特点,并基于Wind River Hypervisor实现了多种虚拟化架构,通过对不同架构的对比展示了每种架构的特征,同时借助workbench+vxworks653环境证实了在机载嵌入式系统部署Wind River Hypervisor架构的可行性。展开更多
Topographic map evidence from the Wyoming Wind River-Sweetwater River drainage divide area is used to test a recently proposed regional geomorphology paradigm defined by massive south- and southeast-oriented continent...Topographic map evidence from the Wyoming Wind River-Sweetwater River drainage divide area is used to test a recently proposed regional geomorphology paradigm defined by massive south- and southeast-oriented continental ice sheet melt water floods that flowed across the entire Missouri River drainage basin. The new paradigm forces recognition of an ice sheet created and occupied deep “hole” and is fundamentally different from the commonly accepted paradigm in which a pre-glacial north- and northeast-oriented slope would have prevented continental ice sheet melt water from reaching or crossing the Wind River-Sweetwater River drainage divide. Divide crossings (or low points) are identified as places where water once flowed across the drainage divide. Map evidence is interpreted first from the accepted paradigm perspective and second from the new paradigm perspective to determine the simplest explanation. Both paradigm perspectives suggest south-oriented water crossed the drainage divide, although accepted paradigm interpretations do not satisfactorily explain the large number of observed divide crossings and are complicated by the need to bury the Owl Creek and Bridger Mountains to explain why the Wind River now flows in a north direction through Wind River Canyon. New paradigm interpretations explain the large number of divide crossings as diverging and converging channel evidence (as in flood-formed anastomosing channel complexes), Owl Creek and Bridger Mountain uplift to have occurred as south-oriented floodwaters carved Wind River Canyon, and a major flood flow reversal (caused by ice sheet related crustal warping and the opening up of deep “hole” space by ice sheet melting) as being responsible for the Wind River abrupt turn to the north. While this test only addresses topographic map evidence, Occam’s Razor suggests the new paradigm offers what in science should be the preferred Wind River-Sweetwater River drainage divide origin interpretations.展开更多
The Wind River Indian Reservation undertook the development of an agricultural resource management plan in 2015. The reservation is 8903 sq.km of which 63% is in crop and grazing lands. This project’s aim was to crea...The Wind River Indian Reservation undertook the development of an agricultural resource management plan in 2015. The reservation is 8903 sq.km of which 63% is in crop and grazing lands. This project’s aim was to create a community-based integrated plan. A series of community meetings identified 83 issues and topics relating to agricultural development on the reservation. Using information from community meetings, the final agricultural resource management plan consists of 9 major elements, with 12 goals, 46 objectives and 88 policies. Three key issues are addressed in the plan: provide the reservation with a plan that leads to self-management of their agricultural resources;integrate the major agricultural elements as defined by the community into policies;and, create a governance structure that fosters agricultural development into the future.展开更多
This paper presents an analysis of the impact of wind on the transport of the Changjiang River Diluted Water (CRDW) in August by using the salinity data collected on two zonal sections near Cheju-do. Based on the clim...This paper presents an analysis of the impact of wind on the transport of the Changjiang River Diluted Water (CRDW) in August by using the salinity data collected on two zonal sections near Cheju-do. Based on the climatological mean conditions and four extreme events, the analysis indicates that wind-induced Ekman transport plays an important role in the extension of the CRDW. The strong northeastward Ekman transport induced by southeasterly wind in 1996, 2003, 2004, and 2006 pushes the core of the CRDW to the sea adjacent to Cheju-do. A comparison of the wind variation before observation among these four extreme events indicates that the expansion pattern of the CRDW is primarily changed by synoptic variation with timescales of days to weeks, such as during a typhoon. The weak eastward extension of the CRDW in 2004, accompanied with a relatively strong southerly wind, implies that the oceanographic state (e.g., the depth of halocline) may strongly affect the impact of wind on the extension of the CRDW.展开更多
Data taken in the two large-scale ocean investigations in China in winter 1959 and 1982 are used to analyze the residual current off the Changjiang (Yangtze) River mouth in this paper. The current in wintertime off th...Data taken in the two large-scale ocean investigations in China in winter 1959 and 1982 are used to analyze the residual current off the Changjiang (Yangtze) River mouth in this paper. The current in wintertime off the river mouth consist of the Changjiang runoff, wind-driven current, coastal current, density-driven current and Taiwan Warm Current (TWC). The TWC occurs in wintertime off the mouth. The surface TWC reaches only to the east side of Dinghai, then tums southeastward. The bottom TWC can flow to the area off the Changjiang mouth along west slop of the submerged river valley (SRV) and to the area off the Subei coast. The simulated currents by 3D model are basically consistent with the observed currents, although the model was run with climatological forces and the observations was done in episodic time manner.展开更多
