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141.
南海东北部是寡营养海域,夏季浮游植物叶绿素浓度较低,热带气旋“风泵”效应带来的上层海洋扰动可能引起表层浮游植物的显著增长。以往的研究通常关注热带气旋风应力和海洋中尺度涡对上层海洋浮游植物的影响,本文利用航次CTD、实测叶绿素a浓度、Argo温盐剖面和遥感数据,探讨了台风“风泵”和黑潮共同作用下真光层内浮游植物的变化特征及其成因。结果表明,2015年台风“莲花”过境1周后产生向吕宋海峡西北侧南海海域(A区)入侵的黑潮流套,该入侵的黑潮流套使台风前原有的气旋涡消失,抑制了台风产生的上升流对表层(0~40 m)营养盐供给,使次表层(60~90 m)营养盐富集,进而抑制了表层的叶绿素a增长,促进了次表层叶绿素a的增长;吕宋海峡西侧南海海域(B区)表层的浮游植物叶绿素a浓度增加不仅是源于叶绿素最大层浮游植物的向上输运,更是由于浮游植物的繁殖增长;A区台风引起的流套式的黑潮入侵,促进了B区台风后气旋式流场的形成,产生的持续增强的气旋涡为B区表层叶绿素持续增长提供了充足的营养盐供给。 相似文献
142.
城镇发展适宜性研究有助于了解城镇发展的优势条件,为确定城镇建设规划的扩展方向提供依据。在北极与亚北极开展研究对中国开展在城镇化、重大基础设施、廊道建设方面的国际合作有重大意义。本文使用多源数据,在采样的基础上利用逐步法的思想进行变量筛选,共筛选出5个显著指标,用logistic方法拟合出最终的模型进行城镇发展适宜性评价,最终得到研究区城镇发展适宜性分级图。研究结果表明:筛选后的显著指标对研究区城镇分布的影响作用大小排序为,温度(正向)、交通网密度(正向)、海拔高度(反向)、人口密度(正向)、距港口距离(反向);温度、交通网密度、海拔高度、人口密度、距最近港口距离增加1个单位,城镇发展的几率分别比原来增加了38.4%、16.7%、9%、0.4%、0.1%;研究区的Ⅰ(不适宜)、Ⅱ(中度适宜)、Ⅲ(高度适宜)的城镇发展适宜性均值分别为0.03、0.16、0.68(分别约占研究区总面积的76.82%、21.82%、1.37%);城镇发展适宜性总体呈现出随纬度升高而降低、随经度升高而增加的趋势,适宜城镇发展的气候地理条件是温带大陆性湿润气候带和温带海洋性气候带以及平原与低地地区;研究区的城镇发展适宜性俄罗斯西北部为0.08、瑞典为0.07、芬兰为0.06、挪威为0.03。俄罗斯西北部城镇发展适宜性整体上呈现出北低南高,南部呈现两边高中间低的空间布局;瑞典呈现出西北低东南高,沿海大于内陆的空间布局;芬兰呈现出北(高原)低南(沿海)高,中部次高的空间布局;挪威呈现出南部沿海高,西部沿海次高,其他区域低的空间布局。 相似文献
143.
Landform‐oriented flow‐routing algorithm for the dual‐structure loess terrain based on digital elevation models 下载免费PDF全文
The loess landform in the Loess Plateau of China is with typical dual structure, namely, the upper smooth positive terrain and the lower cliffy negative terrain (P–N terrain for short). Obvious differences in their morphological feature, geomorphological mechanism, and hydrological process could be found in the both areas. Based on the differences, a flow‐routing algorithm that separately addresses the dual‐structure terrain would be necessary to encompass this spatial variation in their hydrological behaviour. This paper proposes a mixed flow‐routing algorithm to address aforementioned problems. First, the loess landform surface is divided into P–N terrains based on digital elevation models. Then, specific catchment area is calculated with the new algorithm to simulate the water flows in both positive and negative terrain areas. The mixed algorithm consists of the multiple flow‐routing algorithm (multiple‐flow direction) for positive areas and the D8 algorithm for negative areas, respectively. The approach is validated in two typical geomorphologic areas with low hills and dense gullies in the northern Shaanxi Loess Plateau. Four indices are used to examine the results, which show that the new algorithm is more suitable for loess terrain in simulating the spatial distribution of water accumulation, as well as in modeling the flow characteristics of the true surface by considering the morphological structures of the terrain. Copyright © 2013 John Wiley & Sons, Ltd. 相似文献
144.
Due to the specific dynamics, the probes located at the halo orbits or Lissajous orbits around the Earth-Moon collinear libration point L1 or L2 are always studied in the synodic system to understand their trajectories. In fact, they are also orbiting the Earth in a distant Keplerian ellipse. Because of their intrinsic orbital instability, in the orbit prediction the initial errors propagate more prominently than those of the normal orbiting satellites, this requires special attention in the orbit design, maneuver, and control. Despite of all this, they are similar to the normal orbiting satellites in orbit determination and hardly require other special attentions. In this paper, the quantitative results of error propagation under the unstable dynamics, together with the theoretical analysis are presented. The results of precise orbit determination and short-arc orbit predictions are also shown, and compared with the results from the Beijing Aerospace Control Center. 相似文献
145.
146.
