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Effects of Light and Temperature Factors on Biomass Accumulation of Winter Wheat
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作者 pengli ma Yihao ma +2 位作者 Jinyong Pu Chunyu Zhao Weitai Wang 《Meteorological and Environmental Research》 CAS 2013年第8期41-46,共6页
[Objective] The study aimed to discuss the influence of light and temperature factors on biomass accumulation of winter wheat at each growth stage and changes in biomass of each organ. [Method] Based on the observatio... [Objective] The study aimed to discuss the influence of light and temperature factors on biomass accumulation of winter wheat at each growth stage and changes in biomass of each organ. [Method] Based on the observation data from Xifeng Agrometeorological Experiment Station of Gansu Province, including phenophase and yield factors of winter wheat in 1981 -2008, biomass at three-leaves, overwintering, jointing, heading, milky maturity, and maturity stages in 1995 -2008, and meteorological data in 1995 -2008, the variation patterns of the biomass accumulation and the influence of TEP (thermal effectiveness photosynthetically active radiation) on the biomass of winter wheat at every growth stage were ana- lyzed. [Result] The biomass accumulation of winter wheat in the whole growth period presented "S" curve, with the maximum value from heading to milky maturity stage. Since 1981, TEP from heading to milky maturity stage increased with a rate of 3. 314 MJ/(m2 · a), and the changing curves of TEP at other stages were like parable curves. TEP from turning green to jointing stage and from milky maturity to maturity stage had a higher value in the 1990s and a lower val.ue in the 1980s and early 21st century, while that from jointing to heading stage had a lower value in the 1990s but a higher value in the 1980s and early 21st century. There was a significant correlation between TEP at each growth stage and the actual yield. LAI (leaf area index) at each development stage also had a significant correlation with the utilization rate of TEP at corresponding stage. When LAI at jointing and heading stages increased by I, the utilization rate of TEP correspondingly increased by 0. 049 and 0.259 g/MJ respectively. [ Conclusion] The research could provide theoretical references for the scientific planting and management of winter wheat in future. Key words Light and temperature factors; Winter wheat; Biomass; Influence; China 展开更多
关键词 Light and temperature factors Winter wheat BIOMASS INFLUENCE China
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2022年长江流域重大干旱发展过程中西太平洋副热带高压的多维度异常特征
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作者 段欣妤 张强 +4 位作者 张良 马鹏里 方锋 杨金虎 朱飙 《科学通报》 EI CAS CSCD 北大核心 2024年第15期2081-2092,共12页
2022年长江流域发生了罕见的夏秋冬连旱.此次干旱是伏秋季降水异常偏少和气温异常偏高叠加形成的复合型干旱,与冬季干旱连在一起的超长事件;其中8月全流域的高温干旱异常特征最为显著.以往关于西太平洋副热带高压(简称西太副高)的异常... 2022年长江流域发生了罕见的夏秋冬连旱.此次干旱是伏秋季降水异常偏少和气温异常偏高叠加形成的复合型干旱,与冬季干旱连在一起的超长事件;其中8月全流域的高温干旱异常特征最为显著.以往关于西太平洋副热带高压(简称西太副高)的异常变化对长江流域高温热浪和干旱的影响的相关研究主要侧重于纬向异常这种单一维度的异常,而较少关注其经向、厚度、面积、持续时间的多个维度异常;且单一维度的异常不足以刻画其作为主控环流因子对极端高温干旱事件的影响.为了揭示西太副高的多维度异常特征对此次长江流域重大干旱的影响,本文重点分析了干旱发展过程中西太副高的多个维度异常特征.结果表明,在整个干旱发展过程中,8月西太副高在500 hPa上纬向偏西异常最为显著,无明显的经向异常.覆盖长江流域的面积为历年同期最大.在垂直方向上自低层往高层不断西伸;400~200 h Pa上西太副高与南亚高压位置相互联通,以高压坝的形式覆盖长江流域,西太副高的厚度异常深厚.通过与历史同期8月不同程度干旱年份进行对比分析,结果发现,只有当西太副高的空间异常持续维持,才能造成流域严重的高温干旱. 展开更多
关键词 2022年 长江流域 重大干旱 西太平洋副热带高压 多维度异常特征
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Climatic Warming and Humidification in the Arid Region of Northwest China: Multi-Scale Characteristics and Impacts on Ecological Vegetation 被引量:33
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作者 Qiang ZHANG Jinhu YANG +5 位作者 Wei WANG pengli ma Guoyang LU Xiaoyun LIU Haipeng YU Feng FANG 《Journal of Meteorological Research》 SCIE CSCD 2021年第1期113-127,共15页