文摘为了提高机载嵌入式系统软件开发效率,快速生成软件原型,同时提升机载嵌入式系统软件的可移植性,研究了基于Wind River Hypervisor的机载嵌入式系统虚拟化技术,对Wind River Hypervisor架构进行了剖析,阐述了hyperkernel的内部结构,指明了Wind River Hypervisor中不同类型线程在系统运行过程中所承担的角色以及运行特点,并基于Wind River Hypervisor实现了多种虚拟化架构,通过对不同架构的对比展示了每种架构的特征,同时借助workbench+vxworks653环境证实了在机载嵌入式系统部署Wind River Hypervisor架构的可行性。
文摘Topographic map evidence from the Wyoming Wind River-Sweetwater River drainage divide area is used to test a recently proposed regional geomorphology paradigm defined by massive south- and southeast-oriented continental ice sheet melt water floods that flowed across the entire Missouri River drainage basin. The new paradigm forces recognition of an ice sheet created and occupied deep “hole” and is fundamentally different from the commonly accepted paradigm in which a pre-glacial north- and northeast-oriented slope would have prevented continental ice sheet melt water from reaching or crossing the Wind River-Sweetwater River drainage divide. Divide crossings (or low points) are identified as places where water once flowed across the drainage divide. Map evidence is interpreted first from the accepted paradigm perspective and second from the new paradigm perspective to determine the simplest explanation. Both paradigm perspectives suggest south-oriented water crossed the drainage divide, although accepted paradigm interpretations do not satisfactorily explain the large number of observed divide crossings and are complicated by the need to bury the Owl Creek and Bridger Mountains to explain why the Wind River now flows in a north direction through Wind River Canyon. New paradigm interpretations explain the large number of divide crossings as diverging and converging channel evidence (as in flood-formed anastomosing channel complexes), Owl Creek and Bridger Mountain uplift to have occurred as south-oriented floodwaters carved Wind River Canyon, and a major flood flow reversal (caused by ice sheet related crustal warping and the opening up of deep “hole” space by ice sheet melting) as being responsible for the Wind River abrupt turn to the north. While this test only addresses topographic map evidence, Occam’s Razor suggests the new paradigm offers what in science should be the preferred Wind River-Sweetwater River drainage divide origin interpretations.
文摘The Wind River Indian Reservation undertook the development of an agricultural resource management plan in 2015. The reservation is 8903 sq.km of which 63% is in crop and grazing lands. This project’s aim was to create a community-based integrated plan. A series of community meetings identified 83 issues and topics relating to agricultural development on the reservation. Using information from community meetings, the final agricultural resource management plan consists of 9 major elements, with 12 goals, 46 objectives and 88 policies. Three key issues are addressed in the plan: provide the reservation with a plan that leads to self-management of their agricultural resources;integrate the major agricultural elements as defined by the community into policies;and, create a governance structure that fosters agricultural development into the future.
基金supported by the National Natural Science Foundation of China (40906014 and 40976015)the Marine Science Foundation of State Oceanic Administration of China for the Youth (2010218)
文摘This paper presents an analysis of the impact of wind on the transport of the Changjiang River Diluted Water (CRDW) in August by using the salinity data collected on two zonal sections near Cheju-do. Based on the climatological mean conditions and four extreme events, the analysis indicates that wind-induced Ekman transport plays an important role in the extension of the CRDW. The strong northeastward Ekman transport induced by southeasterly wind in 1996, 2003, 2004, and 2006 pushes the core of the CRDW to the sea adjacent to Cheju-do. A comparison of the wind variation before observation among these four extreme events indicates that the expansion pattern of the CRDW is primarily changed by synoptic variation with timescales of days to weeks, such as during a typhoon. The weak eastward extension of the CRDW in 2004, accompanied with a relatively strong southerly wind, implies that the oceanographic state (e.g., the depth of halocline) may strongly affect the impact of wind on the extension of the CRDW.
文摘Data taken in the two large-scale ocean investigations in China in winter 1959 and 1982 are used to analyze the residual current off the Changjiang (Yangtze) River mouth in this paper. The current in wintertime off the river mouth consist of the Changjiang runoff, wind-driven current, coastal current, density-driven current and Taiwan Warm Current (TWC). The TWC occurs in wintertime off the mouth. The surface TWC reaches only to the east side of Dinghai, then tums southeastward. The bottom TWC can flow to the area off the Changjiang mouth along west slop of the submerged river valley (SRV) and to the area off the Subei coast. The simulated currents by 3D model are basically consistent with the observed currents, although the model was run with climatological forces and the observations was done in episodic time manner.