The community dynamics and potential carbon ?xation of intertidal macroalgae were investigated monthly from April 2014 to April 2015 in the northwest coast of Yellow Sea. Seasonal variations in biomass and carbon ?xation were presented and showed close relationship with community structure.The carbon ?xation rate ranged from 0.48±0.13 mg C/(g FW ·d) to 4.35±0.12 mg C/(g FW ·d). Sargassum thunbergii, Chondrus ocellatus and Ulva intestinalis were three most in?uential species which contributed27%, 21.9% and 18.5% variation of carbon ?xation rate, respectively. Standing carbon stocks ranged from7.52 g C/m~2 to 41.31 g C/m~2, and estimated carbon stocks varied from 11.77 g C/m 2 to 96.49 g C/m~2. The larger dif ference between estimated and standing carbon stocks implied that more ?xed carbon was exported from the community in summer and autumn than in winter. This study suggested that intertidal macroalgal community could provide a potential function in carbon ?xation of coastal ecosystem. 相似文献
147.
Tang Xinbao Zhang Qinghao Zhou Yan Ma Depeng 《Geotechnical and Geological Engineering》2021,39(8):5895-5906
Geotechnical and Geological Engineering - Soft and hard rock assemblages and anchor solids have important effects on rock mechanics properties under different inclinations and assemblages, so it is... 相似文献
148.
Variability in the vertical hyporheic water exchange affected by hydraulic conductivity and river morphology at a natural confluent meander bend 下载免费PDF全文
Jinxi Song Guotao Zhang Weize Wang Qi Liu Weiwei Jiang Weiqiang Guo Bin Tang Haifeng Bai Xinyi Dou 《水文研究》2017,31(19):3407-3420
River confluences and their associated tributaries are key morphodynamic nodes that play important roles in controlling hydraulic geometry and hyporheic water exchange in fluvial networks. However, the existing knowledge regarding hyporheic water exchange associated with river confluence morphology is relatively scarce. On January 14 and 15, 2016, the general hydraulic and morphological characteristics of the confluent meander bend (CMB) between the Juehe River and the Haohe River in the southern region of Xi'an City, Shaanxi Province, China, were investigated. The patterns and magnitudes of vertical hyporheic water exchange (VHWE) were estimated based on a one‐dimensional heat steady‐state model, whereas the sediment vertical hydraulic conductivity (Kv) was calculated via in situ permeameter tests. The results demonstrated that 6 hydrodynamic zones and their extensions were observed at the CMB during the test period. These zones were likely controlled by the obtuse junction angle and low momentum flux ratio, influencing the sediment grain size distribution of the CMB. The VHWE patterns at the test site during the test period mostly showed upwelling flow dominated by regional groundwater discharging into the river. The occurrence of longitudinal downwelling and upwelling patterns along the meander bend at the CMB was likely subjected to the comprehensive influences of the local sinuosity of the meander bend and regional groundwater discharge and finally formed regional and local flow paths. Additionally, in dominated upwelling areas, the change in VHWE magnitudes was nearly consistent with that in Kv values, and higher values of both variables generally occurred in erosional zones near the thalweg paths of the CMB, which were mostly made up of sand and gravel. This was potentially caused by the erosional and depositional processes subjected to confluence morphology. Furthermore, lower Kv values observed in downwelling areas at the CMB were attributed to sediment clogging caused by local downwelling flow. The confluence morphology and sediment Kv are thus likely the driving factors that cause local variations in the VHWE of fluvial systems. 相似文献
149.
Using stable isotopes to understand seasonal and interannual dynamics in moisture sources and atmospheric circulation in precipitation 下载免费PDF全文
Yu Tang Xianfang Song Yinghua Zhang Dongmei Han Likun Ai Tianbao Zhao Yajun Wang 《水文研究》2017,31(26):4682-4692
Stable isotopes in precipitation are useful tracers to strengthen understanding of climate change and hydrological processes. In this study, the moisture sources of 190 precipitation events in Beijing were analysed using the Hybrid Single‐particle Lagrangian Integrated Trajectory model, based on which we studied the relation between variations in precipitation δ18O and dynamics in moisture sources and atmospheric circulation in seasonal and interannual timescales. Categorization of 7 groups of moisture sources was performed, among which oceanic moisture sources presented lower δ18O in precipitation than continental moisture sources. The results show that seasonal variations of precipitation δ18O were caused by changes of moisture sources. In summer, moisture from proximal oceans dominated vapour transport to Beijing due to increasing monsoon strength and resulted in a relatively small variation of precipitation δ18O. At the interannual timescale, the variations of δ18O in summer precipitation were related to dynamics in oceanic moistures, showing depleted values when the contribution of oceanic moistures, especially the proportion of long‐distance oceanic moisture, was high. Further analysis indicated that changes of oceanic moisture sources were controlled by the strength of summer monsoons. These findings address the complexity of moisture sources in midlatitude monsoon areas and suggest that isotopic signals in precipitation have the potential to deduce changes in moisture sources and atmospheric circulation and can therefore serve for palaeoclimate reconstruction. 相似文献
150.
Natural Hazards - Meteorological disasters (MDs), including drought, flood, hail, low temperature and frost (LTF), are causing severe damage to human life and economic development in China. Mapping... 相似文献