The climatic warming and humidification observed in the arid region of Northwest China(ARNC) and their impacts on the ecological environment have become an issue of concern. The associated multi-scale characteristics ... The climatic warming and humidification observed in the arid region of Northwest China(ARNC) and their impacts on the ecological environment have become an issue of concern. The associated multi-scale characteristics and environmental responses are currently poorly understood. Using data from satellite remote sensing, field observations, and the Coupled Model Intercomparison Project phase 6, this paper systematically analyzes the process and scale characteristics of the climatic warming and humidification in the ARNC and their impacts on ecological vegetation. The results show that not only have temperature and precipitation increased significantly in the ARNC over the past 60 years, but the increasing trend of precipitation is also obviously intensifying. The dryness index, which comprehensively considers the effects of precipitation and temperature, has clearly decreased, and the trend in humidification has increased. Spatially, the trend of temperature increase has occurred over the entire region, while 93.4% of the region has experienced an increase in precipitation, suggesting a spatially consistent climatic warming and humidification throughout the ARNC. Long-term trends and interannual changes in temperature and precipitation dominate the changes in climatic warming and humidification. Compared to interannual variations in temperature, the trend change of temperature contributes more to the overall temperature change. However, the contribution of interannual variations in precipitation is greater than that of the precipitation trend to the overall precipitation change. The current climatic warming and humidification generally promote the growth of ecological vegetation. Since the 1980 s,82.4% of the regional vegetation has thrived. The vegetation index has a significant positive correlation with precipitation and temperature. However, it responds more significantly to interannual precipitation variation, although the vegetation response varies significantly under different types of land use. The warming and humidification of the climate in the ARNC are probably related to intensifications of the westerly wind circulation and ascending air motions.They are expected to continue in the future, although the strength of the changes will probably be insufficient to significantly change the basic climate pattern in the ARNC. The results of this study provide helpful information for decision making related to China's "Belt and Road" development strategies. 展开更多
关键词 arid region of Northwest China(ARNC) climatic warming and humidification ecological vegetation MULTI-SCALE synergistic effect
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西北地区气候湿化趋势的新特征 被引量:54
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作者 张强 朱飙 +7 位作者 杨金虎 马鹏里 刘晓云 卢国阳 王有恒 于海鹏 刘卫平 王大为 《科学通报》 EI CAS CSCD 北大核心 2021年第28期3757-3771,共15页
21世纪初有研究提出西北气候暖湿化,但由于当时变湿时段短、变幅小,对此观点有不少存疑,并且对暖湿化的趋势发展、持续时间及影响程度等问题缺乏明确结论.本研究通过构建变湿综合指数,利用多元数据,系统分析了西北暖湿化的时空特征.研... 21世纪初有研究提出西北气候暖湿化,但由于当时变湿时段短、变幅小,对此观点有不少存疑,并且对暖湿化的趋势发展、持续时间及影响程度等问题缺乏明确结论.本研究通过构建变湿综合指数,利用多元数据,系统分析了西北暖湿化的时空特征.研究表明,在百年尺度上,西北西部和东部温度均经历了20世纪40年代和60年代至今的两个增暖期,且当前的暖期更强;西部与东部的降水在很多时期呈跷跷板变化,但21世纪开始西部与东部同时进入增湿期.1961年以来西北西部基本为一致变湿趋势,1987年以来更为显著;而东部在1961~1997年呈干化趋势,1997年也转为湿化趋势.西部的温度、降水和干燥度变化一致性较好,大多时段以冷干和暖湿为主;而东部变化的一致性较差,21世纪之前很少出现暖湿时段,直至21世纪暖湿配置才较为频繁.西北地区温度呈现空间一致的增加特征,且变暖程度逐渐增强;降水则呈西增东减的空间变化,但西增东减的分界线近3个气候态时段以来持续东扩.西北地区降水、干燥度和变湿综合指数均表现为非线性增强,变湿的增强、东扩征兆显著,21世纪以来尤为突出.不过,当前气候暖湿化并没有改变基本的气候形态,但如果未来气候趋势持续当前的增强特征,对基本气候形态的改变并非没有可能.气候变湿的增强、东扩特征可能是21世纪以来西风环流和东亚夏季风环流协同增强作用的结果. 展开更多
关键词 西北地区 暖湿化趋势 变湿综合指数 增强与东扩
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