海风辐合线对雷暴系统触发、合并的动热力过程

利用加密自动气象站和雷达监测资料,结合VDRAS资料(其时间分辨率12 min、水平垂直分辨率分别是3和1 km左右),分别针对单纯海风辐合线触发和海风辐合线与已有雷暴系统合并的两个实例,揭示海风辐合线对雷暴系统影响的动力和热力过程。结果表明:(1)在环境系统风很弱时,天津沿海海风伸入内陆的移速约为15~18 km·h~(-1),且海风过后,气温降低、湿度加大。(2)海风辐合线配合地面高不稳定区,从而触发和加强了雷暴系统,对雷暴系统的预警时间可达2 h。(3)雷暴单体在海风辐合线附近产生,这与倾斜海风锋锋面(向海洋一侧倾斜)上的中尺度垂直环流相对应。(4)海风辐合线与雷暴系统合并后,雷暴系统强烈发展是由于海风辐合线附近积聚着水汽,同时也是辐合上升运动大值区的缘故。     

基于小波变换的薄层地震信号奇点的检测

通过小波变换的局部极大模可检测出奇点的位置,本文对反射地震信号小波变换进行了数值计算和聚焦处理,发现小波变换后奇点的位置仅受奇点实际位置及地震子波长度两因素制约,与子波形状无关．子波长度可以通过信号的小波变换本身求取,并进一步加以消除,从而实现了薄层地震信息的检测,得出薄层的地震分辨率可达1/32波长．实际资料处理表明,有效信号通过奇点分析可得到突出,剖面分辨率可得到提高．     

Mapping the resting cysts of dinoflagellate Alexandrium catenella along the coast of Qinhuangdao,China

Dinoflagellate Alexandrium catenella is a cosmopolitan bloom-forming species with complex life cycle, the formation and germination of resting cysts are critical for its bloom dynamics. In the coastal waters of Qinhuangdao, A. catenella has been identified as the major causative agent for paralytic shellfish poisoning, but there is little knowledge concerning its resting cysts in this region. In this study, three surveys were carried out along the coast of Qinhuangdao from 2020 to 2021 to map the distribution of A. catenella resting cysts, using a quantitative PCR (qPCR) assay specific for A. catenella. The resting cysts were detected in surface sediments during all the three surveys, and their distribution patterns were similar. High abundance of resting cysts (maximum 1 300 cysts/g sediment (wet weight)) were found in a region (119.62°E–119.99°E, 39.67°N–39.98°N) northeast to the coastal waters of Qinhuangdao, where surface sediments were mainly composed of clay and silt (percentage above 50%). Prior to the formation of the A. catenella bloom in March 2021, the abundance of A. catenella vegetative cells in seawater had extremely significant positive correlation with the abundance of resting cysts in surface sediments, reflecting the important role of resting cysts in the initiation of A. catenella blooms. As far as we know, this is the first report on the distribution of A. catenella cysts along the coast of Qinhuangdao. The results will offer a sound basis for the future monitoring and mitigation of toxic A. catenella blooms and paralytic shellfish poisoning events in this region.

     

Variations in nano- and pico-eukaryotic phytoplankton assemblages in the Qinhuangdao green-tide area

Journal of Oceanology and Limnology - Qinhuangdao coastal waters have been frequently hitting by nano- and pico-eukaryotic phytoplankton (NPEP) blooms and green tides (macroalgal blooms) in the...     

有无1墨水点亚对数空间限定交替式下推自动机之间的关系

该文引入 1墨水点 2方向交替式下推自动机 ,它是 1个具有额外能力的 2方向交替式下推自动机 ,能够用 1个墨水点在输入带上标记出最多 1个单元格。对具有 1个墨水点的和没有墨水点的亚对数空间限定交替式下推自动机之间的关系进行研究。实例证明了具有 1个墨水点的亚对数空间限定交替式下推自动机的语言受理能力强于没有墨水点的亚对数空间限定交替式下推自动机     

Will harmful dinoflagellate Karenia mikimotoi grow phagotrophically?

We studied the phagotrophic ability of dinoflagellate strain Karenia mikimotoi KM-Lü (isolated from the South China Sea), using fluorescent microspheres, bacteria isolated from the culture of K. mikimotoi and a marine microalgae Isochrysis galbana. We found that K. mikimotoi cultured under conditions of high light intensity could ingest fluorescent microspheres (diameters 0.5 and 2.0 μm) and fluorescence-labeled bacteria and microalgae. Under a low light intensity, however, only fluorescent microspheres (diameter 0.5 μm) and fluorescence-labeled microalgae were ingested. K. mikimotoi showed better growth by ingesting living marine bacteria or microalgae I. galbana than the controls, either in nutrient-depleted or nutrient-replete conditions. In nutrient-depleted conditions, the growth of K. mikimotoi was more significant with I. galbana as the prey item. In conclusion, the harmful dinoflagellate K. mikimotoi from the South China Sea has apparent phagotrophic ability, and some marine bacteria and microalgae may promote the growth of K. mikimotoi.     

TEXTUAL RESEARCH ON THE MAIN SOURCE OF THE CHANGJIANG RIVER

The Chinese people began to research the main source of the Changjiang (Yangtze) River 2,400 years ago. Limited by the scientific level, they did not discover it.The Tuotuo River was determined as the main source of the Changjiang River in the 1970s. However, this was not correct, because when comparing the length of the Tuotuo River with the Dam River, the glacier length at the headwaters was added to the Tuotuo River, resulting in that the Tuotuo River is 1 km longer than the Dam River, keeping in mind that the glacier can not be regarded as part of the river.In the summer of 1986, we investigated the source of the Changjiang River, we accurately measured the length of both the Tuotuo and Dam rivers, we discovered that the Dam River was 353.1 km long, and the Tuotuo River was 346.3 km long, the Dam River thus being 6.8 km longer than the Tuotuo River. The discharge of the Dam River is 196.18 m3/ sec., 2.6 times as large as that of the Tuotuo River, that of the Tuotuo River is 75.10 m3/sec. The drainag     

北京夏季不同等级降水过程与旱涝关系的分析

利用北京地区近百年的逐日降水资料,对北京夏季（６￣８月）不同等级降水过程的时间演变及其与夏季旱涝的关系进行了分析。提出北京夏季的旱涝与暴雨过程的关系最为密切,也就是说北京夏季暴雨过程的多少直接反映出夏季反映出夏季旱涝情况;并分析了偏旱和偏涝年代不同降水过程出现的频次。指出,年代偏旱或偏涝与降水过程次数的多少关系不大,而与降水强度即暴雨过程的多少和暴雨的强度有密切的关系。因此旱涝的短期气候预测必须与     

青藏高原年降水量的气候变化及其异常类型研究

利用青藏高原的80个气象台站近34a来年降水量资料，采用EOF、REOF、气候趋势线性趋势分析以及累积距平法等方法对青藏高原年降水量的时空分布特征及其异常进行了分析。结果表明：EOF分解的前三个主向量的累积方差贡献占总方差的44．9％，地形特别是高原主体的阻挡和抬升作用对年降水量的空间变化影响显著；年降水量的时间变化在缓慢减少的过程中于1982年和1995年发生了2次突变，并经历了减少、增多和再次减少的3个变化阶段；青藏高原年降水量的空间异常类型均可分为高原中东区、高原南部区、高原北部区、高原腹地区和西藏西南区共5个区，其分区主要受地形和低涡的影响较明显。