[ Objective ] To study economic growth of grassland animal husbandry in Sichuan Tibetan region after the liberation and predict long-term trend and regular features of growth and development of grassland animal husban...[ Objective ] To study economic growth of grassland animal husbandry in Sichuan Tibetan region after the liberation and predict long-term trend and regular features of growth and development of grassland animal husbandry. [ Method] Using econometric models and methods, the gov- ernment statistical data after the liberation on grassland animal husbandry of Sichuan Tibetan region were analyzed, and the factors increasing econ- omy of grassland animal husbandry were determined by analyzing time series data of different periods. [ Result] The grassland animal husbandry of Sichuan Tibetan region had significant characteristics of traditional pastoral economy. Before the reform and opening-up, the increase of animal hus- bandry economy was mainly manifested by increase in amount of livestock and laborers, and the increase in amount of livestock was principal pro- moting factor. After the reform and opening-up, the increase in integrated production factors became the primary cause to push the increase of ani- mal husbandry economy. [ Conclusion] Some new measures must be taken to promote the increase of animal husbandry economy of Sichuan Tibetan region, including transforming traditional production mode of animal husbandry, relying on scientific and technological advances, further improving socio- economic system, cultivating more highly sldlled workforce and effectively guiding rational shift and orderly migration of surplus pasture laborers.展开更多
本文利用约束变分客观分析法构建的物理协调大气变分客观分析模型,通过融合地面、探空、卫星等多源观测资料和ERA-Interim再分析资料,建立了青藏高原那曲试验区5年(2013~2017年)长时间序列的热力、动力相协调的大气分析数据集,并以此分...本文利用约束变分客观分析法构建的物理协调大气变分客观分析模型,通过融合地面、探空、卫星等多源观测资料和ERA-Interim再分析资料,建立了青藏高原那曲试验区5年(2013~2017年)长时间序列的热力、动力相协调的大气分析数据集,并以此分析那曲试验区大气的基本环境特征与云—降水演变和大气动力、热力的垂直结构。分析表明:(1)试验区350 h Pa以上风速的季节变化非常明显,风速在冬季11月至次年2月达到最大(>50 m s),盛夏7~8月风速的垂直变化最弱,温度的垂直变化最强,大气高湿区在夏秋雨季位于350~550 h Pa,在冬春干季升至300~400 h Pa。(2)试验区6~7月上旬降水最多;春、秋、冬三季,300~400 h Pa高度层作为大气上升运动和下沉运动的交界处,是云量的集中区;夏季,增多的水汽和增强的大气上升运动导致高云和总云量明显增多,中、低云减少。(3)夏季的地表潜热通量与大气总的潜热释放最强,大气净辐射冷却最弱,高原地区较强的地面感热导致试验区500 h Pa以下的近地面全年存在暖平流,500 h Pa以上则由于强烈的西风和辐射冷却存在冷平流。此外,试验区整层大气全年以干平流为主,但在夏季出现了较弱的湿平流。(4)视热源Q具有明显的垂直分层特征:全年500 h Pa以下大气表现为冷源,300~500 h Pa和100~150 h Pa表现为热源,150~300 h Pa则在冬春干季表现为冷源,在夏秋雨季表现为热源,不同高度层的冷、热源的形成原因不同,其中夏季由于增强的上升运动、感热垂直输送和水汽凝结潜热以及高云的形成,因此几乎整层大气表现为热源。展开更多
基金funded by the Soft Science Project of Sichuan Province ( 2010ZR0033)
文摘[ Objective ] To study economic growth of grassland animal husbandry in Sichuan Tibetan region after the liberation and predict long-term trend and regular features of growth and development of grassland animal husbandry. [ Method] Using econometric models and methods, the gov- ernment statistical data after the liberation on grassland animal husbandry of Sichuan Tibetan region were analyzed, and the factors increasing econ- omy of grassland animal husbandry were determined by analyzing time series data of different periods. [ Result] The grassland animal husbandry of Sichuan Tibetan region had significant characteristics of traditional pastoral economy. Before the reform and opening-up, the increase of animal hus- bandry economy was mainly manifested by increase in amount of livestock and laborers, and the increase in amount of livestock was principal pro- moting factor. After the reform and opening-up, the increase in integrated production factors became the primary cause to push the increase of ani- mal husbandry economy. [ Conclusion] Some new measures must be taken to promote the increase of animal husbandry economy of Sichuan Tibetan region, including transforming traditional production mode of animal husbandry, relying on scientific and technological advances, further improving socio- economic system, cultivating more highly sldlled workforce and effectively guiding rational shift and orderly migration of surplus pasture laborers.
文摘本文利用约束变分客观分析法构建的物理协调大气变分客观分析模型,通过融合地面、探空、卫星等多源观测资料和ERA-Interim再分析资料,建立了青藏高原那曲试验区5年(2013~2017年)长时间序列的热力、动力相协调的大气分析数据集,并以此分析那曲试验区大气的基本环境特征与云—降水演变和大气动力、热力的垂直结构。分析表明:(1)试验区350 h Pa以上风速的季节变化非常明显,风速在冬季11月至次年2月达到最大(>50 m s),盛夏7~8月风速的垂直变化最弱,温度的垂直变化最强,大气高湿区在夏秋雨季位于350~550 h Pa,在冬春干季升至300~400 h Pa。(2)试验区6~7月上旬降水最多;春、秋、冬三季,300~400 h Pa高度层作为大气上升运动和下沉运动的交界处,是云量的集中区;夏季,增多的水汽和增强的大气上升运动导致高云和总云量明显增多,中、低云减少。(3)夏季的地表潜热通量与大气总的潜热释放最强,大气净辐射冷却最弱,高原地区较强的地面感热导致试验区500 h Pa以下的近地面全年存在暖平流,500 h Pa以上则由于强烈的西风和辐射冷却存在冷平流。此外,试验区整层大气全年以干平流为主,但在夏季出现了较弱的湿平流。(4)视热源Q具有明显的垂直分层特征:全年500 h Pa以下大气表现为冷源,300~500 h Pa和100~150 h Pa表现为热源,150~300 h Pa则在冬春干季表现为冷源,在夏秋雨季表现为热源,不同高度层的冷、热源的形成原因不同,其中夏季由于增强的上升运动、感热垂直输送和水汽凝结潜热以及高云的形成,因此几乎整层大气表现为热源。
